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Middle and late Permian foraminifers from the Chichibu Belt, Takachiho Area, Kyushu, Japan: implications for faunal events

Published online by Cambridge University Press:  20 May 2016

Fumio Kobayashi
Fumio Kobayashi*
Affiliation:
Division of Earth Sciences, Institute of Natural and Environmental Sciences, University of Hyogo, Yayoigaoka 6, Sanda, Hyogo, 669-1546, Japan,
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Abstract

The middle and late Permian to Triassic sequence of carbonate rocks in the Takachiho area, central Kyushu, Japan, originated as a Panthalassan seamount and formed parts of far-traveled accreted terranes. This succession is divided into the Permian Guadalupian Iwato and Lopingian Mitai formations, and the Triassic Kamura Formation. The Iwato Formation is further into three zones, the Neoschwagerina, Yabeina higoensis, and Neoendothyra permica zones in ascending order; the Mitai Formation includes the Nanlingella suzukii Zone. Biotic turnovers are recorded twice in the Iwato and Mitai formations. The first and more remarkable biotic event is the total disappearance of fusulines at the top of the Yabeina higoensis Zone. The Neoendothyra permica Zone is characterized by black fine-grained micritic limestones having only sparse non-fusuline foraminifers. The second biotic event is the first appearance of Wuchiapingian fusulines by which the Nanlingella suzukii Zone is defined. The Capitanian–Wuchiapingian boundary is drawn between the Neoendothyra permica and Nanlingella suzukii zones. Above this boundary both the numbers of individual foraminifers and diversity of species gradually increase. The turnovers recorded in the Takachiho area were the result of late Capitanian–Wuchiapingian environmental changes which were sufficient to cause the disappearance of large, multi-chambered fusulines and allow the new appearance of an ‘ultimate’ Paleozoic foraminiferal assemblage. Ten species of foraminifers, including Yabeina higoensis and Yabeina Columbiana, are described.

Type
Research Article
Information
Journal of Paleontology , Volume 86 , Issue 4 , July 2012 , pp. 669 - 687
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Copyright © The Paleontological Society 

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References

Brady, H. B. 1884. Report on the Foraminifera dredged by H. M. S. Challenger, drilling the Year 1873–1876. InReport on the Scientific Results on the Voyage of the H. M. S. Challenger during the Years 1873–1876, Zoology, 9:1–814.Google Scholar
Chisaka, T. 1960. On some Permian fusulinids from the Takagami Conglomerate, Choshi Peninsula, Chiba Prefecture, Japan. Journal of the College of Arts and Sciences, Chiba University, 3:235–254.Google Scholar
Ciarapica, G. and Zaninetti, L. 1985. Gandinella apenninica, n. gen. n. sp. (Foraminifère) dans le Trias Supérieur (Rhetian, Biozone à Triasina hantkeni) du Monte Cetona, Apennin Septentrional. Revue de Paléobiologie, 4:307–310.Google Scholar
Clapham, M. E., Shen, S., and Bottjer, D. J. 2009. The double mass extinction revisited: Reassessing the severity, selectivity, and causes of the end-Guadalupian biotic crisis. Paleobiology, 35:32–50.Google Scholar
Colani, M. 1924. Nouvelle contribution à l'étude des Fusulinides de l'Extreme-Orient. Mémoires du Service Géologique de l'Indochine, 11:9–191.Google Scholar
Dawson, G. M. 1879. On a new species of Loftusia from British Columbia. Quarterly Journal of the Geological Society of London, 35:69–75.CrossRefGoogle Scholar
Delage, Y. and Hérouard, E. 1896. Traité de Zoologie Concrète, Tome 1. La Cellule et les Protozoaires. Schleicher Frères, Paris, 584 p.Google Scholar
Deprat, J. 1913. Étude des fusulidés de Chine et d'Indochine. Les fusulinidés des calcaires Carbonifériens et Permiens du Tonkin, du Laos et du Nord-Annam. Mémoires du Service Géologique de l'Indo-Chine, 2:1–74.Google Scholar
Deprat, J. 1914. Étude des fusulidés du Japon, de Chine et d'Indochine. Étude comparative des Fusulinidés d'Akasaka (Japon) et des Fusulinidés de Chine et d'Indochine. Mémoires du Service Géologique de l'Indo-Chine, 3:1–45.Google Scholar
Dunbar, C. O. and Condra, G. E. 1927. The Fusulinidae of the Pennsylvanian System in Nebraska. Bulletin of the Nebraska Geological Survey, series 2, 2:1–135.Google Scholar
Dunbar, C. O. and Skinner, J. W. 1937. Permian Fusulinidae of Texas,. p. 517–825. InThe Geology of Texas, 3, Upper Paleozoic Ammonites and Fusulinids, Pt. 2. The University of Texas Bulletin 3701.Google Scholar
Eichwald, C. E. Von. 1830. Zoologia specialis pars Altera. J. Zawadzki, Vilius, 323 p.Google Scholar
Gaillot, J. and Vachard, D. 2007. The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. Coloquios de Paleontología, 57:37–223.Google Scholar
Geinitz, H. B. 1876. Zur Geologie von Sumatra. Palaeontographica, 22 399–404.Google Scholar
Han, J. 1982. The late early Permian foraminifera in the north part of Northeast China. Bulletin of the Shenyang Institute of Geology and Mineral Resources, 4:99–112. (In Chinese).Google Scholar
Huzimoto, H. 1936. Stratigraphical and palaeontological studies of the Titibu System of the Kanto-mountainland, Pt. 2, Palaeontology. Science Reports of the Tokyo Bunrika Daigaku, section C, 4:29–125.Google Scholar
Igo, H. and Igo, H. 1977. Upper Permian fusulinaceans contained in the pebbles of the basal conglomerate of the Adoyama Formation, Kuzu, Tochigi Prefecture, Japan. Transactions and Proceedings of the Palaeontological Society of Japan, new series, 106:89–99.Google Scholar
Isozaki, Y. 1997. Permo–Triassic boundary superanoxia and stratified superocean. Science, 267:235–238.Google Scholar
Isozaki, Y., Kawahata, H., and Ota, A. 2007. A unique carbon isotope records across the Guadalupian–Lopingian (middle–upper Permian) boundary in mid-oceanic paleo-atoll carbonates: The high-productivity “Kamura event” and its collapse in Panthalassa. Global and Planetary Change, 55:21–38.Google Scholar
Isozaki, Y. and Ota, A. 2001. Middle–upper Permian (Maokouan–Wuchiapingian) boundary in mid-oceanic paleo-atoll limestone of Kamura and Akasaka, Japan. Proceedings of the Japan Academy, 77:104109.Google Scholar
Kambe, N. 1963. On the boundary between the Permian and Triassic Systems in Japan with the description of the Permian–Triassic formations at Takachiho-cho, Miyazaki Prefecture in Kyushu and the Skytic fossils contained. Geological Survey of Japan, Report 198, 1–68.Google Scholar
Kanmera, K. 1954. Fusulinids from the upper Permian Kuma Formation, southern Kyushu, Japan―with special reference to the fusulinid zone in the upper Permian of Japan. Memoirs of the Faculty of Science, Kyushu University, series D, 4:1–38.Google Scholar
Kanmera, K. and Nakazawa, K. 1973. Permian–Triassic relationships and faunal changes in the eastern Tethys,. p. 100–119. InLogan, A. and Hills, L. V.(eds.), The Permian–Triassic Systems and their Mutual Boundary. Canadian Society of Petroleum Geologists, Memoir 2.Google Scholar
Kobayashi, F. 1986. Middle Permian foraminifers of the Gozenyama Formation, southern Kwanto Mountains, Japan. Bulletin of the National Science Museum, series C, 12:131–163.Google Scholar
Kobayashi, F. 1996. Middle Triassic (Anisian) foraminifers from the Kaizawa Formation, southern Kanto Mountains, Japan. Transactions and Proceedings of the Palaeontological Society of Japan, new series, 183:528–539.Google Scholar
Kobayashi, F. 1997. Upper Permian foraminifers from the Iwai-Kanyo area, west Tokyo, Japan. Journal of Foraminiferal Research, 27:186–195.CrossRefGoogle Scholar
Kobayashi, F. 1999. Tethyan uppermost Permian (Dzhulfian and Dorashamian) foraminiferal faunas and their paleobiogeographic and tectonic implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 150:279–307.Google Scholar
Kobayashi, F. 2001a. Early late Permian (Wujiapingian) foraminiferal fauna newly found from the limestone block of the Sambosan Belt in the southern Kanto Mountains, Japan. The Journal of the Geological Society of Japan, 107:701–705. (In Japanese).Google Scholar
Kobayashi, F. 2001b. Faunal analysis of Permian foraminifers of the Kuma Formation in the Kurosegawa Belt of west Kyushu, Southwest Japan,. p. 61–84. InTakemura, A. and Furutani, H.(eds.), News of Osaka Micropaleontologists, Special volume., no. 12.Google Scholar
Kobayashi, F. 2002. Lithology and foraminiferal fauna of the allochthonous limestone (Changhsingian) in the upper part of the Toyoma Formation in the South Kitakami Belt, Northeast Japan. Paleontological Research, 6:331–342.Google Scholar
Kobayashi, F. 2003. Palaeogeographic constraints on the tectonic evolution of the Maizuru Terrane of Southwest Japan to the eastern continental margin of South China during the Permian and Triassic. Palaeogeography, Palaeoclimatology, Palaeoecology, 195:299–317.Google Scholar
Kobayashi, F. 2004. Late Permian foraminifers from the limestone block in the Southern Chichibu Terrane of west Shikoku, SW Japan. Journal of Paleontology, 78:62–70.Google Scholar
Kobayashi, F. 2005. Permian foraminifers from the Itsukaichi-Ome area, west Tokyo, Japan. Journal of Paleontology, 79:413–432.Google Scholar
Kobayashi, F. 2006a. Middle Permian foraminifers of the Izuru and Nabeyama Formations in the Kuzu area, Tochigi Prefecture, Japan, Part 2. Schubertellid and ozawainellid fusulinoideans, and non-fusulinoidean foraminifers. Paleontological Research, 10:61–77.Google Scholar
Kobayashi, F. 2006b. Middle Permian foraminifers of Kaize, southern part of the Saku Basin, Nagano prefecture, central Japan. Paleontological Research, 10:179–194.Google Scholar
Kobayashi, F. 2006c. Early late Permian (Wuchiapingian) foraminifers in the Tatsuno area, Hyogo—Late Paleozoic and Early Mesozoic foraminifers of Hyogo, Japan, Part 4. Nature and Human Activities, 10:25–33.Google Scholar
Kobayashi, F. 2007. Foraminiferal fauna and lithofacies of middle Permian limestone blocks in the middle course of Kuma River (Osakama), southern margin of the Chichibu Terrane in west Kyushu, Japan. Paleontological Research, 11:337–347.Google Scholar
Kobayashi, F. 2010. Late Paleozoic foraminifers contained in limestone conglomerate of the Maizuru Group in the Oye area, Kyoto Prefecture, Japan. Humans and Nature, 21:79–91.Google Scholar
Kobayashi, F. 2011. Permian fusuline faunas and biostratigraphy of the Akasaka Limestone (Japan). Revue de Paléobiologie, 30:431–574.Google Scholar
Kobayashi, F. 2012. Comparative study of the Capitanian (late Guadalupian) foraminiferal faunas in the Lepidolina shiraiwensis Zone of the Akiyoshi Limestone Group, Japan. Journal of Foraminiferal Research, 42:82–101.Google Scholar
Kobayashi, F., Martini, R., and Zaninetti, L. 2005. Anisian foraminifers from allochthonous limestones of the Tanoura formation (Kurosegawa Terrane, west Kyushu, Japan). Geobios, 38:751–763.Google Scholar
Kobayashi, F., Ross, C. A., and Ross, J. R. P. 2007. Age and generic assignment of Yabeina columbiana (Guadalupian fusulinaceans) in southern British Columbia. Journal of Paleontology, 81:238–253.Google Scholar
Kobayashi, F., Ross, C. A., and Ross, J. R. P. 2010. Classification, phylogeny, and paleobiogeography of the new Subfamily Gifuellinae and a revision of the Family Neoschwagerinidae (Superorder Fusulinida); Guadalupian (middle Permian). Journal of Foraminiferal Research, 40:283–300.Google Scholar
Kobayashi, F., Shiino, Y., and Suzuki, Y. 2009. Middle Permian (Midian) foraminifers of the Kamiyasse Formation in the Southern Kitakami Terrane, NE Japan. Paleontological Research, 13:79–99.Google Scholar
Koike, T. 1996. The first occurrence of Griesbachian conodonts in Japan. Transactions and Proceedings of the Palaeontological Society of Japan, new series, 181:337–346.Google Scholar
Kozur, H. and Pjatakova, M. 1976. Die Conodontenart Anchignathodus parvus n. sp. eine wichtige Leitform der basalen Trias. Koninklijke Nederlandse Akademie van Wetenschappen, Amsterdam, Proceedings, series B, 79:123–128.Google Scholar
Lai, X., Wang, W., Wignall, P. B., Bond, D. P. G., Jiang, H., Ali, J. R., John, E. H., and Sun, Y. 2008. Palaeoenvironmental change during the end-Guadalupian (Permian) mass extinction in Sichuan, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 269:78–93.Google Scholar
Lee, J. S. 1934. Taxonomic criteria of Fusulinidae with notes on seven new Permian genera. Memoirs of National Research Institute of Geology, Nanking (1933), 14:1–21.Google Scholar
Lin, J. 1978. Foraminifers of Carboniferous and Permian,. p. 10–43. InHubei Institute of Geological Sciences (ed.), Paleontological Atlas of the Central South China (4). Geological Publishing House, Beijing. (In Chinese)Google Scholar
Lin, J. 1984. Order Foraminiferida, p. 110–177. InBiostratigraphy of the Yangtze Gorge Area (3) Late Paleozoic Era, Geological Publishing House, Beijing. (In Chinese)Google Scholar
Lin, J., Li, J., and Sun, Q. 1990. Late Paleozoic Foraminifers in South China. Scientific Publishing House, Beijing, 297 p. (In Chinese)Google Scholar
Loeblich, A. R. Jr. and Tappan, H. 1988. Foraminiferal genera and their Classification. Van Nostrand Reinhold Company, New York, 2 vols., 970 p. plus 212 p. and 847 pls.Google Scholar
Miklukho-Maklay, A. D. 1949. Upper Paleozoic fusulinids of Middle Asia (Darvas, Fergana, Pamir). Izdatel'stvo Leningradskogo Universiteta, Leningrad, 114 p. (In Russian)Google Scholar
Miklukho-Maklay, A. D. 1953. On the systematics of the family Archdiscidae. Ezhegodnik Vsesoyuznogo Paleontologicheskogo Obshchestva (1948–1953), 14:127–131. (In Russian)Google Scholar
Miklukho-Maklay, K. V. 1954. Foraminifera of upper Permian strata of the northern Caucasus,. 163 p. Trudy Vsesoyuznogo Nauchno-Issledoovatel'skogo Geologicheskogo Instituta (VSEGEI), Akademiya Nauk SSSR. (In Russian)Google Scholar
Möller, V. Von. 1878. Die spiral-gewunden Foraminiferen des russischen Kohlenkalkes. Mémoires de l'Académie Impériale des Sciences de St. Pétersbourg, série. 7, 25:1–147.Google Scholar
Morikawa, R. and Suzuki, Y. 1961. Fusulinids from the Akasaka Limestone (Part 2). Science Reports of the Saitama University, series B, 4:43–74.Google Scholar
Neumayr, M. 1887. Die natürlichen Verwandtschaftsverhältnisse der schalentragenden Foraminiferen. Sitzungsberichte der K. Akademie der Wissenschaften in Wien, Mathematisch-Naturwissenschaftliche Klasse, 95:156–186.Google Scholar
Nikitina, A. P. 1969. The genus Hemigordiopsis (Foraminifera) in the upper Permian of the Primorye. Paleontologichesskiy Zhurnal, 1969:63–69. (In Russian)Google Scholar
Nogami, Y. 1958. Fusulinids from the Maizuru Zone, Southwest Japan, Part 1, Ozawainellinae, Schubertellinae and Neoschwagerininae. Memoirs of the College of Science, University of Kyoto, series B, 25:97–115.Google Scholar
Ota, A., Kanmera, K., and Isozaki, Y. 2000. Stratigraphy of the Permian Iwato and Mitai Formations in the Kamura area, Southwest Japan: Maokouan, Wuchiapingian, and Changhsingian carbonates formed on paleo-seamount. The Journal of the Geological Society of Japan, 106:853–864. (In Japanese)CrossRefGoogle Scholar
Ota, A. and Isozaki, Y. 2006. Fusuline biotic turnover across the Guadalupian–Lopingian (middle–upper Permian) boundary in mid-oceanic carbonate buildups: Biostratigraphy of accreted limestone in Japan. Journal of Asian Earth Sciences, 26:353–368.Google Scholar
Ozawa, Y. 1925. Paleontological and stratigraphical studies on the Permo-Carboniferous limestone of Nagato, Part 2, Paleontology. Journal of the College of Science, Imperial University of Tokyo, 45:1–90.Google Scholar
Ozawa, Y. 1927. Stratigraphical studies of the fusulina limestone of Akasaka, Province of Mino. Journal of the Faculty of Science, Imperial University of Tokyo, section 2, 2:121–146.Google Scholar
Pronina-Nestell, G. P. and Nestell, M. K. 2001. Late Changhsingian foraminifers of the northwestern Caucasus. Micropaleontology, 47:205–234.Google Scholar
Reitlinger, E. A. 1965. Foraminiferal development in the late Permian and Early Triassic epochs in the territory of Transcaucasia. Voprosy Mikropaleontologii, 9:45–70. (In Russian)Google Scholar
Reuss, A. E. 1862. Entwurf einer systematischen Zusammenstellung der Foraminiferen. Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften in Wien, Mathematisch-Naturwissenchaftliche Classe (1861), 44:355–396.Google Scholar
Rui, L. 1979. Upper Permian fusulinids from western Guizhou. Acta Palaeintologica Sinica, 18:271–297. (In Chinese)Google Scholar
Rui, L. and Sheng, J. Z. 1981. On the genus Palaeofusulina. Geological Society of America, Special Paper 187, 33–37.Google Scholar
Rui, L., Zhao, J. M., Mu, X. N., Wang, K. L., and Wang, Z. H. 1984. Restudies of the Wujiaping limestone from Liangshan, Shaanxi. Journal of Stratigraphy, 8:179–193. (In Chinese)Google Scholar
Rzehak, A. 1885. Bemerkungen über einige Foraminiferen der Oligocän Formation. Verhandlungen des Naturforschenden Vereins in Brünn (1884), 23:123–129.Google Scholar
Saidova, K. M. 1981. On an up-to-date system of supraspecific taxonomy of Cenozoic benthic foraminifers. InRauser-Chernousova, D. M., Isakova, T. N., and Reitlinger, E. A.(eds.), Institut Okeanologii P. P. Shirshova, Akademiya Nauk SSSR, Moscow, 73 p. (In Russian)Google Scholar
Saito, M., Kambe, N., and Katada, M. 1958. Geology of the Mitai district, with geological sheet map at 1:50,000. Geological Survey of Japan, Kawasaki, 91 p. (In Japanese)Google Scholar
Sano, H. and Nakashima, K. 1997. Lowest Triassic (Griesbachian) microbial bindstone-cementstone facies, Southwest Japan. Facies, 36:1–24.Google Scholar
Schultze, M. S. 1854. Über den Organismus der Polythalamien (Foraminiferen), nebst Bermerkungen über die Rhizopoden im Allgemeinen. Wilhelm Engelman, Leipzig, 68 p.Google Scholar
Sheng, J. C. 1955. Some fusulinids from the Changhsing Limestone. Acta Palaeontologica Sinica, 3:287–308.Google Scholar
Sheng, J. C. 1963. Permian fusulinids of Kwangsi, Kueichow and Szechuan. Palaeontologica Sinica, new series B, 10:1–247.Google Scholar
Sheng, J. C. and Chang, L. H. 1958. Fusulinids from the type locality of Changhsing Limestone. Acta Palaeontologica Sinica, 6:205–214.Google Scholar
Skinner, J. W. 1931. Primitive fusulinids of the Mid-Continent region. Journal of Paleontology, 5:253–259.Google Scholar
Skinner, J. W. and Wilde, G. 1966. Permian Fusulinids from Pacific Northwest and Alaska. The University of Kansas Paleontological Contributions, Paper 4, 59 p.Google Scholar
Stanley, S. M. and Yang, X. N. 1994. A double mass extinction at the end of the Paleozoic Era. Science, 266:1340–1344.Google Scholar
Tazawa, J. and Hasegawa, Y. 2007. Permian fusulinoideans from the Atagoyama Formation of Choshi, Chiba Prefecture, central Japan. The Journal of the Geological Society of Japan, 113:406–416. (In Japanese)Google Scholar
Thompson, M. L. and Wheeleer, H. E. 1942. Permian fusulinids from British Columbia, Washington, and Oregon. Journal of Paleontology, 16:700–711.Google Scholar
Thompson, M. L., Wheeleer, H. E., and Danner, W. R. 1950. Middle and upper Permian fusulinids of Washington and British Columbia. Contribution from the Cushman Foundation for Foraminiferal Research, 1:46–63.Google Scholar
Toriyama, R. 1958. Geology of Akiyoshi, Part 3. Fusulinids of Akiyoshi. Memoirs of the Faculty of Science, Kyushu University, Ser. D, 7:1–246.Google Scholar
Vachard, D., Rettori, R., Angiolini, L., and Checconi, A. 2008. Glomomidiella gen. n. (Foraminifera, Mioliolata, Neodiscidae): A new genus from the late Guadalupian–Lopingian of Hydra Island (Greece). Rivista Italiana di Paleontologia e Stratigrafia, 114:349–361.Google Scholar
Wang, K. 1976. The foraminifera from the Changsing Formation in western Guizhou. Acta Palaeontologica Sinica, 15:187–194. (In Chinese)Google Scholar
Wang, K. and Sun, X. 1973. Carboniferous and Permian foraminifera of the Chinling Range and its geologic significance. Acta Geologica Sinica, 2:137–178. (In Chinese)Google Scholar
Watanabe, K., Kanmera, K., and Nakashima, K. 1979. Conodont biostratigraphy in the Kamura Limestone (Triassic), Takachiho-cho, Nishiusuki-gun, Miyazaki Prefecture,. p. 127–137. InKoike, T. and Igo, H.(eds.), Biostratigraphy of Permian and Triassic Conodonts and Holothurian Sclerites in Japan, Commemoration vol. of Retirement of Professor Mosaburo Kanuma, Koganei, Tokyo. (In Japanese)Google Scholar
Wedekind, P. R. 1937. Einführung in die Grundlagen der historischen Geologie. Band, Mikrobiostratigraphie die Korallen- und Foraminiferenzeit. Ferdinand Enke, Stuttgart, 136 p.Google Scholar
Wignall, P. B. 2001. Large igneous provinces and mass extinctions. Earth-Science Reviews, 53:1–33.CrossRefGoogle Scholar
Working Group on the Permian–Triassic Systems. 1975. Stratigraphy near the Permian–Triassic boundary in Japan and its correlation. Journal of the Geological Society of Japan, 81:165–184. (In Japanese)Google Scholar
Yabe, H. 1906. A contribution to the genus Fusulina, with notes on fusulina limestone from Korea. Journal of College of Science, Imperial University of Tokyo.Google Scholar
Zhou, M., Malpas, J., Song, X., Robinson, P. T., Sun, M., Kennedy, A. K., Lesher, C. M., and Keays, R. R. 2002. A temporal link between the Emeishan large igneous province (southwest China) and end-Guadalupian mass extinction. Earth and Planetary Science Letters, 196:113–122.CrossRefGoogle Scholar