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Silicified microfossils from the Ediacaran Doushantuo Formation along a shelf margin-slope-basin transect in Hunan Province, South China, with stratigraphical implications

Published online by Cambridge University Press:  24 February 2025

Qing Ouyang*
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, China
Chuanming Zhou
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Nanjing, Nanjing 211135, China
Shuhai Xiao
Affiliation:
Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, USA
Chengxi Wu
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Beijing 100049, China
Zhe Chen
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , ,
Xianguo Lang
Affiliation:
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, and Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
Hongyi Shi
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Beijing 100049, China
Yunpeng Sun
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Beijing 100049, China
*
*Corresponding author

Abstract

Silicified microfossils are reported from nine stratigraphic sections of the Ediacaran Doushantuo Formation deposited in shelf margin, slope, and basin environments in Hunan Province of South China. These microfossils include sphaeromorphic and acanthomorphic acritarchs (15 genera and 29 species, including three new acanthomorph species, Bullatosphaera? colliformis n. sp., Eotylotopalla inflata n. sp., and Verrucosphaera? undulata n. sp.), multicellular algae, tubular microfossils, and other problematic forms, representing major fossil groups similar to those from the Doushantuo Formation in more proximal facies (e.g., inner shelf and shelf lagoon). A database of the abundance and occurrences of Doushantuo acanthomorphs is assembled and analyzed using quantitative and data-visualization methods (e.g., rarefaction analysis, non-parametric multidimensional scaling, and network analysis). The results show that, at the genus and species levels, taxonomic richness of Doushantuo acanthomorphs exhibits considerable variation among facies, but this variation is largely due to sampling and taphonomic biases. The results also show that numerous acanthomorph taxa have broad facies distribution, affirming their biostratigraphic value. The analysis confirms that acanthomorphs in the Weng'an biota of shelf margin facies are composed of a mixture of Member II and Member III assemblages of shelf-lagoon facies in the Yangtze Gorges area. The study shows the biostratigraphic potential of acanthomorphs in the establishment of regional biozones using the first appearance datum of widely distributed taxa, highlighting the importance of continuing exploration of under-sampled Doushantuo sections in slope and basinal facies.

UUID: http://zoobank.org/6fc92858-4054-4117-8043-1f06cfe77155

Type
Memoir
Copyright
Copyright © The Author(s), 2025. Published by Cambridge University Press on behalf of Paleontological Society

Non-technical Summary

The Ediacaran (ca. 635–539 million years ago) Doushantuo Formation in South China yields abundant microfossils preserved in cherts and phosphorites, yet most of the published materials originate from paleogeographically more proximal shelf-lagoon and shelf margin environments. In this paper, we report microfossils preserved in chert nodules from the Doushantuo Formation in a variety of environments, from the shallow-water shelf margin, to the distal, deep-water slope and basinal environments. We also analyze the abundance and occurrence data of Doushantuo acanthomorphs based on the present and previously published studies. The results show that different environments have largely similar fossil composition at the level of major morphological groups. However, acanthomorphic acritarchs, as a biostratigraphically important fossil group in the correlation of lower–middle Ediacaran strata, vary significantly in diversity among different environments. Using quantitative and data-visualization methods (e.g., rarefaction analysis, non-parametric multidimensional scaling, and network analysis), we show that variations in acritarch diversity among environments are largely due to insufficient sampling in slope and basinal areas, as well as differences in preservational modes. Nonetheless, numerous acritarch species occur widely in different environments, highlighting their potential in regional stratigraphic correlation of the Doushantuo Formation.

Introduction

Globally distributed organic-walled microfossil assemblages from lower–middle Ediacaran strata indicate that microscopic eukaryotes dominated the diversity of the marine ecosystem shortly after the Cryogenian Marinoan global glaciation (Knoll and Walter, Reference Knoll and Walter1992; Xiao, Reference Xiao, Jenkins, McMenamin, McKay and Sohl2004a; Peterson and Butterfield, Reference Peterson and Butterfield2005; Butterfield, Reference Butterfield2007; Zhou et al., Reference Zhou, Xie, McFadden, Xiao and Yuan2007; Moczydłowska, Reference Moczydłowska2008; Narbonne et al., Reference Narbonne, Xiao, Shields, Gehling, Gradstein, Ogg, Schmitz and Ogg2012). Because these microfossil assemblages are preserved in multiple taphonomic windows and in various depositional environments with relatively few age constraints (e.g., Grey, Reference Grey2005; Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; Anderson et al., Reference Anderson, Macdonald, Jones, McMahon and Briggs2017; Willman et al., Reference Willman, Peel, Ineson, Schovsbo, Rugen and Frei2020), the integration of these assemblages to form a global picture is a challenging task. Acanthomorphic acritarchs are the most diverse eukaryotic microfossils that widely occur in lower–middle Ediacaran strata (Xiao and Narbonne, Reference Xiao, Narbonne, Gradstein, Ogg, Schmitz and Ogg2020). Currently available paleontological data indicate that most Ediacaran acanthomorphs are constrained between the basal Ediacaran cap dolostone and the ca. 574–567 Ma Shuram negative carbon isotope excursion (Rooney et al., Reference Rooney, Cantine, Bergmann, Gómez-Pérez, Al Baloushi, Boag, Busch, Sperling and Strauss2020), although some acanthomorph taxa appear to extend into the late Ediacaran Period (e.g., Anderson et al., Reference Anderson, Macdonald, Jones, McMahon and Briggs2017; Arvestål and Willman, Reference Arvestål and Willman2020; Morais et al., Reference Morais, Fairchild, Freitas, Rudnitzki, Silva, Lahr, Moreira, Abrahão Filho, Leme and Trindade2021), and even younger strata (e.g., Grazhdankin et al., Reference Grazhdankin, Nagovitsin, Golubkova, Karlova, Kochnev, Rogov and Marusin2020). Thus, Ediacaran acanthomorphic acritarchs are particularly useful for stratigraphic correlation of lower–middle Ediacaran strata (Knoll and Walter, Reference Knoll and Walter1992; Knoll et al., Reference Knoll, Walter, Narbonne and Christie-Blick2006b; Xiao et al., Reference Xiao, Narbonne, Zhou, Laflamme, Grazhdankin, Moczydlowska-Vidal and Cui2016; Xiao and Narbonne, Reference Xiao, Narbonne, Gradstein, Ogg, Schmitz and Ogg2020).

As the first attempt to establish acritarch-based Ediacaran biostratigraphy, five biozones, including four defined by acanthomorphs, were proposed and successfully applied to the subdivision and correlation of Ediacaran strata in Australia (Grey, Reference Grey2005; Grey and Calver, Reference Grey and Calver2007; Willman and Moczydłowska, Reference Willman and Moczydłowska2008, Reference Willman and Moczydłowska2011). Later studies, however, concluded that these acritarch biozones cannot be recognized and applied in Ediacaran biostratigraphic correlation in Siberia and South China (Golubkova et al., Reference Golubkova, Raevskaya and Kuznetsov2010; Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012; Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013). Acritarch biozones were also proposed based on materials from the Ediacaran Doushantuo Formation in South China, where acritarchs are as abundant and diverse as in Australia (McFadden et al., Reference McFadden, Xiao, Zhou and Kowalewski2009; C. Yin et al., Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011; Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, Reference Liu, Chen, Zhu, Li, Yin and Shangb; Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; Liu and Moczydłowska, Reference Liu and Moczydłowska2019). Constrained by litho- and chemostratigraphic records, acritarch biozones recognized in South China were considered promising in the subdivision and correlation of the Ediacaran System (Xiao et al., Reference Xiao, Narbonne, Zhou, Laflamme, Grazhdankin, Moczydlowska-Vidal and Cui2016; Xiao and Narbonne, Reference Xiao, Narbonne, Gradstein, Ogg, Schmitz and Ogg2020). However, as has been the case in Australia, efforts to recognize these biozones outside South China achieved only limited success (e.g., Xiao et al., Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022). Thus, a more comprehensive understanding of the distribution of Ediacaran acanthomorphs and their controlling factors is needed before acanthomorph biozones can be applied globally.

Permineralized microfossils from the Ediacaran Doushantuo Formation, including diverse acanthomorphic acritarchs, have been intensively studied for nearly half a century since Yin and Li (Reference Yin and Li1978), with data recovered from various depositional environments and stratigraphic intervals (Liu and Moczydłowska, Reference Liu and Moczydłowska2019, and references therein). Most published data came from shelf-lagoon facies in the Yangtze Gorges area of western Hubei Province, where the stratigraphic framework of the Doushantuo Formation based on litho- and chemostratigraphy has been well established (Zhou et al., Reference Zhou, Yuan, Xiao, Chen and Hua2019). Using data from the Yangtze Gorges area, acritarch biozonation schemes were recognized, based on stratigraphic variations in taxonomic composition of acritarchs and the first appearance of specific acritarch taxa (McFadden et al., Reference McFadden, Xiao, Zhou and Kowalewski2009; C. Yin et al., Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011; Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, Reference Liu, Chen, Zhu, Li, Yin and Shangb; Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; Liu and Moczydłowska, Reference Liu and Moczydłowska2019). Whether these variations represent evolutionary changes, environmental shifts, or preservational vagaries, however, has not been thoroughly investigated.

To assess these possibilities, microfossil investigation of the Doushantuo Formation needs to expand beyond the shelf-lagoon facies in order to capture a broader understanding of regional variations in environment and taphonomy. Several recent studies offer promising insights into Doushantuo micropaleontology in inner shelf facies in the Zhangcunping and Shennongjia areas (e.g., Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019; Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022) and slope facies in western Hunan Province (e.g., Hawkins et al., Reference Hawkins, Xiao, Jiang, Wang and Shi2017; Ouyang et al., Reference Ouyang, Guan, Zhou and Xiao2017). However, the sampling intensity of the slope facies remains low compared with the shelf-lagoon facies in the Yangtze Gorges area. Importantly, there has been no report of Doushantuo acanthomorphs from basinal facies, representing a key knowledge gap to be addressed.

In this study, we present and describe new microfossils from the Doushantuo Formation deposited in shelf margin, slope, and basinal facies in Hunan Province. Based on a compilation of Doushantuo data and updated taxonomy, we are able to present a summary of the paleogeographic and stratigraphic distribution of Ediacaran acritarch species in South China. Building upon the paleogeographic and stratigraphic distribution, we assess the wider applicability of acritarch biozones previously recognized in the Yangtze Gorges area, and tentatively correlate the Doushantuo Formation at a basinal section with the Yangtze Gorges area using these biozones. Results from this study may contribute to a more comprehensive understanding of acritarch biostratigraphy in South China and may have implications for the subdivision and correlation of the Ediacaran System.

Geological setting

The South China block consists of the Yangtze and Cathaysia blocks, which amalgamated during assembly of the Rodinia supercontinent in the early Neoproterozoic (Li et al., Reference Li, Li, Li, Lo, Wang, Ye and Yang2009; Li and Zhao, Reference Li and Zhao2020). The South China block was positioned in middle–low latitudes in the Ediacaran Period, with a stable passive continental margin facing to the southeast (Macouin et al., Reference Macouin, Besse, Ader, Gilder, Yang, Sun and Agrinier2004; Zhang et al., Reference Zhang, Li, Jiang, Evans, Dong, Wu, Yang, Liu and Xiao2015). Overlying the Cryogenian Nantuo Formation diamictite, the Ediacaran succession in the Yangtze block consists of, in ascending order, the Doushantuo and Dengying formations or their equivalents (Cao et al., Reference Cao, Tang, Xue, Yu, Yin and Zhao1989).

The passive continental margin on the Yangtze block exhibited a southeastward deepening facies trend when the Doushantuo Formation was deposited, with depositional facies transitioning from shallow-water platform facies (including inner shelf, shelf lagoon, and carbonate shoal complex at the platform margin) in the northwest, to deep-water slope and basinal facies in the southeast of the Yangtze block (Fig. 1.1; Cao et al., Reference Cao, Tang, Xue, Yu, Yin and Zhao1989; Zhu et al., Reference Zhu, Zhang, Yang, Li, Steiner and Erdtmann2003; Jiang et al., Reference Jiang, Shi, Zhang, Wang and Xiao2011). This first-order facies trend provides a framework for understanding the environmental distribution of early–middle Ediacaran microfossils in the Yangtze block (e.g., Xiao et al., Reference Xiao, McFadden, Peek, Kaufman, Zhou, Jiang and Hu2012; Muscente et al., Reference Muscente, Hawkins and Xiao2015), although a number of nuances (such as the spatial continuity and temporal extent of the carbonate shoal complex) are still debated (e.g., Zhu et al., Reference Zhu, Zhao, Yin, Zeng and Li2019).

Figure 1. Ediacaran paleogeography and Proterozoic outcrop distribution in Hunan Province of South China. (1) Paleogeographic map of the Yangtze block during deposition of the Doushantuo Formation (modified from Jiang et al., Reference Jiang, Shi, Zhang, Wang and Xiao2011). Rectangle frame marks the location of (2). (2) Simplified geological map (modified from Luo et al., Reference Luo, Du, Jiang and Ma2002) showing the distribution of Proterozoic strata in northern Hunan Province where the studied sections are located. Section abbreviations: CJB, Caojunba; LJYZ, Lujiayuanzi; HP, Heping; TP, Tianping; CW, Caowan; SDP, Siduping; MJD, Majindong; LHK, Lianghekou; JSC, Jinshichong.

Despite the facies changes, first-order stratigraphic correlation of the Doushantuo Formation across the Yangtze block is supported by lithostratigraphic marker beds, sedimentary sequences, and carbon-isotope chemostratigraphic features. The Doushantuo Formation is subdivided into four lithostratigraphic members at its type locality in the Yangtze Gorges area (Fig. 2.1; Wang et al., Reference Wang, Erdtmann, Chen and Mao1998; Jiang et al., Reference Jiang, Shi, Zhang, Wang and Xiao2011). Member I cap dolostone can be traced across the entire Yangtze block (Zhou et al., Reference Zhou, Tucker, Xiao, Peng, Yuan and Chen2004a; Jiang et al., Reference Jiang, Shi, Zhang, Wang and Xiao2011). Two shallowing-upward sequences developed in members II and III and can be recognized in different facies in the Yangtze block (Jiang et al., Reference Jiang, Shi, Zhang, Wang and Xiao2011). Member IV in the uppermost Doushantuo Formation is a black shale unit at the type section and can be used as a marker bed in the Yangtze Gorges area. In addition to lithostratigraphy, carbon isotopic profiles also serve as a useful correlation tool, especially the negative δ13C excursions at the basal and in the upper Doushantuo Formation, EN1 and EN3, respectively, which have been recognized globally (Zhou et al., Reference Zhou, Yuan, Xiao, Chen and Hua2019, and references therein). These litho- and chemostratigraphic features allow us to bookend the Doushantuo Formation, even if the precise correlation of the subunits within the Doushantuo Formation can be sometimes ambiguous.

Figure 2. (1) Lithostratigraphic sequence of the Doushantuo Formation at studied localities, acanthomorph-bearing sampling horizons, and their correlations with those in the Yangtze Gorges area (represented by the Jiulongwan section). Lithostratigraphic column and C-isotopic profile of the Jiulongwan section modified from McFadden et al. (Reference McFadden, Huang, Chu, Jiang, Kaufman, Zhou, Yuan and Xiao2008). (2) Generalized paleobathymetric profile showing location of Doushantuo Formation sections known to be fossiliferous. Horizontal distances and water depth are not to scale.

The nine study sections are located in northern Hunan Province and represent shelf margin, slope, and basinal facies in the Yangtze block (Fig. 1). At some sections (e.g., the Caowan section), the Doushantuo Formation is not well exposed due to vegetation and weathering, thus field observations were made, and samples were collected from multiple adjacent outcrops, resulting in imprecise measurements of the stratigraphic heights.

The Caojunba section (GPS: 29°53′53″N, 110°32′54″E) crops out on a hill near Caojunba village, Nanbeizhen Town, Shimen County (Fig. 1.2). The Doushantuo Formation at Caojunba is composed of a lower part of grayish calcareous shale intercalated with argillaceous dolostones, and an upper part of carbonate rocks (Fig. 2.1). Detailed lithostratigraphic information on the Doushantuo Formation at Caojunba and its correlation with the adjacent Yangjiaping and Zhongling sections can be found in Shi et al. (Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022). Phosphatic and silicified intraclasts occur at multiple horizons in both lower and upper parts of the Doushantuo Formation, and pisoid layers occur in the upper Doushantuo Formation, indicating a high-energy, likely upper subtidal environment. Storm-induced breccias occasionally occur in the lower part of the carbonate interval, possibly indicating a relatively deeper environment below fair-weather wave base. Millimeter-sized chert nodules occur commonly in the shales of the lower Doushantuo Formation, and centimeter-sized chert nodules occur in a 6-m-thick interval of carbonates in the upper Doushantuo Formation.

The Lujiayuanzi section (GPS: 29°13′51″N, 110°47′43″E) crops out along a country road from Lujiayuanzi village to Hu'ao village in Xikou Town, Cili County (Fig. 1.2). The Doushantuo Formation at Lujiayuanzi has a total thickness of about 280 m, beginning with the basal Ediacaran cap dolostone that is succeeded by calcareous shale and argillaceous dolostone, micritic carbonates, organic-rich limestone, and peloidal and dolomitic limestones capped by massive dolostones of the overlying Dengying Formation (Fig. 2.1). Detailed lithostratigraphic data of the Doushantuo Formation at Lujiayuanzi can be found in Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017). Abundant intraclasts were found at multiple horizons in the Doushantuo Formation at Lujiayuanzi, and cross-bedding structures occur in the upper Doushantuo Formation, possibly indicating a subtidal environment. Centimeter- and meter-scale slump structures were observed in the lower and upper Doushantuo Formation, respectively, indicating deposition in a slope environment, as is the case for many other sections in western Hunan Province (Vernhet et al., Reference Vernhet, Heubeck, Zhu and Zhang2006; Vernhet and Reijmer, Reference Vernhet and Reijmer2010). Chert nodules were found throughout the Doushantuo Formation at Lujiayuanzi.

The Caowan, Heping, Siduping, and Tianping sections are all located near Zhangjiajie City (Fig. 1.2), and the Doushantuo Formation at these sections shares similar sequences. The Siduping section (GPS: 28°55′1″N, 110°26′56″E), cropping out along a river near Siduping village about 25 km to the south of Zhangjiajie City, is one of the well-studied sections in this area (e.g., Wang et al., Reference Wang, Jiang, Shi and Xiao2016; Hawkins et al., Reference Hawkins, Xiao, Jiang, Wang and Shi2017; Nie et al., Reference Nie, Liu and Dong2017). At Siduping, the Doushantuo Formation is subdivided into four members similar to those in the Yangtze Gorges area. Detailed lithostratigraphic data can be found in Wang et al. (Reference Wang, Jiang, Shi and Xiao2016). Olistostromes occur at multiple horizons throughout the Doushantuo Formation at Siduping. This study mainly focuses on the second member of the Doushantuo Formation, which is about 60 m in total thickness (Fig. 2.1). The lower 19 m is primarily shales or mudstones with olistostrome beds containing breccia that might have originated from debris flows (Fig. 3.1), and the upper 41 m mainly consist of carbonates of various bed thicknesses. Eight chert-nodule horizons were collected in the second member (Fig. 3.2), with two in olistostrome beds.

Figure 3. Outcrop photos of the Doushantuo Formation at the studied sections. (1) Olistostrome containing breccia (arrowheads) in shales of the lower Member II at Siduping section. (2) Chert nodules from the lower Member II at Siduping section (sample 19SDP-2). (3) Chert nodules (arrowheads) from the lower Doushantuo Formation at Tianping section (sample 19TP-1). (4) Olistostrome from the lower Doushantuo Formation at Tianping section. (5) Chert nodules (arrowheads) from shales of the lower Doushantuo Formation at Caowan section (sample 19CW-8). (6) A chert nodule (arrowheads) from the middle Doushantuo Formation at Lianghekou section (sample 21LHK-1). (7) Stratigraphic sequence of Nantuo Formation diamictite, basal Doushantuo Formation cap dolostone, and lower Doushantuo Formation calcareous shale and mudstone at Majindong section.

The Caowan section (GPS: 28°59′56″N, 110°28′25″E), about 2 km to the southwest of Tianmenshan Town, crops out along the road from Tianmenshan Town to Huangzhuang village. Outcrops of the Doushantuo Formation at Caowan are scattered. One outcrop of the lower Doushantuo Formation containing four chert nodule-bearing layers (Fig. 3.5) is exposed near Caowan village, and is mainly argillaceous dolostone interbedded with shales (Fig. 2.1).

The Heping section (GPS: 28°57′43″N, 110°15′21″E) is located near Heping village close to Yongmao Town, about 28 km to the southwest of Zhangjiajie City. At the Heping section, strata of the uppermost Nantuo Formation to basal Doushantuo Formation (cap dolostone and a few meters of black shale) are relatively well exposed, but overlying strata (mainly black shales with pyrite nodules) are mostly covered. Abundant millimeter- to centimeter-sized chert nodules occur in an ~0.5-m-thick shale interval of the lower–middle Doushantuo Formation and were found as float in an outcrop of the lower Doushantuo Formation.

The Tianping section (GPS: 28°57′44″N, 110°23′54″E) crops out along a creek near Tianping village, which is on the road from Caowan to Siduping. Here the Doushantuo Formation is composed of the basal Ediacaran cap dolostone, followed by a lower unit of argillaceous dolostone and dolomitic mudstone, and then an upper unit of carbonate rocks with olistostrome blocks (Fig. 3.4) and cross-stratification structures. A detailed description of the Doushantuo lithostratigraphic sequence at Tianping can be found in Shang and Liu (Reference Shang and Liu2020). Chert nodules occur in both the lower and upper Doushantuo Formation, and the sampled horizon in the present study (Fig. 3.3) likely correlates with the chert nodule interval in the lower Doushantuo Formation reported by Shang and Liu (Reference Shang and Liu2020).

The Lianghekou and Majindong sections are both in the western part of Taoyuan County (Fig. 1.2). At the Lianghekou section (GPS: 29°0′46″N, 111°8′56″E) near Dingjiafang village, the Doushantuo Formation is about 40 m thick, and is composed mainly of argillaceous dolostone and dolomitic shale (Fig. 2.1). Chert nodules (Fig. 3.6) were found at one horizon about 20 m above the cap dolostone or about 20 m below the bedded cherts of the overlying Liuchapo Formation. At the Majindong section (GPS: 29°4′57″N, 111°9′21″E) near Majindong village, which is about 6 km to the west of Ligonggang Town, the lower Doushantuo Formation crops out along a river and consists of, in ascending order, ~3 m of cap dolostone (Fig. 3.7), ~5 m of chert-nodule-bearing argillaceous dolostone and dolomitic mudstone, and ~10 m of thick-bedded dolostone (Fig. 2.1). The middle–upper Doushantuo Formation at Majindong is largely covered, and the overlying Liuchapo Formation consists of bedded cherts intercalated with black shales that yield fragments of carbonaceous compressions. At both Lianghekou and Majindong sections, the highly condensed Doushantuo Formation (total thickness less than 50 m) is characterized by the occurrence of horizontal laminations, whereas slump structures or olistostrome blocks, which are common in slope facies, have not been observed.

The Jinshichong section (GPS: 28°16′22″N, 113°52′22″E) is located at a phosphorite mine near Jinshichong village, about 3 km to the southeast of Yonghe Town, Liuyang City (Fig. 1.2). Here only several meters of black shales with millimeter- to centimeter-sized chert nodules were observed (Fig. 2.1), which belong to the lower Doushantuo Formation according to a report of the local geological survey (Geological Bureau of the Hunan Provincial Revolutionary Committee, 1976).

Lithostratigraphic sequences of the Doushantuo Formation, supplemented with carbon isotope profiles, have been applied to the correlation among different areas in South China (e.g., Wang et al., Reference Wang, Jiang, Shi and Xiao2016, Reference Wang, Guan, Hu, Cui, Muscente, Chen and Zhou2020; Ouyang et al., Reference Ouyang, Guan, Zhou and Xiao2017, Reference Ouyang, Zhou, Xiao, Chen and Shao2019; Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022). In most areas of South China, the Doushantuo Formation above the cap dolostone can be generally divided into two parts: the lower part dominated by siliciclastic rocks or argillaceous carbonate rocks (corresponding to Member II in the Yangtze Gorges area), and the upper part dominated by carbonates (corresponding to Member III in the Yangtze Gorges area) (Fig. 2.1). These two parts are widely interpreted by various authors as representing two shallowing-upward sequences, although recognition of a particular physical surface that separate these two sequences is still open to debate (e.g., Jiang et al., Reference Jiang, Kaufman, Christie-Blick, Zhang and Wu2007, Reference Jiang, Shi, Zhang, Wang and Xiao2011; Zhou et al., Reference Zhou, Xie, McFadden, Xiao and Yuan2007; Zhu et al., Reference Zhu, Zhang and Yang2007; McFadden et al., Reference McFadden, Huang, Chu, Jiang, Kaufman, Zhou, Yuan and Xiao2008). The lower and the upper parts of the Doushantuo Formation each exhibits chemo- and biostratigraphic features that are regionally consistent (e.g., Zhou et al., Reference Zhou, Xie, McFadden, Xiao and Yuan2007; Xiao et al., Reference Xiao, McFadden, Peek, Kaufman, Zhou, Jiang and Hu2012; Liu and Moczydłowska, Reference Liu and Moczydłowska2019), indicating that they likely represent chronostratigraphic units. Under this bipartite framework, samples of the studied Doushantuo successions can be correlated with either the lower part (all sampled horizons at sections in the Zhangjiajie area, at the Majindong section, and at the Jinshichong section; the lower five sampled horizons at the Caojunba section; and the lower four sampled horizons at the Lujiayuanzi section), or the upper part (the upper six sampled horizons at the Caojunba section; and the upper 15 sampled horizons at the Lujiayuanzi section) of the Doushantuo Formation (Table 1, Fig. 2.1). The Doushantuo Formation at the Lianghekou section is not well exposed and for most part is dominated by argillaceous carbonates, making it difficult to correlate the single sample horizon at the Lianghekou section. However, since the lower part of the Doushantuo Formation is generally stratigraphically thicker than the upper part in sections where they are easily recognizable, the sampled horizon in the middle of the Doushantuo Formation at the Lianghekou section more likely correlates to the lower part of the Doushantuo Formation elsewhere.

Table 1. Sample number, stratigraphic height, number for thin sections, and microfossil abundance data of the Doushantuo Formation from the nine studied sections in Hunan Province. Refer to Figure 2 for stratigraphic height measurements. Refer to Geological setting section for GPS coordinates of the sections. PN = present, not counted; \ = not observed.

Combined with sedimentary structures and lithofacies analyses, lithostratigraphic sequence data of the Doushantuo Formation are also used to determine the paleogeographic locations of the studied sections during the early Ediacaran Period. The Caojunba section, with plenty of intraclast-rich carbonate deposits (such as reworked breccia and pisoidal layers) in its upper part, is inferred to be located on the proximal side of the shelf margin carbonate shoal complex, with the Doushantuo Formation being deposited in a shallow subtidal environment (Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022). The Doushantuo Formation at the Lujiayuanzi section has the greatest stratigraphic thickness, is dominated by carbonate lithologies, and contains intraclasts, cross-beds, and slump structures at different scales. These structures indicate that the Lujiayuanzi section was likely deposited in a shallow subtidal environment of the upper slope facies (Ouyang et al., Reference Ouyang, Guan, Zhou and Xiao2017). Sections in the Zhangjiajie area were likely located in the lower slope facies, considering the occurrence of olistostromes and debris flows (e.g., Vernhet et al., Reference Vernhet, Heubeck, Zhu and Zhang2006; Wang et al., Reference Wang, Jiang, Shi and Xiao2016; Hawkins et al., Reference Hawkins, Xiao, Jiang, Wang and Shi2017). The Doushantuo Formation at Lianghekou and Majindong is highly condensed and rich in fine-grained siliciclastic sediments, potentially indicating deposition in an offshore low-energy basinal environment, which is consistent with the absence of olistostromes and with previously published paleogeographic reconstructions (e.g., Vernhet et al., Reference Vernhet, Heubeck, Zhu and Zhang2006; Jiang et al., Reference Jiang, Shi, Zhang, Wang and Xiao2011; Zhu et al., Reference Zhu, Zhao, Yin, Zeng and Li2019). Eastern Hunan Province is generally considered to have been in the basin during deposition of the Doushantuo Formation (Cao et al., Reference Cao, Tang, Xue, Yu, Yin and Zhao1989; Zhu et al., Reference Zhu, Zhang, Yang, Li, Steiner and Erdtmann2003; Jiang et al., Reference Jiang, Shi, Zhang, Wang and Xiao2011; Zhu et al., Reference Zhu, Zhao, Yin, Zeng and Li2019). However, the local occurrence of intraclastic phosphorite at the Jinshichong section indicates deposition in relatively shallow-water environments (Muscente et al., Reference Muscente, Hawkins and Xiao2015). In this study, we provisionally accept the traditional view that the Jinshichong section was deposited in a basinal environment, but this interpretation may be revised pending further detailed sedimentological investigations in this area.

Variation in the abundance of chert nodule layers in the studied successions also supports the inferred paleogeographic location of the studied sections (see Fig. 2.2). At the shallow-water Caojunba and Lujiayuanzi sections, chert nodule horizons are found throughout the Doushantuo Formation (i.e., >10 horizons at each section). At the sections in the Zhangjiajie area, chert nodules are also abundant, but occur at fewer horizons (maximum eight horizons in each section). At the Majindong and the Lianghekou sections, chert nodules are only found at one horizon in the entire Doushantuo Formation. The decrease in the number of chert nodule horizons from the shallow-water shelf margin (Caojunba and Lujiayuanzi sections) to the deep-water basinal environment (Majindong and Lianghekou sections) is consistent with the view that chert nodules are more likely to form in shallow-water settings with enriched SiO42− and sufficient supply of organic matter (Knoll, Reference Knoll1985; Muscente et al., Reference Muscente, Hawkins and Xiao2015; Gao et al., Reference Gao, He, Lash, Li and Zhang2020).

Materials and methods

Sample collection, microfossil examination, and systematic descriptions

Forty-nine rock samples were collected from chert-nodule and -band horizons in the Doushantuo Formation at Caojunba, Lujiayuanzi, Tianping, Caowan, Heping, Siduping, Majindong, Lianghekou, and Jinshichong sections (Fig. 2.1, Table 1), from which 508 thin sections (mostly cut parallel to bedding surfaces) were made for micropaleontological investigations. Details of samples and thin sections are given in Table 1. Thin sections were examined for microfossils under Olympus BX-51 and Zeiss Axioscope A1 transmitted light microscopes, with microfossils photographed using Olympus DP 72 and DP 74 digital cameras attached to the microscopes. All microfossils encountered in thin sections were recorded with stage coordinates, and illustrated specimens were additionally positioned using an England Finder slide. Dimensions of microfossils were measured using Image Pro Express and ImageJ software on digital photographs. Numbers of specimens were counted for each acanthomorphic acritarch species in each chert sample and at each stratigraphic section, and the relative abundance of each species was calculated.

Systematic descriptions are given for acanthomorphic acritarchs that are identifiable at the species level, with descriptive terminology following that of Xiao et al. (Reference Xiao, Zhou, Liu, Wang and Yuan2014), and taxonomical nomenclature following the International Code of Nomenclature for Algae, Fungi, and Plants (Turland et al., Reference Turland, Wiersema, Barrie, Greuter and Hawksworth2018). Statistics relating to dimension measurements are given in the systematic description of each taxon: “n” represents the number of specimens measured, “mean” the average among the specimens, and “SD” the standard deviation among the specimens. For each specimen, the measurement of each morphological feature was repeated multiple times (depending on preservation state) on different positions to obtain an average value.

Taxonomic revision and data analysis

Occurrence data of Doushantuo acanthomorphic acritarchs and certain sphaeromorphic taxa considered stratigraphically useful (e.g., Schizofusa zangwenlongii Grey, Reference Grey2005) are compiled from 55 previously published studies, with many taxonomic revisions based on systematic treatments in this study and in recently published systematic works (e.g., Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021; Xiao et al., Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022; Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022). Details of taxonomic revisions of published acanthomorph specimens from the Doushantuo Formation are summarized in the Supplemental Materials and described in the Systematic paleontology section. Fossil occurrence data without clear, published, microfossil images or stratigraphic horizons were excluded from our compilation. Also excluded were fossils described in open nomenclature, with the exception of Weissiella cf. W. grandistella, which has been systematically reviewed by Ouyang et al. (Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021), confirming its presence from multiple localities and facies.

Rarefaction analysis was performed on selected acritarch abundance data from this and previously published studies to assess the influence of sample size on taxonomic richness (Raup, Reference Raup1975). Rarefaction curves were generated in Rstudio using the rarefy function in the vegan package (R Core Team, 2018; Oksanen et al., Reference Oksanen, Blanchet, Friendly, Kindt, Legendre, McGlinn and Minchin2019).

A non-parametric multidimensional scaling (NMDS) analysis was employed to compare taxonomically revised acanthomorph occurrence data from 82 Doushantuo collections in this and 55 previously published studies (see Supplemental Materials). A collection is defined as an acanthomorphic acritarch assemblage from a stratigraphic unit (differentiated as Member II or Member III and their correlatives) at a specific area reported in an independent study. The NMDS analysis was applied on presence/absence data of taxonomic occurrences in each collection, using the metaMDS function from the vegan package in Rstudio, with distance using the Raup-Crick similarity and maximum iteration = 100. The collections ordinated by two-dimensional NMDS were then shown in a scatterplot defined by NMDS1 and NMDS2, with collections grouped into and color-coded by depositional facies or stratigraphic intervals, which were outlined by convex hulls.

Network analysis was performed to visualize the spatial and stratigraphic distribution of Ediacaran acanthomorphs in South China. The graph_from_incidence_matrix function in the Rstudio igraph package (Csárdi and Nepusz, Reference Csárdi and Nepusz2006) with its default parameters was used to analyze the same taxonomic occurrence data of Doushantuo acanthomorphs used in the NMDS analysis in order to generate an unweighted bipartite network graph, in which each species is linked to its hosting collections. As in NMDS plots, collections are grouped into and color-coded by depositional facies or stratigraphic intervals.

Repository and institutional abbreviation

All samples and thin sections are reposited in the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS). Illustrated specimens are housed at the Fossil Repository of NIGPAS, with a catalog number prefix of PB.

Systematic paleontology

Group Acritarcha Evitt, Reference Evitt1963
Genus Appendisphaera Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, emend. Moczydłowska, Reference Moczydłowska2005

Type species

Appendisphaera grandis Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, emend. Moczydłowska, Reference Moczydłowska2005.

Other species

Appendisphaera anguina Grey, Reference Grey2005; A.? brevispina Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; A. clava Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; A. clustera Liu and Moczydłowska, Reference Liu and Moczydłowska2019; A. fragilis Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993; A. heliaca (Liu and Moczydłowska, Reference Liu and Moczydłowska2019) Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021; A.? hemisphaerica Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; A. lemniscata Liu and Moczydłowska, Reference Liu and Moczydłowska2019; A. longispina Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; A. longitubularis (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) Liu and Moczydłowska, Reference Liu and Moczydłowska2019; A. magnifica (Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998) Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; A. setosa Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; A. tabifica Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993; A. tenuis Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993.

Remarks

The latest emendation diagnoses Appendisphaera as a genus of acanthomorphic acritarch with “simple, homomorphic, slim, cylindrical or ciliate” processes, which can be either straight or tapering, and can have a basal expansion and a rounded or blunt termination (Moczydłowska, Reference Moczydłowska2005, p. 293). These features, however, are found in many other genera such as Cavaspina, Knollisphaeridium, Tanarium, and even Xenosphaera. Therefore, systematic morphometric work is required to develop a practical workflow to distinguish these taxa, including Appendisphaera, that fall into the category of “acanthomorphs with hollow, tapering, conical processes” by Grey (Reference Grey2005, p. 172–175).

Appendisphaera grandis Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, emend. Moczydłowska, Reference Moczydłowska2005
Figure 4

Figure 4. Appendisphaera grandis Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, emend. Moczydłowska, Reference Moczydłowska2005. (1, 2) PB201998, thin section 18JSC-2-5, U40/4; circled 2 in (1) marks area magnified in (2). (3, 4) PB201999, thin section 19HP-1-33, N41/1; circled 4 in (3) marks area magnified in (4). (5, 6) PB202000, thin section 19TP-1-19, D49/4; circled 6 in (5) marks area magnified in (6). (7–9) PB202001, thin section 19SDP-2-d1, Y24/1; circled 8 and 9 in (7) mark areas magnified in (8) and (9), respectively. (10, 11) PB202002, thin section 21DC-5-4, V34/1; circled 11 in (10) marks area magnified in (11).

Reference Moczydłowska, Vidal and Rudavskaya1993

Appendisphaera grandis Moczydłowska, Vidal, and Rudavskaya, p. 503, text-fig. 5, pl. 1, figs. 1, 2.

Reference Moczydłowska2005

Appendisphaera grandis Moczydłowska et al.; Moczydłowska, p. 294, figs. 3, 4.

Reference Knoll, Javaux, Hewitt and Cohen2006a

Appendisphaera grandis; Knoll et al., fig. 3g.

Reference Moczydłowska2008

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Willman and Moczydłowska, p. 519, fig. 6C.

Reference Chen, Yin, Liu, Gao, Tang and Wang2010

Appendisphaera grandis; Chen et al., fig. 2.1.

Reference Golubkova, Raevskaya and Kuznetsov2010

Appendisphaera grandis Moczydłowska et al.; Golubkova et al., pl. 1, fig. 1, pl. 3, figs 4, 10.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Xiao et al., p. 9, fig. 3.1–3.3.

non Reference Shukla and Tiwari2014

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Shukla and Tiwari, p. 215, fig. 4D, E.

Reference Nagovitsin and Kochnev2015

Appendisphaera grandis Moczydlowska et al. [sic]; Nagovitsin and Kochnev, fig. 4.I.1, 4.I.2.

Reference Prasad and Asher2016

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Prasad and Asher, p. 42, pl. II, figs. 3, 4.

Reference Anderson, Macdonald, Jones, McMahon and Briggs2017

Appendisphaera grandis; Anderson et al., fig. 2B.

Reference Hawkins, Xiao, Jiang, Wang and Shi2017

Appendisphaera crebra; Hawkins et al., fig. 9E, F.

Reference Ouyang, Guan, Zhou and Xiao2017

Appendisphaera fragilis; Ouyang et al., fig. 8D–F.

Reference Anderson, McMahon, Macdonald, Jones and Briggs2019

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Anderson et al., p. 507, fig. 6A–D.

Reference Liu and Moczydłowska2019

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Liu and Moczydłowska, p. 48, figs. 21–23.

Reference Ouyang, Zhou, Xiao, Chen and Shao2019

Appendisphaera grandis; Ouyang et al., fig. 8I–K.

Reference Shang, Liu and Moczydłowska2019

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Shang et al., p. 7, fig. 3.

Reference Ouyang, Zhou, Xiao, Chen and Shao2019

Appendisphaera clava; Ouyang et al., fig. 8E, F.

Reference Shang and Liu2020

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Shang and Liu, p. 156, fig. 4.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Ouyang et al., fig. 10M–P.

non Reference Liu, Qi, Fan, Guo and Pei2021

Appendisphaera grandis; Liu et al., fig. 5.4.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Shi et al., fig. 7A, B.

Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Xiao et al., fig. 7.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Ye et al., fig. 10A–D.

non Reference Ye, Li, Tong, An, Hu and Xiao2022

Appendisphaera grandis Moczydłowska et al., emend. Moczydłowska; Ye et al., fig. 10E, F.

Reference Golubkova2023

Appendisphaera grandis (Moczydłowska et al.) emend. Moczydłowska; Golubkova, pl. 7, fig. 1.

Holotype

PMU-Sib.1-R/63/2, reposited at Uppsala University, from the Ediacaran Khamaka Formation, Nepa–Botuoba region, Yakutia, Siberia (Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, p. 503, text-fig. 5A–D).

Description and measurements

Vesicle mostly compressed but originally spheroidal, medium to large in size, bearing numerous, evenly and densely distributed processes. Processes hollow, long and slim, cylindrical for most part, lack significant basal expansion. Three least-deformed specimens yield vesicle diameters of ~152–373 μm. Approximately 12–28 processes per 100 μm of vesicle periphery. Full length of processes difficult to measure due to deformation but estimated to exceed 20 μm and making up >10% of vesicle diameter (18.5–39.5 μm, 9.0–12.2% of vesicle diameter). Process width 0.1–1.3 μm (N = 8, mean = 0.6 μm, SD = 0.4 μm).

Material

Five illustrated specimens (Fig. 4) and three additional specimens.

Remarks

As for the type species of Appendisphaera, A. grandis was initially distinguished by its proportionally long and hair-like processes (Moczydłowska et al., Reference Moczydłowska, Vidal and Rudavskaya1993), but the processes were later found to be hollow and cylindrical (Moczydłowska, Reference Moczydłowska2005). Measurements on photos of the eight A. grandis specimens from its type locality published by Moczydłowska et al. (Reference Moczydłowska, Vidal and Rudavskaya1993) and Moczydłowska (Reference Moczydłowska2005) reveal relatively small morphological variations: small to medium-sized vesicle (diameter 77–130 μm, mean = 107 μm, SD = 16 μm), relatively long and thin processes (process length 12.0–25.3 μm, mean = 18.4 μm, SD = 5.4 μm; process length to vesicle diameter ratio 10.8–23.0%, mean = 17.2%, SD = 4.7%; process basal width 0.4–1.8 μm, mean = 1.2 μm, SD = 0.4 μm), and large process density (46–65 processes per 100 μm of vesicle periphery, but this may be an overestimation since these eight specimens are all preserved as carbonaceous compressions). In summary, the processes of A. grandis from the type locality make up almost 20% of vesicle diameter and are so thin (basal width ~1 μm) that their shape is better described as cylindrical than conical, even though gradual terminal tapering can be observed on both holotype and paratype of this species.

With additional specimens assigned to this species in recent years (especially permineralized specimens), the morphospace of A. grandis has grown rapidly. Appendisphaera grandis currently contains specimens with a large vesicle (diameter up to several hundred microns) and process lengths about 10% of vesicle diameter. Despite this, A. grandis is still characterized by its relatively long, thin, and almost cylindrical processes, which differentiates it from other Appendisphaera species with relatively short processes (e.g., A. clava and A. tenuis) and those species with basally expanded processes (e.g., A. longitubularis, A. longispina, and A. magnifica; see also remarks under A. magnifica). In this study, only specimens with process basal width around 1 μm and no more than 2 μm, and process proportional length greater than 10% of vesicle diameter are accepted as A. grandis. Based on these criteria, the specimen illustrated by Liu et al. (Reference Liu, Qi, Fan, Guo and Pei2021, fig. 5.4) is removed from A. grandis. Its long, thick, terminally cylindrical processes resemble those of A. longitubularis and Tanarium gracilentum (Yin in Yin and Liu, Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988) Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021, which also have distally tapered and densely arranged processes. Similarly, the specimen illustrated as A. grandis by Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022, fig. 10E, F), bearing apparently conical processes with a basal width exceeding 5 μm, is more appropriately placed in A. longispina.

Appendisphaera magnifica (Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998) Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a
Figure 5

Reference Zhang, Yin, Xiao and Knoll1998

Meghystrichosphaeridium magnificum Zhang et al., p. 36, fig. 10.5, 10.6.

?Reference Zhou, Xie, McFadden, Xiao and Yuan2007

Meghystrichosphaeridium magnificum; Zhou et al., fig. 4E.

Reference Yin, Wang, Yuan and Zhou2011

Meghystrichosphaeridium magnificum; C. Yin et al., fig. 5d.

Reference Liu, Yin, Chen, Tang and Gao2013

Meghystrichosphaeridium magnificum Zhang et al.; Liu et al., fig. 11I, J.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Appendisphaera magnifica (Zhang et al.), Liu et al., p. 21, figs. 5.8, 19.1–19.6, 20.1–20.6.

Reference Ouyang, Zhou, Guan and Wang2015

Appendisphaera magnifica (Zhang et al.) Liu et al.; Ouyang et al., p. 215, pl. I, figs. 1, 2, 4.

Reference Hawkins, Xiao, Jiang, Wang and Shi2017

Appendisphaera magnifica; Hawkins et al., fig. 9A, B.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Appendisphaera magnifica (Zhang et al.) Liu et al.; Ouyang et al., fig. 11I, J.

Figure 5. Appendisphaera magnifica (Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998) Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a. (1) PB202003, thin section 19SDP-7-1, N38/3. (2) PB202004, thin section 19SDP-7-3, E39/2. (3) PB202005, thin section 19SDP-7-3, E30/2. (4) PB202006, thin section 19SDP-7-3, K30/2. (5) PB202007, thin section 19SDP-7-24, H37. (6) PB202008, thin section 19SDP-7-24, H34.

Holotype

WCHB-789b-24, reposited at Peking University Paleontological Collection, from the Ediacaran Doushantuo Formation, Weng'an area, Guizhou Province, South China (Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998, p. 36, fig. 10.5, 10.6).

Description and measurements

Vesicle medium-sized, originally spheroidal but some deformed to varying degrees. Processes uniformly conical, long, and thin, tapering gradually toward the terminal end, evenly and densely arranged on the vesicle, basally separate. Vesicle diameter 98–167 μm (N = 16, mean = 132 μm, SD = 19 μm); process length 12.2–26.3 μm (N = 17, mean = 18.6 μm, SD = 3.8 μm), 9.5–21.3% of vesicle diameter (N = 16, mean = 14.2%, SD = 3.0%), process basal width 2.0–4.9 μm (N = 17, mean = 3.0 μm, SD = 0.8 μm); 16–30 processes (N = 16, mean = 22, SD = 4) per 100 μm of vesicle periphery.

Material

Six illustrated specimens (Fig. 5) and 11 additional specimens.

Remarks

The 17 specimens described here are similar to the holotype of Appendisphaera magnifica in the closely arranged, basally separate, and acutely tapering processes. But they are significantly smaller than the holotype, whose vesicle diameter is about 350 μm. However, they are similar to the A. magnifica specimens in Liu et al. (Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) in dimensions, with the latter yielding a vesicle diameter of 100–160 μm, process length of 19–36 μm (14–30% of vesicle diameter), process basal width of 2.1–3.4 μm, and 20–24 processes per 100 μm of vesicle periphery.

Liu et al. (Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) transferred “Meghystrichosphaeridiummagnificum to Appendisphaera, on the basis of its very thin and densely distributed processes. However, Liu and Moczydłowska (Reference Liu and Moczydłowska2019) synonymized Appendisphaera magnifica with A. grandis without justification. Appendisphaera is one of the richly speciose genera of Ediacaran acanthomorphs (Xiao et al., Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022), and the differentiation of species within this genus has become a problem. Morphological analysis of the Cambrian acanthomorphic genus Skiagia indicates that morphological variation of this richly speciose genus may reflect phenotypic plasticity (Wallet et al., Reference Wallet, Willman and Slater2022). The same can be said of Appendisphaera, and it is possible that A. magnifica and A. grandis are synonymous. Although A. magnifica and A. grandis do share morphological similarities (e.g., process density, proportional length), the processes of A. magnifica have a relatively wider base, making its processes more conical in shape and different from the more cylindrical processes of A. grandis (Moczydłowska, Reference Moczydłowska2005). Post-mortem degradation or deformation may cause process shrinkage and account for the thinner processes of A. grandis, but there are many delicately preserved specimens of A. grandis, both permineralized (e.g., Liu and Moczydłowska, Reference Liu and Moczydłowska2019, figs. 21, 22) and preserved as carbonaceous compressions (e.g., type specimens from Siberia, Moczydłowska et al. Reference Moczydłowska, Vidal and Rudavskaya1993) that are unlikely to be deformed variants of A. magnifica. Thus, we retain A. magnifica as a distinct form species.

Appendisphaera tenuis Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, emend. Moczydłowska, Reference Moczydłowska2005
Figure 6

Reference Moczydłowska, Vidal and Rudavskaya1993

Appendisphaera tenuis Moczydłowska, Vidal, and Rudavskaya, p. 506, text-fig. 7.

Reference Nagovitsin, Faizullin and Yakshin2004

Appendisphaera minima Nagovitsin and Faizullin in Nagovitsin et al., p. 12, pl. I, figs. 1–3.

Reference Grey2005

Appendisphaera tenuis Moczydłowska et al.; Grey, p. 224, figs. 88F, 113A–D.

Reference Moczydłowska2005

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska, p. 296, fig. 5.

Reference Grey2005

Ericiasphaera polystacha Grey, p. 264, figs. 169, 170.

non Reference Yin, Zhu, Knoll, Yuan, Zhang and Hu2007

Appendisphaera tenuis; Yin et al., fig. 1b.

?Reference Vorob'eva, Sergeev and Chumakov2008

Appendisphaera tenuis Moczydłowska; Vorob'eva et al., fig. 2k, l.

Reference Willman and Moczydłowska2008

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Willman and Moczydłowska, p. 520, figs. 7B, C, 8A, B.

Reference Golubkova, Raevskaya and Kuznetsov2010

Appendisphaera tenuis Moczydłowska et al.; Golubkova et al., pl. I, fig. 2, pl. III, figs. 5, 6.

?Reference Golubkova, Raevskaya and Kuznetsov2010

Ericiasphaera aff. E. addspersa Grey; Golubkova et al., pl. IV, fig. 6a, b.

Reference Sergeev, Knoll and Vorob'eva2011

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Sergeev et al., p. 1002, fig. 5.4–5.6.

?Reference Willman and Moczydłowska2011

Cavaspina amplitudinis Willman in Willman and Moczydłowska, p. 25, pl. I, figs. 1–6.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Liu et al., p. 31, fig. 23.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Xiao et al., p. 9, fig. 3.4.

Reference Shukla and Tiwari2014

Appendisphaera grandis; Shukla and Tiwari, p. 215, fig. 4D, E.

Reference Golubkova, Zaitseva, Kuznetsov, Dovzhikova and Maslov2015

Appendisphaera tenuis Moczydłowska et al.; Golubkova et al., fig. 2a.

Reference Nagovitsin and Kochnev2015

Appendisphaera tenuis Moczydlowska [sic]; Nagovitsin and Kochnev, fig. 4.I.3.

?Reference Ye, Tong, An, Tian, Zhao and Zhu2015

Appendisphaera sp.; Ye et al., p. 48, pl. I, figs. 9–14.

Reference Prasad and Asher2016

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Prasad and Asher, p. 44, pl. III, figs. 3–6.

Reference Prasad and Asher2016

Gyalosphaeridium multispinulosum Grey; Prasad and Asher, p. 52, pl. VI, figs. 3, 4.

Reference Prasad and Asher2016

Gyalosphaeridium pulchrum Zang in Zang and Walter; Prasad and Asher, p. 52, pl. VI, figs. 5, 6.

Reference Liu and Moczydłowska2019

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Liu and Moczydłowska, p. 61, figs. 29, 30.

Reference Anderson, McMahon, Macdonald, Jones and Briggs2019

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Anderson et al., p. 509, fig. 6H, I.

Reference Shang, Liu and Moczydłowska2019

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Shang et al., p. 10, fig. 5.

Reference Shang, Liu and Liu2020

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Shang and Liu, p. 157, fig. 5A, B.

Reference Vorob'eva and Petrov2020

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Vorob'eva and Petrov, p. 370, pl. I, figs. 3, 4.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Ouyang et al., fig. 11Q, R.

Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Xiao et al., fig. 17.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Appendisphaera tenuis Moczydłowska et al., emend. Moczydłowska; Ye et al., fig. 12E, F.

Reference Golubkova2023

Appendisphaera tenuis (Moczydłowska et al.) emend. Moczydłowska; Golubkova, pl. 7, fig. 2.

Figure 6. Appendisphaera tenuis Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, emend. Moczydłowska, Reference Moczydłowska2005. (1, 2) PB202009, thin section 19TP-1-14, J27; circled 2 in (1) marks area magnified in (2). (3–5) PB202010, thin section 19TP-1-39, J47/1; circled 4 and 5 in (3) mark areas magnified in (4) and (5), respectively. (6–8) PB202011, thin section 19TP-1-40, F37; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively.

Holotype

PMU-Sib.1-M/33, reposited at Uppsala University, from the Ediacaran Khamaka Formation, Nepa–Botuoba region, Yakutia, Siberia (Moczydłowska et al., Reference Moczydłowska, Vidal and Rudavskaya1993, p. 506, text-fig. 7).

Description and measurements

Vesicle large, with relatively short, slim processes evenly distributed on the vesicle. Processes thin, cylindrical or acutely conical, some with a minute basal expansion (Fig. 6.5), closely arranged but basally separated. Vesicle diameter 224–276 μm (N = 4, mean = 248 μm, SD = 22 μm); process length 11.6–18.4 μm (N = 4, mean = 14.1 μm, SD = 3.0 μm), 4.6–7.7% of vesicle diameter (N = 4, mean = 5.7%, SD = 1.4%), process basal width 1.3–3.1 μm (N = 3, mean = 2.1 μm, SD = 0.9 μm); 16–21 processes (N = 4, mean = 20, SD = 2) per 100 μm of vesicle periphery.

Material

Three illustrated specimens (Fig. 6) and one additional specimen.

Remarks

Appendisphaera tenuis was originally diagnosed as an Appendisphaera species that has relatively short processes with a possible minute basal expansion—features used to differentiate this species from A. grandis (Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993). The hollow nature of the processes was later recognized and added to the emended diagnosis of A. tenuis (Moczydłowska, Reference Moczydłowska2005), with other diagnostic features unchanged. Specimens assigned to A. tenuis in subsequent studies mostly resemble the holotype and other specimens from the type locality in Siberia in their relatively short, densely arranged, conical or cylindrical processes, with or without a small basal expansion, except that some of them (including those reported here) have larger vesicles than the Siberian specimens.

Appendisphaera tenuis shares some morphological similarities with A. clava. Both species have relatively short and densely distributed processes, which were described as cylindrical despite the slightly expanded bases (Moczydłowska, Reference Moczydłowska2005; Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a). The holotype of A. clava has a vesicle diameter of 420 μm, process length of 12 μm, which is 2.9% of vesicle diameter, process basal width of ~1 μm, and about 40 processes per 100 μm of vesicle periphery. Other A. clava specimens published together with the holotype have vesicle diameters of 250–510 μm, process length of 6–13 μm (1.7–4% of vesicle diameter), and process width and density similar to the type specimen, although basal width can be up to 3.6 μm (measured on Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 8.5). These dimensions show that A. clava has overall larger vesicles (>200 μm and up to 500 μm), proportionally shorter processes (<5% of vesicle diameter), and possibly larger process density than A. tenuis, which has a medium-sized vesicle with process length about 10% of vesicle diameter based on measurements of specimens from the type locality in Siberia. However, several specimens listed as synonyms of A. tenuis by Liu and Moczydłowska (Reference Liu and Moczydłowska2019) are similar to A. clava in measurements: one A. tenuis specimen (vesicle diameter 280 μm, process length 7.1–8.9 μm, which is 2.5–3.2% of vesicle diameter, process basal width 0.4–2.2 μm, Vorob'eva et al., Reference Vorob'eva, Sergeev and Chumakov2008), specimens originally published as Cavaspina amplitudinis (vesicle diameter 500–900 μm, process length 20–30 μm, which is 3.3–5.5% of vesicle diameter, process basal width 2–5 μm, Willman and Moczydłowska, Reference Willman and Moczydłowska2011), and two specimens originally identified as Appendisphaera sp. (vesicle diameter 550 μm, process length 10–20 μm, process basal width 2–5 μm, Ye et al., Reference Ye, Tong, An, Tian, Zhao and Zhu2015). The assignment of these specimens to A. tenuis may obscure the morphological boundary between A. clava and A. tenuis, and thus remains questionable. The same argument goes for the specimen originally identified as Ericiasphaera aff. E. addspersa by Golubkova et al. (Reference Golubkova, Raevskaya and Kuznetsov2010, pl. IV, fig. 6a, b) that was later synonymized with A. tenuis by Sergeev et al. (Reference Sergeev, Knoll and Vorob'eva2011).

In some cases, Appendisphaera tenuis can also be akin to Cavaspina basiconica, which is differentiated from A. tenuis by its less densely arranged processes with a more prominent basal expansion. In practice, however, some specimens with a moderate density of processes can fit the diagnosis of either A. tenuis or C. basiconica (e.g., Liu and Moczydłowska, Reference Liu and Moczydłowska2019, fig. 39A–D), and more quantitative criteria are needed to distinguish these two species.

Genus Asterocapsoides Yin and Li, Reference Yin and Li1978, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014

Type species

Asterocapsoides sinensis Yin and Li, Reference Yin and Li1978, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Other species

Asterocapsoides fluctuensis Liu and Moczydłowska, Reference Liu and Moczydłowska2019; A. robustus Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; A. wenganensis (Chen and Liu, Reference Chen and Liu1986) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Asterocapsoides wenganensis (Chen and Liu, Reference Chen and Liu1986) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014
Figure 7

Reference Chen and Liu1986

Meghystrichosphaeridium wenganensis Chen and Liu, p. 51, pl. II, figs. 1, 3.

non Reference Yuan and Hofmann1998

Meghystrichosphaeridium wenganensis Chen and Liu; Yuan and Hofmann, p. 203, fig. 10C, D.

Reference Zhou, Brasier and Xue2001

Meghystrichosphaeridium chadianensis; Zhou et al., p. 1166, pl. 2, figs. 1–4.

non Reference Zhou, Brasier and Xue2001

Meghystrichosphaeridium chadianensis; Zhou et al., p. 1166, pl. 1, figs. 1–8; pl. 2, figs. 5–8.

Reference Zhou, Chen and Xue2002

Meghystrichosphaeridium chadianensis; Yuan et al., p. 75, fig. 103.

Reference Zhou, Yuan, Xiao, Chen and Xue2004b

Meghystrichosphaeridium chadianensis; Zhou et al., pl. V, fig. 4.

non Reference Zhou, Yuan, Xiao, Chen and Xue2004b

Meghystrichosphaeridium sp., Zhou et al., p. 354, pl. V, figs. 5, 6.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Asterocapsoides wenganensis (Chen and Liu) Xiao et al., p. 14, fig. 5.4–5.12.

Reference Shang, Liu and Moczydłowska2019

Asterocapsoides wenganensis (Chen and Liu) Xiao et al.; Shang et al., p. 11, fig. 6.

?Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2019

Asterocapsoides sp.; Ouyang et al., fig. 9C–E.

Reference Willman, Peel, Ineson, Schovsbo, Rugen and Frei2020

Asterocapsoides wenganensis; Willman et al., fig. 4c, d.

Figure 7. Asterocapsoides wenganensis (Chen and Liu, Reference Chen and Liu1986) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014. (1, 2) PB202012, thin section 21LHK-1-10, R34/4. (1) and (2) show the same area at different focal levels; red arrowheads denote large conical processes.

Neotype

The specimen illustrated by Xiao et al. (Reference Xiao, Zhou, Liu, Wang and Yuan2014, fig. 5.7) is here designated as a neotype (NIGPAS-94038-3193), reposited at NIGPAS, from Doushantuo Formation in Weng'an area, Guizhou Province, South China.

Description and measurements

Only a tangentially cut specimen was observed in thin section. The vesicle is estimated to be medium to large in size, originally spheroidal, with homomorphic, large conical processes that are likely basally in contact. Vesicle diameter of the tangential cross section is about 127 μm. The full length and basal width of processes are not captured in the thin section, but the process length is at least 42.7 μm and basal width is at least 24.2 μm based on measurements of processes partially captured in the thin section.

Material

One illustrated specimen (Fig. 7).

Remarks

Although the true vesicle diameter of the illustrated specimen cannot be determined for this specimen, which seems to be cut tangentially at the periphery of its vesicle, the specimen is probably around 200 μm in vesicle diameter. Accepting the estimated vesicle and process sizes, this specimen is most appropriately identified as Asterocapsoides wenganensis, which differs from A. robustus mainly in its fewer and proportionally larger conical processes.

One specimen identified as Asterocapsoides sp. (Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019, fig. 9C–E) is similar to A. wenganensis based on its large spheroidal vesicle (~389 μm in diameter) with uniform, conical processes that are about 63.9 μm in length (16.4% of vesicle diameter), about 41.8 μm in basal width, and basally connected. Despite these similarities, however, its processes have slim and slender tips that are bent and twisted, apparently supporting an outer membrane. The process tips may be too fragile to be preserved in the phosphatized A. wenganensis specimens reported in Chen and Liu (Reference Chen and Liu1986) and Xiao et al. (Reference Xiao, Zhou, Liu, Wang and Yuan2014). It is also possible that the process tips may have been lost due to mechanical breakage during reworking or acid extraction of the phosphatized specimens. These possibilities need to be confirmed or rejected with thin-section observation of the phosphatized specimens. Thus, this specimen, illustrated as Asterocapsoides sp. in Ouyang et al. (Reference Ouyang, Zhou, Xiao, Chen and Shao2019), is here tentatively accepted as A. wenganensis.

A neotype is designated here for Asterocapsoides wenganensis because the repository of the original holotype (specimen illustrated in Chen and Liu, Reference Chen and Liu1986, pl. II, figs. 1, 3) from the Doushantuo Formation in Baiyan, Weng'an area, Guizhou Province, South China, cannot be located.

Genus Bullatosphaera Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009

Type species

Bullatosphaera velata Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009.

Other species

Bullatosphaera? colliformis n. sp.

Bullatosphaera? colliformis new species
 Figures 8, 9

Holotype

PB202013, thin section 19CW-6-2, ZEISS Scope A1 coordinates 11×106, England Finder coordinates K30/3 (Fig. 8.18.6), reposited at NIGPAS, from Doushantuo Formation at the Caowan section in Zhangjiajie area, Hunan Province, South China.

Figure 8. Bullatosphaera? colliformis new species. Red arrowheads denote basally constricted spherical or hemispherical ornamentations. (1–6) Holotype, PB202013, thin section 19CW-6-2, K30/3; circled 2, 3, and 6 in (1) mark areas magnified in (2, 3, 6), respectively; circled 4 in (1) marks areas in (4, 5), which show the same area at different focal levels. (7–10, 13) PB202014, thin section 19CW-6-12, L31/4. (7, 8) Show the same area at different focal levels; circled 9 in (7) marks area magnified in (9); circled 10 and 13 in (8) mark areas magnified in (10) and (13), respectively. (11, 12, 14) PB202015, thin section 19CW-9-7, O35/4; circled 12 and 14 in (11) mark areas magnified in (12) and (14), respectively. Scale bars in (3) and (6) also apply to (2, 4, 5); scale bars in (9) and (12) also apply to (10, 13, 14).

Figure 9. Sketch of Bullatosphaera? colliformis new species.

Diagnosis

Vesicle spheroidal, small to medium-sized, covered by closely packed, small, spherical or hemispherical structures that are analogous to processes. The spherical or hemispherical structures are uniform in size, hollow, and attached to the vesicle surface by a thin, short, cylindrical, neck-like basal stem, but they do not communicate with the vesicle interior.

Description and measurements

Vesicle diameter 94 μm in holotype, 81 and 88 μm in the two other specimens. Spherical or hemispherical structures 8.1 μm wide and 5.5 μm high in holotype, whereas those structures in the two other specimens are 7.7 and 9.9 μm wide and 6.5 and 8.1 μm high, respectively, with a density of 11–14 such structures (13 in holotype) per 100 μm of vesicle periphery.

Etymology

From Latin collum, neck, with reference to the neck-like stem that connects the spherical processes to the vesicle wall.

Material

Three illustrated specimens (Fig. 8).

Remarks

The three illustrated specimens are characterized by the uniform spherical or hemispherical structures surrounding their vesicles, which are distinctive structures of Bullatosphaera. The lack of a second vesicle wall that surrounds the ornamentations, which is a diagnostic feature of Bullatosphaera, could be a result of degradation and diagenesis, as is possibly the case for Bullatosphaera sp. that was illustrated by Xiao et al. (Reference Xiao, Zhou, Liu, Wang and Yuan2014, p. 16, fig. 6.7, 6.8). The basally constricted stem differentiates B.? colliformis n. sp. from B. velata Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009, and Bullatosphaera sp. (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014). However, this feature is not included in the diagnosis for the genus Bullatosphaera, therefore the placement of this new species in the genus Bullatosphaera remains provisional.

Genus Cavaspina Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993

Type species

Cavaspina acuminata (Kolosova, Reference Kolosova1991) Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993.

Other species

Cavaspina basiconica Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993; C. conica Liu and Moczydłowska, Reference Liu and Moczydłowska2019; C. tiwariae Xiao in Xiao et al., Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022; C. uria (Nagovitsin and Faizullin in Nagovitsin et al., Reference Nagovitsin, Faizullin and Yakshin2004) Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012.

Cavaspina acuminata (Kolosova, Reference Kolosova1991) Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993
 Figure 10.1

Reference Yin, Xue and Yuan1990

3-D preserved spinose microsphere; Yin et al., pl. II.A–B.

Reference Moczydłowska, Vidal and Rudavskaya1993

Cavaspina acuminata (Kolosova) Moczydłowska, Vidal, and Rudavskaya, p. 509, text-fig. 10A–B.

Reference Zhang, Yin, Xiao and Knoll1998

Goniosphaeridium acuminatun (Kolosova); Zhang et al., p. 28, fig. 8.3.

Reference Yuan, Xiao, Yin, Knoll, Zhou and Mu2002

Goniosphaeridium acuminatun (Kolosova) Zhang et al.; Yuan et al., p. 74, fig. 99.

Reference Nagovitsin, Faizullin and Yakshin2004

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Nagovitsin et al., p. 12, pl. II, figs. 7, 8.

Reference Moczydłowska2005

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Moczydłowska, p. 298, fig. 6A, B.

Reference Veis, Vorob'eva and Golubkova2006

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Veis et al., pl. I, figs. 5, 6, pl. II, fig. 1.

Reference Willman and Moczydłowska2008

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Willman and Moczydłowska, p. 522, fig. 9C.

Reference Vorob'eva, Sergeev and Knoll2009

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Vorob'eva et al., p. 177, fig. 7.11.

Reference Willman and Moczydłowska2011

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Willman and Moczydłowska, p. 24, pl. II, fig. 3.

Reference Moczydłowska and Nagovitsin2012

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Moczydłowska and Nagovitsin, p. 13, fig. 4C, E, F.

Reference Zeng, Chen, Li, Zhou, Zhang and Peng2013

Tanarium sp.; Zeng et al., fig. 3.5.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Xiao et al., p. 16, fig. 7.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Liu et al., p. 44, fig. 27.1, 27.2.

Reference Shukla and Tiwari2014

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Shukla and Tiwari, p. 216, fig. 5C, D.

Reference Prasad and Asher2016

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Prasad and Asher, p. 46, pl. IV, figs. 5, 6.

Reference Nie, Liu and Dong2017

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Nie et al., p. 374, fig. 5.1–5.4.

Reference Liu and Moczydłowska2019

Cavaspina acuminata (Kolosova, Reference Kolosova1991) Moczydłowska et al. Reference Moczydłowska, Vidal and Rudavskaya1993; Liu and Moczydłowska, p. 76, fig. 38.

Reference Shang, Liu and Moczydłowska2019

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Shang et al., p. 19, fig. 8A–D.

Reference Shang, Liu and Liu2020

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Shang and Liu, p. 157, fig. 5D–H.

Reference Grazhdankin, Nagovitsin, Golubkova, Karlova, Kochnev, Rogov and Marusin2020

Cavaspina acuminata; Grazhdankin et al., fig. 4H.

Reference Willman, Peel, Ineson, Schovsbo, Rugen and Frei2020

Cavaspina acuminata; Willman et al., fig. 4a, b.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Ouyang et al., fig. 13A.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Shi et al., fig. 7C–E (illustrated in Fig. 11.1, one of the two specimens described here).

?Reference Ye, Li, Tong, An, Hu and Xiao2022

Cavaspina acuminata (Kolosova) Moczydłowska et al.; Ye et al., fig. 13A, B.

Reference Golubkova2023

Cavaspina acuminata (Kolosova) emend. Moczydłowska; Golubkova, pl. 7, fig. 5.

Figure 10. (1) Cavaspina acuminata (Kolosova, Reference Kolosova1991) Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, PB202016, thin section 21DC-3-1, Q30/4. (2) Cavaspina basiconica Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, PB202017, thin section 21DC-5-4, M40/1. (3, 4) Cavaspina uria (Nagovitsin and Faizullin in Nagovitsin et al., Reference Nagovitsin, Faizullin and Yakshin2004) Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012, thin section 21DC-5-4; red arrowheads in (1–4) denote conical processes; (3) PB202018, G41/1; (4) PB202019, E45/4. (5–7) Eotylotopalla sp. PB202025, thin section 19CW-6-15, O41/1, showing the same area at different focal levels. Scale bars in (5) and (7) also apply to (6).

Figure 11. (1–4, 7, 8) Eotylotopalla dactylos Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998. (1) PB202020, thin section 19TP-1-13; (2) PB202021 (left) and PB202022 (right), thin section 21DC-2-38, Q48; (3, 4) PB202023, thin section 14HA-115-1, D47/3, showing the same area at different focal levels; (7, 8) PB202024, thin section 21DC-5-3, Q30/3, showing the same area at different focal levels. (5, 6, 9–12) Eotylotopalla cf. E. dactylos Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998, PB202026, thin section 21DC-2-12, O21/4. (5, 6) The same area at different focal levels; (9–12) magnified views of the processes denoted by circled 9–12 in (6) under cross-polarized light; red arrowheads denote the angular transition from the side wall of the processes to the distal end.

Holotype

YIGS Nr 87-123, reposited at the Geological Museum of Yakutian Institute of Geologic Sciences (present Diamond and Precious Metal Geology Institute, Siberian Branch, Russian Academy of Sciences), from the Ediacaran Torgo Formation, Berezovo area, eastern Siberia (Kolosova, Reference Kolosova1991, p. 57, fig. 4.1).

Description and measurements

Vesicle small, spheroidal, bearing sparsely and evenly distributed, acutely conical processes. The illustrated specimen has a vesicle diameter of about 84 μm, process length about 6.3 μm (7.5% of vesicle diameter), and process basal width about 1.5 μm (process length to basal width ratio ~4.2), with about 23 processes per 100 μm of vesicle periphery. The other specimen has a vesicle diameter of about 41 μm, process length about 5.7 μm (13.8% of vesicle diameter), and process basal width about 1.8 μm (process length to basal width ratio ~3.2), with 12 processes per 100 μm of vesicle periphery.

Material

One illustrated specimen (Fig. 10.1) and one additional specimen.

Remarks

Being one of the most widely distributed Ediacaran acanthomorphic species, Cavaspina acuminata is characterized by its relatively sparsely distributed, short, and acutely conical processes. Both specimens described here, although not well preserved and together covering a large variation in size and process density, meet the diagnosis of C. acuminata, best demonstrated by the process basal width (<2 μm) and process length to basal width ratio (>3).

One Cavaspina acuminata specimen reported by Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022, fig. 13A, B) appears to have terminally branching processes and, if confirmed, would be better identified as Variomargosphaeridium gracile Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014 (see Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021, fig. 22A). Therefore, the identification of the specimen illustrated in Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022) as C. acuminata is questioned here, pending re-examination of the specimen to confirm or reject the terminal branching structures.

Cavaspina basiconica Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993
Figure 10.2

Reference Moczydłowska, Vidal and Rudavskaya1993

Cavaspina basiconica Moczydłowska, Vidal, and Rudavskaya, p. 510, text-fig. 11.

Reference Zhang, Yin, Xiao and Knoll1998

Meghystrichosphaeridium perfectum (Kolosova, Reference Kolosova1991) Zhang et al., p. 36, fig. 10.7, 10.8.

Reference Zhou, Brasier and Xue2001

Meghystrichosphaeridium chadianensis Chen and Liu, Reference Chen and Liu1986, emend. Zhang et al.; Zhou et al., p. 1166, pl. II, figs. 5, 6.

Reference Moczydłowska2005

Cavaspina basiconica Moczydłowska et al.; Moczydłowska, p. 300, fig. 6C.

Reference Grey2005

Gyalosphaeridium basiconicum (Moczydłowska et al.) Grey, p. 277.

Reference Grey2005

Gyalosphaeridium multispinulosum Grey, p. 273, figs. 11I, 44I, 179A–D, 180A–E.

Reference Willman, Moczydłowska and Grey2006

Cavaspina basiconica Moczydłowska et al.; Willman et al., p. 26, pl. I, figs. 3, 4.

Reference Willman and Moczydłowska2008

Cavaspina basiconica Moczydłowska et al.; Willman and Moczydłowska, p. 522, fig. 9D–E.

Reference McFadden, Xiao, Zhou and Kowalewski2009

Meghystrichosphaeridium perfectum (Kolosova) Zhang et al.; McFadden et al., fig. 5D.

Reference Willman and Moczydłowska2011

Cavaspina basiconica Moczydłowska et al.; Willman and Moczydłowska, p. 25, pl. II, figs. 1, 2.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Cavaspina basiconica Moczydłowska et al.; Xiao et al., p. 16, fig. 8.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Cavaspina basiconica Moczydłowska et al.; Liu et al., p. 44, fig. 27.3–27.6.

Reference Shukla and Tiwari2014

Cavaspina basiconica Moczydłowska et al.; Shukla and Tiwari, p. 216, fig. 5E, F.

Reference Prasad and Asher2016

Cavaspina basiconica Moczydłowska et al.; Prasad and Asher, p. 46, pl. IV, figs. 7, 8.

Reference Nie, Liu and Dong2017

Cavaspina basiconica Moczydłowska et al.; Nie et al., p. 374, fig. 5.5, 5.6.

Reference Ouyang, Guan, Zhou and Xiao2017

?Cavaspina basiconica; Ouyang et al., fig. 8A–C.

Reference Liu and Moczydłowska2019

Cavaspina basiconica Moczydłowska et al.; Liu and Moczydłowska, p. 78, fig. 39.

Reference Anderson, McMahon, Macdonald, Jones and Briggs2019

Cavaspina basiconica Moczydłowska et al.; Anderson et al., p. 509, fig. 7A–F.

Reference Shang, Liu and Moczydłowska2019

Cavaspina basiconica Moczydłowska et al.; Shang et al., p. 21, fig. 8E–G.

Reference Vorob'eva and Petrov2020

Cavaspina basiconica Moczydłowska et al.; Vorob'eva and Petrov, p. 374, pl. II, figs. 16–18.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Cavaspina basiconica Moczydłowska et al.; Ye et al., p. 27, figs. 13C, D, 14E–J.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Cavaspina cf. C. basiconica; Shi et al., fig. 7F–H (illustrated in Fig. 10.2 of this paper, one of the two specimens described here).

Holotype

PMU-Sib.1-Y/55/2, reposited at Uppsala University, from the Ediacaran Khamaka Formation, Nepa–Botuoba region, Yakutia, Siberia (Moczydłowska et al., Reference Moczydłowska, Vidal and Rudavskaya1993, p. 510, text-fig. 11A, B, D).

Description and measurements

Vesicle small to medium-sized, spheroidal, bearing a small to moderate number of evenly distributed processes. Processes conical, with a small but clearly defined basal expansion that is deflated. The illustrated specimen has a vesicle diameter of about 138 μm, process length about 12.3 μm (8.9% of vesicle diameter), and process basal width about 10.2 μm (process length to basal width ratio ~1.2), with about one process per 100 μm of vesicle periphery. The other specimen has a vesicle diameter of about 94 μm, process length about 12.5 μm (13.2% of vesicle diameter), and process basal width about 3.8 μm (process length to basal width ratio ~3.3), with 17 processes per 100 μm of vesicle periphery.

Material

One illustrated specimen (Fig. 10.2) and one additional specimen illustrated in Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017, fig. 8A–C).

Remarks

Both specimens described here are poorly preserved, thus the seemingly ciliate apical part of the processes are likely a result of diagenetic contraction of originally acutely tapering processes. Although resembling Cavaspina acuminata in morphometrics of process shape, the two C. basiconica specimens described here can be readily recognized by their processes with a deflated basal expansion. This feature also distinguishes them from C. uria, whose processes have a broad base that is not deflated.

Cavaspina uria (Nagovitsin and Faizullin in Nagovitsin et al., Reference Nagovitsin, Faizullin and Yakshin2004) Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012 Figure 10.3, 10.4

Reference Nagovitsin, Faizullin and Yakshin2004

Goniosphaeridium urium Nagovitsin and Faizullin in Nagovitsin et al., p. 13, pl. II, fig. 1.

Reference Veis, Vorob'eva and Golubkova2006

Cavaspina sp.; Veis et al., pl. I, fig. 7, pl. II, figs. 3–5.

Reference Sergeev, Knoll and Vorob'eva2011

Goniosphaeridium minutum Nagovitsin and Faizullin; Sergeev et al., p. 1003, fig. 7.7.

Reference Moczydłowska and Nagovitsin2012

Cavaspina uria (Nagovitsin and Faizullin) Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, p. 14, fig. 4G–I.

Reference Ouyang, Zhou, Xiao, Chen and Shao2019

Asterocapsoides robustus; Ouyang et al., fig. 9A, B.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Cavaspina uria (Nagovitsin and Faizullin in Nagovitsin et al.) Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin; Shi et al., fig. 7I–M (specimens illustrated in Fig. 10.3, 10.4, and described here).

Holotype

Copy 7 of preparation PN 8/17(2)-1, No. 673 CSGM, reposited at Central Siberian Geological Museum of the United Institute of Geology, Geophysics and Mineralogy (present Trofimuk Institute of Petroleum–Gas Geology and Geophysics), Siberian Branch, Russian Academy of Sciences, from the Ediacaran Ura Formation, Patom Uplift, eastern Siberia (Nagovitsin et al., Reference Nagovitsin, Faizullin and Yakshin2004, pl. II, fig. 1).

Description and measurements

Vesicle spheroidal, small, bearing evenly distributed conical processes. Process uniform, with a triangular outline in thin-sectional view. Vesicle diameter 41–99 μm (N = 6, mean = 60 μm, SD = 20 μm). Based on measurements of four better preserved specimens among the six available ones, process length is 5.2–7.2 μm (N = 4, mean = 6.0 μm, SD = 1.0 μm), representing 8.8–13.4% of vesicle diameter (N = 4, mean = 10.8%, SD = 2.0%), process basal width 3.3–4.6 μm (N = 4, mean = 3.8 μm, SD = 0.6 μm), process length to basal width ratio 1.5–1.8 (N = 4, mean = 1.6, SD = 0.1), and 11–17 processes (N = 4, mean = 15, SD = 3) per 100 μm of vesicle periphery.

Material

Two illustrated specimens (Fig. 10.3, 10.4), two specimens illustrated in Shi et al. (Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 7J, M), and two additional specimens.

Remarks

With conical processes whose length accounts for about 10% of vesicle diameter, Cavaspina uria is somewhat similar to Asterocapsoides robustus in process shape. However, most published specimens of A. robustus are much larger in vesicle size. The specimen identified as A. robustus from the Doushantuo Formation in Zhangcunping area, South China (Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019, fig. 9A, B) has evenly distributed conical processes, with vesicle diameter of about 70 μm, process length of 7.0 μm, and process basal width of 4.0 μm, which are comparable to those of C. uria, especially the holotype (vesicle diameter 80 μm, process length 7–8 μm, process basal width 4–5 μm), but differ significantly from typical A. robustus specimens. Thus, we reassign this specimen to C. uria.

Genus Eotylotopalla Yin, Reference Yin1987

Type species

Eotylotopalla delicata Yin, Reference Yin1987.

Other species

Eotylotopalla apophysa (Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009) Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022; E. dactylos Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998; E. quadrata Liu and Moczydłowska, Reference Liu and Moczydłowska2019; E. strobilata (Faizullin, Reference Faizullin1998) Sergeev et al., Reference Sergeev, Knoll and Vorob'eva2011 (E. minorosphaera Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009); E. inflata n. sp.

Remarks

Eotylotopalla now accommodates most of the Ediacaran acanthomorphs with inflated processes that are terminally rounded or truncated (i.e., lacking a pointed process tip). Processes of Eotylotopalla can be cylindrical (E. dactylos), hemispherical (E. apophysa, E. delicata, E. strobilata, differentiated mainly by their proportional process size relative to vesicle diameter), cuboidal (E. quadrata), or distally inflated (E. inflata n. sp.). With the addition of E. inflata n. sp., Eotylotopalla can also have biform processes (although different from the basally inflated biform processes of Mengeosphaera). Despite these morphological variations, Eotylotopalla remains a very distinctive genus characterized by its distally expanded, rounded, flat or truncated processes.

Eotylotopalla dactylos Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998
Figure 11.111.4, 11.7, 11.8

Reference Zhang, Yin, Xiao and Knoll1998

Eotylotopalla dactylos Zhang et al., p. 26, fig. 7.8, 7.9.

Reference Zhou, Xie, McFadden, Xiao and Yuan2007

Eotylotopalla dactylos; Zhou et al., fig. 4F.

Reference Yin, Wang, Yuan and Zhou2011

Eotylotopalla dactylos; L. Yin et al., fig. 3G.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Eotylotopalla dactylos Zhang et al.; Xiao et al., p. 20, fig. 11.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Eotylotopalla dactylos Zhang et al.; Liu et al., p. 50, fig. 31.1–31.9.

Reference Liu, Chen, Zhu, Li, Yin and Shang2014b

Eotylotopalla dactylos; Liu et al., fig. 7B.

Reference Shukla and Tiwari2014

Eotylotopalla dactylos Zhang et al.; Shukla and Tiwari, p. 217, fig. 6A, B.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Eotylotopalla sp.; Liu et al., p. 61, fig. 31.10–31.13.

Reference Ouyang, Zhou, Guan and Wang2015

Eotylotopalla dactylos Zhang et al.; Ouyang et al., p. 217, pl. I, fig. 11.

Reference Liu and Moczydłowska2019

Eotylotopalla dactylos Zhang et al.; Liu and Moczydłowska, p. 95, fig. 48.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Eotylotopalla dactylos Zhang et al.; Ouyang et al., fig. 14K, L.

?Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Eotylotopalla dactylos Zhang et al.; Ouyang et al., fig. 14J.

Reference Liu, Qi, Fan, Guo and Pei2021

Eotylotopalla dactylos Zhang et al.; Liu et al., fig. 5.6, 5.7.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Eotylotopalla dactylos Zhang et al.; Shi et al., fig. 8A (illustrated in Fig. 11.7, 11.8, one of the specimens described here).

Reference Ye, Li, Tong, An, Hu and Xiao2022

Eotylotopalla dactylos Zhang et al.; Ye et al., p. 37, fig. 23A–F.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Eotylotopalla sp.; Ye et al., p. 37, fig. 23H–J.

Holotype

Specimen illustrated in Zhang et al. (Reference Zhang, Yin, Xiao and Knoll1998, fig. 7.8), thin section #XDV-29m-6, Leitz coordinates 48×123, reposited at NIGPAS, from the Ediacaran Doushantuo Formation at Xiaofenghe in the Yangtze Gorges area, Hubei Province, South China.

Description and measurements

Vesicle small and spheroidal, with uniform, near evenly distributed processes that can be either basally connected or separated. Processes are cylindrical or taper slightly toward the distal end, with a rounded or blunt terminal end. Vesicle diameter 39–60 μm (N = 5, mean = 49 μm, SD = 7 μm), with 5–11 processes per 100 μm of vesicle periphery (N = 3, mean = 7 μm, SD = 4); process lengths 6.4–10.2 μm (N = 5, mean = 7.7 μm, SD = 0.7 μm) or 13.2–26.0% of vesicle diameter (N = 5, mean = 16.4%, SD = 5.4%), and process basal width 7.1–13.2 μm (N = 5, mean = 9.9 μm, SD = 3.0 μm) or 14.9–24.4% of vesicle diameter (N = 5, mean = 20.3%, SD = 4.0%).

Material

Five illustrated specimens (Fig. 11.111.4, 11.7, 11.8), including one (Fig. 11.7, 11.8) previously illustrated in Shi et al. (Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 8A) and another (Fig. 11.3, 11.4) previously assigned to “indeterminate acanthomorphs” by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017, table 1).

Remarks

Compared with other Eotylotopalla species with very limited intraspecific morphological variation (E. delicata, E. inflata n. sp., E. quadrata, E. strobilata), processes of E. dactylos are relatively more variable in morphology, which can be cylindrical (digitate) or conical, basally separate, connected, or joined, with moderate basal or terminal expansions. Measurements of previously published E. dactylos illustrations (as listed in synonym list, Fig. 12) show that most published specimens have vesicle diameters of 30–105 μm, 5–31 μm in process length (10–30% of vesicle diameter), 6–26 μm in process basal width (11–28% of vesicle diameter), with 3–12 processes per 100 μm of vesicle periphery. Specimens described here fit the diagnostic features of E. dactylos both qualitatively and quantitatively.

Figure 12. Morphological comparisons between Eotylotopalla specimens described here, published Eotylotopalla dactylos, and specimens identified as Eotylotopalla sp. by Liu et al. (Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) and by Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022) but reassigned to Eotylotopalla dactylos in this study. Symbols with black outline represent specimens described in this study. Note that two of the three specimens published as Eotylotopalla sp. (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 31.10, 31.11, and Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022, fig. 23H–J) are very poorly preserved thus their process density (number of processes per 100 μm of vesicle periphery) is unmeasurable.

Three poorly preserved specimens previously published by Liu et al. (Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 31.10–31.13) and Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022, fig. 23H–J) have been identified as Eotylotopalla sp. despite their similarities to E. dactylos acknowledged by the original authors. These specimens were considered different from E. dactylos in their more sparsely distributed processes (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022). However, if we quantitively assess previously published specimens of E. dactylos, there is a wide range of process density (Fig. 12). Several E. dactylos specimens accepted by various authors also have sparsely distributed processes (e.g., Zhou et al., Reference Zhou, Xie, McFadden, Xiao and Yuan2007, fig. 4F), with 2–3 processes per 100 μm of vesicle periphery, which is not much different from the three specimens of Eotylotopalla sp. cited above (Fig. 12). Thus, considering the intraspecific variation in process density, we reassign these Eotylotopalla sp. specimens to E. dactylos.

Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022) transferred Timanisphaera apophysa Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009, to Eotylotopalla and synonymized it with E. grandis Tang et al., Reference Tang, Pang, Xiao, Yuan, Ou and Wan2013, thus forming a new combination E. apophysa (Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009) Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022, characterized by its large vesicles with sparse but proportionally large, hemispherical processes. One specimen assigned to T. apophysa (Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022, fig. 23G) is about 170 μm in vesicle diameter and notably smaller than the holotype measurements mentioned in the original diagnosis (vesicle size 265–450 μm in diameter, process 70–110 μm in length and 50–90 μm in width). However, considering that Ye et al.'s (Reference Ye, Li, Tong, An, Hu and Xiao2022) specimen is silicified and was examined in a petrographic thin section, its vesicle diameter measurement is likely a minimum estimate because the specimen may be tangentially cut. Similarly, a specimen of E. dactylos illustrated by Ouyang et al. (Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021, fig. 14J), characterized by an even smaller vesicle (~59 μm in diameter) and a small number of large processes (~22 μm in length or 37% of vesicle diameter) also may be assigned to E. apophysa. Thus, the specimen of E. dactylos published in Ouyang et al. (Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021) is questionably included in the synonym list.

Eotylotopalla cf. E. dactylos Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998
Figure 11.5, 11.6, 11.911.12

cf. Reference Zhang, Yin, Xiao and Knoll1998

Eotylotopalla dactylos Zhang et al., p. 26, fig. 7.8, 7.9.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Eotylotopalla cf. E. dactylos; Shi et al., fig. 8B (the specimen described here and illustrated in Fig. 11.5, 11.6, 11.911.12).

Description and measurements

Vesicle small and spheroidal, with basally separated processes densely distributed on the vesicle. Processes are uniform and truncated conical in shape. The side walls of processes are straight. Vesicle diameter about 64 μm, with about 7 processes per 100 μm of vesicle periphery; processes length 6.9–10.9 μm (with an average of 8.9 μm measured on four processes) or 10.7–17.0% of vesicle diameter (with an average of 13.8%), process basal width 7.6–12.5 μm (with an average of 10.7 μm measured on four processes), process terminal width 3.7–6.4 μm (with an average of 5.0 μm measured on four processes).

Material

One illustrated specimen (Fig. 11.5, 11.6, 11.911.12).

Remarks

The illustrated specimen is distinct in its sharply terminated processes but is otherwise comparable to Eotylotopalla. Examination under polarized light (Fig. 11.911.12) shows that the process terminal truncation is not a taphonomic artifact (e.g., recrystallization). Truncated terminations are common in previously reported E. dactylos specimens, but the transition from the side wall to distal end of the processes in these specimens is smooth and gradual, as opposed to the angular transition observed in the illustrated specimen (red arrowheads in Fig. 11.911.12). We cannot rule out the possibility that the angular transition is due to mechanical breakage of the processes, however the uniform length of the processes is remarkable for broken processes. Abrasion by tumbling at a constant rate may result in similar process lengths but is unlikely to form flat terminations as observed. Thus, this specimen is currently placed in an open nomenclature related to E. dactylos.

Eotylotopalla inflata new species
 Figure 13

Holotype

PB202027, thin section 19TP-1-38, ZEISS Scope A1 coordinates 14×105, England Finder coordinates N30/3 (Fig. 13), reposited at NIGPAS, from Doushantuo Formation at the Tianping section in Zhangjiajie area, Hunan Province, South China.

Figure 13. Eotylotopalla inflata new species. (1–4) Holotype, PB202027, thin section 19TP-1-38, N30/3, showing the same area at different focal levels.

Diagnosis

A species of Eotylotopalla with terminally inflated processes that have a slightly expanded base, a neck, and a bulbous distal end, with an overall shape resembling a button mushroom.

Description and measurements

Vesicle small, spheroidal or ovoidal, with evenly distributed, basally connected or separated processes. Processes hollow and open to vesicle cavity, homomorphic, with a widened base, and an inflated bulbous termination, and a neck- or waist-like structure in between. Vesicle diameter about 64 μm, about 12 processes per 100 μm of vesicle periphery; processes length 8.7–11.5 μm with an average of 10.4 μm measured on eight processes or 13.6–18.0% of vesicle diameter with an average of 16.1%, process basal width 5.7–8.5 μm with an average value of 7.1 μm measured on eight processes, maximal width of inflated process termination 4.4–6.4 μm with an average value of 5.5 μm measured on eight processes, minimal width of process waist 2.5–3.2 μm with an average value of 2.8 μm measured on seven processes.

Etymology

From Latin inflatus, inflated, with reference to the inflated terminal end of the processes.

Material

A single well-preserved specimen (the holotype, Fig. 13).

Remarks

The illustrated specimen is distinctive in its basally widened and terminally swollen processes that resemble a button mushroom. This distinctive morphology is observed in more than 20 processes in the specimen, supporting the repeatability and arguing against a taphonomic origin of this diagnostic feature. Somewhat similar process morphology has been described in Stellarossica ampla Vorob'eva and Sergeev, Reference Vorob'eva and Sergeev2018, from the Ura Formation in Siberia and two species of Keltmia (K. cornifera Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009, and K. irregularia Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009) from the Vychegda Formation in East European Platform. However, these latter species can be distinguished from Eotylotopalla inflata n. sp. by their much larger vesicle, notably fewer processes, much larger proportional lengths of processes, and most importantly, the terminal end of their processes is not as strongly inflated as in the new species where the maximum width of process termination is almost double the minimum width of process waist. There are other acanthomorphs with significantly expanded process bases and terminations, including all Urasphaera species and Weissiella brevis Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014. However, Urasphaera species and Weissiella brevis are characterized by processes with flat or truncated terminations, thus different from the bulbous terminations reported here.

Papillomembrana Spjeldnaes, Reference Spjeldnaes1963, emend. Vidal, Reference Vidal1990, is another genus characterized by processes with a bulbous terminal end, but it is diagnosed as an acanthomorph with medium to large vesicle size (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014), and the processes of both P. boletiformis Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014, and P. compta Spjeldnaes, Reference Spjeldnaes1963, emend. Vidal, Reference Vidal1990, lack a well-defined basal expansion and have a basal width smaller than the terminal width. The illustrated specimen is small in vesicle size, and its processes are basally widened, thus different from known Papillomembrana species. To assign the illustrated specimen to Papillomembrana would require an emendation to this genus and would significantly increase the morphological perimeter of this genus. Considering that the small vesicle with densely distributed, distally rounded processes of the specimen described here (Fig. 13) fits the genus diagnosis of Eotylotopalla, and that it is different from other existing species of Eotylotopalla species in its basally and distally expanded processes, we establish a new species of Eotylotopalla even though there is only one available specimen.

Eotylotopalla sp.
Figure 10.510.7

Description and measurements

Small spheroidal vesicle with large, hollow, heteromorphic processes that can be either cylindrical or bulbous. Cylindrical-shaped processes have rounded or blunt terminal ends. Some processes show a notable constriction in the basal or middle part, resulting in mushroom- or dumbbell-like morphology. The processes vary in basal width and the presence of a constriction but are more consistent in length and the rounded terminal end. Vesicle diameter about 73 μm; process length 21.4–30.5 μm (measured on seven processes, with an average of 25.1 μm and a standard deviation of 3.0 μm), process basal width 12.6–30.5 μm (on seven processes, with an average of 20.2 μm and a standard deviation of 6.0 μm), process terminal width 14.7–27.4 μm (on five processes, with an average of 19.3 μm and a standard deviation of 4.6 μm), process constriction width 6.2–19.1 μm (on four processes, with an average of 10.1 μm and a standard deviation of 5.2 μm). About seven processes are present around half of the vesicle periphery, equivalent to three processes per 100 μm of vesicle periphery.

Material

One specimen illustrated in Figure 10.510.7.

Remarks

The specimen described here is similar to Eotylotopalla dactylos in vesicle size (Fig. 12) and the presence of cylindrical processes with rounded or blunt terminal ends. It is also similar to E. apophysa and E. delicata in the presence of bulbous-shaped processes, and to E. inflata n. sp. in the presence of mushroom-like processes. However, it is distinct in its remarkably heteromorphic processes, which can be 12.6–30.5 μm in basal width and can be cylindrical or mushroom-like due to the presence of a constriction (Fig. 10.7). Variation in process size and shape has been reported for E. dactylos (e.g., Zhou et al., Reference Zhou, Xie, McFadden, Xiao and Yuan2007, fig. 4F; Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 31.4), but the amount of morphological variation observed in the single specimen illustrated here is remarkable. On the other hand, the irregular morphology of the only available specimen dissuades us from establishing a new species. Therefore, although this specimen probably represents a new form, it is temporarily placed in open nomenclature.

Genus Hocosphaeridium Zang in Zang and Walter, Reference Zang and Walter1992, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Type species

Hocosphaeridium scaberfacium Zang in Zang and Walter, Reference Zang and Walter1992, emend. Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a.

Other species

Hocosphaeridium anozos (Willman in Willman and Moczydłowska, Reference Willman and Moczydłowska2008) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; H. dilatatum Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a.

Hocosphaeridium anozos (Willman in Willman and Moczydłowska, Reference Willman and Moczydłowska2008), Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014
 Figure 14

Reference Zang and Walter1992

Hocosphaeridium scaberfacium Zang in Zang and Walter, fig. 45 G (not 45A–F).

Reference Grey2005

Tanarium irregulare? Moczydłowska, Vidal, and Rudavskaya; Grey, p. 309, fig. 225.

Reference Willman and Moczydłowska2008

Tanarium anozos Willman in Willman and Moczydłowska, p. 526, fig. 13A–F.

Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011

Tanarium anozos Willman; C. Yin et al., fig. 6d.

Reference Liu, Yin, Chen, Tang and Gao2012

Tanarium anozos Willman and Moczydłowska; Liu et al., fig. 3A–C.

Reference Liu, Yin, Chen, Tang and Gao2013

Tanarium anozos; Liu et al., fig. 11B.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Hocosphaeridium anozos (Willman in Willman and Moczydłowska) Xiao et al., p. 28, fig. 16.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Hocosphaeridium anozos (Willman in Willman and Moczydłowska) Xiao et al.; Liu et al., p. 75, figs. 37, 38, 39.1.

Reference Liu, Chen, Zhu, Li, Yin and Shang2014b

Hocosphaeridium anozos; Liu et al., fig. 8A, B.

non Reference Prasad and Asher2016

Tanarium anozos Willman in Willman and Moczydłowska; Prasad and Asher, p. 54, pl. VII, figs. 6, 7.

Reference Hawkins, Xiao, Jiang, Wang and Shi2017

Hocosphaeridium anozos; Hawkins et al., fig. 7E, F.

Reference Liu and Moczydłowska2019

Hocosphaeridium anozos (Willman in Willman and Moczydłowska) Xiao et al.; Liu and Moczydłowska, p. 113, fig. 60.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Hocosphaeridium anozos (Willman in Willman and Moczydłowska) Xiao et al.; Shi et al., fig. 8G–K (two of the 20 specimens described here).

Figure 14. Hocosphaeridium anozos (Willman in Willman and Moczydłowska, Reference Willman and Moczydłowska2008) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; red arrowheads denote hooked process terminations. (1–5) PB202028, thin section 21DC-2-20, R20/2; circled 2–5 in (1) mark areas magnified in (2–5), respectively; scale bars in (3) and (5) also apply to (2) and (4). (6–8) PB202029, thin section 21DC-2-20, P18/2; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively; scale bar in (8) also applies to (7). (9–11) PB202030, thin section 21DC-2-20, R21; circled 10 and 11 in (9) mark areas magnified in (10) and (11), respectively. (12–14) PB202031, thin section 21DC-2-20, O18/3; circled 13 and 14 in (12) mark areas magnified in (13) and (14), respectively.

Holotype

CPC 39635, reposited at Commonwealth Palaeontological Collection (CPC) at Geoscience Australia, Canberra, from the Ediacaran Tanana Formation of the Giles 1 drillhole in Officer Basin, South Australia.

Description and measurements

Most vesicles are deformed to various degrees, but were originally spheroidal in shape, and measurements can be taken on relatively well-preserved specimens. Processes evenly distributed on the vesicle surface, cylindrical or slightly tapering toward a distal end that is hooked or recurved. Vesicle diameter 88–227 μm (N = 13, mean = 143 μm, SD = 39 μm); process length 20.8–54.8 μm (N = 19, mean = 33.4 μm, SD = 7.4 μm), 14.0–34.9% of vesicle diameter (N = 13, mean = 24.6%, SD = 7.3%); process width (diameter) 1.0–2.4 μm (N = 20, mean = 1.9 μm, SD = 0.3 μm); process density unmeasurable due to the small number of processes with a well-preserved base.

Material

Four illustrated specimens (Fig. 14) and 16 additional specimens (including the one illustrated by Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 8J, K).

Remarks

These specimens are poorly preserved in general, but all bear a characteristically hooked tip in the terminal end of their thin, cylindrical processes. They can be differentiated from Hocosphaeridium scaberfacium by their cylindrical processes, and from H. dilatatum by their low process density and the lack of a process basal expansion in most specimens. In some processes, an obtusely conical or even slightly inflated base is observed (e.g., process on the right in Fig. 14.13). However, such structures only appear in deformed specimens, and thus are likely to be taphonomic in origin. Only specimens with well-defined process terminal ends are accepted as Hocosphaeridium. There are far more acanthomorphic specimens that resemble H. anozos in overall size and morphology but are taxonomically unidentifiable because the terminal ends of their processes are not captured in thin sections. Therefore, the reported abundance of H. anozos in this study is likely an underestimate.

Hocosphaeridium scaberfacium Zang in Zang and Walter, Reference Zang and Walter1992, emend. Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a
 Figure 15

Reference Zang and Walter1992

Hocosphaeridium scaberfacium Zang in Zang and Walter, p. 61, fig. 45A–F (not 45G).

Reference Yuan and Hofmann1998

Hocosphaeridium scaberfacium Zang and Walter; Yuan and Hofmann, p. 203, fig. 10A, B.

Reference Zhang, Yin, Xiao and Knoll1998

Goniosphaeridium conoideum (Kolosova) Zhang et al., p. 32, fig. 9.1–9.4.

Reference Yuan, Xiao, Yin, Knoll, Zhou and Mu2002

Goniosphaeridium conoideum (Kolosova) Zhang et al.; Yuan et al., p. 74, fig. 100.

Reference Grey2005

Tanarium conoideum Kolosova; emend. Moczydłowska et al.; Grey, p. 299, figs. 212, 213.

Reference Willman, Moczydłowska and Grey2006

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Willman et al., p. 32, pl. VI, figs. 1, 2.

Reference Willman and Moczydłowska2008

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Willman and Moczydłowska, p. 526, fig. 12C.

Reference Golubkova, Raevskaya and Kuznetsov2010

Tanarium conoideum (Kolosova) emend. Moczydłowska et al.; Golubkova et al., pl. III, fig. 7, pl. IV, fig. 2.

Reference Moczydłowska and Nagovitsin2012

Tanarium anozos Willman in Willman and Moczydłowska; Moczydłowska and Nagovitsin, p. 18, fig. 8A–C.

Reference Liu, Yin, Chen, Tang and Gao2012

Tanarium anozos Kolosova; Liu et al., fig. 3D–F.

Reference Liu, Yin, Chen, Tang and Gao2013

Tanarium conoideum; Liu et al., fig. 11A.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Hocosphaeridium scaberfacium Zang in Zang and Walter; Xiao et al., p. 27.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Hocosphaeridium scaberfacium Zang in Zang and Walter, emend. Liu et al., p. 78, figs. 39.3, 41, 42.

Reference Liu, Chen, Zhu, Li, Yin and Shang2014b

Hocosphaeridium scaberfacium; Liu et al., fig. 8C.

Reference Liu, Qi, Fan, Guo and Pei2021

Hocosphaeridium scaberfacium; Liu et al., fig. 6.3, 6.4.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Hocosphaeridium scaberfacium Zang in Zang and Walter; Shi et al., fig. 8L, M (one of the specimens described here).

Reference Ye, Li, Tong, An, Hu and Xiao2022

Hocosphaeridium scaberfacium Zang in Zang and Walter, Reference Zang and Walter1992, emend. Liu et al.; Ye et al., p. 41, fig. 26H–J.

Figure 15. Hocosphaeridium scaberfacium Zang in Zang and Walter, Reference Zang and Walter1992, emend. Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; red arrowheads denote hooked process terminations. (1–3) PB202032, thin section 19HP-1-28, Q33; circled 2 and 3 in (1) mark the same area magnified in (2) and (3), respectively, at different focal levels to show different processes. (4–6) PB202033, thin section 19TP-1-40, K44; circled 5 and 6 in (4) mark areas magnified in (5) and (6), respectively. (7, 8) PB202034, thin section 19CW-6-15, N40/4; circled 8 in (7) marks the area magnified in (8). (9) PB202035, thin section 19SDP-7-3, G41/1. (10–12) PB202036, thin section 21DC-2-20, P18; circled 11 and 12 in (10) mark areas magnified in (11) and (12), respectively.

Holotype

CPC 27765, thin section 87ZW01-8, reposited at Commonwealth Palaeontological Collection (CPC) at Geoscience Australia, Canberra, from the Ediacaran Pertatataka Formation of the Rodinga 4 drill core in Amadeus Basin, Northern Territory, Australia.

Description and measurements

Vesicles mostly medium-sized, compressed to different degrees but were originally spheroidal based on several less severely compressed specimens (Fig. 15.115.3, 15.415.7). Vesicles bear a varying number of conical and distally tapering processes with a relatively wide base and a hooked or recurved tip. Vesicle diameter 114–212 μm (N = 6, mean = 170 μm, SD = 38 μm); process length 36.3–58.3 μm (N = 9, mean = 45.2 μm, SD = 7.9 μm), 18.6–39.5% of vesicle diameter (N = 6, mean = 26.5%, SD = 8.4%); process basal width 6.8–22.8 μm (N = 9, mean = 12.9 μm, SD = 4.8 μm). As measured on one specimen (Fig. 15.115.3), there are about two processes per 100 μm of vesicle periphery.

Material

Five illustrated specimens (Fig. 15) and four additional specimens (including the one illustrated by Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 8L, M).

Remarks

Despite the modest preservation quality, the conical processes with a hooked termination and the lack of a basal expansion structure are clearly discernable in our specimens. These features allow the taxonomical identification to Hocosphaeridium scaberfacium. Although the distal part of processes is recurved for at least 180° and up to 270° (e.g., Fig. 15.2, 15.3), the basal part of the processes remains straight, indicating that the hooked structures are biological in origin. As in the case of H. anozos, there are some specimens in our collection that could be H. scaberfacium but are currently placed in the category of unidentified acanthomorphs because the distal part of the processes is not captured in the thin sections.

Genus Knollisphaeridium Willman and Moczydłowska, Reference Willman and Moczydłowska2008, emend. Liu and Moczydłowska, Reference Liu and Moczydłowska2019

Type species

Knollisphaeridium maximum (Yin, Reference Yin1987) Willman and Moczydłowska, Reference Willman and Moczydłowska2008, emend. Liu and Moczydłowska, Reference Liu and Moczydłowska2019.

Other species

Knollisphaeridium? bifurcatum Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; K. coniformum Liu and Moczydłowska, Reference Liu and Moczydłowska2019; K. denticulatum Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; K. gravestockii (Grey, Reference Grey2005) Willman and Moczydłowska, Reference Willman and Moczydłowska2008; K. longilatum Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; K. obtusum Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; K. parvum Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; K. triangulum (Zang in Zang and Walter, Reference Zang and Walter1992) Willman and Moczydłowska, Reference Willman and Moczydłowska2008, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Knollisphaeridium maximum (Yin, Reference Yin1987), Willman and Moczydłowska, Reference Willman and Moczydłowska2008, emend. Liu and Moczydłowska, Reference Liu and Moczydłowska2019
 Figure 16

Reference Yin1987

Baltisphaeridium maximum Yin, p. 439, pl. 14, figs. 14, 15.

Reference Knoll and Walter1992

Echinosphaeridium maximum (Yin) Knoll, p. 765, pl. 5, figs. 5, 6.

Reference Tiwari and Knoll1994

Echinosphaeridium maximum (Yin) Knoll; Tiwari and Knoll, p. 196, pl. I, fig. 3.

Reference Zhang, Yin, Xiao and Knoll1998

Echinosphaeridium maximum (Yin) Knoll; Zhang et al., p. 26, figs. 6.9, 6.10, 7.1, 7.2.

non Reference Zhang, Yin, Xiao and Knoll1998

Echinosphaeridium maximum (Yin) Knoll; Zhang et al., p. 26, fig. 6.7, 6.8.

non Reference Yuan and Hofmann1998

Echinosphaeridium maximum (Yin) Knoll; Yuan and Hofmann, p. 202, fig. 8A–D.

non Reference Yin1999

Echinosphaeridium maximum (Yin) Knoll; Yin, pl. 4, figs., 4, 5.

non Reference Xiao and Knoll1999

Echinosphaeridium maximum; Xiao and Knoll, fig. 11A–C.

non Reference Zhou, Brasier and Xue2001

Echinosphaeridium maximum; Zhou et al., pl. 3, figs. 1, 2.

Reference Zhou, Yuan, Xiao, Chen and Xue2004b

Echinosphaeridium maximum (Yin) Knoll; Zhou et al., p. 353, pl. IV, figs. 1–4.

Reference Willman and Moczydłowska2008

Knollisphaeridium maximum (Yin) Knoll; Willman and Moczydłowska, p. 523, fig. 5E, F.

Reference Liu, Yin, Gao, Tang and Chen2009

Echinosphaeridium maximum; Liu et al., fig. 2m, n.

Reference Yin, Liu, Chen, Tang, Gao and Wang2009a

Echinosphaeridium maximum (Yin) Knoll; Yin et al., pl. 1, fig. 5.

Reference Chen, Yin, Liu, Gao, Tang and Wang2010

Echinosphaeridium maximum; Chen et al., fig. 2.2, 2.3.

Reference Sergeev, Knoll and Vorob'eva2011

Knollisphaeridium maximum (Yin) Willman and Moczydłowska; Sergeev et al., p. 1004, fig. 7.5.

Reference Willman and Moczydłowska2011

Knollisphaeridium maximum (Yin, Reference Yin1987; Knoll, Reference Knoll1992) Willman, 2007 [sic]; C. Yin et al., figs. 5f, 6e.

Reference Liu, Yin, Chen, Tang and Gao2013

Knollisphaeridium maximum; Liu et al., fig. 11N, O.

Reference Zeng, Chen, Li, Zhou, Zhang and Peng2013

Knollisphaeridium sp.; Zeng et al., fig. 4.3, 4.4.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Knollisphaeridium maximum (Yin) Willman and Moczydłowska; Liu et al., p. 83, figs. 44.4, 46, 47.

Reference Liu, Chen, Zhu, Li, Yin and Shang2014b

Knollisphaeridium maximum; Liu et al., fig. 8D, E.

Reference Liu, Chen, Zhu, Li, Yin and Shang2014b

Knollisphaeridium sp.; Liu et al., fig. 8H.

non Reference Xiao, Zhou, Liu, Wang and Yuan2014

Knollisphaeridium maximum (Yin) Willman and Moczydłowska; Xiao et al., p. 30, fig. 19.

Reference Ouyang, Guan, Zhou and Xiao2017

Knollisphaeridium maximum; Ouyang et al., fig. 9A–H.

Reference Liu and Moczydłowska2019

Knollisphaeridium maximum (Yin) Willman and Moczydłowska, emend. Liu and Moczydłowska, p. 118, fig. 64.

non Reference Liu and Moczydłowska2019

Knollisphaeridium maximum (Yin) Willman and Moczydłowska, emend. Liu and Moczydłowska, fig. 65.

Reference Ouyang, Zhou, Xiao, Chen and Shao2019

Knollisphaeridium maximum; Ouyang et al., fig. 13A–D.

Reference Vorob'eva and Petrov2020

Knollisphaeridium maximum (Yin) emend. Willman and Moczydłowska; Vorob'eva and Petrov, p. 374, pl. II, figs. 19, 20.

non Reference Grazhdankin, Nagovitsin, Golubkova, Karlova, Kochnev, Rogov and Marusin2020

Knollisphaeridium maximum; Grazhdankin et al., fig. 3D.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Knollisphaeridium maximum (Yin) Willman and Moczydłowska; Ouyang et al., fig. 15K–N.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Knollisphaeridium maximum (Yin) Willman and Moczydłowska; Shi et al., fig. 9A–C (illustrated in Fig. 16.5, 16.7, 16.8, one of the specimens described here).

Reference Li, Zhang, Han, Zhong, Ding, Wu and Liu2022

Knollisphaeridium maximum (Yin) Willman and Moczydłowska, emend. Liu and Moczydłowska; Ye et al., p. 42, fig. 28D–G.

Reference Golubkova2023

Knollisphaeridium maximum (Yin) emend. Willman; Golubkova, pl. 7, fig. 7.

Figure 16. Knollisphaeridium maximum (Yin, Reference Yin1987) Willman and Moczydłowska, Reference Willman and Moczydłowska2008, emend. Liu and Moczydłowska, Reference Liu and Moczydłowska2019. (1–3) PB202037, thin section 14HA-140-1, S53/4; circled 2 and 3 in (1) mark areas magnified in (2) and (3), respectively. (4, 6) PB202038, thin section 14HA-140-3, E28/4; circled 6 in (4) marks the area magnified in (6). (5, 7, 8) PB202039, thin section 21DC-6-9, H34; circled 7 and 8 in (5) mark areas magnified in (7) and (8), respectively; scale bar in (7) also applies to (8); red and blue arrowheads in (7) denote undeformed and slightly deformed processes, respectively.

Holotype

Specimen illustrated in Yin (Reference Yin1987, pl. 14, figs. 14, 15), thin section #Hm80-8-6, reposited at NIGPAS, from the Ediacaran Doushantuo Formation at Shipai in the Yangtze Gorges area, Hubei Province, South China (also illustrated in Liu and Moczydłowska, Reference Liu and Moczydłowska2019, fig. 64A–C).

Description and measurements

Vesicle large, spheroidal (some deformed to various degrees), covered by evenly and closely distributed, basally separated processes. Processes homomorphic, conical, most taper gradually toward a pointed tip. In some specimens, processes with (blue arrowhead in Fig. 16.7) and without (red arrowhead in Fig. 16.7) a basal expansion can be found on the same vesicle. No outer membrane is observed. Vesicle diameter 193–448 μm (N = 9, mean = 332 μm, SD = 114 μm); process length 9.5–19.0 μm (N = 11, mean = 14.9 μm, SD = 2.9 μm), 2.9–8.5% of vesicle diameter (N = 8, mean = 5.0%, SD = 2.0%); process basal width 2.4–5.6 μm (N = 12, mean = 3.7 μm, SD = 1.1 μm); 15–27 processes per 100 μm of vesicle periphery (N = 11, mean = 20, SD = 4 μm).

Material

Three illustrated specimens (Fig. 16) and nine additional specimens (including the two illustrated in Ouyang et al., Reference Ouyang, Guan, Zhou and Xiao2017, fig. 9A–C, 9F–H).

Remarks

Knollisphaeridium maximum is one of the most widely distributed Ediacaran acanthomorphic taxa and is distinctive in its large vesicle size and proportionally small, densely distributed, echinate conical processes. As most previously reported specimens of this species, the current specimens lack a multilayered membrane, which is considered diagnostic of K. maximum as emended by Liu and Moczydłowska (Reference Liu and Moczydłowska2019), but they possess all other diagnostic features of this species. Some specimens described here have processes with a slightly broadened basal expansion (blue arrowhead in Fig. 16.7), resembling processes of K. coniformum or K. triangulum. However, most processes do not have a basal expansion (red arrowhead in Fig. 16.7), indicating the apparent basal expansions may be taphonomic artifacts (e.g., subtle deformation at the process base during degradation and compression in early diagenesis).

Sixty-one specimens identified as small-sized Knollisphaeridium maximum by Liu and Moczydłowska (Reference Liu and Moczydłowska2019, fig. 65, vesicle diameter 40–86 μm and process length 4.2–10.5% of vesicle diameter) are here excluded from this species, and likely belong to Appendisphaera heliaca. These specimens have small vesicles and proportionally long processes, features that contradict the diagnosis of Knollisphaeridium. According to the emended diagnosis of Liu and Moczydłowska, Reference Liu and Moczydłowska2019, this genus is characterized by its medium-sized to large vesicle. Instead, these specimens are similar to A. heliaca in almost all morphological features, including vesicle size (55 μm for holotype, 43–72 μm for other published specimens; Liu and Moczydłowska, Reference Liu and Moczydłowska2019; Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021), relative process length (14.5% of vesicle diameter for holotype, 5.7–21.1% for other published specimens; Liu and Moczydłowska, Reference Liu and Moczydłowska2019; Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021), and process density and distribution.

Genus Megasphaera Chen and Liu, Reference Chen and Liu1986, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Type species

Megasphaera inornata Chen and Liu, Reference Chen and Liu1986, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Other species

Megasphaera cymbala Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; M. ornata Xiao and Knoll, Reference Xiao and Knoll2000, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; M. patella Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; M. puncticulosa Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; M. minuscula Anderson et al., Reference Anderson, McMahon, Macdonald, Jones and Briggs2019 (although the validity of this species is questionable).

Remarks

Generally described together with acanthomorphs, Megasphaera is a special genus that contains both ornamented and unornamented species. To date, two unornamented species have been erected under the genus Megasphaera, including M. inornata and M. minuscula, with the former as the type species. Vesicle ornamentations are the key feature that distinguish acanthomorphs from sphaeromorphs (e.g., leiospheres). Therefore, the validity of M. inornata (thus also Megasphaera) is related with how it differs from leiospheres. Morphological and structural differences between M. inornata and leiospheres are threefold. Firstly, although leiospheres also contain large species, they are mostly small to medium-sized (Butterfield et al., Reference Butterfield, Knoll and Swett1994). On the contrary, Megasphaera was erected emphasizing its large size (Chen and Liu, Reference Chen and Liu1986), and a large vesicle is still the major diagnostic feature of this genus (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014, in which a large vesicle is defined as vesicle diameter > 200 μm). Secondly, M. inornata exhibits a cell division sequence as recorded by various numbers (one to more than 100) of uniformly shaped and tightly packed daughter cells within the vesicle, which were separately named Megaspheara, Parapandorina, and Megaclonophycus (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014). Leiospheres may also contain cells within the vesicle, but these cells are irregular in shape and size (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a), do not form a closely compacted spheroidal body, and do not form a cell division sequence as generally seen in Megasphaera specimens. Third and importantly, the smooth-walled M. inornata may represent a taphonomic or developmental variation of M. ornata, which does have a sculptured vesicle surrounding a smooth vesicle, therefore these two species may be biologically conspecific (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014). However, the above-mentioned features that distinguish M. inornata from leiospheres do not apply to M. minuscula, which has a relatively small vesicle (inconsistent with current diagnosis of Megasphaera) that contains internal bodies of various size and has no ornamented counterpart. Thus, it is uncertain whether M. minuscula should be accepted as a species of Megasphaera.

Megasphaera inornata Chen and Liu, Reference Chen and Liu1986, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014
 Figure 17.1

Reference Chen and Liu1986

Megasphaera inornata Chen and Liu, p. 51, pl. 1, fig. 4.

Reference Xue, Tang, Yu and Zhou1995

Parapandorina raphospissa Xue et al., p. 692, pl. I, figs. 1–3.

Reference Xue, Tang, Yu and Zhou1995

Parapandorina beidoushanensis Xue et al., p. 692, pl. II, figs. 1, 3–5.

Reference Xue, Tang, Yu and Zhou1995

Parapandorina beidoushanensis var. cylindrica Xue et al., p. 693, pl. II, fig. 2.

Reference Xue, Tang, Yu and Zhou1995

Megacolonophycus onustus Xue et al., p. 695, pl. III, figs. 3, 4, pl. IV, figs. 1–6, pl. V, figs. 2, 6–9.

Reference Xue, Tang, Yu and Zhou1995

Colossotetrahedrion ovimpositum Xue et al., p. 696, pl. V, figs. 3, 5.

Reference Xiao and Knoll2000

Megasphaera inornata Chen and Liu, Reference Chen and Liu1986, emend. Xiao and Knoll, p. 773, fig. 3.1, 3.2, 3.4, 3.5, 3.7, 3.11.

Reference Zhou, Chen and Xue2002

Megasphaera inornata Chen and Liu; Zhou et al., p. 182, pl. II, figs. 1, 2.

Reference Zhou, Yuan, Xiao, Chen and Xue2004b

Parapandorina raphospissa Xue et al.; Zhou et al., pl. VI, figs. 5–9.

Reference Zhou, Yuan, Xiao, Chen and Xue2004b

Megacolonophycus onustus Xue et al.; Zhou et al., pl. VI, fig. 10.

Reference Xie, Zhou, Mcfadden, Xiao and Yuan2008

Parapandorina raphospissa (Xue et al.) Xiao and Knoll; Xie et al., p. 285, pl. II, fig. 4.

Reference Xie, Zhou, Mcfadden, Xiao and Yuan2008

Megacolonophycus onustus Xue et al.; Xie et al., p. 284, pl. II, figs. 5, 6.

Reference Yin, Liu, Gao, Tang and Chen2009b

Megasphaera inornata Chen and Liu; Yin et al., fig. 3a, b.

Reference Yin, Liu, Gao, Tang and Chen2009b

Megacolonophycus onustus Xue et al.; Yin et al., fig. 4b–d.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Megasphaera inornata Chen and Liu, emend. Xiao et al., p. 35.

Reference Ye, Tong, An, Tian, Zhao and Zhu2015

Megasphaera inornata Chen and Liu, emend. Xiao et al.; Ye et al., p. 50, pl. II, figs. 1–13.

Reference Nie, Liu and Dong2017

Megasphaera inornata Chen and Liu, emend. Xiao et al.; Nie et al., p. 380, fig. 10.

Reference Ouyang, Zhou, Xiao, Chen and Shao2019

Megasphaera inornata; Ouyang et al., fig. 9L.

Reference Shang, Liu and Moczydłowska2019

Megasphaera inornata Chen and Liu, emend. Xiao et al.; Shang et al., p. 24, fig. 14A, B.

Reference Ouyang, Zhou and Liu2020

Megasphaera inornata; Ouyang et al., figs. 3A–J, 4.

Reference Shang, Liu and Liu2020

Megasphaera inornata Chen and Liu, emend. Xiao et al.; Shang and Liu, p. 158, fig. 5C.

Reference Yang, Pang, Chen, Zhong and Yang2020

Megasphaera inornata Chen and Liu, emend. Xiao et al.; Yang et al., p. 9, fig. 3.

Reference Shang and Liu2020

Acritarcha gen. et sp. indet.; Shang and Liu, p. 159, fig. 6D, E.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Megasphaera inornata Chen and Liu, emend. Xiao et al.; Ouyang et al., fig. 16A–D.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Megasphaera inornata Chen and Liu, emend. Xiao et al.; Ye et al., p. 47, fig. 49.

Figure 17. (1) Megasphaera inornata Chen and Liu, Reference Chen and Liu1986, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; PB202040, thin section 19SDP-1-13, K42/2. (2) Megasphaera ornata Xiao and Knoll, Reference Xiao and Knoll2000, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; PB202041, thin section 19SDP-1-22, P39/2; red arrowhead denotes the outer surface of the sculptured vesicle wall.

Neotype

The specimen illustrated by Xiao and Knoll (Reference Xiao and Knoll2000, fig. 3.1) was designated as a neotype (HUHPC-64837, SRA-1, photo 419) by Xiao et al. (Reference Xiao, Zhou, Liu, Wang and Yuan2014).

Description and measurements

A large, oval vesicle with a diameter of about 896 μm. No ornamentation is observed.

Material

One illustrated specimen (Fig. 17.1).

Remarks

With a relatively regular shape, the described specimen is likely an acritarch vesicle without ornamentation. Its large size and uniformly thick vesicle wall are comparable to those of Megasphaera inornata. No primary internal structures, such as internal bodies, are present, likely due to degradation and secondary mineral precipitation, as evinced by the abundance of botryoidal cements and spherules, which are interpreted as possible bacterial infection in degrading specimens (Xiao and Knoll, Reference Xiao and Knoll1999).

Megasphaera ornata Xiao and Knoll, Reference Xiao and Knoll2000, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014
Figure 17.2

Reference Yin and Xue1993

tubercle-spheroidal type with tortuous tumour; Yin and Xue, pl. I, figs. a, b.

Reference Yin and Xue1993

plate-spheroidal type with polygonal plates; Yin and Xue, pl. I, fig. e, pl. II, figs. g–l.

Reference Xiao and Knoll2000

Megasphaera ornata Xiao and Knoll, p. 773, figs. 3.12, 3.13, 4.11, 4.12, 5.1–5.4.

Reference Yin, Bengtson and Yue2003

Tianzhushania ornata (Xiao and Knoll) Yin et al., Reference Yin, Bengtson and Yue2004; Yin et al., pl. II, figs. 1–8.

Reference Yin, Gao and Yue2003

Unnamed specimens; Yin et al., pl. II, figs. 9–12.

Reference Yin, Bengtson and Yue2004

Tianzhushania ornata (Xiao and Knoll) Yin et al., figs. 4A, 5C, 6, 7A.

Reference Yin, Bengtson and Yue2004

Tianzhushania sp.; Yin et al., fig. 4B, C.

Reference Xiao, Hagadorn, Zhou and Yuan2007

Megasphaera ornata; Xiao et al., fig. 1A.

Reference Xie, Zhou, Mcfadden, Xiao and Yuan2008

Megasphaera ornata Xiao and Knoll; Xie et al., p. 284, pl. I, figs. 4, 5.

Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011

Tianzhushania ornata; C. Yin et al., fig. 4c, e.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Megasphaera ornata Xiao and Knoll, emend. Xiao et al., p. 35, fig. 22.

Reference Zhang and Zhang2017

Megasphaera ornata; Zhang and Zhang, figs. 3h–l, 4a–d.

Reference Ouyang, Zhou and Liu2020

Megasphaera ornata; Ouyang et al., fig. 3M–R.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Megasphaera ornata Xiao and Knoll, emend. Xiao et al.; Ouyang et al., fig. 15R, S.

Holotype

HUHPC-62990, reposited at the Harvard University Herbaria Paleobotanical Collection, from the Ediacaran Doushantuo Formation in the Weng'an area, Guizhou Province, South China (Xiao and Knoll, Reference Xiao and Knoll2000, fig. 5.4).

Description and measurements

A large, spheroidal body with a diameter of about 709 μm, surrounded by an outer layer with sculptures of various size.

Material

One illustrated specimen (Fig. 17.2).

Remarks

This specimen is assigned to Megasphaera ornata based on its large vesicle and an outer layer with sculptures that manifest as indentations in thin-section view (red arrowhead in Fig. 17.2). The light-colored zone between the outer sculpture layer and the internal spheroidal body represents secondary cement of micro-quartz. The uneven thickness of the light-colored zone may be caused by taphonomic deformation of the outer vesicle wall and displacement of the internal spheroidal body.

Genus Mengeosphaera Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014

Type species

Mengeosphaera chadianensis (Chen and Liu, Reference Chen and Liu1986) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Other species

Mengeosphaera angusta Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. bellula Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. constricta Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. eccentrica Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; M. flammelata Liu and Moczydłowska, Reference Liu and Moczydłowska2019; M. gracilis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. grandispina Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. latibasis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. lunula Liu and Moczydłowska, Reference Liu and Moczydłowska2019; M. mamma Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022; M. matryoshkaformis Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021; M. membranifera Shang, Liu, and Moczydłowska, Reference Liu and Moczydłowska2019; M. minima Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. reticulata (Xiao and Knoll, Reference Xiao and Knoll1999) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; M. spinula Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. stegosauriformis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; M. uniformis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a.

Mengeosphaera bellula Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a
 Figure 18.118.3

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Mengeosphaera bellula Liu et al., p. 90, figs. 51.2, 52, 53.

Figure 18. (1–3) Mengeosphaera bellula Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, PB202042, thin section 19CW-6-12, K33; circled 2 and 3 in (1) mark areas magnified in (2) and (3), respectively. (4–8) Mengeosphaera constricta Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, PB202043, thin section 14HA-115-2, W43/2; circled 5 in (4) marks the same area magnified in (5) and (6) at different focal levels; circled 7 and 8 in (4) mark areas magnified in (7) and (8), respectively. (9–14) Mengeosphaera gracilis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a. (9, 10, 12) PB202044, thin section 19TP-1-12, H43/1; circled 10 and 12 in (9) mark areas magnified in (10) and (12), respectively; (11, 13, 14) PB202045, thin section 19CW-6-15, G36; circled 13 and 14 in (11) mark areas magnified in (13) and (14), respectively. Scale bar in (8) represents 5 μm and applies to (5–7); scale bar in (14) applies to (13).

Holotype

IGCAGS-NPIII-266, reposited at Institute of Geology, Chinese Academy of Geological Sciences, from Member III of the Ediacaran Doushantuo Formation at Niuping section in the Yangtze Gorges area, Hubei Province, South China (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 52.1–52.3).

Description and measurements

Vesicle small, originally spheroidal, with homomorphic biform processes closely distributed on the vesicle. The process is composed of a basal expansion that tapers rapidly toward a long and thin apical spine. Specimen illustrated (Fig. 18.118.3): vesicle diameter about 73 μm, process length about 17.1 μm (23.5% of vesicle diameter) and basal width about 5.6 μm, with about 21 processes per 100 μm of vesicle periphery; length (height) of basal part (from vesicle wall to the point where the process begins to taper significantly) about 2.8 μm (16.4% of process total length), apical spine width (diameter) about 0.9 μm. The other available specimen: vesicle diameter not measured due to compression, process length about 17.7 μm and basal width about 5.4 μm, about 25 processes per 100 μm of vesicle periphery; length of basal part about 4.8 μm (27.1% of process total length), apical spine width about 1.1 μm.

Material

One illustrated specimen (Fig. 18.118.3) and one additional specimen.

Remarks

The two described specimens have densely arranged biform processes with a basal expansion and a relatively long, thin apical spine. These features, as well as their measurements, are similar to those in Mengeosphaera bellula (holotype 75 μm in vesicle diameter, 16 μm in process length or 21% of vesicle diameter, and 5 μm in process basal width). The two available specimens can alternatively be compared to M. chadianensis, but M. chadianensis commonly has larger vesicles (500–800 μm in diameter for the holotype), and thus the processes of M. chadianensis are proportionally shorter and smaller. In addition, the apical spine of M. chadianensis typically takes a smaller percentage of the overall process length than in M. bellula. Thus, the two specimens described here are more appropriately identified as M. bellula.

Two specimens from the Doushantuo Formation in the Shennongjia area that are identified as Mengeosphaera chadianensis in Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022, figs. 32A–C, 33A, B) have homomorphic and biform processes resembling those in M. bellula, with the lower part of the basal expansion more or less cylindrical, supporting a long and distally tapering apical spine. Process morphology, proportional process length, and relatively long apical spine of the two Shennongjia specimens are more similar to previously reported M. bellula than to M. chadianensis. However, the two Shennongjia specimens (vesicle diameter about 142 μm for fig. 32A and about 138 μm for fig. 33A in Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022) are both much larger than M. bellula specimens from the type locality in the Yangtze Gorges area (50–90 μm in vesicle diameter). Thus, these two specimens are questionably retained as M. chadianensis.

Mengeosphaera constricta Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a
Figure 18.418.8

Reference Liu, Yin, Chen, Tang and Gao2013

Unnamed F; Liu et al., fig. 12E, F.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Mengeosphaera constricta Liu et al., p. 95, figs. 51.4, 56–58.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Mengeosphaera spicata Liu et al., p. 101, figs. 51.10, 64.

Reference Ouyang, Guan, Zhou and Xiao2017

Mengeosphaera spicata?; Ouyang et al., fig. 8O, P (the specimen described here and illustrated in Fig. 18.418.8).

Reference Ye, Li, Tong, An, Hu and Xiao2022

Mengeosphaera constricta Liu et al.; Ye et al., p. 53, fig. 34A–C.

Holotype

IGCAGS–WFG–826, reposited at Institute of Geology, Chinese Academy of Geological Sciences, from lower Member III of the Ediacaran Doushantuo Formation at Wangfenggang section in the Yangtze Gorges area, Hubei Province, South China (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 56.1, 56.2).

Description and measurements

Vesicle spheroidal, with uniform processes closely arranged on vesicle surface, although only three processes completely preserved. Processes consist of an overall inflated, near-cylindrical basal part and a conical terminal part. The inflated basal expansion is constricted at the contact with the vesicle wall (Fig. 18.518.8), and the terminal part tapers gradually to a pointed tip, thus forming an onion-like process. The processes are separated from each other at their base, but are in contact at the inflated basal expansion. Vesicle diameter about 110 μm; process length about 15.6 μm (14.2% of vesicle diameter), maximum width of basal expansion about 9.7 μm, and width of constricted base about 6.9 μm; length of basal expansion (from process base to the point where the process begins to taper significantly) about 11.1 μm (71.2% of process total length).

Material

One illustrated specimen (Fig. 18.418.8).

Remarks

This specimen was previously published in Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017) as Mengeosphaera spicata. Although Liu and Moczydłowska (Reference Liu and Moczydłowska2019) synonymized M. spicata and M. constricta, they did not provide any explanation. We follow Xiao et al. (Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022) to tentatively accept this synonymy, and thus reassign this specimen to M. constricta. Due to the poor preservation, only three processes (magnified in Fig. 18.518.8) are completely preserved with a discernable basal constriction. The consistent morphology of these three processes, however, indicates that the basal constriction is not a taphonomic artifact.

Mengeosphaera gracilis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a
Figure 18.918.14

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Mengeosphaera? gracilis Liu et al., p. 96, fig. 60.

Reference Liu and Moczydłowska2019

Mengeosphaera gracilis Liu et al.; Liu and Moczydłowska, p. 132, fig. 71.

Reference Shang, Liu and Moczydłowska2019

Mengeosphaera gracilis Liu et al.; Shang et al., p. 25, fig. 14F–G.

Reference Shang, Liu and Liu2020

Mengeosphaera gracilis Liu et al.; Shang and Liu, p. 158, fig. 6F–L.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Mengeosphaera gracilis Liu et al.; Ouyang et al., fig. 16K–M.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Mengeosphaera gracilis Liu et al.; Ye et al., p. 56, fig. 34D–F.

Holotype

IGCAGS-WFG-727, reposited at Institute of Geology, Chinese Academy of Geological Sciences, from lower Member III of the Ediacaran Doushantuo Formation at Wangfenggang section in the Yangtze Gorges area, Hubei Province, South China (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 60.1, 60.2).

Description and measurements

Vesicle large and spheroidal, bearing densely distributed, basally connected biform processes. Processes uniform, with a conical basal expansion and a thin cylindrical apical spine. First specimen (Fig. 18.9, 18.10, 18.12): vesicle diameter about 226 μm; process length about 17.4 μm (7.7% of vesicle diameter), basal width about 6.4 μm, basal expansion length about 4.8 μm (27.6% of process total length); about 14 processes per 100 μm of vesicle periphery. Second specimen (Fig. 18.11, 18.13, 18.14): vesicle diameter about 250 μm; process length about 30.4 μm (12.2% of vesicle diameter), basal width about 8.5 μm, basal expansion length about 6.9 μm (22.7% of process total length); about seven processes per 100 μm of vesicle periphery.

Material

Two illustrated specimens (Fig. 18.918.14).

Remarks

Mengeosphaera gracilis can be differentiated from Cavaspina basiconica by its clearly defined biform processes with a more prominent and wider basal expansion. The two available specimens have processes with a conical basal expansion, unlike the deflated base of processes in C. basiconica. These two specimens also differ from Appendisphaera hemisphaerica in their relatively shorter and thicker process apical spine (process length ~14.3% of vesicle diameter in holotype of A. hemisphaerica), and especially the smaller process density (~21 processes per 100 μm of vesicle periphery in the holotype of A. hemisphaerica).

Mengeosphaera latibasis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, emend. Liu and Moczydłowska, Reference Liu and Moczydłowska2019
 Figure 19.1, 19.2

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Mengeosphaera latibasis Liu et al., p. 97, figs. 51.7, 62.

?Reference Nie, Liu and Dong2017

Mengeosphaera latibasis Liu et al.; Nie et al., p. 376, fig. 6.3–6.7.

Reference Ouyang, Guan, Zhou and Xiao2017

Mengeosphaera latibasis?; Ouyang et al., fig. 8K–N (the specimen described here and illustrated in Fig. 19.1, 19.2).

Reference Liu and Moczydłowska2019

Mengeosphaera latibasis Liu et al., emend. Liu and Moczydłowska, p. 133, fig. 72.

Reference Liu, Qi, Fan, Guo and Pei2021

Mengeosphaera latibasis Liu et al., emend. Liu and Moczydłowska; Ouyang et al., fig. 17A, B.

Figure 19. (1, 2) Mengeosphaera latibasis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, emend. Liu and Moczydłowska, Reference Liu and Moczydłowska2019, PB202046, thin section 14HA-115-1, T49/4; circled 2 in (1) marks the area magnified in (2). (3) Mengeosphaera minima Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, PB202047, thin section 21DC-5-4, T31/2. (4) Mengeosphaera minima? PB202048, thin section 21DC-3-1, G23/3. (5–11) Mengeosphaera mamma Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022. (5–7) PB202049, thin section 21LHK-1-10, L38/1; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively; (8, 10) PB202050, thin section 21MJD-1-10, L45; circled 10 in (8) marks the area magnified in (10); (9, 11) PB202051, thin section 21MJD-1-11, L33; circled 11 in (9) marks the area magnified in (11). Red arrowheads in (2), (57), (10), and (11) denote reflection points of biform processes; red arrowheads in (4) denote the basally joined, strongly inflated processes.

Holotype

IGCAGS–NPIII–540, reposited at Institute of Geology, Chinese Academy of Geological Sciences, from the upper Member III of the Ediacaran Doushantuo Formation at Niuping section in the Yangtze Gorges area, Hubei Province, South China (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 62.1, 62.2).

Description and measurements

Vesicle large, originally spheroidal but slightly deformed. Processes densely arranged on vesicle surface, basally connected or separated. Processes biform, with a broad, obtusely conical, and slightly inflated basal expansion, and a relatively thick but flexible apical spine that is more or less cylindrical in shape. Vesicle diameter about 465 μm; process length about 52.2 μm (11.2% of vesicle diameter), basal width about 31.2 μm, basal expansion length about 16.6 μm (31.8% of process total length), apical spine width about 4.9 μm; about three processes per 100 μm of vesicle periphery.

Material

One illustrated specimen (Fig. 19.1, 19.2).

Remarks

Mengeosphaera latibasis is distinct in its inflated basal expansion that is wider than long. In many Mengeosphaera specimens, processes with a slightly obtuse basal expansion are common (as in the two specimens of M. gracilis described above), but basal expansions that are twice as wide as they are long are characteristic of M. latibasis.

Mengeosphaera mamma Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022
Figure 19.519.11

Reference Yin1996

Unnamed form A; Yin, pl. I, figs. 4–6.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Mengeosphaera sp. 2; Ouyang et al., fig. 17H, L.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Mengeosphaera mamma Ye et al., p. 57, figs. 35, 36.

Holotype

The specimen illustrated in Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022, fig. 35A–C), thin section LHGd3 + 30 cm-1–17 (36.3×76.1), reposited at China University of Geosciences (CUG), Wuhan, China, from the Ediacaran Doushantuo Formation at Lianhuacun section in Shennongjia area, Hubei Province, South China.

Description and measurements

Most specimens are not entirely captured in thin section due to their large size. Vesicles range from oval to completely compressed, but were originally spheroidal. Processes large, biform, with the apical spine in most specimens poorly preserved and their full length unavailable. Four specimens with adequately preserved vesicles reveal a vesicle diameter of 350–632 μm, with the largest illustrated in Figure 19.8. Process basal width 37.7–77.0 μm (N = 9, mean = 50.5 μm, SD = 11.3 μm), basal expansion length 30.0–69.0 μm (N = 5, mean = 40.0 μm, SD = 16.3 μm), apical spine width 6.8–18.6 μm (N = 2); 1–2 processes per 100 μm of vesicle periphery. In some better-preserved processes (e.g., Fig. 19.10, 19.11), the basal expansion is as long as or longer than it is wide, and it is possible that the measurements of basal expansion length given above may be underestimates when the basal expansions are cut obliquely (in which case the apical spines are often missed in the thin section).

Material

Three illustrated specimens (Fig. 19.519.11) and six additional specimens (including the one illustrated in Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 8E, F).

Remarks

Of all Mengeosphaera species, M. flammelata, M. grandispina, M. mamma, and M. stegosauriformis have processes tens of micrometers in basal width. Among these four species, processes are flame-shaped in M. flammelata, have a conical and somewhat deflated basal expansion in M. grandispina, have a strongly inflated basal expansion in M. stegosauriformis. The nine specimens described here are most similar to M. mamma in both process size and shape.

The specimen published as “unnamed form A” from the Doushantuo Formation at the Diaoyapo section in the Yangtze Gorges area (Yin, Reference Yin1996) has processes with large, significantly inflated basal expansions (35–55 μm in basal length, ~40 μm in basal width), and cylindrical apical spine. These features fall within the perimeter of Mengeosphaera mamma, and this specimen is here reassigned to M. mamma.

Mengeosphaera minima Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a
Figure 19.3

Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011

Meghystrichosphaeridium chadianensis; L. Yin et al., fig. 5A, H.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Mengeosphaera minima Liu et al., p. 101, figs. 51.8, 63.

Reference Hawkins, Xiao, Jiang, Wang and Shi2017

Mengeosphaera minima; Hawkins et al., fig. 7C.

non Reference Grazhdankin, Nagovitsin, Golubkova, Karlova, Kochnev, Rogov and Marusin2020

Mengeosphaera minima; Grazhdankin et al., fig. 4A.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Mengeosphaera minima Liu et al.; Ouyang et al., fig. 17M, N.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Mengeosphaera minima Liu et al.; Ye et al., p. 57, fig. 34G, H.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Mengeosphaera minima Liu et al.; Shi et al., fig. 8C (illustrated in Fig. 19.3, one of the two specimens described here).

Holotype

IGCAGS–NPIII–090A, reposited at Institute of Geology, Chinese Academy of Geological Sciences, from the upper Member III of the Ediacaran Doushantuo Formation at Niuping section in the Yangtze Gorges area, Hubei Province, South China (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 63.1).

Description and measurements

Vesicle small, spheroidal, with uniform processes evenly distributed on the vesicle. Processes closely arranged but basally separated. Processes biform, with a conical basal expansion and a thin, cylindrical or distally tapering apical spine. The specimen illustrated in Figure 19.3 has a vesicle diameter of about 54 μm, process length about 7.0 μm (13.0% of vesicle diameter), basal expansion width about 4.1 μm, basal expansion length about 3.0 μm (42.9% of process total length), with about 14 processes per 100 μm of vesicle periphery. The other specimen has a vesicle diameter of about 92 μm, process length about 20.3 μm (22.0% of vesicle diameter), basal expansion width about 4.2 μm, basal expansion length about 4.6 μm (22.7% of process total length); process density unavailable due to poor preservation.

Material

One illustrated specimen (Fig. 19.3) and one additional specimen.

Remarks

Most Mengeosphaera species have large or at least medium-sized vesicles. To date, M. bellula, M. minima, and M. stegosauriformis are the only three Mengeosphaera species that have small vesicles, with M. minima being the smallest of all. The two available specimens are assigned to M. minima for their small size with biform processes that consist of a generally conical and proportionally large (at least 20% of process total length) basal expansion.

Mengeosphaera minima?
Figure 19.4

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Mengeosphaera minima?; Shi et al., fig. 8D (the same specimen described here and illustrated in Fig. 19.4).

Description and measurements

Vesicle small, spheroidal, bearing basally connected uniform processes. Processes biform, with clearly inflated basal expansions that take up about half of the total length of processes. Vesicle diameter about 48 μm, process length about 5.8 μm (12.1% of vesicle diameter) and basal width about 3.1 μm, length of basal expansion about 3.0 μm (51.7% of process total length), with about 32 processes per 100 μm of vesicle periphery.

Material

One illustrated specimen (Fig. 19.4).

Remarks

Resembling Mengeosphaera minima in the small vesicle size and the biform processes, this specimen is distinct in its basally connected and strongly inflated processes (red arrowheads in Fig. 19.4). Since these features appear consistently on all processes of this specimen, they are unlikely to be taphonomic artifacts, and probably represent morphological variations of taxonomic importance. Since there is only one such specimen in our collection, it is uncertain whether these variations are intraspecific or interspecific in nature. As such, we tentatively assign this specimen in an open nomenclature but note its similarity to M. minima.

Genus Tanarium Kolosova, Reference Kolosova1991, emend. Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993

Type species

Tanarium conoideum Kolosova, Reference Kolosova1991, emend. Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993.

Other species

Tanarium acus Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; T. araithekum Grey, Reference Grey2005; T. capitatum Liu and Moczydłowska, Reference Liu and Moczydłowska2019; T. columnatum Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022; T. cuspidatum (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) Liu and Moczydłowska, Reference Liu and Moczydłowska2019; T. digitiforme (Nagovitsin and Faizullin in Nagovitsin et al., Reference Nagovitsin, Faizullin and Yakshin2004) Sergeev, Knoll, and Vorob'eva, Reference Sergeev, Knoll and Vorob'eva2011; T. elegans Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; T. gracilentum (Yin in Yin and Liu, Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988) Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021; T. irregulare Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993; T. longidigitatum Golubkova, Reference Golubkova2023; T. mattoides Grey, Reference Grey2005; T. megaconicum Grey, Reference Grey2005; T.? minimum Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; T.? muntense Grey, Reference Grey2005; T. obesum Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; T. paucispinosum Grey, Reference Grey2005; T. pilosiusculum Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009; T. pluriprotensum Grey, Reference Grey2005; T. pycnacanthum Grey, Reference Grey2005; T. triangulare (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) Liu and Moczydłowska, Reference Liu and Moczydłowska2019; T. tuberosum Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993; T. uniformum Liu and Moczydłowska, Reference Liu and Moczydłowska2019; T. varium Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; T. victor Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Remarks

Like Appendisphaera, Tanarium encompasses a remarkably large range of morphological variations. The currently accepted species of Tanarium contain taxa with homomorphic (e.g., T.? muntense) or heteromorphic (T. irregulare) processes, with slim (e.g., T. gracilentum) to obtusely conical (e.g., T. tuberosum) processes, with cylindrical (e.g., T. digitiforme) to biform (e.g., T. triangulare) processes, with terminally pointed (e.g., T. acus) to bifurcated (e.g., T. victor) processes, with sparsely arranged (e.g., T. megaconicum) to densely arranged (e.g., T. pycnacanthum) processes, and with relatively short (process length <10% of vesicle diameter, e.g., T. pilosiusculum) to remarkably long (process length >50% of vesicle diameter, e.g., T. mattoides) processes. These morphological variations make it nearly impossible to define the genus Tanarium, and a taxonomical revision, preferably based on morphometric analyses, is urgently needed.

Tanarium cf. T. capitatum Liu and Moczydłowska, Reference Liu and Moczydłowska2019
 Figure 20.1, 20.2

cf. Reference Liu and Moczydłowska2019

Tanarium capitatum Liu and Moczydłowska, p. 143, fig. 79.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Tanarium cf. T. capitatum; Shi et al., fig. 8N, O (the specimen described here and illustrated in Fig. 20.1, 20.2).

Figure 20. (1, 2) Tanarium cf. T. capitatum Liu and Moczydłowska, Reference Liu and Moczydłowska2019, PB202052, thin section 21DC-2-35, M32/1, showing the same area at different focal levels. (3, 5) Tanarium conoideum Kolosova, Reference Kolosova1991, emend. Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, PB202053, thin section 21DC-5-4, R43/3, showing the same area at different focal levels. (4, 6, 7) Tanarium paucispinosum Grey, Reference Grey2005: (4) PB202054, thin section 19CW-6-9, N35/3; (6, 7) PB202055, thin section 19CW-5-29, H38, showing the same area at different focal levels.

Description and measurements

Vesicle large, compressed but originally spheroidal. Processes evenly distributed with moderate density, basally departed. Processes conical, with a wide base and tapering gradually toward a thin terminal end. Vesicle diameter approximately 348 μm. The full length of processes is difficult to obtain due to the relatively large size of the processes (so the terminal part is often not captured in thin sections), with one measurement of about 62.6 μm (18.0% of vesicle diameter) and two partially preserved processes 42.5 μm and 49.6 μm in length. Process basal width about 16.3 μm, process basal spacing about 13.2 μm, and about 3 processes per 100 μm of vesicle periphery.

Material

One specimen illustrated in Figure 20.1, 20.2.

Remarks

The described specimen is morphologically similar to Tanarium capitatum in vesicle size, process shape and proportional size, and process density and distribution. However, it lacks the key diagnostic feature of T. capitatum—the knob-like, bulge process tip. It is possible that the process tips are not preserved due to taphonomic loss, and this specimen is otherwise more similar to T. capitatum than to other species. The processes in this specimen are also similar to those of T. pilosiusculum in proportional length, but they are thinner and more acutely conical than processes in T. pilosiusculum (Vorob'eva et al., Reference Vorob'eva, Sergeev and Knoll2009). Therefore, we compare this specimen to T. capitatum but tentatively place it in an open nomenclature.

Tanarium conoideum Kolosova, Reference Kolosova1991, emend. Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993
Figure 20.3, 20.5

Reference Kolosova1991

Tanarium conoideum Kolosova, p. 57, fig. 5.1–5.3.

Reference Moczydłowska, Vidal and Rudavskaya1993

Tanarium conoideum Kolosova, emend. Moczydłowska, Vidal, and Rudavskaya, p. 514, 516, text-fig. 10C–D.

Reference Moczydłowska2005

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Moczydłowska, p. 302, fig. 7A, C, E.

non Reference Grey2005

Tanarium conoideum Kolosova; emend. Moczydłowska et al.; Grey, p. 299, figs. 212, 213.

non Reference Willman, Moczydłowska and Grey2006

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Willman et al., p. 32, pl. VI, figs. 1, 2.

non Reference Willman and Moczydłowska2008

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Willman and Moczydłowska, p. 526, fig. 12C.

non Reference Vorob'eva, Sergeev and Chumakov2008

Tanarium conoideum Kolosova; Vorob'eva et al., fig. 2a.

non Reference Vorob'eva, Sergeev and Knoll2009

Tanarium conoideum Kolosova, Moczydłowska et al.; Vorob'eva et al., p. 180, fig. 7.4, 7.7.

non Reference Yin, Liu, Chen, Tang, Gao and Wang2009a

Tanarium conoideum (Kolosova, Reference Kolosova1991) Moczydłowska et al. [sic]; Yin et al., pl. I, figs. 3, 4.

non Reference Golubkova, Raevskaya and Kuznetsov2010

Tanarium conoideum (Kolosova) emend. Moczydłowska et al. [sic]; Golubkova et al., pl. III, fig. 7, pl. IV, fig. 2.

Reference Sergeev, Knoll and Vorob'eva2011

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Sergeev et al., p. 1005, fig. 6.1, 6.2.

non Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011

Tanarium conoideum (Kolosova, Reference Kolosova1991) Moczydłowska et al. [sic]; C. Yin et al., fig. 6c (the same specimen as pl. I, figs. 3, 4 in Yin et al., Reference Yin, Liu, Chen, Tang, Gao and Wang2009a).

non Reference Liu, Yin, Chen, Tang and Gao2013

Tanarium conoideum; Liu et al., fig. 11A.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Xiao et al., p. 51, fig. 33.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Liu et al., p. 109, figs. 76.2, 77.

Reference Shang, Liu and Moczydłowska2019

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Shang et al., p. 26, fig. 16A–E.

Reference Vorob'eva and Petrov2020

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Vorob'eva and Petrov, p. 374, pl. I, fig. 15.

non Reference Yang, Pang, Chen, Zhong and Yang2020

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Yang et al., p. 6, fig. 2K.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Tanarium conoideum; Shi et al., fig. 9D, E (the specimen described here and illustrated in Fig. 21.3, 21.5).

Reference Ye, Li, Tong, An, Hu and Xiao2022

Tanarium conoideum Kolosova, emend. Moczydłowska et al.; Ye et al., p. 65, figs. 42, 43A–E.

Reference Golubkova2023

Tanarium conoideum (Kolosova) emend. Moczydłowska [sic]; Golubkova, pl. 7, fig. 6.

Figure 21. Tanarium pilosiusculum Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009. (1–4) PB202056, thin section 19CW-6-15, O41; circled 2–4 in (1) mark areas magnified in (2–4), respectively; (5–7) PB202057, thin section 21LHK-1-10, M31/2; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively.

Holotype

YIGS Nr 87-115, reposited at the Geological Museum of Yakutian Institute of Geologic Sciences (present Diamond and Precious Metal Geology Institute, Siberian Branch, Russian Academy of Sciences), from the Ediacaran Kursov Formation, Anabar area, eastern Siberia (Kolosova, Reference Kolosova1991, p. 57, fig. 5.1, 5.2).

Description and measurements

Vesicle spheroidal, medium-sized, bearing evenly distributed processes. Processes uniform, conical, distally tapering toward a pointed tip. Vesicle diameter about 108 μm; process length about 24.9 μm (23.1% of vesicle diameter), basal width about 8.8 μm, about seven processes per 100 μm of vesicle periphery.

Material

One specimen illustrated in Figure 20.3, 20.5.

Remarks

Previously published specimens of Tanarium conoideum represent a large range of morphological variations. The specimen described here is comparable to the holotype of T. conoideum in many morphological aspects, including the vesicle size, proportional size of processes, and process shape (for comparison, the holotype of T. conoideum has a vesicle diameter of ~114 μm, process length ~34.3 μm, and process basal width ~16.2 μm, as remeasured on fig. 5.1–5.3 of Kolosova, Reference Kolosova1991). The specimen described here differs from the holotype and many other published T. conoideum specimens in its greater process density; the holotype of T. conoideum has only about 1–2 processes per 100 μm of vesicle periphery, although it should be noted that the holotype has a relatively larger vesicle. However, process density is somewhat variable among previously published specimens of T. conoideum (e.g., ~4 processes per 100 μm of vesicle periphery in both Moczydłowska, Reference Moczydłowska2005, fig. 7C and in Golubkova, Reference Golubkova2023, pl. 7, fig. 6, and about 7 processes per 100 μm of vesicle periphery in Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014, fig. 33.3). Thus, we chose to place the specimen illustrated in Figure 20.3 and 20.5 in T. conoideum.

Tanarium paucispinosum Grey, Reference Grey2005
Figure 20.4, 20.6, 20.7

Reference Grey2005

Tanarium paucispinosum Grey, p. 318, figs. 45G, 208G, 237, 239.

Reference Golubkova, Raevskaya and Kuznetsov2010

Tanarium paucispinosum Grey; Golubkova et al., pl. II, fig. 1, pl. III, fig. 8.

Reference Liu and Moczydłowska2019

Tanarium paucispinosum Grey; Liu and Moczydłowska, p. 149, 151, fig. 83.

Reference Liu, Qi, Fan, Guo and Pei2021

Tanarium paucispinosum; Liu et al., fig. 4.7.

Reference Ye, Li, Tong, An, Hu and Xiao2022

Tanarium paucispinosum Grey; Ye et al., p. 66, fig. 44E–F.

Holotype

CPC 36552, reposited at Commonwealth Palaeontological Collection (CPC) at Geoscience Australia, Canberra, from the Ediacaran Wilari Dolomite Member of Observatory Hill I drill core in Officer Basin, South Australia (Grey, Reference Grey2005, fig. 237D).

Description and measurements

Vesicle medium-sized to large, originally spheroidal but may be deformed to different degrees. A small number of conical processes unevenly distributed on the vesicle wall. Vesicle diameter 149–201 μm (N = 5, mean = 170 μm, SD = 19 μm); processes length 38.1–83.8 μm (N = 7, mean = 62.2 μm, SD = 15.4 μm) and 23.7–36.2% of vesicle diameter (N = 4, mean = 32.8%, SD = 6.1%); process basal width 9.7–16.2 μm (N = 9, mean = 12.1 μm, SD = 2.0 μm); on average one process per 100 μm of vesicle periphery (measured on one specimen illustrated in Figure 20.6, 20.7).

Material

Two illustrated specimens (Fig. 20.4, 20.6, 20.7) and seven additional specimens.

Remarks

The described specimens are placed in Tanarium paucispinosum mainly for their sparsity of processes, which is the key diagnosis of T. paucispinosum. These two specimens also resemble specimens of T. paucispinosum reported from Australia in proportional length of the processes (~20–40% of vesicle diameter, calculated based on dimensions provided in Grey, Reference Grey2005) and the thin conical shape of the processes, although the vesicle size of the current specimens is greater than the Australian specimens (64–148 μm in vesicle diameter).

Tanarium pilosiusculum Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009
Figure 21

Reference Vorob'eva, Sergeev and Semikhatov2006

Echinosphaeridium sp.; Vorob'eva et al., fig. 2l.

Reference Vorob'eva, Sergeev and Knoll2009

Tanarium pilosiusculum Vorob'eva, Sergeev, and Knoll, p. 182, fig. 7.1, 7.2.

Reference Liu, Yin, Chen, Tang and Gao2013

Tanarium pilosiusculum; Liu et al., fig. 13B.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Tanarium pilosiusculum Vorob'eva et al.; Liu et al., p. 113, figs. 76.7, 83.

Reference Liu and Moczydłowska2019

Tanarium pilosiusculum Vorob'eva et al.; Liu and Moczydłowska, p. 151, fig. 84.

Reference Shang, Liu and Moczydłowska2019

Tanarium pilosiusculum Vorob'eva et al.; Shang et al., p. 27, fig. 17A–C.

Reference Yang, Pang, Chen, Zhong and Yang2020

Tanarium pilosiusculum Vorob'eva et al.; Yang et al., p. 7, fig. 2N, O.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Tanarium pilosiusculum Vorob'eva et al.; Ouyang et al., fig. 19K–M.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

?Tanarium pilosiusculum Vorob'eva et al.; Shi et al., fig. 9F, G (one of the specimens described here).

Holotype

Specimen 14700-74 (illustrated in Vorob'eva et al., Reference Vorob'eva, Sergeev and Knoll2009, fig. 7.1), reposited at the Paleontological Collection of the Geological Institute of the Russian Academy of Sciences, from the upper part of the early Ediacaran Vychegda Formation of the Kel'tminskaya-1 borehole in the East European Platform, Russia.

Description and measurements

Vesicle spheroidal, bearing a moderate number of relatively short processes randomly distributed on the vesicle. Processes conical and simple in shape, taper gradually toward a pointed tip. The specimen illustrated in Figure 21.1–21.4 has a vesicle diameter of about 201 μm, process length about 26.9 μm (13.4% of vesicle diameter), and basal width about 12.0 μm, with about 2–3 processes per 100 μm of vesicle periphery. The specimen illustrated in Figure 21.521.7 has a vesicle diameter of about 257 μm, process length about 49.7 μm (19.4% of vesicle diameter), and basal width about 21.5 μm, with 1–2 processes per 100 μm of vesicle periphery. The third specimen (illustrated in Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 9F, G) has a vesicle diameter of about 84 μm, process length about 11.0 μm (12.9% of vesicle diameter), and basal width about 12.3 μm, with about 7 processes per 100 μm of vesicle periphery.

Material

Two specimens illustrated in Figure 21, and one additional specimen illustrated in Shi et al. (Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 9F, G).

Remarks

Tanarium pilosiusculum is characterized by processes proportionally shorter (~5–10% of vesicle diameter) than those of other Tanarium species (typically >20% of vesicle diameter, as proposed by Grey, Reference Grey2005). Compared with the holotype of T. pilosiusculum, specimens described in this paper have proportionally longer processes that exceed 10% and can be up to 20% of vesicle diameter. However, they are otherwise comparable to T. pilosiusculum in process density and distribution; both have numerous conical and basally separated processes that are occasionally wider than long. They also meet the diagnosis of T. pilosiusculum in having processes “generally shorter than those of other Tanarium species,” (Vorob'eva et al., Reference Vorob'eva, Sergeev and Knoll2009, p. 182) considering that most other Tanarium species are characterized by longer processes that are greater than 20% of vesicle diameter. We note that other acanthomorph taxa, including several species of Appendisphaera, Urasphaera fungiformis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, and Variomargosphaeridium floridum Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012, also have processes that are 10–20% of vesicle diameter, but their processes can be easily distinguished from the simple conical processes in the specimens described here, which are most appropriately placed in T. pilosiusculum on account of their process morphology and density.

Tanarium triangulare (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) Liu and Moczydłowska, Reference Liu and Moczydłowska2019
 Figure 22.122.3

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Mengeosphaera triangularis Liu et al., p. 103, figs. 51.13, 68.

Reference Ouyang, Guan, Zhou and Xiao2017

Mengeosphaera? cuspidata; Ouyang et al., fig. 9I–K (specimens described here).

Reference Ouyang, Guan, Zhou and Xiao2017

Mengeosphaera chadianensis; Ouyang et al., fig. 9L, M (specimen described here).

Reference Liu and Moczydłowska2019

Tanarium triangularis (Liu et al.) Liu and Moczydłowska, p. 151, fig. 85.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Tanarium triangulare (Liu et al.) Liu and Moczydłowska; Ouyang et al., fig. 20D.

Figure 22. (1–3) Tanarium triangulare (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) Liu and Moczydłowska, Reference Liu and Moczydłowska2019: (1, 2) PB202058, thin section 14HA-140-5, F24/1, same area at different focal levels; (3) PB202059, thin section 14HA-140-3, D31/1. (4) Tanarium tuberosum Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993, PB202060, thin section 21DC-4-11, U45. Red arrowheads in (1) and (2) denote typical conical basal part of some processes.

Holotype

IGCAGS–NPIII–280, reposited at Institute of Geology, Chinese Academy of Geological Sciences, from the upper Member III of the Ediacaran Doushantuo Formation at Niuping section in the Yangtze Gorges area, Hubei Province, South China (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 68.1).

Description and measurements

Vesicle medium-sized to large, oval but originally spheroidal. Processes biform, with a conical or slightly inflated basal expansion supporting a thin and cylindrical apical spine. Processes evenly distributed and basally separated. Vesicle diameter of three specimens 182–194 μm (mean = 187 μm), and a larger specimen about 262 μm in vesicle diameter (Fig. 22.1, 22.2); process length 39.5–75.2 μm (N = 5; mean = 53.4 μm, SD = 2.6 μm) or 21.0–41.4% of vesicle diameter (N = 4; mean = 28.3%; SD = 9.3%), basal width 21.2–31.5 μm (N = 5; mean = 26.8 μm, SD = 3.8 μm); process basal expansion length 16.3–22.9 μm (N = 5; mean = 19.6 μm, SD = 3.0 μm) or 30.1–56.3% of vesicle diameter (N = 5; mean = 38.6%; SD = 10.8%); about 2–3 processes per 100 μm of vesicle periphery.

Material

Two specimens illustrated in Figure 22.1–22.3 (the specimen in Fig. 22.1, 22.2 also was illustrated in Ouyang et al., Reference Ouyang, Guan, Zhou and Xiao2017, fig. 9J), two specimens illustrated in Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017, fig. 9I, L, M), and one additional specimen.

Remarks

Both Mengeosphaera? cuspidata Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, and M. triangularis have been transferred to Tanarium (Liu and Moczydłowska, Reference Liu and Moczydłowska2019), although both are characterized by biform processes with a clearly defined inflection. Two of the specimens described here were originally illustrated as M.? cuspidata by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017, fig. 9I–K), and reassigned to T. triangulare by Liu and Moczydłowska (Reference Liu and Moczydłowska2019) without justification, but then again considered to be T. cuspidatum (Shang et al., Reference Shang, Liu and Moczydłowska2019; Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022). These specimens have processes that seem to exhibit a deflated base and thus resemble T. cuspidatum, but a re-examination of them has convinced us that most basal expansions are conical or slightly inflated with an inflection point (see red arrowheads in Fig. 22.1, 22.2). Thus, we follow Liu and Moczydłowska (Reference Liu and Moczydłowska2019) and identify the two specimens illustrated in Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017, fig. 9I–K) as T. triangulare. One specimen illustrated as Mengeosphaera chadianensis in Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017, fig. 9L–M) is similar to the two specimens mentioned above in process shape, size, and arrangement, and is also re-assigned to T. triangulare.

Tanarium tuberosum Moczydłowska, Vidal, and Rudavskaya, Reference Moczydłowska, Vidal and Rudavskaya1993
Figure 22.4

Reference Moczydłowska, Vidal and Rudavskaya1993

Tanarium tuberosum Moczydłowska, Vidal, and Rudavskaya, p. 516, text-fig. 15A–D.

Reference Faizullin1998

Tanarium conoideum Moczydłowska et al.; Faizullin, pl. II, fig. 1, pl. II, figs 2–4, 8.

Reference Nagovitsin, Faizullin and Yakshin2004

Tanarium stellatum Nagovitsin and Faizullin in Nagovitsin et al., p. 14, pl. II, figs 16–18.

Reference Moczydłowska2005

Tanarium tuberosum Moczydłowska et al.; Moczydłowska, p. 303, fig. 7B–D.

Reference Willman, Moczydłowska and Grey2006

Tanarium tuberosum Moczydłowska et al.; Willman et al., p. 36, pl. VII, figs 3, 4.

Reference Willman and Moczydłowska2008

Tanarium tuberosum Moczydłowska et al.; Willman and Moczydłowska, p. 527, fig. 12F.

Reference Vorob'eva, Sergeev and Knoll2009

Tanarium tuberosum Moczydłowska et al.; Vorob'eva et al., p. 182, fig. 7.6, 7.8.

Reference Golubkova, Raevskaya and Kuznetsov2010

Tanarium tuberosum Moczydłowska et al.; Golubkova et al., pl. II, fig. 2, pl. III, fig. 11.

Reference Sergeev, Knoll and Vorob'eva2011

Tanarium tuberosum Moczydłowska et al.; Sergeev et al., p. 1006, fig. 6.3.

Reference Moczydłowska and Nagovitsin2012

Tanarium tuberosum Moczydłowska et al.; Moczydłowska and Nagovitsin, p. 20, fig. 8G–J.

Reference Moczydłowska2016

Tanarium tuberosum Moczydłowska et al., emend. Moczydłowska, p. 93, pl. 3, figs 1–6.

Reference Liu and Moczydłowska2019

Tanarium tuberosum Moczydłowska et al., emend. Moczydłowska; Liu and Moczydłowska, p. 153, fig. 86.

Reference Shang, Liu and Moczydłowska2019

Tanarium tuberosum Moczydłowska et al., emend. Moczydłowska; Shang et al., p. 27, fig. 18A.

Reference Shang, Liu and Liu2020

Tanarium tuberosum Moczydłowska et al., emend. Moczydłowska; Shang et al., p. 159, fig. 6A–C.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Tanarium tuberosum Moczydłowska et al.; Ouyang et al., fig. 19R.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Tanarium tuberosum Moczydłowska et al.; Shi et al., fig. 9H (the specimen described here and illustrated in Fig. 22.4).

Reference Golubkova2023

Tanarium tuberosum (Moczydłowska et al.) emend. Moczydłowska [sic]; Golubkova, pl. 7, fig. 8.

Holotype

PMU-Sib.4-J/30/3, reposited at Uppsala University, from the Ediacaran Khamaka Formation, Nepa-Botuoba region, Yakutia, Siberia (Moczydłowska et al., Reference Moczydłowska, Vidal and Rudavskaya1993, p. 517, text-fig. 15A, B, D).

Description and measurements

Vesicle spheroidal, medium-sized, bearing basally connected, large conical processes. Vesicle diameter about 113 μm, process length about 32.0 μm (28.3% of vesicle diameter), and basal width about 32.4 μm (28.7% of vesicle diameter), with 1–2 processes per 100 μm of vesicle periphery.

Material

One specimen illustrated in Figure 22.4.

Remarks

Among all species of Tanarium, T. tuberosum is unique in its proportionally large conical processes with the broadest base. The specimen described here is larger than but otherwise similar to the holotype of T. tuberosum in process morphology and proportional size. For comparison, process length is about 22.8% of vesicle diameter, process basal width is about 20.9% of vesicle diameter, and length to basal width ratio is about 1.1 in the holotype, based on measurements taken from Moczydłowska et al. (Reference Moczydłowska, Vidal and Rudavskaya1993, text-fig. 15A, B, D). Our specimen differs from the holotype and some other published specimens of T. tuberosum in its relatively high process density; however, similar process density is also reported in a few specimens identified as T. tuberosum (e.g., Liu and Moczydłowska, Reference Liu and Moczydłowska2019, fig. 86A, B). We thus identified our specimen as T. tuberosum.

Genus Tianzhushania Yin and Li, Reference Yin and Li1978, emend. Yin et al., Reference Yin, Zhou and Yuan2008

Type species

Tianzhushania spinosa Yin and Li, Reference Yin and Li1978, emend. Yin in Yin and Liu, Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988.

Other species

Tianzhushania polysiphonia Yin in Yin and Liu, Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988; T. rara Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014.

Tianzhushania spinosa Yin and Li, Reference Yin and Li1978, emend. Yin in Yin and Liu, Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988
 Figure 23

Reference Yin and Li1978

Tianzhushania spinosa Yin and Li, p. 95, pl. 8, fig. 13.

Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu, p. 178, pl. 10, figs. 1–4.

Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988

Tianzhushania tubaeformis Yin in Yin and Liu, p. 178, pl. 9, figs. 8, 9.

Reference Yin1990

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin, pl. I, figs. 3, 4.

Reference Yin and Gao1995

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin and Gao, pl. II, fig. 10.

Reference Yin1996

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin, p. 326, pl. I, fig. 1.

Reference Zhang, Yin, Xiao and Knoll1998

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Zhang et al., p. 40, fig. 13.1, 13.4.

non Reference Zhang, Yin, Xiao and Knoll1998

Tianzhushania spinosa Yin in Yin and Li; Zhang et al., p. 40, fig. 13.2, 13.3.

Reference Yin1999

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin, p. 12, pl. 4, figs. 1–3.

Reference Yin2001

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin, pl. I, fig. 8.

Reference Yin, Gao and Xing2001

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin et al., p. 500, pl. I, figs. 1–4, pl. II, figs. 1, 2, 6.

non Reference Yin2001

Tianzhushania spinosa Yin in Yin and Li, emend. Yin in Yin and Liu; Yin, pl. II, figs. 1, 2.

non Reference Yin2001

Tianzhushania spinosa Yin in Yin and Li, emend. Yin in Yin and Liu; Yin et al., pl. II, figs. 3–5.

Reference Yin, Gao and Yue2003

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin et al., pl, I, figs, 5, 6.

Reference Yin, Bengtson and Yue2004

Tianzhushania spinosa Yin and Li; Yin et al., figs. 2A, 5D.

Reference Yin, Bengtson and Yue2004

Tianzhushania sp.; Yin et al., fig. 3A.

non Reference Yin, Bengtson and Yue2004

Tianzhushania spinosa Yin in Yin and Li; Yin et al., fig. 3B.

Reference Yin, Zhu, Knoll, Yuan, Zhang and Hu2007

Tianzhushania spinosa; Yin et al., fig. 1c–l.

Reference Zhou, Xie, McFadden, Xiao and Yuan2007

Tianzhushania spinosa; Zhou et al., fig. 4A.

Reference Yin, Zhou and Yuan2008

Tianzhushania conferta Yin et al., p. 138, pl. I, figs. 11–13.

Reference Yin, Zhou and Yuan2008

Tianzhushania fissura Yin et al., p. 138, pl. I, figs. 2–10.

non Reference Shukla, Mathur, Babu and Srivastava2008

Tianzhushania spinosa; Shukla et al., p. 374, pl. III, figs. 1, 2.

Reference Liu, Yin, Gao, Tang and Chen2009

Tianzhushania spinosa; Liu et al., fig. 2o–q.

Reference Yin, Liu, Chen, Tang, Gao and Wang2009a

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Yin et al., pl. I, figs. 1, 8.

Reference Chen, Yin, Liu, Gao, Tang and Wang2010

Tianzhushania spinosa; Chen et al., fig. 2.13, 2.17.

Reference Yin, Wang, Yuan and Zhou2011

Tianzhushania spinosa; C. Yin et al., fig. 4a, b.

Reference Xiao, McFadden, Peek, Kaufman, Zhou, Jiang and Hu2012

Tianzhushania spinosa; Xiao et al., fig. 4C–H.

Reference Liu, Yin, Chen, Tang and Gao2013

Tianzhushania spinosa; Liu et al., fig. 10A.

Reference Zeng, Chen, Li, Zhou, Zhang and Peng2013

Tianzhushania spinosa; Zeng et al., fig. 3.2.

Reference Liu, Yin, Chen, Tang and Gao2013

Tianzhushania conferta Yin et al.; Liu et al., fig. 10E.

Reference Liu, Yin, Chen, Tang and Gao2013

Tianzhushania fissura Yin et al.; Liu et al., fig. 10D.

Reference Zeng, Chen, Li, Zhou, Zhang and Peng2013

Tianzhushania fissura; Zeng et al., fig. 3.1.

Reference Zeng, Chen, Li, Zhou, Zhang and Peng2013

Tianzhushania sp.; Zeng et al., fig. 3.3.

Reference Xiao, Zhou, Liu, Wang and Yuan2014

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Xiao et al., p. 56.

Reference Liu, Chen, Zhu, Li, Yin and Shang2014b

Tianzhushania spinosa; Liu et al., fig. 7D–F.

Reference Ouyang, Zhou, Guan and Wang2015

Tianzhushania spinosa Yin and Li, emend. Yin in Yin and Liu; Ouyang et al., p. 219, pl. III, figs. 1–6.

Reference Joshi and Tiwari2016

Tianzhushania spinosa; Joshi and Tiwari, p. 332, fig. 4B–E.

Reference Hawkins, Xiao, Jiang, Wang and Shi2017

Tianzhushania spinosa; Hawkins et al., fig. 6A, B.

non Reference Hawkins, Xiao, Jiang, Wang and Shi2017

possibly Tianzhushania spinosa; Hawkins et al., fig. 7A, B.

Reference Ouyang, Zhou, Xiao, Chen and Shao2019

Tianzhushania spinosa; Ouyang et al., fig. 11A, B.

Reference Yang, Pang, Chen, Zhong and Yang2020

Tianzhushania sp.; Yang et al., p. 9, fig. 2P, Q.

Reference Liu, Qi, Fan, Guo and Pei2021

Tianzhushania spinosa; Liu et al., fig. 5.1.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Tianzhushania spinosa Yin in Yin and Li, emend. Yin in Yin and Liu; Ouyang et al., fig. 21A–L.

non Reference Sharma, Shukla and Sergeev2021

Tianzhushania spinosa Yin and Li; Sharma et al., fig. 9A, D.

Reference Joshi, Mishra and Tiwari2022

Tianzhushania spinosa; Joshi et al., fig. 4d (mistakenly presented as 4c in figure caption; fig. 4c is T. polysiphonia).

Figure 23. Tianzhushania spinosa Yin and Li, Reference Yin and Li1978, emend. Yin in Yin and Liu, Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988. (1–6) PB202061, thin section 21LHK-1-10, O41/4; circled 2 and 6 in (1) mark the areas magnified in (2) and (6), respectively; circled 3 in (2) marks the area magnified in (3); circled 4 in (2) marks the same area magnified in (4) and (5) at different focal levels. Red arrowheads denote hollow cylindrical processes embedded in multilaminate membrane; blue arrowheads denote poorly preserved multilaminate membrane.

Holotype

Tian R29 X150, reposited at NIGPAS, from the Ediacaran Doushantuo Formation at Tianzhushan in Changyang area, Hubei Province, South China (Yin and Li, Reference Yin and Li1978, pl. 8, fig. 13).

Description and measurements

Vesicle large, strongly deformed, originally spheroidal. Processes hollow and cylindrical (Fig. 23.2, 23.4, 23.5), evenly distributed, penetrating a multilaminate outer membrane (Fig. 23.3, 23.6) that surrounds the vesicle wall. Vesicle diameter unmeasurable due to deformation. Processes about 61.6 μm long and 1.4 μm wide, with about six processes per 100 μm of vesicle periphery. The thickness of the multilaminate outer membrane was not measured because it is likely cut obliquely in the thin section but is estimated to be similar to the length of cylindrical processes.

Material

One illustrated specimen (Fig. 23).

Remarks

Although poorly preserved, the specimen does show hollow cylindrical processes penetrating a multilaminate membrane, which are features diagnostic of Tianzhushania. The long, evenly and densely arranged processes identify this specimen to T. spinosa, which is different from the clustered distribution of processes in T. polysiphonia and the short and sparse processes in T. rara. Since Ouyang et al. (Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021) reassigned the possible T. spinosa specimen reported from the Siduping section by Hawkins et al. (Reference Hawkins, Xiao, Jiang, Wang and Shi2017, fig. 7A, B) to Crassimembrana multitunica Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021, the specimen reported here represents the only known occurrence of Tianzhushania from the Doushantuo Formation in basinal facies or deep-water settings.

Three specimens identified as Tianzhushania sp. from the Weng'an, Yangtze Gorges, and Baokang areas (Yin et al., Reference Yin, Bengtson and Yue2004; Zeng et al., Reference Zeng, Chen, Li, Zhou, Zhang and Peng2013; Yang et al., Reference Yang, Pang, Chen, Zhong and Yang2020) all bear numerous hollow cylindrical processes that are embedded in a thick multilaminate layer and evenly distributed, and are here reassigned to T. spinosa. The specimen identified as T. spinosa from the Krol'A Formation in northern India (Sharma et al., Reference Sharma, Shukla and Sergeev2021, fig. 9A, D) has small conical processes and thus should be excluded from Tianzhushania. Considering its small and densely distributed processes, that specimen may belong to Knollisphaeridium, possibly K. coniformum, as noted in Xiao et al. (Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022).

Genus Trachyhystrichosphaera Timofeev and Hermann in Timofeev et al., Reference Timofeev, Hermann and Mikhailova1976, emend. Tang et al., Reference Tang, Pang, Xiao, Yuan, Ou and Wan2013

Type species

Trachyhystrichosphaera aimika Hermann in Timofeev et al., Reference Timofeev, Hermann and Mikhailova1976.

Other species

Trachyhystrichosphaera botula Tang et al., Reference Tang, Pang, Xiao, Yuan, Ou and Wan2013; T. polaris Butterfield in Butterfield et al., Reference Butterfield, Knoll and Swett1994.

Trachyhystrichosphaera? sp.
 Figure 24

non Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988

Trachyhystrichosphaera sp.; Yin and Liu, p. 177, p. 180, pl. 11, figs. 3, 4.

non Reference Knoll and Walter1992

?Trachyhystrichosphaera sp.; Knoll, p. 770, pl. 4, fig. 1, pl. 5, figs. 1, 2.

non Reference Yin1999

?Trachyhystrichosphaera sp.; Yin, p. 14, pl. 3, fig. 3.

?Reference Nagovitsin, Faizullin and Yakshin2004

Trachyhystrichosphaera aff. aimica Hermann, 1976 [sic]; Nagovitsin et al., p. 14, pl. I, fig. 10.

Figure 24. Trachyhystrichosphaera? sp. (1–8) PB202062, thin section 19CW-6-16, M40/3; circled 2–5 and 8 in (1) mark areas magnified in (2–5) and (8), respectively; circled 6 in (1) marks the same area magnified in (6) and (7) at different focal levels to show different processes. Scale bar in (5) also applies to (2–4, 6–8). Red arrowheads denote cylindrical processes, yellow arrowheads denote conical processes, blue arrowheads denote outer membrane.

Description and measurements

Vesicle small, spheroidal or ovoidal, with sparsely and irregularly distributed hollow processes. Processes bimorphic, with larger conical and smaller cylindrical ones. Vesicle diameter about 248 μm; conical processes 6.2–14.8 μm in length with an average of 10.7 μm, or 2.5–6.0% of vesicle diameter with an average of 4.3%, and 4.4–11.1 μm in basal width with an average of 7.6 μm; cylindrical processes 5.3–8.1 μm in length with an average of 6.9 μm, or 2.1–3.3% of vesicle diameter with an average of 2.8%, and 0.9–1.6 μm (with an average of 1.3 μm in width). An outer membrane can be found on top of some conical (Fig. 24.224.4) and cylindrical (Fig. 24.524.8) processes.

Material

A single fairly well-preserved specimen (Fig. 24).

Remarks

The illustrated specimen is tentatively assigned to Trachyhystrichosphaera based on its bimorphic processes and outer membrane. Some other genera are also characterized by bimorphic or heteromorphic processes, including Alicesphaeridium, Asseserium, Bispinosphaera, Distosphaera, Duospinosphaera, Sinosphaera, and Verrucosphaera. Among them, Alicesphaeridium, Bispinosphaera, Distosphaera, Duospinosphaera, Sinosphaera, and Verrucosphaera are all characterized by their abundant, densely, and somewhat evenly distributed processes that cover the entire vesicle surface. Asseserium diversum Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012, bears heteromorphic and irregularly distributed hollow processes (Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012), and its process density is similar to the illustrated specimen. However, compared with Asseserium, which has a small to medium-sized vesicle bearing processes whose length is 10–40% of the vesicle diameter, the illustrated specimen has a vesicle several times larger and thus proportionally shorter processes. In addition, none of the above-mentioned bimorphic or heteromorphic taxa have an outer membrane, which is observed in the illustrated specimen (blue arrowheads in Fig. 24.3, 24.524.8), and diagnostic of Trachyhystrichosphaera (Tang et al., Reference Tang, Pang, Xiao, Yuan, Ou and Wan2013).

Trachyhystrichosphaera is a typical Tonian genus (Pang et al., Reference Pang, Tang, Wan and Yuan2020), and has been only infrequently reported, mostly as open nomenclature, from Ediacaran strata (Knoll, Reference Knoll1992; Faizullin, Reference Faizullin1998; Nagovitsin et al., Reference Nagovitsin, Faizullin and Yakshin2004). Several previously published specimens of Trachyhystrichosphaera lack the diagnostic features of and thus should be excluded from this genus, including Trachyhystrichosphaera sp. in Yin and Liu (Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988, p. 177, pl. 11, figs. 3, 4), ?Trachyhystrichosphaera sp. in Knoll (Reference Knoll1992, p. 770, pl. 4, fig. 1, pl. 5, figs. 1, 2), ?Trachyhystrichosphaera sp. in Yin (Reference Yin1999, p. 14, pl. 3, fig. 3), Trachyhystrichosphaera aff. aimica [sic] in Nagovitsin et al. (Reference Nagovitsin, Faizullin and Yakshin2004, pl. I, figs. 7 and 11 only), and T. aimika in Shukla et al. (Reference Shukla, Mathur, Babu and Srivastava2008, p. 374, pl. 2, fig. 1). The specimen identified as Trachyhystrichosphaera sp. in Faizullin (Reference Faizullin1998, pl. I, fig. 16) was poorly illustrated and a re-examination of the specimen is required to assess its taxonomic identification. One of the three specimens identified as Trachyhystrichosphaera aff. aimica [sic] extracted from shales of the Ediacaran Ura Formation in Siberia (Nagovitsin et al., Reference Nagovitsin, Faizullin and Yakshin2004, pl. I, fig. 10) contains an outer layer enveloping short, hollow, and sparsely distributed processes, resembling the specimen illustrated here, and fits the diagnosis of Trachyhystrichosphaera. However, these two possible occurrences of Ediacaran Trachyhystrichosphaera are each represented by a single specimen, and may represent morphological variations of other acanthomorphs such as Tianzhushania rara. Therefore, we place the illustrated specimen in an open nomenclature.

Genus Urasphaera Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012

Type species

Urasphaera capitalis Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, Reference Moczydłowska and Nagovitsin2012.

Other species

Urasphaera fungiformis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a; U. nupta Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a.

Urasphaera fungiformis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a
 Figure 25

Reference Liu, Yin, Chen, Tang and Gao2013

Gyalosphaeridium pulchrum Zang in Zang and Walter, Reference Zang and Walter1992; Liu et al., fig. 13G.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Urasphaera fungiformis Liu et al., p. 119, figs. 87, 88, 89.1.

Reference Nie, Liu and Dong2017

Urasphaera fungiformis Liu et al.; Nie et al., p. 380, fig. 9.

Reference Ouyang, Guan, Zhou and Xiao2017

Urasphaera fungiformis; Ouyang et al., fig. 8G–J (the specimen described here and illustrated in Fig. 26).

Reference Ye, Li, Tong, An, Hu and Xiao2022

Urasphaera fungiformis Liu et al.; Ye et al., fig. 48A–C.

Figure 25. Urasphaera fungiformis Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a. (13) PB202063, thin section 14HA-115-1, N50; circled 2 in (1) marks the same area magnified in (2) and (3) at different focal levels to show different processes.

Figure 26. Verrucosphaera? undulata new species. (1–5) Holotype, PB202064, thin section 21DC-6-1, H44; circled 2 in (1) marks the same area magnified in (2) and (3) at different focal levels to show different processes; circled 4 in (1) marks the same area magnified in (4) and (5) at different focal levels to show different processes; (6–8) PB202065, thin section 21DC-5-4, S47; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively. Red arrowheads denote thin cylindrical processes on top of thick conical processes.

Holotype

IGCAGS-NPIII-482, thin section NPIII13-3-5, Nikon 80i coordinates 23.8×111, England Finder coordinates E23/4, reposited at the Institute of Geology, Chinese Academy of Geological Science, from the Ediacaran Doushantuo Formation at the Niuping section in Yichang area, Hubei Province, South China (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, fig. 87.1–87.4).

Description and measurements

Vesicle large, spheroidal, bearing evenly distributed processes. Processes begin with a wide and deflated base that tapers to form a waist and then expands distally to form a truncated terminal end. Vesicle diameter about 400 μm, with 1–2 processes per 100 μm of vesicle periphery. Process length about 39.3 μm and 9.8% of vesicle diameter, basal width about 27.2 μm, terminal width about 9.3 μm, minimum width of process (waist width) about 3.2 μm.

Material

One well-preserved specimen (Fig. 25).

Remarks

The specimen at hand is larger than specimens of Urasphaera fungiformis from the type locality at the Niuping section in the Yangtze Gorges area of Hubei Province (Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a), but comparable to those from the Shennongjia area reported by Ye et al. (Reference Ye, Li, Tong, An, Hu and Xiao2022, fig. 48A–C). Nonetheless, this specimen resembles those from the Yangtze Gorges area in the moderate number of proportionally short processes with a broadened base, features that distinguish U. fungiformis from U. capitalis and U. nupta. The small distal expansion may not be captured in all processes of Urasphaera if the processes are cut obliquely in the thin section, thus some processes may appear conical in shape.

Genus Verrucosphaera Liu and Moczydłowska, Reference Liu and Moczydłowska2019

Type species

Verrucosphaera minima Liu and Moczydłowska, Reference Liu and Moczydłowska2019.

Other species

Verrucosphaera? undulata n. sp.

Verrucosphaera? undulata new species
 Figures 26–28

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

?Verrucosphaera sp.; Shi et al., fig. 10A–F (including the type specimen in fig. 10A, B, D).

Figure 27. Verrucosphaera? undulata new species. (1–4) PB202066, thin section 21DC-5-4, P41/2; circled 2–4 in (1) mark areas magnified in (2–4), respectively; (5–7) PB202067, thin section 21DC-5-4, T32/4; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively; (8–10) PB202068, thin section 21DC-5-4, L43/3; circled 9 and 10 in (8) mark areas magnified in (9) and (10), respectively. Red arrowheads denote thin cylindrical processes on top of thick conical processes.

Figure 28. Sketch of Verrucosphaera? undulata new species.

Holotype

PB202064, thin section 21DC-6-1, ZEISS Scope A1 coordinates 8×92, England Finder coordinates H44, illustrated in Figure 26.1–26.5, reposited at NIGPAS, from Doushantuo Formation at the Caojunba section in Shimen area, Hunan Province, South China.

Diagnosis

Vesicle medium-sized, spheroidal or ovoidal, bearing two sets of bimorphic processes: a set of large conical processes supporting a set of thin filamentous processes. The large processes are hollow, obtusely conical, basally connected or separated, terminally rounded or truncated, irregularly distributed, and variable in both length and basal width. The thin filamentous processes are cylindrical, more or less uniform in length and thickness, densely arranged but basally separated, and evenly distributed on both the vesicle wall and the large processes. The large conical and thin filamentous processes are comparable in length, accounting for about 5% of vesicle diameter.

Description and measurements

Holotype: vesicle diameter 172 μm; large processes 4.8 μm in length (2.8% of vesicle diameter) and 7.9 μm in basal width; thin processes 4.9 μm in length (2.8% of vesicle diameter) and 0.2 μm in diameter, 27 processes per 100 μm of vesicle periphery. Other specimens: vesicle diameter 126–192 μm (N = 30, mean = 162 μm, SD = 16 μm); large process length 3.8–18.7 μm (N = 25, mean = 8.2 μm, SD = 3.4 μm) or 2.3–10.0% of vesicle diameter (N = 25, mean = 5.1%, SD = 1.9%), process basal width 6.7–44.8 μm (N = 23, mean = 18.5 μm, SD = 9.4 μm); thin process length 2.8–8.7 μm (N = 24, mean = 5.6 μm, SD = 1.3 μm) or 1.7–5.6% of vesicle diameter (N = 24, mean = 3.5%, SD = 0.9%), process width 0.2–0.6 μm (N = 22, mean = 0.3 μm, SD = 0.1 μm), 23–47 processes per 100 μm of vesicle periphery.

Etymology

From Latin undulatus, wavy, with reference to the wavy profile of the vesicle wall as viewed in thin sections due to the irregular arrangement of large processes which are obtusely conical in shape.

Material

Five illustrated specimens (Figs. 26, 27) and 26 additional specimens.

Remarks

There are several other taxa that are characterized by bimorphic processes, with a set of large hollow processes and another set of thin cylindrical processes. These taxa, including Bispinosphaera, Distosphaera, and Duospinosphaera, differ from Verrucosphaera in the spatial relationship between the two set of processes: the thin processes in Bispinosphaera, Distosphaera, and Duospinosphaera are initiated from either the inner or outer surface of the vesicle wall and they are not found on top of the large processes. Verrucosphaera? undulata n. sp. is different from V. minima in that the thin processes are only found on top of the large processes in the latter species, but they can be on top of both the large processes and the vesicle wall in the former species. Additionally, the large processes are more or less conical in V.? undulata n. sp. but hemispherical in V. minima. Considering these similarities and differences, V.? undulata n. sp. is tentatively placed in the genus Verrucosphaera, pending an emendation of the genus diagnosis.

Genus Weissiella Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009

Type species

Weissiella grandistella Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009.

Other species

Weissiella brevis Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014, emend. Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021; Weissiella concentrica Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022.

Remarks

The genus Weissiella is characterized by hollow and internally septate processes. Several other Ediacaran acanthomorph taxa are also known for their hollow and internally decorated processes. These internal decorations include either transverse septa (as in Bispinosphaera peregrina Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, Weissiella, and Yushengia ramispina Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) or domal structures (as in Mengeosphaera matryoshkaformis). Among these taxa, Weissiella has the widest paleogeographic distribution and the greatest morphological variation. Thus far, three species of Weissiella have been recognized (W. grandistella, W. brevis, W. concentrica), differentiated from each other by their process morphologies and the presence of an outer wall. In addition to these three species, Ouyang et al. (Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021) proposed the assignment of all silicified Weissiella specimens from the Doushantuo Formation with large conical processes to Weissiella cf. W. grandistella, emphasizing both their morphological similarities to and difference from W. grandistella specimens from the type locality. Two unnamed species of Weissiella (Ye et al., Reference Ye, Tong, An, Tian, Zhao and Zhu2015, pl. I, figs. 15–19, and Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019, fig. 10E–G) were reassigned to W. brevis (Xiao et al., Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022); the processes in the former (Ye et al., Reference Ye, Tong, An, Tian, Zhao and Zhu2015) are irregularly shaped with occasional branches, whereas those in the latter (Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019) are likely biform, both of which are different from W. brevis from the type locality but considered as representing intraspecific variations of W. brevis. The existence of transverse septa or cross-walls in the processes of Weissiella and other taxa raises the interesting question about their functions, a topic worthy of further investigation in the future.

Weissiella cf. W. grandistella Vorob'eva, Sergeev, and Knoll, Reference Vorob'eva, Sergeev and Knoll2009
 Figure 29

Reference Liu, Yin, Chen, Tang and Gao2013

Weissiella grandistella; Liu et al., fig. 13E.

Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a

Weissiella grandistella Vorob'eva et al.; Liu et al., p. 128, figs. 94, 95.

Reference Liu, Chen, Zhu, Li, Yin and Shang2014b

Weissiella grandistella; Liu et al., fig. 9E.

non Reference Shukla and Tiwari2014

Weissiella cf. W. grandistella; Shukla and Tiwari, p. 219, fig. 8A–E.

Reference Liu and Moczydłowska2019

Weissiella grandistella Vorob'eva et al.; Liu and Moczydłowska, p. 163, figs. 91F, G, 92.

Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021

Weissiella cf. W. grandistella; Ouyang et al., fig. 24A–H.

Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022

Weissiella cf. W. grandistella; Shi et al., fig. 10G–I (the specimen described here and illustrated in Fig. 29).

Reference Ye, Li, Tong, An, Hu and Xiao2022

Weissiella cf. grandistella Vorob'eva et al.; Ye et al., fig. 49D–F.

Figure 29. Weissiella cf. W. grandistella. (1–7) PB202069, thin section 21DC-2-30, T35; circled 2–4 in (1) mark areas magnified in (2–4), respectively; red arrowheads denote cross-walls in the processes; (5–7) cross-polarized light microscopic photographs of (1); circled 6 in (2) and circled 7 in (3) showing areas in (6) and (7), respectively; recrystallized micro-quartz indicated by yellow arrowheads; scale bar in (6) also applies to (7).

Description and measurements

Vesicle medium-sized, spheroidal, bearing a modest number of large conical processes evenly distributed on the vesicle surface. Processes hollow but each contains about two thin cross-walls or transverse septa that divide the process into several compartments (red arrowheads in Fig. 29.229.4). Cross-walls occur near the base of each process. Vesicle diameter about 114 μm, maximum measurable length of processes 45.0 μm (or 39.6% of vesicle diameter), process basal width 23.4 μm, about 3 processes per 100 μm of vesicle periphery.

Material

One well-preserved specimen (Fig. 29).

Remarks

As for specimens identified as Weissiella cf. W. grandistella from the Doushantuo Formation in Yangtze Gorges area, the specimen described here from the Caojunba section is also much smaller than W. grandistella from its type locality and is placed in an open nomenclature (see Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021, for a detailed comparison among W. grandistella, W. brevis, and permineralized Doushantuo acritarchs identified as Weissiella cf. W. grandistella). One distinctive feature of this specimen is that the cross-walls occur near the base of the processes. Examination under polarized light microscopy (e.g., Fig. 29.529.7) indicates that the lack of cross-walls in the distal portion of processes is not a taphonomic artifact related to recrystallization and may thus reflect intraspecific variation.

All specimens of Weissiella cf. W. grandistella from the Doushantuo Formation in South China are morphologically similar and may constitute a new species of Weissiella. However, except for their smaller size, they are otherwise similar to W. grandistella, which led Liu and Moczydłowska (Reference Liu and Moczydłowska2019) to assign them to W. grandistella. Current morphological data are not sufficient to conclusively resolve this issue, and these specimens are here treated as an open nomenclature.

Results

Morphological groups of Doushantuo microfossils from the studied sections

Microfossils from the Doushantuo Formation at the studied localities include acanthomorphic and sphaeromorphic acritarchs, multicellular algae, tubular microfossils, filaments and coccoids, and other problematic fossils (Tables 1, 2). Although chert nodules in these localities are composed mainly of micro-quartz and thus petrographically similar to fossiliferous chert nodules previously obtained from the Doushantuo Formation elsewhere, many microfossils found in this study underwent more severe degradation and destruction due to recrystallization of micro-quartz (up to several micrometers in size; e.g., yellow arrowheads in Figs. 29.5, 29.7, 30), leading to poor preservation of delicate structures. To facilitate discussion, the Doushantuo microfossils recovered in this study are briefly described below in several morphological groups.

Figure 30. Recrystallized micro-quartz in chert nodules. (1, 3) A poorly preserved microfossil under plane- (1) and cross- (3) polarized light, showing recrystallized micro-quartz up to 7 μm in size (yellow arrowheads); thin section 19TP-1-39. (2) A well-preserved microfossil under cross-polarized light, showing recrystallized micro-quartz in various sizes (yellow arrowheads); thin section 21DC-5-3. (4) A poorly preserved microfossil under cross-polarized light, with the vesicle interior filled with sightly recrystallized chalcedony (red arrowhead), vesicle wall destroyed by three large calcite crystals, and extra-vesicle matrix filled with micro-quartz in various sizes (yellow arrowheads); thin section 19TP-1-25.

Table 2. Summary of acanthomorph occurrence and abundance data at the nine studied sections. Each occurrence is denoted by fossiliferous sample name and number of specimens. For example, “21DC-4, 1” means one acanthomorph specimen recovered from the sample 21DC-4. Notes for superscripts: (1) Identified as Cavaspina cf. C. basiconica by Shi et al. (Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022). (2) Identified as ?Verrucosphaera sp. by Shi et al. (Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022). (3) Identified as Appendisphaera fragilis by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017). (4) Identified as ?Cavaspina basiconica by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017). (5) Identified as indeterminate acanthomorph by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017). (6) Identified as Mengeosphaera spicata by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017). (7) Identified as Mengeosphaera latibasis? by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017). (8) Identified as Mengeosphaera chadianensis, Mengeosphaera sp. indet., and M.? cuspidata by Ouyang et al. (Reference Ouyang, Guan, Zhou and Xiao2017).

Acanthomorphic acritarchs (Table 2, Figs. 4–29, 31).—Acanthomorphic acritarchs appear in the Doushantuo Formation at all studied sections and are a major component of eukaryotic microfossils in most fossiliferous samples. The 206 acanthomorphic acritarch specimens that were recognized from the nine studied stratigraphic sections are classified into 15 genera, 29 species (including three new species: Bullatosphaera? colliformis n. sp., Eotylotopalla inflata n. sp., and Verrucosphaera? undulata n. sp.), and six unnamed forms (Eotylotopalla sp., Mengeosphaera minima?, Tanarium cf. T. capitatum, Trachyhystrichosphaera? sp., and Weissiella cf. W. grandistella), which may represent new taxa. Most of these taxa are represented by only one or a few specimens, and the very few taxa that are relatively abundant (i.e., accounting for ~10% of all acanthomorphic specimens), such as Appendisphaera magnifica, Hocosphaeridium anozos, and Verrucosphaera? undulata n. sp., are each found at only one stratigraphic section. Consequently, diversity and relative abundance of different acanthomorphic taxa vary significantly among localities. For example, four of the five species recovered from the basinal facies are from the Lianghekou section. Only two species occur at more than half of the studied sections: Appendisphaera grandis at six sections, and Hocosphaeridium scaberfacium at five sections. The two species of Megasphaera were recovered only from one olistostrome sample (19SDP-1) at Siduping, and thus may not be representative of the local assemblage.

Figure 31. Indeterminate acanthomorphs. (1) PB202070, thin section 19SDP-1-5, O23/4. (2) PB202071, thin section 19SDP-7-3, J28. (3) PB202072, thin section 19CW-5-21, K39. (4) PB202073, thin section 21LHK-1-2, P35. Red arrowheads denote processes.

Sphaeromorphic acritarchs (Fig. 32).—Appearing at eight out of the nine studied sections (Table 1), sphaeromorphic acritarchs are represented by leiospheres of various sizes. The abundance and preservational state of sphaeromorphs vary significantly among localities. In the upper part of the Doushantuo Formation at Caojunba, almost all fossiliferous samples contain clustered or even tightly compacted leiospheres, with many clusters consisting of tens of specimens of similar size (generally about 100–200 μm in diameter; Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022, fig. 6C–G). For samples from other sections or the lower part of the Doushantuo Formation at Caojunba, however, most leiospheres are solitary (Fig. 32.1, 32.2), and only occasionally form small or loosely arranged aggregates (Fig. 32.3, 32.4).

Figure 32. Sphaeromorphic acritarchs. (1) PB202074, thin section 21LHK-1-6, E42. (2) PB202075, thin section 19HP-1-20, O33/3. (3) PB202076, thin section 19CW-5-30, Q36/3. (4) PB202077, thin section 19TP-1-26, B40.

Multicellular algae (Fig. 33).—Multicellular algae recovered in this study are represented by one specimen (Wengania minuta Xiao, Reference Xiao2004b; Ouyang et al., Reference Ouyang, Guan, Zhou and Xiao2017, fig. 7A) from the Lujiayuanzi section, one specimen (unnamed thallus, Fig. 33.6) at the Caowan section, and four specimens (one identified as W. minuta and three unnamed, all from the olistostrome sample 19SDP-1) at the Siduping section. The three unnamed specimens from the Siduping section (Fig. 33.333.5, 33.7) are similar to “Unnamed multicellular form with relatively large cells” (Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021, fig. 9I) and “Unnamed species B” (Shang and Liu, Reference Shang and Liu2022, fig. 13) in their exceptionally large (commonly exceeding 20 μm), cuboidal or polyhedral cells with apparently rigid cell walls.

Figure 33. Multicellular algae. (1, 2) Wengania minuta Xiao, Reference Xiao2004b, PB202078, thin section 19SDP-1-19, N41/4, showing the same area at different focal levels. (3–5, 7) Unnamed thalli with large cells; (3–5) PB202079, thin section 19SDP-1-19, M35; (7) PB202081, thin section 19SDP-1-25, K42/3. (6) Unnamed multicellular thallus, PB202080, thin section 19CW-6-15, M41.

Tubular microfossils (Fig. 34).—Seven tubular microfossil specimens are found from the Doushantuo Formation at Caojunba, Caowan, Siduping, and Majindong sections (Table 1). One specimen (Fig. 34.1) with square cross-sectional view fits the diagnosis of Quadratitubus orbigoniatus Xue, Tang, and Yu, Reference Xue, Tang and Yu1992, emend. Liu et al., Reference Liu, Xiao, Yin, Zhou, Gao and Tang2008, and three additional specimens (Fig. 34.2) preserved together may represent oblique sectional views of Q. orbigoniatus. The remaining three specimens (Fig. 34.3, 34.4) are identified as Sinocyclocyclicus guizhouensis Xue, Tang, and Yu, Reference Xue, Tang and Yu1992, emend. Liu et al., Reference Liu, Xiao, Yin, Zhou, Gao and Tang2008.

Figure 34. Tubular microfossils. (1) Quadratitubus orbigoniatus Xue, Tang, and Yu, Reference Xue, Tang and Yu1992, emend. Liu et al., Reference Liu, Xiao, Yin, Zhou, Gao and Tang2008, PB202082, thin section 19CW-6-13, M44/3. (2) Possible Quadratitubus orbigoniatus, PB202083, thin section 21DC-2-36, L40/2. (3, 4) Sinocyclocyclicus guizhouensis Xue, Tang, and Yu, Reference Xue, Tang and Yu1992, emend. Liu et al., Reference Liu, Xiao, Yin, Zhou, Gao and Tang2008; (3) PB202084, thin section 19SDP-7-3, J37/2; (4) PB202085, thin section 21MJD-1-10, K36/3.

Filamentous and coccoidal microfossils (Figs. 35–37).—Filamentous and coccoidal microfossils, likely of prokaryotic affinities (Butterfield et al., Reference Butterfield, Knoll and Swett1994), occur at all studied sections, and are abundant in many fossiliferous samples (Table 1). Among them, the filamentous taxa Siphonophycus Schopf, Reference Schopf1968, emend. Knoll et al., Reference Knoll, Swett and Mark1991 (Fig. 35) and Salome Knoll, Reference Knoll1982 (Figs. 35.3, 36.236.4) with varying filament diameters, are the two most abundant forms, preserved either as solitary specimens or in microbial mats. Other filamentous microfossils include one specimen of Obruchevella Reitlinger, Reference Reitlinger1948, emend. Yakshin and Luchinina, Reference Yakshin, Luchinina, Meshkova and Nikolaeva1981 (Fig. 36.1), one bundle of thin filaments resembling Polytrichoides Hermann, Reference Hermann and Timofeev1974, emend. Hermann in Timofeev et al., Reference Timofeev, Hermann and Mikhailova1976 (Fig. 36.5), and one short fragment of a septate filament with an exceptionally large cell width-to-length ratio (on average 257 μm wide and 11 μm long, Fig. 36.6), which to some extent resembles a specimen described as “Large fragment with longitudinal structures” (Arvestål and Willman, Reference Arvestål and Willman2020, fig. 12S). Other septate filamentous microfossils, such as Cyanonema Schopf, Reference Schopf1968, emend. Butterfield et al., Reference Butterfield, Knoll and Swett1994, and Oscillatoriopsis Schopf, Reference Schopf1968, emend. Butterfield et al., Reference Butterfield, Knoll and Swett1994, which are common Ediacaran taxa, are not confirmed in our materials, possibly due to the loss of trichomes or cellular details of the filaments during degradation and/or diagenesis. Coccoidal microfossils are rare compared with filaments, with only two aggregated coccoid specimens discovered from the Lianghekou section (Fig. 36.7, 36.8), and some possible coccoidal microfossils scattered in silicified matrices at other localities. Microbial mats (Fig. 37), which appear to have been built by various species of Siphonophycus, are common. Some thin sections are composed entirely of silicified microbial mats. Many observed microbial mats are fragmented, and some mat fragments from the Siduping and Lianghekou sections show evidence of reworking (e.g., rounded outline, Fig. 37.137.3; or sharp contact with surrounding matrix, Fig. 37.4).

Figure 35. Microbial mats consist of filamentous microfossils. (1) A small fragment of Siphonophycus mat, PB202086, thin section 21MJD-1-3, K32/2. (2, 4) Mat with thin filaments interwoven into spherical structures, PB202087, thin section 19CW-6-9, L38; circled 4 in (2) marks the area magnified in (4). (3) Microbial mat consists of various filamentous microfossils including Siphonophycus Schopf, Reference Schopf1968, emend. Knoll et al., Reference Knoll, Swett and Mark1991, and Salome Knoll, Reference Knoll1982, PB202088, thin section 18JSC-2-3, H34/4. (5, 6) Microbial mat consisting of filamentous microfossils of various sizes; (5) PB202089, thin section 19CW-6-6; (6) PB202090, thin section 19SDP-7-19, Q36.

Figure 36. Filamentous and coccoidal microfossils. (1) Obruchevella minor Zhang, Reference Zhang1984a, PB202091, thin section 18JSC-2-4, T22/2. (2) Salome svalbardense Knoll, Reference Knoll1982, PB202092, thin section 21LHK-1-6, J38. (3, 4) Salome hubeiensis Zhang, Reference Zhang1986: (3) PB202093, thin section 19TP-1-40, J33/3, (4) PB202094, thin section 19CW-6-14, J36/2. (5) Bundled filaments resembling Polytrichoides Hermann, Reference Hermann and Timofeev1974, emend. Hermann in Timofeev et al., Reference Timofeev, Hermann and Mikhailova1976, PB202095, thin section 19HP-2-6, M40. (6) Septate trichome with cells much wider than length resembling Oscillatoriopsis Schopf, Reference Schopf1968, emend. Butterfield et al., Reference Butterfield, Knoll and Swett1994, PB202096, thin section 19HP-2-3, Q38/3. (7, 8) Aggregated coccoids resembling Myxococcoides Schopf, Reference Schopf1968: (7) PB202097, thin section 21LHK-1-10, Q43/2; (8) PB202098, thin section 21LHK-1-10, N48/3.

Figure 37. Microbial mat preserved as reworked clasts. (1, 2) PB202099, thin section 21LHK-1-15, N42/2; circled 2 in (1) mark the area magnified in (2); (3) PB202100, thin section 19SDP-7-22, F38/2; (4) PB202101, thin section 21LHK-1-3, O44.

Problematic microfossils (Fig. 38).—There are some problematic microfossils not readily assigned to any of the groups described above. One is a branching filamentous microfossil that appears to branch unidirectionally and dichotomously (Fig. 38.138.4). Its filament diameter is around 1.2 μm (0.8–2.1 μm, SD = 0.4 μm). At least two orders of branching can be observed, but segment lengths between the nodes are hard to measure because the specimen is preserved three-dimensionally, and nodes are captured at different focal levels. The relatively uniform and extremely thin filament diameter indicates a uniseriate rather than multiseriate construction, even though no cellular details are preserved in the available specimen.

Figure 38. Problematic microfossils. (1–4) Microfossil with branching filaments, PB202102, thin section 19SDP-3-14, H34/3, same area at different focal levels to show different branches and bifurcations; red arrowheads denote bifurcations. (5, 6) Polybessurus sp. (5) PB202103, thin section 21MJD-1-13, P37/2; (6) PB202104, thin section 19TP-1-25, M39/4.

Two specimens of Polybessurus sp. (Fig. 38.5, 38.6) were recovered from the Majindong section in basinal facies (the large one, Fig. 38.5) and the Tianping section in slope facies (the small one, Fig. 38.6). The larger specimen captured in thin section is about 0.7 mm wide and about 1.9 mm long, and the smaller one is about 30 μm wide and about 120 μm long. The smaller specimen from the Tianping section is similar to Polybessurus bipartitus Fairchild, Reference Fairchild1975, ex Green et al., Reference Green, Knoll, Golubic and Swett1987, but here we follow Ouyang et al. (Reference Ouyang, Zhou, Pang and Chen2022) and place all Polybessurus specimens from the Doushantuo Formation in an open nomenclature. As discussed by Ouyang et al. (Reference Ouyang, Zhou, Pang and Chen2022), Polybessurus likely represent a biogenic structure formed by various microorganisms that share a similar movement or migration mechanism, and thus is here considered as a problematic microfossil.

Occurrence of Doushantuo acanthomorphs based on taxonomically revised records

Together with fossil data presented in this study, the taxonomically revised dataset contains 49 genera and 160 species reported from the Doushantuo Formation (Table 3). Taxonomic diversity is greatest in the shelf-lagoon environment: about 89% of the genera and 84% of the species (44 genera and 135 species) have been reported from shelf-lagoon settings. Only about 10% of the genera and 3% of the species (5 genera and 5 species) are documented in the basinal environment (Fig. 39). Because the presence of Appendisphaera grandis in the basinal facies is solely based on its occurrence at the Jinshichong section, the taxonomic richness of acanthomorphs in basinal facies would be even lower if the Jinshichong section were actually classified as the platform environment (see “Geological setting” for the uncertainty about the depositional environment of the Jinshichong section). Regardless, all taxa from slope and basinal facies (except new species) also occur in inner shelf, shelf-lagoon, or shelf margin facies. Among the five species that are present in the basinal facies, A. grandis and Tianzhushania spinosa are among the most widely distributed and the longest-ranging taxa across all facies in South China. Tanarium pilosiusculum, Asterocapsoides wenganensis, and Mengeosphaera mamma also occur in other facies.

Table 3. Paleoenvironmental distribution of reported acanthomorphic acritarchs from the Doushantuo Formation in South China. Numbers in each cell refer to data sources, as detailed below. Hashtag sign (#) indicates that the reported specimen was mistakenly assigned to Briareus vasformis Liu and Moczydłowska, Reference Liu and Moczydłowska2019, by Ouyang et al. (Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021), and should be B. robustus Liu and Moczydłowska, Reference Liu and Moczydłowska2019. Data sources shown in the table: (1) This study. (2) Yin and Li, Reference Yin and Li1978. (3) Awramik et al., Reference Awramik, McMenamin, Yin, Zhao, Ding and Zhang1985. (4) Chen and Liu, Reference Chen and Liu1986. (5) Yin, Reference Yin1987. (6) Yin and Liu, Reference Yin, Liu, Zhao, Xing, Ding, Liu, Zhao, Zhang, Meng, Yin, Ning and Han1988. (7) Yin, Reference Yin1990. (8) Yin et al., Reference Yin, Xue and Yuan1990. (9) Yin and Xue, Reference Yin and Xue1993. (10) Yuan et al., Reference Yuan, Wang and Zhang1993. (11) Xue et al., Reference Xue, Tang, Yu and Zhou1995. (12) Yin, Reference Yin1996. (13) Yuan and Hofmann, Reference Yuan and Hofmann1998. (14) Zhang et al., Reference Zhang, Yin, Xiao and Knoll1998. (15) Xiao and Knoll, Reference Xiao and Knoll1999. (16) Yin, Reference Yin1999. (17) Xiao and Knoll, Reference Xiao and Knoll2000. (18) Yin, Reference Yin2001. (19) Yin et al., Reference Yin, Gao and Xing2001. (20) Zhou et al., Reference Zhou, Brasier and Xue2001. (21) Zhou et al., Reference Zhou, Chen and Xue2002. (22) Yin et al., Reference Yin, Gao and Yue2003. (23) Xiao, Reference Xiao2004b. (24) Yin et al., Reference Yin, Bengtson and Yue2004. (25) Zhou et al., Reference Zhou, Yuan, Xiao, Chen and Xue2004b. (26) Liu and Yin, Reference Liu and Yin2005. (27) Xiao et al., Reference Xiao, Hagadorn, Zhou and Yuan2007. (28) Yin et al., Reference Yin, Zhu, Knoll, Yuan, Zhang and Hu2007. (29) Zhou et al., Reference Zhou, Xie, McFadden, Xiao and Yuan2007. (30) Xie et al., Reference Xie, Zhou, Mcfadden, Xiao and Yuan2008. (31) Liu et al., Reference Liu, Yin, Gao, Tang and Chen2009. (32) McFadden et al., Reference McFadden, Xiao, Zhou and Kowalewski2009. (33) Yin et al., Reference Yin, Liu, Chen, Tang, Gao and Wang2009a. (34) Yin et al., Reference Yin, Liu, Gao, Tang and Chen2009b. (35) Chen et al., Reference Chen, Yin, Liu, Gao, Tang and Wang2010. (36) C. Yin et al., Reference Yin, Wang, Yuan and Zhou2011. (37) L. Yin et al., Reference Yin, Wang, Yuan and Zhou2011. (38) Liu et al., Reference Liu, Yin, Chen, Tang and Gao2012. (39) Wang et al., Reference Wang, Chen, Tang and Pang2012. (40) Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013. (41) Zeng et al., Reference Zeng, Chen, Li, Zhou, Zhang and Peng2013. (42) Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a. (43) Liu et al., Reference Liu, Chen, Zhu, Li, Yin and Shang2014b. (44) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014. (45) Ouyang et al., Reference Ouyang, Zhou, Guan and Wang2015. (46) Ye et al., Reference Ye, Tong, An, Tian, Zhao and Zhu2015. (47) Hawkins et al., Reference Hawkins, Xiao, Jiang, Wang and Shi2017. (48) Nie et al., Reference Nie, Liu and Dong2017. (49) Liu and Moczydłowska, Reference Liu and Moczydłowska2019. (50) Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019. (51) Shang et al., Reference Shang, Liu and Moczydłowska2019. (52) Shang and Liu, Reference Shang and Liu2020. (53) Yang et al., Reference Yang, Pang, Chen, Zhong and Yang2020. (54) Liu et al., Reference Liu, Qi, Fan, Guo and Pei2021. (55) Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021. (56) Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022.

Figure 39. Comparison of acanthomorph diversity among different depositional facies at species and genus levels.

Sampling bias and rarefaction analysis

As shown in Table 2, there are notable variations in the number of fossiliferous samples and the number of acanthomorph specimens recovered from Doushantuo sections. A rarefaction analysis was carried out to correct such sampling bias. Raw abundance data of acanthomorphs from the Caojunba, Caowan, Lujiayuanzi, and Siduping sections (this study), together with previously published abundance data from six localities in inner shelf (the Bailu section, Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019; the Lianhua section, Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022) and shelf-lagoon facies (the Liujing section, Shang et al., Reference Shang, Liu and Moczydłowska2019; the Jiulongwan, Jinguadun, and Wuzhishan sections, Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021) were selected for the rarefaction analysis. The rarefaction curves are shown in Figure 40. With the exception of the Lianhua section in the Shennongjia area representing the inner shelf facies, none of the rarefaction curves reaches a clear asymptote, indicating that current sampling intensity is inadequate and greater taxonomic richness would be expected with additional sampling in the future.

Figure 40. Rarefaction analysis of Doushantuo acanthomorphs. (1) Rarefaction curves with 1σ error bars of Doushantuo acanthomorph assemblages published with abundance data from 10 sections in inner shelf, shelf-lagoon, and slope facies. (2) Magnification of gray box in bottom-left of (1), showing rarefied species richness with subsampled size of 1–40 specimens. Sample sizes of Lianghekou section and basinal facies sections are small, therefore they were not rarefied. Rather, observed specimen number and species richness are plotted for Lianghekou section and pooled basinal facies data.

NMDS analysis

To visualize the similarity and difference in taxonomic composition of different acanthomorph collections from different facies, stratigraphic intervals, and localities, an NMDS analysis was conducted on the acanthomorph occurrence data from 82 collections (see Methods for how a collection is defined and see Supplemental Materials for data). The NMDS results are shown in Figure 41 (grouped by depositional facies in Fig. 41.1 and by both depositional facies and stratigraphic intervals in Fig. 41.2). The stress value of the NMDS analysis is 0.13, indicating acceptable representation of ranked distances by the NMDS results (Clarke, Reference Clarke1993).

Figure 41. Taxonomic ordination plots based on NMDS analysis of taxonomically updated occurrence data from 82 collections of Doushantuo acanthomorphs in South China (see Supplemental Materials for data). (1) NMDS scatter plots and convex hulls differentiated by depositional facies. (2) NMDS scatter plots and convex hulls differentiated by depositional facies and stratigraphic intervals. (3) Species loading diagram. Note that some species are not labeled because of the limited space; see Supplemental Materials for loading data. Red and green circled points represent eponymous species of the lower and upper biozones of the Doushantuo Formation (Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Chen, Zhu, Li, Yin and Shang2014b; Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014), respectively. Blue filled points represent eponymous species of the biozones of Liu and Moczydłowska (Reference Liu and Moczydłowska2019). See Figure 42 for abbreviations.

The NMDS plots visualize the taxonomic similarity among different facies or different stratigraphic intervals. In Figure 41.1, for example, the convex hulls for the slope and basinal facies are completely nested within those of the shelf margin and shelf-lagoon facies, consistent with the observation that acanthomorph taxa from the former are also found in the latter. Among the inner shelf, shelf-lagoon, and shelf margin facies, the convex hulls show a notable degree of overlap, indicating a number of shared taxa. On the other hand, as shown in Figure 41.2, the convex hulls for Member II and Member III in the shelf-lagoon facies are completely separated, indicating that these two stratigraphic intervals contain taxonomically distinct acanthomorphs.

Network analysis

To further visualize the shared taxonomic occurrences among different acanthomorph collections, we carried out a network analysis of the same dataset used in the NMDS analysis (see Supplemental Materials for data). The bipartite network (Fig. 42) shows that collections from the inner shelf facies (yellow and light blue symbols) and shelf margin facies (orange symbols) are linked to taxa such as Megasphaera inornata and M. ornata, collections from Member II in shelf-lagoon facies (red symbols) are linked to taxa such as Tianzhushania and Yinitianzhushania tuberifera (Yin, Gao, and Xing, Reference Yin, Gao and Xing2001) Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014, and collections from Member III in shelf-lagoon facies (green symbols) are linked to numerous taxa, including various species of Hocosphaeridium and Tanarium.

Figure 42. Bipartite network analysis of the same dataset of Doushantuo acanthomorph occurrences used in NMDS analysis (Fig. 41; see Supplemental Materials for data). Lettered nodes represent acritarch species. Numbered and colored nodes represent collections, with numbers matching source reference numbers in Table 3, and colors matching those of Figure 41.2: red = Member II of the Doushantuo Formation, shelf lagoon; green = Member III of the Doushantuo Formation, shelf lagoon; gray = stratigraphic interval not specified, shelf lagoon; yellow = correlated with upper Member II in shelf-lagoon facies, inner shelf (the Zhangcunping and Shennongjia areas); light blue = stratigraphic correlation relationship unclear, inner shelf (other areas such as Baokang, Chadian, and Chaoyang); orange = correlated with upper Member II or Member II–III transitional interval in shelf-lagoon facies, shelf margin (the Weng'an area); olive = roughly correlated with Member III in shelf-lagoon facies, shelf margin (the Caojunba section); lime, Doushantuo Formation, upper slope (the Lujiayuanzi section); blue = correlated with Member II in shelf-lagoon facies, slope (the Zhangjiajie area); dark blue = basinal facies. Each species is linked to a collection by a straight line if the species is present in the collection. Each acritarch taxon is linked to collections in which it is present. The network shows variation in occurrence frequency among acritarch species of the Doushantuo Formation. Species in the central area of the network generally occur in a greater number of areas, stratigraphic intervals, or studies, than species in the periphery area of the network. Abbreviations: CY-Changyang area, YG-Yangtze Gorges area. Species abbreviations: Alm = Alicesphaeridium medusoidum; Anm = Ancorosphaeridium magnum; Ani = Annularidens inconditus; Apob = Apodastoides basileus; Apa = Appendisphaera anguina; Apc1 = Appendisphaera clava; Apc2 = Appendisphaera clustera; Apf = Appendisphaera fragilis; Apg = Appendisphaera grandis; Aph1 = Appendisphaera heliaca; Apl1 = Appendisphaera lemniscata; Apl2 = Appendisphaera longispina; Apl3 = Appendisphaera longitubularis; Apm = Appendisphaera magnifica; Aps = Appendisphaera setosa; Apt1 = Appendisphaera tabifica; Apt2 = Appendisphaera tenuis; Apb = Appendisphaera? brevispina; Aph2 = Appendisphaera? hemisphaerica; Assd = Asseserium diversum; Assf = Asseserium fusulentum; Astf = Asterocapsoides fluctuensis; Astr = Asterocapsoides robustus; Asts = Asterocapsoides sinensis; Astw = Asterocapsoides wenganensis; Bab = Bacatisphaera baokangensis; Bas = Bacatisphaera sparga; Bip = Bispinosphaera peregrina; Biv = Bispinosphaera vacua; Brb = Briareus borealis; Brr = Briareus robustus; Brv = Briareus vasformis; Buc = Bullatosphaera? colliformis n. sp.; Calx = Calyxia xandaros; Caa = Cavaspina acumincata; Cab = Cavaspina basiconica; Cac = Cavaspina conica; Cau = Cavaspina uria; Cavc = Caveasphaera costata; Ceg = Ceratosphaeridium glaberosum; Crc = Crassimembrana crispans; Crm = Crassimembrana multitunica; Crip = Crinita paucispinosa; Cyf = Cymatiosphaeroides forabilatus; Cyk = Cymatiosphaeroides kullingii; Cyy = Cymatiosphaeroides yinii; Dici = Dicrospinasphaera improcera; Dicv = Dicrospinasphaera virgata; Dicz = Dicrospinasphaera zhangii; Disj = Distosphaera jinguadunensis; Diss = Distosphaera speciosa; Disc = Distosphaera? corniculata; Dub = Duospinosphaera biformis; Dus = Duospinosphaera shennongjiaensis; Eoa = Eotylotopalla apophysa; Eoda = Eotylotopalla dactylos; Eode = Eotylotopalla delicata; Eoi = Eotylotopalla inflata n. sp.; Eoq = Eotylotopalla quadrata; Eos = Eotylotopalla strobilata; Erc = Ericiasphaera crispa; Erd = Ericiasphaera densispina; Erf = Ericiasphaera fibrilla; Erm = Ericiasphaera magna; Err = Ericiasphaera rigida; Ers1 = Ericiasphaera sparsa; Ers2 = Ericiasphaera spjeldnaesii; Esg = Estrella greyae; Esr = Estrella recta; Gyp = Gyalosphaeridium pulchrum; Hew = Helicoforamina wenganica; Hoa = Hocosphaeridium anozos; Hod = Hocosphaeridium dilatatum; Hos = Hocosphaeridium scaberfacium; Knb = Knollisphaeridium bifurcatum; Knc = Knollisphaeridium coniformum; Knd = Knollisphaeridium denticulatum; Knl = Knollisphaeridium longilatum; Knm = Knollisphaeridium maximum; Kno = Knollisphaeridium obtusum; Knp = Knollisphaeridium parvum; Knt = Knollisphaeridium triangulum; Lac = Laminasphaera capillata; Mac = Matosphaera changyangensis; Megc = Megasphaera cymbala; Megi = Megasphaera inornata; Mego = Megasphaera ornata; Megp1 = Megasphaera patella; Megp2 = Megasphaera puncticulosa; Memf = Membranosphaera formosa; Mea = Mengeosphaera angusta; Meb = Mengeosphaera bellula; Mech = Mengeosphaera chadianensis; Meco = Mengeosphaera constricta; Mee = Mengeosphaera eccentrica; Mef = Mengeosphaera flammelata; Meg1 = Mengeosphaera gracilis; Meg2 = Mengeosphaera grandispina; Mela = Mengeosphaera latibasis; Melu = Mengeosphaera lunula; Mem1 = Mengeosphaera mamma; Mem2 = Mengeosphaera matryoshkaformis; Mem3 = Mengeosphaera membranifera; Mem4 = Mengeosphaera minima; Mer = Mengeosphaera reticulata; Mesp = Mengeosphaera spinula; Mest = Mengeosphaera stegosauriformis; Meu = Mengeosphaera uniformis; Mup = Multifronsphaeridium pelorium; Mur = Multifronsphaeridium ramosum; Pab = Papillomembrana boletiformis; Pac = Papillomembrana compta; Poc = Polygonium cratum; Sia = Sinosphaera asteriformis; Sie = Sinosphaera exilis; Sir = Sinosphaera rupina; Sis = Sinosphaera speciosa; Siv = Sinosphaera variabilis; Spb = Spiralicellula bulbifera; Tael = Taedigerasphaera lappacea; Taa = Tanarium acus; Tac1 = Tanarium capitatum; Tac2 = Tanarium columnatum; Tac3 = Tanarium conoideum; Tac4 = Tanarium cuspisatum; Tad = Tanarium digitiforme; Tae = Tanarium elegans; Tag = Tanarium gracilentum; Tai = Tanarium irregulare; Tami = Tanarium minimum; Tamu = Tanarium muntense; Tao = Tanarium obesum; Tap1 = Tanarium paucispinosum; Tap2 = Tanarium pilosiusculum; Tap3 = Tanarium pluriprotensum; Tap4 = Tanarium pycnacanthum; Tatr = Tanarium triangulare; Tatu = Tanarium tuberosum; Tau = Tanarium uniformum; Tava = Tanarium varium; Tavi = Tanarium victor; Tip = Tianzhushania polysiphonia; Tir = Tianzhushania rara; Tis = Tianzhushania spinosa; Scz = Schizofusa zangwenlongii; Urc = Urasphaera capitalis; Urf = Urasphaera fungiformis; Urn = Urasphaera nupta; Vaf = Variomargosphaeridium floridum; Vag = Variomargosphaeridium gracile; Val = Variomargosphaeridium litoschum; Vav = Variomargosphaeridium varietatum; Vem = Verrucosphaera minima; Veu = Verrucosphaera? undulata n. sp.; Web = Weissiella brevis; Wec = Weissiella concentrica; Weg = Weissiella cf. W. grandistella; Xel = Xenosphaera liantuoensis; Yit = Yinitianzhushania tuberifera; Yur = Yushengia ramispinsa.

The position of a species in the network generally reflects its occurrence frequency recorded in the Doushantuo Formation. The closer to the center of the network, the more likely a species occurs in a greater number of areas, stratigraphic intervals, or studies. For example, Appendisphaera grandis is located near the center of the network, consistent with its wide paleogeographic distribution and long stratigraphic ranges. Similarly, many species of Cavaspina, Eotylotopalla, Hocosphaeridium, and Tanarium are also placed near the center of the network, indicating their wide paleogeographic and stratigraphic occurrences. Species in the periphery of the network are those with limited occurrences, and these include numerous taxa (e.g., Ceratosphaeridium glaberosum Grey, Reference Grey2005; Schizofusa zangwenlongii Grey, Reference Grey2005; Xenosphaera liantuoensis Yin, Reference Yin1987, emend. Liu et al., Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) that were only found in the shelf-lagoon facies in the Yangtze Gorges area by Liu and Moczydłowska (Reference Liu and Moczydłowska2019).

Discussion

Taxonomic richness of the Doushantuo microfossils

At the level of major morphological groups, Doushantuo microfossils from different facies do not show substantial differences. Acanthomorphs, sphaeromorphs, and filamentous microfossils occur in all facies from the shallow-water inner shelf to the deep-water basin. Tubular microfossils and Polybessurus that are relatively rare in shallow-water facies also occur at the basinal Majindong section, despite the limited sampling intensity at this section. However, multicellular algae and coccoid microfossils, which are present in shallow-water and slope facies, are absent in basinal facies. This difference could be related to the low sampling intensity in basinal facies or ecological restriction (i.e., these microfossils may represent benthic photosynthetic organisms and thus may have been ecologically restricted to the photic zone). Overall, with the exception of multicellular algae and coccoid microfossils, the major morphological groups of Doushantuo microfossils have a wide distribution across different facies, either because many of them were planktonic organisms (e.g., acanthomorphic acritarchs, Butterfield and Rainbird, Reference Butterfield and Rainbird1998; Moczydłowska, Reference Moczydłowska2016) or because reworking and transportation may have homogenized their paleoenvironmental distribution (e.g., benthic microfossils ecologically restricted to shallow-water facies may have been reworked and transported to slope and basinal facies as microbial mat fragments or olistostromes).

At face value, genus- and species-level taxonomic richness of acanthomorphic acritarchs varies notably among facies (Fig. 39). Taxonomic richness in shelf-lagoon facies is nearly 9× and 27× that in basinal facies at the genus and species levels, respectively; these numbers would be greater if Appendisphaera grandis from the Jinshichong section were excluded from basinal facies (see “Geological Setting” for uncertainty about depositional environment of the Jinshichong section). This difference in taxonomic richness of acanthomorphs is at least partly related to the unequal sampling intensities among localities and facies, since the shelf-lagoon facies, especially in the Yangtze Gorges area, is much more intensively sampled in previous studies than other facies.

The rarefaction analysis supports sampling intensity as a major driver of the observed difference in taxonomic richness of acanthomorphs. The rarefaction curves show that the sampling intensity at the slope–basinal sections surveyed in this study is far from sufficient. However, when compared at a similar subsampling intensity (e.g., number of specimens < 20), species richness at the Caojunba, Caowan, and Lujiayuanzi sections is comparable to the rarefied species richness in most inner shelf and shelf-lagoon sections (Fig. 40.2). Similarly, total species richness of the Lianghekou section and of the pooled basinal data (hollow square and circle in Fig. 40.2, respectively) is also comparable to that of other sections and other facies at a comparable sampling intensity. Therefore, sampling bias plays an important role driving the variation of acanthomorph taxonomic richness across different facies.

Sampling bias is not the only factor affecting the observed variation in taxonomic richness of Doushantuo acanthomorphs across different facies. Taphonomic bias could be another crucial factor. Doushantuo microfossils are preserved through silicification and phosphatization, which are taphonomic windows controlled by environmental conditions and may not be equally represented in different facies. For example, Muscente et al. (Reference Muscente, Hawkins and Xiao2015) argued that in-situ chert nodule formation is facilitated by local ferruginous conditions and is expected to be rare in euxinic slope to basinal environments. Although this study does reveal the occurrence of chert nodules in the basinal facies, they are rare and restricted in stratigraphic distribution, probably because the early Ediacaran geochemical conditions in these areas were generally unfavorable and only occasionally conducive to chert nodule formation. As a result, silicification in slope and basinal facies favors stratigraphically long-ranging taxa that, relative to short-ranging taxa, would be more likely to be captured by rare chert nodules. In addition, diagenetic and metamorphic processes can also bias microfossil preservation in different facies, because the Doushantuo Formation in slope and basinal facies experienced stronger metamorphism during Paleozoic tectonic activities in the southeastern side of the South China block (Li et al., Reference Li, Li, Wartho, Clark, Li, Zhang and Bao2010). As a result, severe recrystallization of micro-quartz and high degree of thermal maturity of organic material may have led to the generally poor preservation of Doushantuo microfossils in the studied areas in Hunan Province. Raman spectroscopic analysis also shows that organic material in silicified microfossils from the Doushantuo Formation at the Tianping section underwent a higher degree of thermal alteration than in the Yangtze Gorges area (Shang et al., Reference Shang, Moczydłowska, Liu and Liu2018, Reference Shang, Liu and Liu2020), which may have contributed to the poor preservation and low abundance of microfossils in the Zhangjiajie area.

Additionally, the different fossil preparation and identification approaches in a study of silicified and phosphatized microfossils may also lead to systematic biases. For example, Doushantuo microfossils in shelf-lagoon, slope, and basinal facies are preserved exclusively in chert nodules, and they can be observed only in thin sections. It is difficult in thin sections to recognize taxa characterized by certain vesicle surface sculptures that can be identified on extracted specimens under SEM (e.g., phosphatized Helicoforamina Wang et al., Reference Wang, Chen, Tang and Pang2012; Spiralicellula Xue et al., Reference Xue, Tang and Yu1992, emend. Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014; some species of Megasphaera), which are abundant in inner shelf and shelf-margin facies where three-dimensionally phosphatized microfossils can be extracted from dolomitic phosphorites by acid maceration (Xiao and Knoll, Reference Xiao and Knoll1999; Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014). On the other hand, internal structures, such as the hollow processes embedded within outer membranes of Tianzhushania and cross-walls in processes of Weissiella, cannot be observed on the macerated specimens preserved in phosphorites. Of course, such biases can be mitigated by combining observations of thin sections and macerated specimens, but this is only practical for phosphatized microfossils.

Taxonomic distribution of the Doushantuo acanthomorphs

Unlike taxonomic richness, which shows considerable difference among facies, the NMDS results indicate that the different facies have a number of shared taxa. In other words, the taxonomic occurrence of acanthomorphs is not strongly controlled by facies, particularly among inner shelf, shelf-lagoon, and shelf marine facies where sampling intensity is relatively good (Fig. 40). This is an encouraging sign for acanthomorph-based biostratigraphic correlation. The similarity in species composition between the inner shelf and shelf-margin facies is further bolstered by their similar stratigraphic distribution of microfossils—most acanthomorphs in these facies come from strata correlated with upper Member II (Zhou et al., Reference Zhou, Li, Xiao, Lan, Ouyang, Guan and Chen2017; Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019; Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022).

Taxonomic compositions in different facies may have also been affected by taphonomic biases. This can be best illustrated by the shelf margin facies, which has less than half the number of species in the shelf-lagoon facies (Fig. 39), but occupies a larger convex hull in the taxonomic ordination space (Fig. 41.1). The contrast between taxonomic richness and taxonomic ordination may be driven by the existence of two taphonomic windows (silicification or phosphatization) in the shelf margin facies (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014), particularly if microfossil assemblages of different preservation modes may be taxonomically distinct (i.e., everything else being equal, two assemblages with different taphonomic modes would share fewer taxa than two with the same taphonomic mode). A similar explanation may also be applied to the inner shelf facies, which has much lower taxonomic richness than the shelf-lagoon facies (Fig. 39), but occupies a convex hull of a similar size (Fig. 41.1), perhaps due to the low availability of both silicification and phosphatization modes in the inner shelf facies (e.g., Zhou et al., Reference Zhou, Brasier and Xue2001).

When grouped by stratigraphic intervals, the acanthomorph collections show clear separation on the ordination space (Fig. 41.2), indicating greater difference in taxonomic composition of acanthomorphs between stratigraphic horizons than among depositional facies. Importantly, there is complete separation between Member II and Member III in shelf-lagoon facies (Fig. 41.2, red and green symbols, respectively), indicating different species composition between the two intervals in shelf-lagoon facies. In the shelf-lagoon Yangtze Gorges area, taxonomic difference in acanthomorphs between the two lithostratigraphic units has been recognized in numerous previous studies (e.g., taxonomic diversity and evenness, Zhou et al., Reference Zhou, Xie, McFadden, Xiao and Yuan2007; quantitative evaluation, McFadden et al., Reference McFadden, Xiao, Zhou and Kowalewski2009; presence/absence of key taxa, Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013). Member II and Member III of the Doushantuo Formation were deposited in early and middle Ediacaran, respectively (Zhou et al., Reference Zhou, Li, Xiao, Lan, Ouyang, Guan and Chen2017, Reference Zhou, Yuan, Xiao, Chen and Hua2019; Sui et al., Reference Sui, Huang, Zhang, Wang, Ogg and Kemp2018, Reference Sui, Huang, Zhang, Wang and Ogg2019; Li et al., Reference Li, Zhang, Han, Zhong, Ding, Wu and Liu2022), and taxonomic difference in acanthomorph composition likely reflects evolutionary changes in eukaryote diversity in early–middle Ediacaran oceans, possibly driven by oceanic oxygenation events, as recorded in various geochemical proxies (e.g., McFadden et al., Reference McFadden, Huang, Chu, Jiang, Kaufman, Zhou, Yuan and Xiao2008; Chen et al., Reference Chen, Hu, Mills, He and Andersen2022).

NMDS results are consistent with published correlations of acritarch assemblages across different facies. Acanthomorph convex hull for the inner shelf Zhangcunping and Shennongjia areas (Fig. 41.2, yellow symbols) largely overlap with the convex hull for shelf-lagoon Member II acanthomorphs, confirming the proposed biostratigraphic correlation of the Zhangcunping and Shennongjia assemblages with upper Member II acanthormophs in the Yangtze Gorges area (Ouyang et al., Reference Ouyang, Zhou, Xiao, Chen and Shao2019; Ye et al., Reference Ye, Li, Tong, An, Hu and Xiao2022). The Weng'an convex hull (Fig. 41.2, orange symbols) overlaps with those of members II and III in the shelf-lagoon facies, supporting the inference that the Weng'an biota represents a transitional stage between the assemblages in Member II and Member III of the Doushantuo Formation in shelf-lagoon facies (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014). The Lujiayuanzi and Caojunba assemblages (Fig. 41.2, lime and olive symbols, respectively) plot near the convex hull of the shelf lagoon Member III assemblage, which also agrees with their possible biostratigraphic correlation (Ouyang et al., Reference Ouyang, Guan, Zhou and Xiao2017; Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022).

Biostratigraphic implications

Spatial and stratigraphic distribution of acanthomorphs discussed above provides useful insights into the biostratigraphic study of the Doushantuo Formation. Previously proposed biozonation schemes for the Doushantuo Formation are based primarily on fossil data from the shelf-lagoon facies in the Yangtze Gorges area, supplemented with data from the shelf margin facies in the Weng'an area (C. Yin et al., Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011; Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013; Liu and Moczydłowska, Reference Liu and Moczydłowska2019). However, if these biozones are to play a greater role in the subdivision and correlation of the Ediacaran System on a global scale (Liu et al., Reference Liu, Chen, Zhu, Li, Yin and Shang2014b; Xiao et al., Reference Xiao, Narbonne, Zhou, Laflamme, Grazhdankin, Moczydlowska-Vidal and Cui2016; Liu and Moczydłowska, Reference Liu and Moczydłowska2019; Xiao and Narbonne, Reference Xiao, Narbonne, Gradstein, Ogg, Schmitz and Ogg2020), we need to affirm that they are independent of depositional facies.

One biozonal scheme was established on taxonomic difference between Member II and Member III in the Yangtze Gorges area (C. Yin et al., Reference Yin, Liu, Chen, Tang, Gao and Wang2009a, Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011; Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, Reference Liu, Chen, Zhu, Li, Yin and Shangb; Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014). In this scheme, two biozones (or two assemblages) were established based mainly on two genera, Tianzhushania and Hocosphaeridium. These two genera were once thought to be restricted to Member II and Member III, respectively, with their first appearance near the base of the respective members (Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, Reference Liu, Chen, Zhu, Li, Yin and Shangb), thus the two biozones were essentially range biozones (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014). However, these two genera were later known to co-exist at Weng'an (Xiao et al., Reference Xiao, Zhou, Liu, Wang and Yuan2014), and Hocosphaeridium has subsequently been reported from Member II or its equivalents at multiple localities (Hawkins et al., Reference Hawkins, Xiao, Jiang, Wang and Shi2017; Liu and Moczydłowska, Reference Liu and Moczydłowska2019; Liu et al., Reference Liu, Qi, Fan, Guo and Pei2021), thus the two biozones as originally proposed need revision. Nevertheless, these two genera both present in four of the five facies, thus are among the most widely distributed species in South China, allowing for potential application in biostratigraphic correlation across different facies.

An alternative biozonal scheme recently proposed by Liu and Moczydłowska (Reference Liu and Moczydłowska2019) includes four biozones. Each of the four biozones is defined by the FAD (first appearance datum) of two or three acritarch species, with the lower three biozones corresponding to Member II in the Yangtze Gorges area, and the uppermost biozone corresponding to Member III. However, many of these eponymous species are rare, even in the Yangtze Gorges area (Table 4), and it is extremely difficult to document the co-existence of two or three rare eponymous species, making these biozones impractical. In addition, although many eponymous species of these zones were selected for their global distribution, some of them (e.g., Ceratosphaeridium glaberosum and Schizofusa zangwenlongii) are only known from shelf-lagoon facies in South China, implying their possible facies-dependent paleoenvironmental distribution.

Table 4. Occurrence of eponymous species of the two previously proposed biozonation schemes for the Doushantuo Formation in South China. Abbreviations for biozones: A1 = Tianzhushania spinosa zone of Liu et al. (Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) and Xiao et al. (Reference Xiao, Zhou, Liu, Wang and Yuan2014), corresponding to Member II in the Yangtze Gorges area; A2 = Hocosphaeridium anozos Zone (or the Tanarium conoideumHocosphaeridium scaberfaciumH. anozos Zone) of Liu et al. (Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a) and Xiao et al. (Reference Xiao, Zhou, Liu, Wang and Yuan2014), corresponding to Member III in the Yangtze Gorges area; B1 = Appendisphaera grandisWeissiella grandistellaTianzhushania spinosa Zone of Liu and Moczydłowska (Reference Liu and Moczydłowska2019), corresponding to lowermost Member II in the Yangtze Gorges area; B2 = Tanarium tuberosumSchizofusa zangwenlongii Zone of Liu and Moczydłowska (Reference Liu and Moczydłowska2019), corresponding to lower–middle Member II in the Yangtze Gorges area; B3 = Tanarium conoideumCavaspina basiconica Zone of Liu and Moczydłowska (Reference Liu and Moczydłowska2019), corresponding to middle–upper Member II in the Yangtze Gorges area; B4 = Tanarium pycnacanthumCeratosphaeridium glaberosum Zone of Liu and Moczydłowska (Reference Liu and Moczydłowska2019), corresponding to lower Member III in the Yangtze Gorges area.

Notes for superscripts: (1) Liu and Moczydłowska (Reference Liu and Moczydłowska2019) synonymized Tanarium obesum with T. tuberosum and proposed the latter to define the biozone, so the occurrence of T. tuberosum here also includes occurrence of T. obesum. (2) These three studies in the Zhangjiajie area all correlated their sampling horizons to Member II of the Doushantuo Formation in the Yangtze Gorges area. (3) Liu and Moczydłowska (Reference Liu and Moczydłowska2019) synonymized Weissiella brevis with W. grandistella, the latter of which is an eponymous taxon of their Appendisphaera grandisWeissiella grandistellaTianzhushania spinosa Assemblage Zone, so the occurrence of W. grandistella here also includes occurrence of W. brevis. See Systematic paleontology for taxonomic comments.

The current situation of Doushantuo acanthomorph biostratigraphy illustrates two challenges in the establishment of regionally recognizable biozones. On one hand, stratigraphically short-ranging taxa such as Ceratosphaeridium glaberosum and Tanarium pycnacanthum are generally rare in abundance, hampering their application in cross-facies correlation of strata where overall acritarch abundance is low. As visualized in the network diagram (Fig. 42), these species are mostly placed in the margin and most of them are each linked to only one edge. On the other hand, facies-independent taxa typically have a relatively long stratigraphic range, making them less useful in range biozones (Xiao et al., Reference Xiao, Jiang, Ye, Ouyang, Banerjee, Singh, Muscente, Zhou and Hughes2022), although their FADs can still be useful in defining acanthomorph biozones. These species include Appendisphaera grandis, Eotylotopalla dactylos, Hocosphaeridium anozos, and Tanarium conoideum. These species are placed in the center of the network diagram (Fig. 42) and are each linked to multiple localities, facies, or stratigraphic horizons.

The challenges identified above can be addressed in multiple ways. First, we need to considerably improve the sampling intensity of Doushantuo acanthomorphs. As shown in the rarefaction analysis, the current sample size at most Doushantuo localities is inadequate, thus it is likely that many widely distributed taxa, including those with short stratigraphic ranges, have not been documented. With increasing sampling intensity, we anticipate that stratigraphically useful species will turn up in slope and basinal facies, which are the least-sampled facies at the present. Second, when defining acanthomorph biozones, we should favor the FADs (over the stratigraphic ranges) of widely and abundantly distributed taxa. Third, the recognition of acanthomorph biozones should be supplemented by abundance data of taxa with long stratigraphic ranges and wide paleoenvironmental distributions (Shi et al., Reference Shi, Ouyang, Zhou, Xiao, Chen and Guan2022). Dominant or abundant taxa of Member II or Member III of the Doushantuo Formation in the Yangtze Gorges area have been described qualitatively in the literature (e.g., C. Yin et al., Reference Yin, Liu, Awramik, Chen, Tang, Gao, Wang and Riedman2011; Liu et al., Reference Liu, Yin, Chen, Tang and Gao2013, Reference Liu, Xiao, Yin, Chen, Zhou and Li2014a, Reference Liu, Chen, Zhu, Li, Yin and Shangb; Ouyang et al., Reference Ouyang, Zhou, Xiao, Guan, Chen, Yuan and Sun2021), but quantitative studies are few (McFadden et al., Reference McFadden, Xiao, Zhou and Kowalewski2009). We are optimistic that more data and quantitative analyses will eventually lead to more robust acanthomorph biozonation in South China.

The newly discovered acanthomorphs from the Lianghekou section in the basinal facies illustrate the biostratigraphic importance of Tianzhushania. In the basinal facies, the Doushantuo Formation is thin and dominated by black shales with sporadic carbonate horizons, thus hindering lithostratigraphic and δ13C chemostratigraphic correlation with the shelf facies (Jiang et al., Reference Jiang, Kaufman, Christie-Blick, Zhang and Wu2007, Reference Jiang, Shi, Zhang, Wang and Xiao2011). At the Lianghekou section, Tianzhushania spinosa is found in a fossiliferous horizon of the middle Doushantuo Formation, supporting a correlation with Member II in shelf-lagoon facies, since T. spinosa is an eponymous species of the lower biozone in Member II and has never been reported from Member III in shelf-lagoon facies. This can be seen as an example of how the currently recognized biozones may contribute to regional correlation of the Doushantuo Formation despite the challenges discussed above.

Conclusions

Silicified microfossils, including sphaeromorphic and acanthomorphic acritarchs, multicellular algae, tubular microfossils, and other problematic forms, are reported from the Doushantuo Formation in a shelf margin–slope–basin transect in Hunan Province, South China. Of these fossils, acanthomorphic acritarchs are reported from the basinal facies for the first time. Fifteen genera and 29 species, including three new species, Bullatosphaera? colliformis n. sp., Eotylotopalla inflata n. sp., and Verrucosphaera? undulata n. sp., and six unnamed forms of acanthomorphic acritarchs are identified and systematically described.

A taxonomically revised dataset of Doushantuo acanthomorphic acritarchs was compiled. Rarefaction, NMDS, and network analyses of this dataset reveal the following five conclusions. (1) To date, 49 genera and 160 species of Ediacaran acanthomorphic acritarchs (including Schizofusa zangwenlongii) have been reported from the five depositional facies and 10 areas in South China. Sampling intensity is uneven across different localities and facies, and inadequate at most localities, indicating that new taxa and new occurrences are likely to be recovered with additional sampling. (2) Observed taxonomic richness varies significantly among facies, mainly due to sampling and taphonomic biases. Rarefaction analysis shows that, when compared at a similar sampling intensity, taxonomic richness among different sections is more or less comparable. (3) NMDS analysis shows that stratigraphic succession plays a greater role than facies in controlling the distribution of Doushantuo acanthomorphs, confirming the distinction of acanthomorph assemblages in Member II and Member III of the Doushantuo Formation in shelf-lagoon facies. (4) NMDS results are consistent with lithostratigraphic correlations of the Doushantuo Formation across different facies, reinforcing that the Weng'an biota is transitional between Member II and Member III assemblages in shelf-lagoon facies, that the Zhangcunping and Shennongjia assemblages are correlated with the upper Member II assemblage, and that the Caojunba assemblage is correlated with the Member III assemblage. (5) More intensive sampling of Doushantuo acanthomorphs is needed to establish regional biozones that can be defined by the FADs of widely distributed taxa and characterized by the relative abundance of common taxa.

Acknowledgments

The research was funded by the National Key Research and Development Program of China (2021YFA0718100 and 2022YFF0802700 to QO), the National Natural Science Foundation of China (41902006 and 42272012 to QO, 41921002 to CZ), the US National Science Foundation (EAR-2021207 to SX), and State Key Laboratory of Biogeology and Environmental Geology (GBL22106 to QO). We thank journal editors S. Zamora and A. Liu, as well as reviewer S. Willman and an anonymous reviewer, for constructive comments that helped improve this paper.

Declaration of competing interests

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Data availability statement

Data available from the Dryad Digital Repository: http://doi.org/10.5061/dryad.7d7wm3822.

Data archiving statement

This published work and the nomenclatural acts it contains, have been registered in ZooBank: http://zoobank.org/References/6FC92858-4054-4117-8043-1F06CFE77155

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Figure 0

Figure 1. Ediacaran paleogeography and Proterozoic outcrop distribution in Hunan Province of South China. (1) Paleogeographic map of the Yangtze block during deposition of the Doushantuo Formation (modified from Jiang et al., 2011). Rectangle frame marks the location of (2). (2) Simplified geological map (modified from Luo et al., 2002) showing the distribution of Proterozoic strata in northern Hunan Province where the studied sections are located. Section abbreviations: CJB, Caojunba; LJYZ, Lujiayuanzi; HP, Heping; TP, Tianping; CW, Caowan; SDP, Siduping; MJD, Majindong; LHK, Lianghekou; JSC, Jinshichong.

Figure 1

Figure 2. (1) Lithostratigraphic sequence of the Doushantuo Formation at studied localities, acanthomorph-bearing sampling horizons, and their correlations with those in the Yangtze Gorges area (represented by the Jiulongwan section). Lithostratigraphic column and C-isotopic profile of the Jiulongwan section modified from McFadden et al. (2008). (2) Generalized paleobathymetric profile showing location of Doushantuo Formation sections known to be fossiliferous. Horizontal distances and water depth are not to scale.

Figure 2

Figure 3. Outcrop photos of the Doushantuo Formation at the studied sections. (1) Olistostrome containing breccia (arrowheads) in shales of the lower Member II at Siduping section. (2) Chert nodules from the lower Member II at Siduping section (sample 19SDP-2). (3) Chert nodules (arrowheads) from the lower Doushantuo Formation at Tianping section (sample 19TP-1). (4) Olistostrome from the lower Doushantuo Formation at Tianping section. (5) Chert nodules (arrowheads) from shales of the lower Doushantuo Formation at Caowan section (sample 19CW-8). (6) A chert nodule (arrowheads) from the middle Doushantuo Formation at Lianghekou section (sample 21LHK-1). (7) Stratigraphic sequence of Nantuo Formation diamictite, basal Doushantuo Formation cap dolostone, and lower Doushantuo Formation calcareous shale and mudstone at Majindong section.

Figure 3

Table 1. Sample number, stratigraphic height, number for thin sections, and microfossil abundance data of the Doushantuo Formation from the nine studied sections in Hunan Province. Refer to Figure 2 for stratigraphic height measurements. Refer to Geological setting section for GPS coordinates of the sections. PN = present, not counted; \ = not observed.

Figure 4

Figure 4. Appendisphaera grandis Moczydłowska, Vidal, and Rudavskaya, 1993, emend. Moczydłowska, 2005. (1, 2) PB201998, thin section 18JSC-2-5, U40/4; circled 2 in (1) marks area magnified in (2). (3, 4) PB201999, thin section 19HP-1-33, N41/1; circled 4 in (3) marks area magnified in (4). (5, 6) PB202000, thin section 19TP-1-19, D49/4; circled 6 in (5) marks area magnified in (6). (7–9) PB202001, thin section 19SDP-2-d1, Y24/1; circled 8 and 9 in (7) mark areas magnified in (8) and (9), respectively. (10, 11) PB202002, thin section 21DC-5-4, V34/1; circled 11 in (10) marks area magnified in (11).

Figure 5

Figure 5. Appendisphaera magnifica (Zhang et al., 1998) Liu et al., 2014a. (1) PB202003, thin section 19SDP-7-1, N38/3. (2) PB202004, thin section 19SDP-7-3, E39/2. (3) PB202005, thin section 19SDP-7-3, E30/2. (4) PB202006, thin section 19SDP-7-3, K30/2. (5) PB202007, thin section 19SDP-7-24, H37. (6) PB202008, thin section 19SDP-7-24, H34.

Figure 6

Figure 6. Appendisphaera tenuis Moczydłowska, Vidal, and Rudavskaya, 1993, emend. Moczydłowska, 2005. (1, 2) PB202009, thin section 19TP-1-14, J27; circled 2 in (1) marks area magnified in (2). (3–5) PB202010, thin section 19TP-1-39, J47/1; circled 4 and 5 in (3) mark areas magnified in (4) and (5), respectively. (6–8) PB202011, thin section 19TP-1-40, F37; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively.

Figure 7

Figure 7. Asterocapsoides wenganensis (Chen and Liu, 1986) Xiao et al., 2014. (1, 2) PB202012, thin section 21LHK-1-10, R34/4. (1) and (2) show the same area at different focal levels; red arrowheads denote large conical processes.

Figure 8

Figure 8. Bullatosphaera? colliformis new species. Red arrowheads denote basally constricted spherical or hemispherical ornamentations. (1–6) Holotype, PB202013, thin section 19CW-6-2, K30/3; circled 2, 3, and 6 in (1) mark areas magnified in (2, 3, 6), respectively; circled 4 in (1) marks areas in (4, 5), which show the same area at different focal levels. (7–10, 13) PB202014, thin section 19CW-6-12, L31/4. (7, 8) Show the same area at different focal levels; circled 9 in (7) marks area magnified in (9); circled 10 and 13 in (8) mark areas magnified in (10) and (13), respectively. (11, 12, 14) PB202015, thin section 19CW-9-7, O35/4; circled 12 and 14 in (11) mark areas magnified in (12) and (14), respectively. Scale bars in (3) and (6) also apply to (2, 4, 5); scale bars in (9) and (12) also apply to (10, 13, 14).

Figure 9

Figure 9. Sketch of Bullatosphaera? colliformis new species.

Figure 10

Figure 10. (1) Cavaspina acuminata (Kolosova, 1991) Moczydłowska, Vidal, and Rudavskaya, 1993, PB202016, thin section 21DC-3-1, Q30/4. (2) Cavaspina basiconica Moczydłowska, Vidal, and Rudavskaya, 1993, PB202017, thin section 21DC-5-4, M40/1. (3, 4) Cavaspina uria (Nagovitsin and Faizullin in Nagovitsin et al., 2004) Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, 2012, thin section 21DC-5-4; red arrowheads in (1–4) denote conical processes; (3) PB202018, G41/1; (4) PB202019, E45/4. (5–7) Eotylotopalla sp. PB202025, thin section 19CW-6-15, O41/1, showing the same area at different focal levels. Scale bars in (5) and (7) also apply to (6).

Figure 11

Figure 11. (1–4, 7, 8) Eotylotopalla dactylos Zhang et al., 1998. (1) PB202020, thin section 19TP-1-13; (2) PB202021 (left) and PB202022 (right), thin section 21DC-2-38, Q48; (3, 4) PB202023, thin section 14HA-115-1, D47/3, showing the same area at different focal levels; (7, 8) PB202024, thin section 21DC-5-3, Q30/3, showing the same area at different focal levels. (5, 6, 9–12) Eotylotopalla cf. E. dactylos Zhang et al., 1998, PB202026, thin section 21DC-2-12, O21/4. (5, 6) The same area at different focal levels; (9–12) magnified views of the processes denoted by circled 9–12 in (6) under cross-polarized light; red arrowheads denote the angular transition from the side wall of the processes to the distal end.

Figure 12

Figure 12. Morphological comparisons between Eotylotopalla specimens described here, published Eotylotopalla dactylos, and specimens identified as Eotylotopalla sp. by Liu et al. (2014a) and by Ye et al. (2022) but reassigned to Eotylotopalla dactylos in this study. Symbols with black outline represent specimens described in this study. Note that two of the three specimens published as Eotylotopalla sp. (Liu et al., 2014a, fig. 31.10, 31.11, and Ye et al., 2022, fig. 23H–J) are very poorly preserved thus their process density (number of processes per 100 μm of vesicle periphery) is unmeasurable.

Figure 13

Figure 13. Eotylotopalla inflata new species. (1–4) Holotype, PB202027, thin section 19TP-1-38, N30/3, showing the same area at different focal levels.

Figure 14

Figure 14. Hocosphaeridium anozos (Willman in Willman and Moczydłowska, 2008) Xiao et al., 2014; red arrowheads denote hooked process terminations. (1–5) PB202028, thin section 21DC-2-20, R20/2; circled 2–5 in (1) mark areas magnified in (2–5), respectively; scale bars in (3) and (5) also apply to (2) and (4). (6–8) PB202029, thin section 21DC-2-20, P18/2; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively; scale bar in (8) also applies to (7). (9–11) PB202030, thin section 21DC-2-20, R21; circled 10 and 11 in (9) mark areas magnified in (10) and (11), respectively. (12–14) PB202031, thin section 21DC-2-20, O18/3; circled 13 and 14 in (12) mark areas magnified in (13) and (14), respectively.

Figure 15

Figure 15. Hocosphaeridium scaberfacium Zang in Zang and Walter, 1992, emend. Liu et al., 2014a; red arrowheads denote hooked process terminations. (1–3) PB202032, thin section 19HP-1-28, Q33; circled 2 and 3 in (1) mark the same area magnified in (2) and (3), respectively, at different focal levels to show different processes. (4–6) PB202033, thin section 19TP-1-40, K44; circled 5 and 6 in (4) mark areas magnified in (5) and (6), respectively. (7, 8) PB202034, thin section 19CW-6-15, N40/4; circled 8 in (7) marks the area magnified in (8). (9) PB202035, thin section 19SDP-7-3, G41/1. (10–12) PB202036, thin section 21DC-2-20, P18; circled 11 and 12 in (10) mark areas magnified in (11) and (12), respectively.

Figure 16

Figure 16. Knollisphaeridium maximum (Yin, 1987) Willman and Moczydłowska, 2008, emend. Liu and Moczydłowska, 2019. (1–3) PB202037, thin section 14HA-140-1, S53/4; circled 2 and 3 in (1) mark areas magnified in (2) and (3), respectively. (4, 6) PB202038, thin section 14HA-140-3, E28/4; circled 6 in (4) marks the area magnified in (6). (5, 7, 8) PB202039, thin section 21DC-6-9, H34; circled 7 and 8 in (5) mark areas magnified in (7) and (8), respectively; scale bar in (7) also applies to (8); red and blue arrowheads in (7) denote undeformed and slightly deformed processes, respectively.

Figure 17

Figure 17. (1) Megasphaera inornata Chen and Liu, 1986, emend. Xiao et al., 2014; PB202040, thin section 19SDP-1-13, K42/2. (2) Megasphaera ornata Xiao and Knoll, 2000, emend. Xiao et al., 2014; PB202041, thin section 19SDP-1-22, P39/2; red arrowhead denotes the outer surface of the sculptured vesicle wall.

Figure 18

Figure 18. (1–3) Mengeosphaera bellula Liu et al., 2014a, PB202042, thin section 19CW-6-12, K33; circled 2 and 3 in (1) mark areas magnified in (2) and (3), respectively. (4–8) Mengeosphaera constricta Liu et al., 2014a, PB202043, thin section 14HA-115-2, W43/2; circled 5 in (4) marks the same area magnified in (5) and (6) at different focal levels; circled 7 and 8 in (4) mark areas magnified in (7) and (8), respectively. (9–14) Mengeosphaera gracilis Liu et al., 2014a. (9, 10, 12) PB202044, thin section 19TP-1-12, H43/1; circled 10 and 12 in (9) mark areas magnified in (10) and (12), respectively; (11, 13, 14) PB202045, thin section 19CW-6-15, G36; circled 13 and 14 in (11) mark areas magnified in (13) and (14), respectively. Scale bar in (8) represents 5 μm and applies to (5–7); scale bar in (14) applies to (13).

Figure 19

Figure 19. (1, 2) Mengeosphaera latibasis Liu et al., 2014a, emend. Liu and Moczydłowska, 2019, PB202046, thin section 14HA-115-1, T49/4; circled 2 in (1) marks the area magnified in (2). (3) Mengeosphaera minima Liu et al., 2014a, PB202047, thin section 21DC-5-4, T31/2. (4) Mengeosphaera minima? PB202048, thin section 21DC-3-1, G23/3. (5–11) Mengeosphaera mamma Ye et al., 2022. (5–7) PB202049, thin section 21LHK-1-10, L38/1; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively; (8, 10) PB202050, thin section 21MJD-1-10, L45; circled 10 in (8) marks the area magnified in (10); (9, 11) PB202051, thin section 21MJD-1-11, L33; circled 11 in (9) marks the area magnified in (11). Red arrowheads in (2), (57), (10), and (11) denote reflection points of biform processes; red arrowheads in (4) denote the basally joined, strongly inflated processes.

Figure 20

Figure 20. (1, 2) Tanarium cf. T. capitatum Liu and Moczydłowska, 2019, PB202052, thin section 21DC-2-35, M32/1, showing the same area at different focal levels. (3, 5) Tanarium conoideum Kolosova, 1991, emend. Moczydłowska, Vidal, and Rudavskaya, 1993, PB202053, thin section 21DC-5-4, R43/3, showing the same area at different focal levels. (4, 6, 7) Tanarium paucispinosum Grey, 2005: (4) PB202054, thin section 19CW-6-9, N35/3; (6, 7) PB202055, thin section 19CW-5-29, H38, showing the same area at different focal levels.

Figure 21

Figure 21. Tanarium pilosiusculum Vorob'eva, Sergeev, and Knoll, 2009. (1–4) PB202056, thin section 19CW-6-15, O41; circled 2–4 in (1) mark areas magnified in (2–4), respectively; (5–7) PB202057, thin section 21LHK-1-10, M31/2; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively.

Figure 22

Figure 22. (1–3) Tanarium triangulare (Liu et al., 2014a) Liu and Moczydłowska, 2019: (1, 2) PB202058, thin section 14HA-140-5, F24/1, same area at different focal levels; (3) PB202059, thin section 14HA-140-3, D31/1. (4) Tanarium tuberosum Moczydłowska, Vidal, and Rudavskaya, 1993, PB202060, thin section 21DC-4-11, U45. Red arrowheads in (1) and (2) denote typical conical basal part of some processes.

Figure 23

Figure 23. Tianzhushania spinosa Yin and Li, 1978, emend. Yin in Yin and Liu, 1988. (1–6) PB202061, thin section 21LHK-1-10, O41/4; circled 2 and 6 in (1) mark the areas magnified in (2) and (6), respectively; circled 3 in (2) marks the area magnified in (3); circled 4 in (2) marks the same area magnified in (4) and (5) at different focal levels. Red arrowheads denote hollow cylindrical processes embedded in multilaminate membrane; blue arrowheads denote poorly preserved multilaminate membrane.

Figure 24

Figure 24. Trachyhystrichosphaera? sp. (1–8) PB202062, thin section 19CW-6-16, M40/3; circled 2–5 and 8 in (1) mark areas magnified in (2–5) and (8), respectively; circled 6 in (1) marks the same area magnified in (6) and (7) at different focal levels to show different processes. Scale bar in (5) also applies to (2–4, 6–8). Red arrowheads denote cylindrical processes, yellow arrowheads denote conical processes, blue arrowheads denote outer membrane.

Figure 25

Figure 25. Urasphaera fungiformis Liu et al., 2014a. (13) PB202063, thin section 14HA-115-1, N50; circled 2 in (1) marks the same area magnified in (2) and (3) at different focal levels to show different processes.

Figure 26

Figure 26. Verrucosphaera? undulata new species. (1–5) Holotype, PB202064, thin section 21DC-6-1, H44; circled 2 in (1) marks the same area magnified in (2) and (3) at different focal levels to show different processes; circled 4 in (1) marks the same area magnified in (4) and (5) at different focal levels to show different processes; (6–8) PB202065, thin section 21DC-5-4, S47; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively. Red arrowheads denote thin cylindrical processes on top of thick conical processes.

Figure 27

Figure 27. Verrucosphaera? undulata new species. (1–4) PB202066, thin section 21DC-5-4, P41/2; circled 2–4 in (1) mark areas magnified in (2–4), respectively; (5–7) PB202067, thin section 21DC-5-4, T32/4; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively; (8–10) PB202068, thin section 21DC-5-4, L43/3; circled 9 and 10 in (8) mark areas magnified in (9) and (10), respectively. Red arrowheads denote thin cylindrical processes on top of thick conical processes.

Figure 28

Figure 28. Sketch of Verrucosphaera? undulata new species.

Figure 29

Figure 29. Weissiella cf. W. grandistella. (1–7) PB202069, thin section 21DC-2-30, T35; circled 2–4 in (1) mark areas magnified in (2–4), respectively; red arrowheads denote cross-walls in the processes; (5–7) cross-polarized light microscopic photographs of (1); circled 6 in (2) and circled 7 in (3) showing areas in (6) and (7), respectively; recrystallized micro-quartz indicated by yellow arrowheads; scale bar in (6) also applies to (7).

Figure 30

Figure 30. Recrystallized micro-quartz in chert nodules. (1, 3) A poorly preserved microfossil under plane- (1) and cross- (3) polarized light, showing recrystallized micro-quartz up to 7 μm in size (yellow arrowheads); thin section 19TP-1-39. (2) A well-preserved microfossil under cross-polarized light, showing recrystallized micro-quartz in various sizes (yellow arrowheads); thin section 21DC-5-3. (4) A poorly preserved microfossil under cross-polarized light, with the vesicle interior filled with sightly recrystallized chalcedony (red arrowhead), vesicle wall destroyed by three large calcite crystals, and extra-vesicle matrix filled with micro-quartz in various sizes (yellow arrowheads); thin section 19TP-1-25.

Figure 31

Table 2. Summary of acanthomorph occurrence and abundance data at the nine studied sections. Each occurrence is denoted by fossiliferous sample name and number of specimens. For example, “21DC-4, 1” means one acanthomorph specimen recovered from the sample 21DC-4. Notes for superscripts: (1) Identified as Cavaspina cf. C. basiconica by Shi et al. (2022). (2) Identified as ?Verrucosphaera sp. by Shi et al. (2022). (3) Identified as Appendisphaera fragilis by Ouyang et al. (2017). (4) Identified as ?Cavaspina basiconica by Ouyang et al. (2017). (5) Identified as indeterminate acanthomorph by Ouyang et al. (2017). (6) Identified as Mengeosphaera spicata by Ouyang et al. (2017). (7) Identified as Mengeosphaera latibasis? by Ouyang et al. (2017). (8) Identified as Mengeosphaera chadianensis, Mengeosphaera sp. indet., and M.? cuspidata by Ouyang et al. (2017).

Figure 32

Figure 31. Indeterminate acanthomorphs. (1) PB202070, thin section 19SDP-1-5, O23/4. (2) PB202071, thin section 19SDP-7-3, J28. (3) PB202072, thin section 19CW-5-21, K39. (4) PB202073, thin section 21LHK-1-2, P35. Red arrowheads denote processes.

Figure 33

Figure 32. Sphaeromorphic acritarchs. (1) PB202074, thin section 21LHK-1-6, E42. (2) PB202075, thin section 19HP-1-20, O33/3. (3) PB202076, thin section 19CW-5-30, Q36/3. (4) PB202077, thin section 19TP-1-26, B40.

Figure 34

Figure 33. Multicellular algae. (1, 2) Wengania minuta Xiao, 2004b, PB202078, thin section 19SDP-1-19, N41/4, showing the same area at different focal levels. (3–5, 7) Unnamed thalli with large cells; (3–5) PB202079, thin section 19SDP-1-19, M35; (7) PB202081, thin section 19SDP-1-25, K42/3. (6) Unnamed multicellular thallus, PB202080, thin section 19CW-6-15, M41.

Figure 35

Figure 34. Tubular microfossils. (1) Quadratitubus orbigoniatus Xue, Tang, and Yu, 1992, emend. Liu et al., 2008, PB202082, thin section 19CW-6-13, M44/3. (2) Possible Quadratitubus orbigoniatus, PB202083, thin section 21DC-2-36, L40/2. (3, 4) Sinocyclocyclicus guizhouensis Xue, Tang, and Yu, 1992, emend. Liu et al., 2008; (3) PB202084, thin section 19SDP-7-3, J37/2; (4) PB202085, thin section 21MJD-1-10, K36/3.

Figure 36

Figure 35. Microbial mats consist of filamentous microfossils. (1) A small fragment of Siphonophycus mat, PB202086, thin section 21MJD-1-3, K32/2. (2, 4) Mat with thin filaments interwoven into spherical structures, PB202087, thin section 19CW-6-9, L38; circled 4 in (2) marks the area magnified in (4). (3) Microbial mat consists of various filamentous microfossils including Siphonophycus Schopf, 1968, emend. Knoll et al., 1991, and Salome Knoll, 1982, PB202088, thin section 18JSC-2-3, H34/4. (5, 6) Microbial mat consisting of filamentous microfossils of various sizes; (5) PB202089, thin section 19CW-6-6; (6) PB202090, thin section 19SDP-7-19, Q36.

Figure 37

Figure 36. Filamentous and coccoidal microfossils. (1) Obruchevella minor Zhang, 1984a, PB202091, thin section 18JSC-2-4, T22/2. (2) Salome svalbardense Knoll, 1982, PB202092, thin section 21LHK-1-6, J38. (3, 4) Salome hubeiensis Zhang, 1986: (3) PB202093, thin section 19TP-1-40, J33/3, (4) PB202094, thin section 19CW-6-14, J36/2. (5) Bundled filaments resembling Polytrichoides Hermann, 1974, emend. Hermann in Timofeev et al., 1976, PB202095, thin section 19HP-2-6, M40. (6) Septate trichome with cells much wider than length resembling Oscillatoriopsis Schopf, 1968, emend. Butterfield et al., 1994, PB202096, thin section 19HP-2-3, Q38/3. (7, 8) Aggregated coccoids resembling Myxococcoides Schopf, 1968: (7) PB202097, thin section 21LHK-1-10, Q43/2; (8) PB202098, thin section 21LHK-1-10, N48/3.

Figure 38

Figure 37. Microbial mat preserved as reworked clasts. (1, 2) PB202099, thin section 21LHK-1-15, N42/2; circled 2 in (1) mark the area magnified in (2); (3) PB202100, thin section 19SDP-7-22, F38/2; (4) PB202101, thin section 21LHK-1-3, O44.

Figure 39

Figure 38. Problematic microfossils. (1–4) Microfossil with branching filaments, PB202102, thin section 19SDP-3-14, H34/3, same area at different focal levels to show different branches and bifurcations; red arrowheads denote bifurcations. (5, 6) Polybessurus sp. (5) PB202103, thin section 21MJD-1-13, P37/2; (6) PB202104, thin section 19TP-1-25, M39/4.

Figure 40

Table 3. Paleoenvironmental distribution of reported acanthomorphic acritarchs from the Doushantuo Formation in South China. Numbers in each cell refer to data sources, as detailed below. Hashtag sign (#) indicates that the reported specimen was mistakenly assigned to Briareus vasformis Liu and Moczydłowska, 2019, by Ouyang et al. (2021), and should be B. robustus Liu and Moczydłowska, 2019. Data sources shown in the table: (1) This study. (2) Yin and Li, 1978. (3) Awramik et al., 1985. (4) Chen and Liu, 1986. (5) Yin, 1987. (6) Yin and Liu, 1988. (7) Yin, 1990. (8) Yin et al., 1990. (9) Yin and Xue, 1993. (10) Yuan et al., 1993. (11) Xue et al., 1995. (12) Yin, 1996. (13) Yuan and Hofmann, 1998. (14) Zhang et al., 1998. (15) Xiao and Knoll, 1999. (16) Yin, 1999. (17) Xiao and Knoll, 2000. (18) Yin, 2001. (19) Yin et al., 2001. (20) Zhou et al., 2001. (21) Zhou et al., 2002. (22) Yin et al., 2003. (23) Xiao, 2004b. (24) Yin et al., 2004. (25) Zhou et al., 2004b. (26) Liu and Yin, 2005. (27) Xiao et al., 2007. (28) Yin et al., 2007. (29) Zhou et al., 2007. (30) Xie et al., 2008. (31) Liu et al., 2009. (32) McFadden et al., 2009. (33) Yin et al., 2009a. (34) Yin et al., 2009b. (35) Chen et al., 2010. (36) C. Yin et al., 2011. (37) L. Yin et al., 2011. (38) Liu et al., 2012. (39) Wang et al., 2012. (40) Liu et al., 2013. (41) Zeng et al., 2013. (42) Liu et al., 2014a. (43) Liu et al., 2014b. (44) Xiao et al., 2014. (45) Ouyang et al., 2015. (46) Ye et al., 2015. (47) Hawkins et al., 2017. (48) Nie et al., 2017. (49) Liu and Moczydłowska, 2019. (50) Ouyang et al., 2019. (51) Shang et al., 2019. (52) Shang and Liu, 2020. (53) Yang et al., 2020. (54) Liu et al., 2021. (55) Ouyang et al., 2021. (56) Ye et al., 2022.

Figure 41

Figure 39. Comparison of acanthomorph diversity among different depositional facies at species and genus levels.

Figure 42

Figure 40. Rarefaction analysis of Doushantuo acanthomorphs. (1) Rarefaction curves with 1σ error bars of Doushantuo acanthomorph assemblages published with abundance data from 10 sections in inner shelf, shelf-lagoon, and slope facies. (2) Magnification of gray box in bottom-left of (1), showing rarefied species richness with subsampled size of 1–40 specimens. Sample sizes of Lianghekou section and basinal facies sections are small, therefore they were not rarefied. Rather, observed specimen number and species richness are plotted for Lianghekou section and pooled basinal facies data.

Figure 43

Figure 41. Taxonomic ordination plots based on NMDS analysis of taxonomically updated occurrence data from 82 collections of Doushantuo acanthomorphs in South China (see Supplemental Materials for data). (1) NMDS scatter plots and convex hulls differentiated by depositional facies. (2) NMDS scatter plots and convex hulls differentiated by depositional facies and stratigraphic intervals. (3) Species loading diagram. Note that some species are not labeled because of the limited space; see Supplemental Materials for loading data. Red and green circled points represent eponymous species of the lower and upper biozones of the Doushantuo Formation (Liu et al., 2013, 2014b; Xiao et al., 2014), respectively. Blue filled points represent eponymous species of the biozones of Liu and Moczydłowska (2019). See Figure 42 for abbreviations.

Figure 44

Figure 42. Bipartite network analysis of the same dataset of Doushantuo acanthomorph occurrences used in NMDS analysis (Fig. 41; see Supplemental Materials for data). Lettered nodes represent acritarch species. Numbered and colored nodes represent collections, with numbers matching source reference numbers in Table 3, and colors matching those of Figure 41.2: red = Member II of the Doushantuo Formation, shelf lagoon; green = Member III of the Doushantuo Formation, shelf lagoon; gray = stratigraphic interval not specified, shelf lagoon; yellow = correlated with upper Member II in shelf-lagoon facies, inner shelf (the Zhangcunping and Shennongjia areas); light blue = stratigraphic correlation relationship unclear, inner shelf (other areas such as Baokang, Chadian, and Chaoyang); orange = correlated with upper Member II or Member II–III transitional interval in shelf-lagoon facies, shelf margin (the Weng'an area); olive = roughly correlated with Member III in shelf-lagoon facies, shelf margin (the Caojunba section); lime, Doushantuo Formation, upper slope (the Lujiayuanzi section); blue = correlated with Member II in shelf-lagoon facies, slope (the Zhangjiajie area); dark blue = basinal facies. Each species is linked to a collection by a straight line if the species is present in the collection. Each acritarch taxon is linked to collections in which it is present. The network shows variation in occurrence frequency among acritarch species of the Doushantuo Formation. Species in the central area of the network generally occur in a greater number of areas, stratigraphic intervals, or studies, than species in the periphery area of the network. Abbreviations: CY-Changyang area, YG-Yangtze Gorges area. Species abbreviations: Alm = Alicesphaeridium medusoidum; Anm = Ancorosphaeridium magnum; Ani = Annularidens inconditus; Apob = Apodastoides basileus; Apa = Appendisphaera anguina; Apc1 = Appendisphaera clava; Apc2 = Appendisphaera clustera; Apf = Appendisphaera fragilis; Apg = Appendisphaera grandis; Aph1 = Appendisphaera heliaca; Apl1 = Appendisphaera lemniscata; Apl2 = Appendisphaera longispina; Apl3 = Appendisphaera longitubularis; Apm = Appendisphaera magnifica; Aps = Appendisphaera setosa; Apt1 = Appendisphaera tabifica; Apt2 = Appendisphaera tenuis; Apb = Appendisphaera? brevispina; Aph2 = Appendisphaera? hemisphaerica; Assd = Asseserium diversum; Assf = Asseserium fusulentum; Astf = Asterocapsoides fluctuensis; Astr = Asterocapsoides robustus; Asts = Asterocapsoides sinensis; Astw = Asterocapsoides wenganensis; Bab = Bacatisphaera baokangensis; Bas = Bacatisphaera sparga; Bip = Bispinosphaera peregrina; Biv = Bispinosphaera vacua; Brb = Briareus borealis; Brr = Briareus robustus; Brv = Briareus vasformis; Buc = Bullatosphaera? colliformis n. sp.; Calx = Calyxia xandaros; Caa = Cavaspina acumincata; Cab = Cavaspina basiconica; Cac = Cavaspina conica; Cau = Cavaspina uria; Cavc = Caveasphaera costata; Ceg = Ceratosphaeridium glaberosum; Crc = Crassimembrana crispans; Crm = Crassimembrana multitunica; Crip = Crinita paucispinosa; Cyf = Cymatiosphaeroides forabilatus; Cyk = Cymatiosphaeroides kullingii; Cyy = Cymatiosphaeroides yinii; Dici = Dicrospinasphaera improcera; Dicv = Dicrospinasphaera virgata; Dicz = Dicrospinasphaera zhangii; Disj = Distosphaera jinguadunensis; Diss = Distosphaera speciosa; Disc = Distosphaera? corniculata; Dub = Duospinosphaera biformis; Dus = Duospinosphaera shennongjiaensis; Eoa = Eotylotopalla apophysa; Eoda = Eotylotopalla dactylos; Eode = Eotylotopalla delicata; Eoi = Eotylotopalla inflata n. sp.; Eoq = Eotylotopalla quadrata; Eos = Eotylotopalla strobilata; Erc = Ericiasphaera crispa; Erd = Ericiasphaera densispina; Erf = Ericiasphaera fibrilla; Erm = Ericiasphaera magna; Err = Ericiasphaera rigida; Ers1 = Ericiasphaera sparsa; Ers2 = Ericiasphaera spjeldnaesii; Esg = Estrella greyae; Esr = Estrella recta; Gyp = Gyalosphaeridium pulchrum; Hew = Helicoforamina wenganica; Hoa = Hocosphaeridium anozos; Hod = Hocosphaeridium dilatatum; Hos = Hocosphaeridium scaberfacium; Knb = Knollisphaeridium bifurcatum; Knc = Knollisphaeridium coniformum; Knd = Knollisphaeridium denticulatum; Knl = Knollisphaeridium longilatum; Knm = Knollisphaeridium maximum; Kno = Knollisphaeridium obtusum; Knp = Knollisphaeridium parvum; Knt = Knollisphaeridium triangulum; Lac = Laminasphaera capillata; Mac = Matosphaera changyangensis; Megc = Megasphaera cymbala; Megi = Megasphaera inornata; Mego = Megasphaera ornata; Megp1 = Megasphaera patella; Megp2 = Megasphaera puncticulosa; Memf = Membranosphaera formosa; Mea = Mengeosphaera angusta; Meb = Mengeosphaera bellula; Mech = Mengeosphaera chadianensis; Meco = Mengeosphaera constricta; Mee = Mengeosphaera eccentrica; Mef = Mengeosphaera flammelata; Meg1 = Mengeosphaera gracilis; Meg2 = Mengeosphaera grandispina; Mela = Mengeosphaera latibasis; Melu = Mengeosphaera lunula; Mem1 = Mengeosphaera mamma; Mem2 = Mengeosphaera matryoshkaformis; Mem3 = Mengeosphaera membranifera; Mem4 = Mengeosphaera minima; Mer = Mengeosphaera reticulata; Mesp = Mengeosphaera spinula; Mest = Mengeosphaera stegosauriformis; Meu = Mengeosphaera uniformis; Mup = Multifronsphaeridium pelorium; Mur = Multifronsphaeridium ramosum; Pab = Papillomembrana boletiformis; Pac = Papillomembrana compta; Poc = Polygonium cratum; Sia = Sinosphaera asteriformis; Sie = Sinosphaera exilis; Sir = Sinosphaera rupina; Sis = Sinosphaera speciosa; Siv = Sinosphaera variabilis; Spb = Spiralicellula bulbifera; Tael = Taedigerasphaera lappacea; Taa = Tanarium acus; Tac1 = Tanarium capitatum; Tac2 = Tanarium columnatum; Tac3 = Tanarium conoideum; Tac4 = Tanarium cuspisatum; Tad = Tanarium digitiforme; Tae = Tanarium elegans; Tag = Tanarium gracilentum; Tai = Tanarium irregulare; Tami = Tanarium minimum; Tamu = Tanarium muntense; Tao = Tanarium obesum; Tap1 = Tanarium paucispinosum; Tap2 = Tanarium pilosiusculum; Tap3 = Tanarium pluriprotensum; Tap4 = Tanarium pycnacanthum; Tatr = Tanarium triangulare; Tatu = Tanarium tuberosum; Tau = Tanarium uniformum; Tava = Tanarium varium; Tavi = Tanarium victor; Tip = Tianzhushania polysiphonia; Tir = Tianzhushania rara; Tis = Tianzhushania spinosa; Scz = Schizofusa zangwenlongii; Urc = Urasphaera capitalis; Urf = Urasphaera fungiformis; Urn = Urasphaera nupta; Vaf = Variomargosphaeridium floridum; Vag = Variomargosphaeridium gracile; Val = Variomargosphaeridium litoschum; Vav = Variomargosphaeridium varietatum; Vem = Verrucosphaera minima; Veu = Verrucosphaera? undulata n. sp.; Web = Weissiella brevis; Wec = Weissiella concentrica; Weg = Weissiella cf. W. grandistella; Xel = Xenosphaera liantuoensis; Yit = Yinitianzhushania tuberifera; Yur = Yushengia ramispinsa.

Figure 45

Table 4. Occurrence of eponymous species of the two previously proposed biozonation schemes for the Doushantuo Formation in South China. Abbreviations for biozones: A1 = Tianzhushania spinosa zone of Liu et al. (2013, 2014a) and Xiao et al. (2014), corresponding to Member II in the Yangtze Gorges area; A2 = Hocosphaeridium anozos Zone (or the Tanarium conoideumHocosphaeridium scaberfaciumH. anozos Zone) of Liu et al. (2013, 2014a) and Xiao et al. (2014), corresponding to Member III in the Yangtze Gorges area; B1 = Appendisphaera grandisWeissiella grandistellaTianzhushania spinosa Zone of Liu and Moczydłowska (2019), corresponding to lowermost Member II in the Yangtze Gorges area; B2 = Tanarium tuberosumSchizofusa zangwenlongii Zone of Liu and Moczydłowska (2019), corresponding to lower–middle Member II in the Yangtze Gorges area; B3 = Tanarium conoideumCavaspina basiconica Zone of Liu and Moczydłowska (2019), corresponding to middle–upper Member II in the Yangtze Gorges area; B4 = Tanarium pycnacanthumCeratosphaeridium glaberosum Zone of Liu and Moczydłowska (2019), corresponding to lower Member III in the Yangtze Gorges area.