Hostname: page-component-586b7cd67f-r5fsc Total loading time: 0 Render date: 2024-11-26T08:06:09.715Z Has data issue: false hasContentIssue false
  • English
  • Français

Asian dust from land to sea: processes, history and effect from modern observation to geological records

Published online by Cambridge University Press:  18 May 2020

Shiming Wan ,
Youbin Sun  and
Kana Nagashima
Shiming Wan*
Affiliation:
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao266071, China CAS Center for Excellence in Quaternary Science and Global Change, Xi’an710061, China Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao266061, China
Youbin Sun
Affiliation:
CAS Center for Excellence in Quaternary Science and Global Change, Xi’an710061, China State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an710061, China
Kana Nagashima
Affiliation:
Research Institute for Global Change (RIGC), JAMSTEC, Yokosuka, Japan
*
Author for correspondence:[email protected] (S. Wan); [email protected] (Y. Sun); [email protected] (K. Nagashima)
Rights & Permissions [Opens in a new window]

Abstract

Production, transport and deposition of aeolian dust from land to sea closely interact with regional environment and global climate. This Special Issue addresses transport of aeolian dust from the Asian inland to the Loess Plateau and North Pacific Ocean and their possible links to oceanic ecosystem, global climate and even human activity, over various timescales. The papers in this volume are multidisciplinary in nature and include sedimentology, mineralogy, geochemistry, environmental magnetism and climate modelling on multi-timescales from interannual, glacial–interglacial to tectonic timescales. Based on modern observation, geological records and modelling, this Special Issue offers new insights especially into aeolian provenance, dynamics controls on dust production, a novel marine aeolian proxy, as well as long-term aeolian input to the marginal basins of NE Asia and its influence on oceanic productivity. This issue provides a good example for future comprehensive studies of source-to-sink processes of Asian dust from land to sea.

Keywords

aeolian dustAsian inlandNorth Pacificsource-to-sinkcarbon cycleclimate change
Type
Preface
Information
Geological Magazine , Volume 157 , Special Issue 5: Asian dust from land to sea: processes, history and effect , May 2020 , pp. 701 - 706
Copyright
© Cambridge University Press 2020

1. Introduction

Aeolian dust, defined as terrestrial materials transported by atmospheric circulation, is a major erosional product of arid land and a significant component of deep-sea sediments (Liu, 1985; Rea, Reference Rea1994). Understanding how aeolian dust cycle interacts with the climate system has been a frontier research topic in Earth science in recent years (Jickells et al. Reference Jickells, An, Andersen, Baker, Bergametti, Brooks, Cao, Boyd, Duce, Hunter, Kawahata, Kubilay, La Roche, Liss, Mahowald, Prospero, Ridgwell, Tegen and Torres2005; Martínez-Garcia et al. Reference Martínez-Garcia, Rosell-Melé, Jaccard, Geibert, Sigman and Haug2011; Jacobel et al. Reference Jacobel, Anderson, Winckler, Costa, Gottschalk, Middleton, Pavia, Shoenfelt and Zhou2019). Modern observations, model simulations and sediment records demonstrate that the production, emission and deposition of aeolian dust are closely linked to Earth’s climate state (Ding et al. Reference Ding, Yu, Rutter and Liu1994; Shao et al. Reference Shao, Wyrwoll, Chappell, Huang, Lin, McTainsh, Mikami, Tanaka, Wang and Yoon2011; An, Reference An2014; Sun et al. Reference Sun, Yin, Crucifix, Clemens, Araya-Melo, Liu, Qiang, Liu, Zhao, Liang, Chen, Li, Zhang, Dong, Li, Zhou, Berger and An2019 and references therein). A dustier Earth during glacial periods is usually associated with greater aridity in source regions, less vegetation and stronger winds (Lambert et al. Reference Lambert, Delmonte, Petit, Bigler, Kaufmann, Hutterli, Stocker, Ruth, Steffensen and Maggi2008; Winckler et al. Reference Winckler, Anderson, Fleisher, McGee and Mahowald2008; Muhs, Reference Muhs2013). On the other hand, dust can influence climate directly, by the reflecting and absorption of solar radiation, or indirectly, by modifying cloud properties (Forster et al. Reference Forster, Ramaswamy, Artaxo, Berntsen, Betts, Fahey, Haywood, Lean, Lowe, Myhre, Nganga, Prinn, Raga, Schulz, Van Dorland, Solomon, Qin, Manning, Chen, Marquis, Averyt, Tignor and Miller2007; Maher et al. Reference Maher, Prospero, Mackie, Gaiero, Hesse and Balkanski2010). Dust transported to the oceans can also affect climate via ocean fertilization, as mineral dust containing iron can modulate the uptake of carbon in marine ecosystems and thus potentially influence the atmospheric CO2 concentration and thus global climate (Martin, Reference Martin1990; Jickells et al. Reference Jickells, An, Andersen, Baker, Bergametti, Brooks, Cao, Boyd, Duce, Hunter, Kawahata, Kubilay, La Roche, Liss, Mahowald, Prospero, Ridgwell, Tegen and Torres2005; Boyd et al. Reference Boyd, Jickells, Law, Blain, Boyle, Buesseler, Coale, Cullen, de Baar, Follows, Harvey, Lancelot, Levasseur, Owens, Pollard, Rivkin, Sarmiento, Schoemann, Smetacek, Takeda, Tsuda, Turner and Watson2007; Murray et al. Reference Murray, Leinen and Knowlton2012; Tagliabue et al. Reference Tagliabue, Bowie, Boyd, Buck, Johnson and Saito2017). The global distribution of monthly mean total iron concentration is closely correlated to the dust flux to the world oceans (Fig. 1a, b), suggesting a dominant control over iron release to the deep sea by dust inputs.

Fig 1. (a) Global distribution of the world’s major deserts and dust emissions. The magnitudes of dust emission from different regions are given in Mt and indicated by bars (Tanaka & Chiba, Reference Tanaka and Chiba2006; Shao et al. Reference Shao, Wyrwoll, Chappell, Huang, Lin, McTainsh, Mikami, Tanaka, Wang and Yoon2011). The main routes of dust transport are indicated by black arrows. The global distribution of monthly mean total iron concentration (μg m−3) (colour spectrum) and the dust flux (g cm−2 a−1) (dotted line) to the world oceans are from Hamilton et al. (Reference Hamilton, Scanza, Feng, Guinness, Kok, Li, Liu, Rathod, Wan, Wu and Mahowald2019) and Jickells et al. (Reference Jickells, An, Andersen, Baker, Bergametti, Brooks, Cao, Boyd, Duce, Hunter, Kawahata, Kubilay, La Roche, Liss, Mahowald, Prospero, Ridgwell, Tegen and Torres2005), respectively. Note the major contribution of Asian dust to the North Pacific. (b) Location map showing major geography of Asia-Pacific and the studied sites in this issue. The sediment sites and aerosol dust sites are indicated by blue dots and open black circles, respectively. Some important sites mentioned in this issue are also shown. The legends of iron concentration and dust flux are the same as in (a). Abbreviations: TK, Taklimakan Desert; Q, Qaidam basin; Or, Ordos Desert; CLP, Chinese Loess Plateau; JS, Japan Sea; SCS, South China Sea; WPS, West Philippine Sea; EAWM, East Asian winter monsoon; EASM, East Asian summer monsoon. The red, white and blue arrows indicate general wind directions of westerlies, EAWM and EASM, respectively.

Asia is the second largest dust source region in the world, with ∼600 Mt and ∼70 Mt annual dust emissions to the atmosphere and ocean, respectively (Fig. 1a) (Shao et al. Reference Shao, Wyrwoll, Chappell, Huang, Lin, McTainsh, Mikami, Tanaka, Wang and Yoon2011). Observational evidence implies that aeolian dust originating from Asia has a significant influence over the marine and continental environment, as well as global climate (Rea, Reference Rea1994; Tanaka & Chiba, Reference Tanaka and Chiba2006; Uno et al. Reference Uno, Eguchi, Yumimoto, Takemura, Shimizu, Uematsu, Liu, Wang, Hara and Sugimoto2009). With the aid of atmospheric circulation (i.e. East Asian winter monsoon and westerlies) (Fig. 1b), aeolian dust from the Asian desert regions has been transported eastward to the Chinese Loess Plateau (Liuet al. 1985), wide areas of the Pacific Ocean (Duce et al. Reference Duce, Liss, Merrill, Atlas, Buat-Menard, Hicks, Miller, Prospero, Arimoto, Church, Ellis, Galloway, Hanson, Jickells, Knap, Reinhardt, Schneider, Sondine, Tokos, Tsungai, Wollast and Zhou1991; Rea, Reference Rea1994; Nagashima et al. Reference Nagashima, Tada, Matsui, Irino, Tani and Toyoda2007; Winckler et al. Reference Winckler, Anderson, Fleisher, McGee and Mahowald2008; Wan et al. Reference Wan, Yu, Clift, Sun, Li and Li2012) and has reached North America (McKendry et al. Reference McKendry, Hacker, Stull, Sakiyama, Mignacca and Reid2001) and even Greenland (Biscaye et al. Reference Biscaye, Grousset, Revel, VanderGaast, Zielinski, Vaars and Kukla1997; Uno et al. Reference Uno, Eguchi, Yumimoto, Takemura, Shimizu, Uematsu, Liu, Wang, Hara and Sugimoto2009). While our knowledge of the Asian aeolian sources, transport and deposition has greatly advanced in the last 30 years (An, 2014; Sun et al. Reference Sun, Yan, Nie, Li, Shi, Qiang, Chang and An2020), large uncertainties and knowledge gaps, especially about the impacts and interactions of aeolian dust with the regional- and global-scale biogeochemical cycles, still exist (Tagliabue et al. Reference Tagliabue, Bowie, Boyd, Buck, Johnson and Saito2017; Jacobel et al. Reference Jacobel, Anderson, Winckler, Costa, Gottschalk, Middleton, Pavia, Shoenfelt and Zhou2019), partly because of a lack of comprehensive studies on source-to-sink processes of Asian dust from land to sea.

Asian topography has dramatically changed during the Cenozoic, with the progressive uplift of the Himalaya and Tibetan Plateau and the westward retreat of Paratethys (Prell & Kutzbach, Reference Prell and Kutzbach1992; Ramstein et al. Reference Ramstein, Fluteau, Besse and Joussaume1997; Wang, Reference Wang, Clift, Wang and Kuhnt2004). At the same time global climate gradually cooled after the Eocene (Zachos et al. Reference Zachos, Pagani, Sloan, Thomas and Billups2001). Driven by both tectonic uplift and global cooling, Asian inland areas experienced a long-term drying, eventually resulting in development of deserts and extensive deposition of loess in Central Asia during the Oligocene to Miocene (Guo et al. Reference Guo, Ruddiman, Hao, Wu, Qiao, Zhu, Peng, Wei, Yuan and Liu2002; Zheng et al. Reference Zheng, Wei, Tada, Clift, Wang, Jourdan, Wang and He2015; Shen et al. Reference Shen, Wan, France-Lanord, Clift, Tada, Révillon, Shi, Zhao, Liu, Yin, Song and Li2017). This general geological background determines the production, emission, transport and deposition of Asian dust from land to sea from the geological past to present (Fig. 2). The huge dust inputs from Asia to the North Pacific supply large amounts of macronutrients (N, P and Si) and micronutrients (e.g. Fe, Mn and Cd) that are essential for phytoplankton growth (Jickells et al. Reference Jickells, An, Andersen, Baker, Bergametti, Brooks, Cao, Boyd, Duce, Hunter, Kawahata, Kubilay, La Roche, Liss, Mahowald, Prospero, Ridgwell, Tegen and Torres2005). The influence of Asian dust on oceanic biogeochemical processes, global carbon cycle and climate change is potentially significant (Fig. 2) (Han et al. Reference Han, Zhao, Song, Fang, Yin, Deng, Wang and Fan2011), but not well understood, which was the initial motivation for this Special Issue we have organized.

Fig. 2. Schematic representation of processes and effects of aeolian dust from Asian land to the North Pacific in the context of Cenozoic uplift of Himalaya and Tibetan Plateau and general drying of the Asian interior. The possible influence of dust iron on oceanic biogeochemical cycle is modified from Martínez-García & Winckler (Reference Martínez-García and Winckler2014). Note the significant role of iron fertilization in the carbon cycle through stimulating oceanic primary productivity, CO2 uptake and burial of organic carbon in deep-sea sediments.

Great spatial (Asian interior to the Pacific) and temporal (modern to the Miocene) span is the main feature of this Special Issue (Fig. 1b). Ten papers address the transport processes and sedimentary records of Asian aeolian dust from the arid interior (Taklimakan Desert) to the Chinese Loess Plateau, marginal basins of NE Asia, the west Philippine Sea and the North Pacific, as well as their possible links to oceanic ecosystem, global climate and even human activity. This issue involves studies over multiple timescales (from interannual, glacial–interglacial to tectonic timescales) of Asian aeolian dust transportation from land to sea. New insights and the significant details from these contributions are outlined below in order of timescale.

2. Modern Asian dust from land to sea

In their contribution Yuko et al. (Reference Yuko, Ryuji, Sun, Zheng, Naomi, Akinori and Hitoshi2020) study the origin of aeolian dust emitted from the Tarim Basin, which is considered to be one of the main sources of fine-grained dust in the northern hemisphere. However, it is unclear whether the source of dust emitted from the Tarim Basin is the Taklimakan or the Gobi Desert and mountain rivers around the basin, as the Gobi and fluvial sources produce more fine-grained detritus than the Taklimakan Desert. They analyse the electron spin resonance (ESR) signal intensity and Crystallinity Index (CI) of quartz from sediment samples of the potential sources surrounding the Tarim Basin. The converged values of the ESR intensity (7.2 ± 5.5) and CI (8.8 ± 0.2) of the fine silt of sediments from the rivers draining the Kunlun and Altyn mountains are similar to those of the aeolian dust emitted from the Tarim Basin, confirming their major contribution to that depocentre. This study highlights the importance of repeated cycling by fluvial and wind processes within the basin to produce homogeneous aeolian dust, which can be further transported to the Loess Plateau and North Pacific.

The west Philippine Sea has been suggested as one of the important sinks of dust transported from the Asian interior by winds. This is largely based on provenance analysis of mixed sediments (i.e. dust, volcanic and authigenic materials) deposited in the deep sea (e.g. Kolla et al. Reference Kolla, Nadler and Bonatti1980; Wan et al. Reference Wan, Yu, Clift, Sun, Li and Li2012; Xu et al. Reference Xu, Li, Clift, Lim, Wan, Chen, Tang, Jiang and Xiong2015), rather than pure dust collected in the air and/or water column by sediment traps, although the latter provides more reliable information on dust. Wang et al. (Reference Wang, Xu, Li, Wan, Cai, Chen, Sun and Lim2020, this issue) investigate the microscopic mineralogy, trace elements and Sr–Nd isotopic compositions of modern dust samples collected in the air and seawater of the west Philippine Sea in 2014–15. The detrital minerals quartz, feldspar and gypsum show similar microscopic characteristics indicative of wind erosion (subangular to sub-round). Provenance analysis based on trace element and Sr–Nd isotopic compositions demonstrates that the modern aeolian dust deposited in the Philippine Sea mainly originates from the Ordos Desert (>80%), with minor supply from the Taklimakan Desert (<20%). Wind back-trajectories suggest that the dust was transported by the East Asian winter monsoon to the sea in 1 week. This result improves our understanding of modern Asian dust source-to-sink processes from land to sea.

Asian dust aerosols carried during some severe spring dust storms can be transported over long distances, even around the globe in a few days (Uno et al. Reference Uno, Eguchi, Yumimoto, Takemura, Shimizu, Uematsu, Liu, Wang, Hara and Sugimoto2009). However, the dominant factors that lead to abrupt changes of dust storm frequency on decadal timescale are not fully understood. Shang & Liu (Reference Shang and Liu2020, this issue) examine the spatial and temporal variations of East Asian dust storm frequency and Arctic sea-ice concentration during 1961–2015 and their possible links. Their results show that the spring dust storm frequency is highly correlated with the preceding winter Arctic sea-ice concentration and both of them experienced a remarkable fluctuating decrease in the past half-century. They further propose a mechanism whereby the Arctic sea-ice loss generates the hemispherical-scale atmospheric teleconnection pattern, including regional-scale circulation anomalies over East Asia and thus results in a reduction in dust storm frequency. This study provides an excellent example how high-latitude climate strongly influences the emission of modern Asian dust.

As an essential micronutrient for marine photosynthetic organisms, iron (Fe) transport to the open ocean primarily originates from terrestrial mineral dust derived from arid regions (Jickells et al. Reference Jickells, An, Andersen, Baker, Bergametti, Brooks, Cao, Boyd, Duce, Hunter, Kawahata, Kubilay, La Roche, Liss, Mahowald, Prospero, Ridgwell, Tegen and Torres2005; Murray et al. Reference Murray, Leinen and Knowlton2012). Due to increased human activity, however, pyrogenic Fe-containing aerosols are another possible source of dissolved iron (DFe) to open ocean (Mahowald et al. Reference Mahowald, Engelstaedter, Luo, Sealy, Artaxo, Benitez-Nelson, Bonnet, Chen, Chuang, Cohen, Dulac, Herut, Johansen, Kubilay, Losno, Maenhaut, Paytan, Prospero, Shank and Siefert2009). Ito et al. (Reference Ito, Ye, Yamamoto, Watanabe and Aita2020, this issue) use one atmospheric chemistry transport model and two ocean biogeochemistry models to investigate the effects of atmospheric deposition of DFe from mineral dust and combustion aerosols on ocean biogeochemistry. The results show a higher sensitivity of net primary production in the North Pacific and North Atlantic to the change in combustion-generated aerosols than to mineral dust, regardless of the relative sedimentary source inputs. This study highlights the influence of the underestimated anthropogenic Fe-containing aerosols on the marine ecosystem in the context of increasing human perturbations.

3. Glacial–interglacial cycles of Asian dust from land to sea

Aeolian flux is widely accepted as a quantitative proxy for assessing the aridity of the dust source region (Rea et al. Reference Rea, Snoechx and Joseph1998; Winckler et al. Reference Winckler, Anderson, Fleisher, McGee and Mahowald2008; An, Reference An2014). However, the reconstruction of temporal–spatial dust flux variability across the Chinese Loess Plateau on glacial–interglacial timescales is rare because of poor constraints on loess age model and bulk density. Liu et al. (Reference Liu, Liu, Ma, Kang, Qiang, Guo and Sun2020, this issue) are the first to present aeolian flux variations from eight loess–palaeosol sequences dating from 150 ka along two N–S-aligned transects on the Chinese Loess Plateau, based on a uniform age model of high-resolution optically stimulated luminescence (OSL) dating and pedostratigraphic correlation and reliable bulk density data. The aeolian flux results show consistent fluctuations, with higher and more variable values during glacial compared to interglacial periods. There is also a clear spatial increase from the southeastern Chinese Loess Plateau to its northwestern part. The high-resolution stacked aeolian flux records of the Loess Plateau since the Last Glacial Maximum (LGM) not only confirm the dominant control of global ice volume on dust production on glacial–interglacial timescales, but also provide a key curve for refining other dust flux datasets and improve models of past dust–climate interactions.

Sr–Nd isotopes, as robust indicators of sedimentary provenance, have been extensively used to constrain the signal of dust contribution to North Pacific sediments (Ziegler et al. Reference Ziegler, Murray, Hovan and Rea2007; Shen et al. Reference Shen, Wan, France-Lanord, Clift, Tada, Révillon, Shi, Zhao, Liu, Yin, Song and Li2017). Due to high cost and the time-consuming character of the analyses however, there are few high-resolution Sr–Nd isotopes records that can reveal how dust input to the deep sea on orbital timescales covaried with global climate. Zhang et al. (Reference Zhang, Li and Chen2020b, this issue) analyse Sr–Nd isotopes, trace elements and the grain-size of the silicate fraction extracted from sediments at high resolution from Ocean Drilling Program (ODP) Site 1209 in the North Pacific since 500 ka. The results show that a two-end-member mixing model between aeolian dust and dispersed volcanic ash accounts for the provenance. Variations of Nd isotopes mimic global deep-sea oxygen isotopes (LR04 stack) over the past five glacial–interglacial cycles, with lower (higher) εNd values during cooling (warm) periods. They propose that the relative contributions of Asian dust to volcanic ash during the glacial–interglacial cycles are the dominant factor controlling the sawtooth patterns of Nd and Sr isotopes. This study provides a potentially useful chronostratigraphy tool by analysing Nd isotope variations in detrital sediment in the North Pacific, especially for deep-sea sediments deposited below the lysocline (∼3000 m) with no or limited amounts of calcareous microfossils.

Geological records from land to sea indicate that dust fluxes during glacial stages were globally two to five times higher than during interglacials (Maher et al. Reference Maher, Prospero, Mackie, Gaiero, Hesse and Balkanski2010). However, the relative contributions of different forcing factors (i.e. ice volume, sea level, CO2, orbital parameters and underlying surface character) on the dust cycle are not well quantified. Li et al. (Reference Li, Liu and Zhou2020, this issue) conducted a series of sensitivity experiments with an Earth system model to evaluate the effects of various factors on Asian dust emission during the LGM. The simulation results show that the high-latitude ice-sheet extent and abnormal surface erosion in the dust source region were the two main forcing factors, which can cause Asian dust emissions to increase 3.77-fold and 1.25-fold compared to those of the present day, respectively. In contrast, the greenhouse gas content and orbital parameters were relatively weak. This study emphasizes the importance of accurate reconstructions of abnormal surface erosion in addition to considering ice-sheet extent during glacial–interglacial cycles.

4. Tectonic timescale Asian dust input to the Pacific

Effective extraction of an aeolian signal from marine sediment is crucial for further aeolian study. In addition to the conventional mineralogical and geochemical proxies, magnetic parameters (i.e. magnetic susceptibility, hard isothermal remanent magnetization (HIRM)) were also commonly used as indicators of long-term aeolian input to deep-sea sediment (Doh et al. Reference Doh, King and Leinen1988; Rea, Reference Rea1994). However, these proxies usually comprise mixed information derived from all the magnetic particles, including dust, volcanic and biogenic components. Zhang et al. (Reference Zhang, Liu and Sun2020a, this issue) review the study progress on mineral magnetism-related aeolian dust deposition in the North Pacific. They summarize the various magnetic minerals (iron sulphides, ferrimagnetic and antiferromagnetic minerals) with different origins in marine sediments and recommend a novel parameter RelHm+Gt to infer the relative concentration of hematite and goethite, both of which have aeolian origin. The consistent variation of this new magnetic proxy with the chemically extracted aeolian content of sediments at ODP Site 885 in the North Pacific since 2.8 Ma confirm its reliability as a discriminator of aeolian provenance.

Long-term evolution of Asian aeolian dust input to the North Pacific has been investigated for nearly half a century (Rea et al. Reference Rea, Snoechx and Joseph1998 and references therein). However, there are very few similar studies from the marginal basins of NE Asia, which are major sediment sinks on the transport path for Asian dust from land to the North Pacific (Shen et al. Reference Shen, Wan, France-Lanord, Clift, Tada, Révillon, Shi, Zhao, Liu, Yin, Song and Li2017) (Fig. 1). Benefiting from samples recovered by Integrated Ocean Drilling Program (IODP) Expedition 346 with good age controls, Anderson et al. (Reference Anderson, Murray, Dunlea, Giosan, Kinsley, McGee and Tada2020, this issue) analyse the major and trace element contents of sediments from IODP Site U1430 located on the southern upper slope of the eastern Korean Plateau (Fig. 1) to reconstruct variations in aeolian flux since ∼13 Ma. Multivariate partitioning analysis indicates that the Taklimakan Desert was the major sediment source of aeolian dust to the marginal basin, especially before the late Miocene (∼12–8 Ma), while the contribution and flux from the Chinese Loess Plateau and Gobi Desert rapidly increased in the Plio-Pleistocene (since ∼3 Ma). The provenance and flux trend at Site U1430 broadly agree with records elsewhere in the North Pacific. This study suggests that variation in dust source regions appears to track step-wise Asian aridification influenced by Cenozoic global cooling and periods of Tibetan uplift.

Both modern observations and glacial–interglacial-scale deep-sea records have demonstrated the significant influence of aeolian dust on oceanic biogeochemical cycles (Boyd et al. Reference Boyd, Jickells, Law, Blain, Boyle, Buesseler, Coale, Cullen, de Baar, Follows, Harvey, Lancelot, Levasseur, Owens, Pollard, Rivkin, Sarmiento, Schoemann, Smetacek, Takeda, Tsuda, Turner and Watson2007; Murray et al. Reference Murray, Leinen and Knowlton2012). However, how this mechanism might operate on million-years timescales and how it would respond to climate change remains unclear (Martínez-Garcia et al. Reference Martínez-Garcia, Rosell-Melé, Jaccard, Geibert, Sigman and Haug2011). Zhai et al. (Reference Zhai, Wan, Tada, Zhao, Shi, Yin, Tan and Li2020, this issue) examine the evolution of palaeoproductity in the marginal basins of NE Asia and its possible links to Asian dust input using bulk elements geochemistry and the total organic carbon (TOC) content of sediments at IODP Site U1430 (Fig. 1) since 4 Ma, during which the Earth experienced dramatic Northern Hemisphere Glaciation and global cooling. The results show that palaeoproductivity in the basin was greatly enhanced, especially at 3–2 Ma, consistent with rapidly increasing aeolian iron input from the Asian interior to the basin and growth of high-latitude ice sheets. Thus, in turn they propose that the enhanced efficiency of organic carbon burial in the marginal basin might contribute to the coeval decrease of atmospheric pCO2 level and global cooling in the late Pliocene.

5. Conclusion

This Special Issue provides new insights about aeolian provenance, dynamic controls on dust production, novel marine aeolian proxies, as well as long-term aeolian inputs to the marginal seas of NE Asia and its influence on oceanic productivity. In the future, it is suggested that continuous in situ observations of aeolian dust transport and deposition processes from land to sea should be conducted, in order to quantitatively reconstruct long-term evolution of aeolian dust to the West Pacific, and to address any biogeochemical links to the carbon cycle and global Cenozoic cooling. Further data–model comparison would provide robust assessment of dust–climate interactions at different timescales.

Acknowledgements

We thank all the contributors to this Special Issue. We acknowledge the support of journal editor-in-chief Peter D. Clift and editor Susie Cox. We are very grateful for the constructive contribution made to this Special Issue by all the reviewers, without whose help this Special Issue would not be possible. Thanks also go to Debo Zhao for his help in preparing Figure 1. This work was partly supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (XDB40010100), the National Program on Global Change and Air–Sea Interaction (GASI-GEOGE-02/03), National Natural Science Foundation of China (41622603, 41576034, U1606401), the Taishan and Aoshan Talents programme (2017ASTCP-ES01), and the Innovation project of the Qingdao National Laboratory for Marine Science and Technology (2016ASKJ13 and MGQNLM-TD201805).

Conflict of interest

None.

References

An, ZS (ed.) (2014) Late Cenozoic Climate Change in Asia: Loess, Monsoon and Monsoon-arid Environment Evolution. Dordrecht: Springer.CrossRefGoogle Scholar
Anderson, CH, Murray, RW, Dunlea, AG, Giosan, L, Kinsley, CW, McGee, D and Tada, R (2020) Aeolian delivery to Ulleung Basin, Korea (Japan Sea), during development of the East Asian Monsoon through the last 12 Ma. Geological Magazine, this issue.CrossRefGoogle Scholar
Biscaye, PE, Grousset, FE, Revel, M, VanderGaast, S, Zielinski, GA, Vaars, A and Kukla, G (1997) Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, Summit, Greenland. Journal of Geophysical Research – Oceans 102, 26765–81.CrossRefGoogle Scholar
Boyd, PW, Jickells, T, Law, CS, Blain, S, Boyle, EA, Buesseler, KO, Coale, KH, Cullen, JJ, de Baar, HJ, Follows, M, Harvey, M, Lancelot, C, Levasseur, M, Owens, NP, Pollard, R, Rivkin, RB, Sarmiento, J, Schoemann, V, Smetacek, V, Takeda, S, Tsuda, A, Turner, S and Watson, AJ (2007) Mesoscale iron enrichment experiments 1993–2005: synthesis and future directions. Science 315, 612–17.CrossRefGoogle ScholarPubMed
Ding, Z, Yu, Z, Rutter, NW and Liu, TS (1994) Towards an orbital time scale for Chinese loess. Quaternary Science Reviews 13, 39–70.CrossRefGoogle Scholar
Doh, SJ, King, JW and Leinen, M (1988) A rock-magnetic study of giant piston core LL44-GPC3 from the central North Pacific and its paleoceanographic implications. Paleoceanography 3, 89–111.CrossRefGoogle Scholar
Duce, RA, Liss, PS, Merrill, JT, Atlas, EL, Buat-Menard, P, Hicks, BB, Miller, JM, Prospero, JM, Arimoto, R, Church, TM, Ellis, W, Galloway, JN, Hanson, J, Jickells, TD, Knap, AH, Reinhardt, KH, Schneider, B, Sondine, A, Tokos, JJ, Tsungai, S, Wollast, R and Zhou, Met al. (1991) The atmospheric input of trace species to the world ocean. Global Biogeochemical Cycles 5, 193–259.CrossRefGoogle Scholar
Forster, P, Ramaswamy, V, Artaxo, P, Berntsen, T, Betts, R, Fahey, DW, Haywood, J, Lean, J, Lowe, DC, Myhre, G, Nganga, J, Prinn, R, Raga, G, Schulz, M and Van Dorland, R (2007) Changes in atmospheric constituents and in radiative forcing. In Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (eds Solomon, S, Qin, D, Manning, M, Chen, Z, Marquis, M, Averyt, KB, Tignor, M and Miller, HL), pp. 129–234. Cambridge: Cambridge University Press.Google Scholar
Guo, Z, Ruddiman, WF, Hao, Q, Wu, H, Qiao, Y, Zhu, RX, Peng, S, Wei, J, Yuan, B and Liu, T (2002) Onset of Asian desertification by 22Myr ago inferred from loess deposits in China. Nature 416, 159–63.CrossRefGoogle ScholarPubMed
Hamilton, DS, Scanza, RA, Feng, Y, Guinness, J, Kok, JF, Li, L, Liu, X, Rathod, SD, Wan, JS, Wu, M and Mahowald, NM (2019) Improved methodologies for Earth system modelling of atmospheric soluble iron and observation comparisons using the Mechanism of Intermediate complexity for Modelling Iron (MIMI v1.0). Geoscientific Model Development 12, 3835–62.CrossRefGoogle Scholar
Han, Y, Zhao, T, Song, L, Fang, X, Yin, Y, Deng, Z, Wang, S and Fan, S (2011) A linkage between Asian dust, dissolved iron and marine export production in the deep ocean. Atmospheric Environment 45, 4291–8.CrossRefGoogle Scholar
Ito, A, Ye, Y, Yamamoto, A., Watanabe, M. and Aita, MN (2020) Responses of ocean biogeochemistry to atmospheric supply of lithogenic and pyrogenic iron-containing aerosols. Geological Magazine, this issue.CrossRefGoogle Scholar
Jacobel, AW, Anderson, RF, Winckler, G, Costa, KM, Gottschalk, J, Middleton, JL, Pavia, FJ, Shoenfelt, EM and Zhou, Y (2019) No evidence for equatorial Pacific dust fertilization. Nature Geoscience 12, 154–5.CrossRefGoogle Scholar
Jickells, TD, An, ZS, Andersen, KK, Baker, AR, Bergametti, G, Brooks, N, Cao, JJ, Boyd, PW, Duce, RA, Hunter, KA, Kawahata, H, Kubilay, N, La Roche, J, Liss, PS, Mahowald, N, Prospero, JM, Ridgwell, AJ, Tegen, I and Torres, R (2005) Global iron connections between dust, ocean biogeochemistry and climate. Science 308, 67–71.CrossRefGoogle ScholarPubMed
Kolla, V, Nadler, L and Bonatti, E (1980) Clay mineral distributions in surface sediments of the Philippine Sea. Oceanologica Acta 3, 245–50.Google Scholar
Lambert, F, Delmonte, B, Petit, JR, Bigler, M, Kaufmann, PR, Hutterli, MA, Stocker, TF, Ruth, U, Steffensen, JP and Maggi, V (2008) Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core. Nature 452, 616–19.CrossRefGoogle ScholarPubMed
Li, X, Liu, X and Zhou, H (2020) Joint influence of surface erosion and high-latitude ice-sheet extent on Asian dust cycle during the Last Glacial Maximum. Geological Magazine, this issue.CrossRefGoogle Scholar
Liu, TS (ed.) (1985) Loess and the Environment. Beijing: China Ocean Press.Google Scholar
Liu, Y, Liu, X, Ma, L, Kang, S, Qiang, X, Guo, F and Sun, Y (2020) Temporal–spatial variations in aeolian flux on the Chinese Loess Plateau during the last 150 ka. Geological Magazine, this issue.CrossRefGoogle Scholar
Maher, BA, Prospero, JM, Mackie, D, Gaiero, D, Hesse, PP and Balkanski, Y (2010) Global connections between aeolian dust, climate and ocean biogeochemistry at the present day and at the Last Glacial Maximum. Earth-Science Reviews 99, 61–97.CrossRefGoogle Scholar
Mahowald, NM, Engelstaedter, S, Luo, C, Sealy, A, Artaxo, P, Benitez-Nelson, C, Bonnet, S, Chen, Y, Chuang, PY, Cohen, DD, Dulac, F, Herut, B, Johansen, AM, Kubilay, N, Losno, R, Maenhaut, W, Paytan, A, Prospero, JM, Shank, LM and Siefert, RL (2009) Atmospheric iron deposition: global distribution, variability, and human perturbations. Annual Review of Marine Science 1, 245–78.CrossRefGoogle ScholarPubMed
Martin, JH (1990) Glacial-interglacial CO2 change: the iron hypothesis. Paleoceanography 5, 1–13.CrossRefGoogle Scholar
Martínez-Garcia, A, Rosell-Melé, A, Jaccard, SL, Geibert, W, Sigman, DM and Haug, GH (2011) Southern Ocean dust–climate coupling over the past four million years. Nature 476, 312–15.CrossRefGoogle ScholarPubMed
Martínez-García, A and Winckler, G (2014) Iron fertilization in the glacial ocean. PAGES Magazine 22, 82–3.CrossRefGoogle Scholar
McKendry, IG, Hacker, JP, Stull, R, Sakiyama, S, Mignacca, D and Reid, K (2001) Long range transport of Asian dust to the Lower Fraser Valley, British Columbia, Canada. Journal of Geophysical Research-Atmospheres 106, 18361–18370.CrossRefGoogle Scholar
Muhs, DR (2013) The geologic records of dust in the Quaternary. Aeolian Research 9, 3–48.CrossRefGoogle Scholar
Murray, RW, Leinen, M and Knowlton, CW (2012) Links between iron input and opal deposition in the Pleistocene equatorial Pacific Ocean. Nature Geoscience 5, 270–4.CrossRefGoogle Scholar
Nagashima, K, Tada, R, Matsui, H, Irino, T, Tani, A and Toyoda, S (2007) Orbital-and millennial-scale variations in Asian dust transport path to the Japan Sea. Palaeogeography, Palaeoclimatology, Palaeoecology 247, 144–61.CrossRefGoogle Scholar
Prell, WL and Kutzbach, JE (1992) Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature 360, 647–52.CrossRefGoogle Scholar
Ramstein, G, Fluteau, F, Besse, J and Joussaume, S (1997) Effect of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years. Nature 386, 788–95.CrossRefGoogle Scholar
Rea, DK (1994) The paleoclimatic record provided by eolian deposition in the deep sea: the geologic history of wind. Reviews of Geophysics 32, 159–95.CrossRefGoogle Scholar
Rea, DK, Snoechx, H and Joseph, LH (1998) Late Cenozoic eolian deposition in the North Pacific: Asian drying, Tibetan uplift, and cooling of the northern hemisphere. Paleoceanography 13, 215–24.CrossRefGoogle Scholar
Shang, K and Liu, X (2020) Relationship between the sharp decrease in dust storm frequency over East Asia and the abrupt loss of Arctic sea ice in the early 1980s. Geological Magazine, this issue.CrossRefGoogle Scholar
Shao, Y, Wyrwoll, K, Chappell, A, Huang, J, Lin, Z, McTainsh, G, Mikami, M, Tanaka, T, Wang, X and Yoon, S, (2011) Dust cycle: an emerging core theme in Earth system science. Aeolian Research 2, 181–204.CrossRefGoogle Scholar
Shen, X, Wan, S, France-Lanord, C, Clift, PD, Tada, R, Révillon, S, Shi, X, Zhao, D, Liu, Y, Yin, X, Song, Z and Li, A (2017) History of Asian eolian input to the Sea of Japan since 15 Ma: links to Tibetan uplift or global cooling? Earth and Planetary Science Letters 474, 296–308.CrossRefGoogle Scholar
Sun, Y, Yan, Y, Nie, JS, Li, GJ, Shi, ZG, Qiang, XK, Chang, H and An, ZS (2020) Source-to-sink fluctuations of Asian aeolian deposits since the late Oligocene. Earth-Science Reviews 20, 102963.CrossRefGoogle Scholar
Sun, Y, Yin, Q, Crucifix, M, Clemens, SC, Araya-Melo, P, Liu, W, Qiang, X, Liu, Q, Zhao, H, Liang, L, Chen, H, Li, Y, Zhang, L, Dong, G, Li, M, Zhou, W, Berger, A and An, Z (2019) Diverse manifestations of the mid-Pleistocene climate transition. Nature Communications 10, 1–11.Google ScholarPubMed
Tagliabue, A, Bowie, AR, Boyd, PW, Buck, KN, Johnson, KS and Saito, MA (2017) The integral role of iron in ocean biogeochemistry. Nature 543, 51–9.CrossRefGoogle ScholarPubMed
Tanaka, TY and Chiba, M (2006) A numerical study of the contributions of dust source regions to the global dust budget. Global and Planetary Change 52, 88–104.CrossRefGoogle Scholar
Uno, I, Eguchi, K, Yumimoto, K, Takemura, T, Shimizu, A, Uematsu, M, Liu, Z, Wang, Z, Hara, Y and Sugimoto, N (2009) Asian dust transport one full circuit around the globe. Nature Geoscience 20, 557–60.CrossRefGoogle Scholar
Wan, S, Yu, Z, Clift, PD, Sun, H, Li, A and Li, T (2012) History of Asian eolian input to the West Philippine Sea over the last one million years. Palaeogeography, Palaeoclimatology, Palaeoecology 326–328, 152–9.CrossRefGoogle Scholar
Wang, PX (2004) Cenozoic deformation and the history of sea–land interactions in Asia. In Continent–Ocean Interactions in the East Asian Marginal Seas (eds Clift, PD, Wang, PX and Kuhnt, W), pp. 1–22. AGU Geophysical Monograph 149. Washington, DC: American Geophysical Union.Google Scholar
Wang, W, Xu, Z, Li, T, Wan, S, Cai, M, Chen, H, Sun, R and Lim, D (2020) Sources and origins of aeolian dust to the Philippine Sea determined by major minerals and elemental geochemistry. Geological Magazine, this issue.CrossRefGoogle Scholar
Winckler, G, Anderson, RF, Fleisher, MQ, McGee, D and Mahowald, N (2008) Covariant glacial–interglacial dust fluxes in the equatorial Pacific and Antarctica. Science 320, 93–6.CrossRefGoogle ScholarPubMed
Xu, Z, Li, T, Clift, PD, Lim, DI, Wan, S, Chen, H, Tang, Z, Jiang, F and Xiong, Z (2015) Quantitative estimates of Asian dust input to the western Philippine Sea in the mid-late Quaternary and its potential significance for paleoenvironment. Geochemistry, Geophysics, Geosystems 16, 3182–96.CrossRefGoogle Scholar
Yuko, I, Ryuji, T, Sun, Y, Zheng, H, Naomi, S, Akinori, K and Hitoshi, H (2020) Origin of aolian dust emitted from the Tarim Basin based on the ESR signal intensity and Crystallinity Index of quartz: recycling system of fine detrital material within the basin. Geological Magazine, this issue.Google Scholar
Zachos, J, Pagani, M, Sloan, L, Thomas, E and Billups, K (2001) Trends, rhythms, and aberrations in global climate 65Ma to present. Science 292, 686–93.CrossRefGoogle Scholar
Zhai, L, Wan, S, Tada, R, Zhao, D, Shi, X, Yin, X, Tan, Y and Li, A (2020) Links between iron supply from Asian dust and marine productivity in the Japan Sea since four million years ago. Geological Magazine, this issue.CrossRefGoogle Scholar
Zhang, Q, Liu, Q and Sun, Y (2020a) Review of recent developments in aeolian dust signals of sediments from the North Pacific Ocean based on magnetic minerals. Geological Magazine, this issue.CrossRefGoogle Scholar
Zhang, W, Li, G and Chen, J (2020b) The application of Neodymium isotope as a chronostratigraphic tool in North Pacific sediments. Geological Magazine, this issue.CrossRefGoogle Scholar
Zheng, H, Wei, X, Tada, R, Clift, PD, Wang, B, Jourdan, F, Wang, P and He, M (2015) Late Oligocene–early Miocene birth of the Taklimakan Desert. Proceedings of the National Academy of Sciences 112, 7662–7.CrossRefGoogle ScholarPubMed
Ziegler, CL, Murray, RW, Hovan, SA and Rea, DK (2007) Resolving eolian, volcanogenic, and authigenic components in pelagic sediment from the Pacific Ocean. Earth and Planetary Science Letters 254, 416–32.CrossRefGoogle Scholar
Figure 0

Fig 1. (a) Global distribution of the world’s major deserts and dust emissions. The magnitudes of dust emission from different regions are given in Mt and indicated by bars (Tanaka & Chiba, 2006; Shao et al.2011). The main routes of dust transport are indicated by black arrows. The global distribution of monthly mean total iron concentration (μg m−3) (colour spectrum) and the dust flux (g cm−2 a−1) (dotted line) to the world oceans are from Hamilton et al. (2019) and Jickells et al. (2005), respectively. Note the major contribution of Asian dust to the North Pacific. (b) Location map showing major geography of Asia-Pacific and the studied sites in this issue. The sediment sites and aerosol dust sites are indicated by blue dots and open black circles, respectively. Some important sites mentioned in this issue are also shown. The legends of iron concentration and dust flux are the same as in (a). Abbreviations: TK, Taklimakan Desert; Q, Qaidam basin; Or, Ordos Desert; CLP, Chinese Loess Plateau; JS, Japan Sea; SCS, South China Sea; WPS, West Philippine Sea; EAWM, East Asian winter monsoon; EASM, East Asian summer monsoon. The red, white and blue arrows indicate general wind directions of westerlies, EAWM and EASM, respectively.

Figure 1

Fig. 2. Schematic representation of processes and effects of aeolian dust from Asian land to the North Pacific in the context of Cenozoic uplift of Himalaya and Tibetan Plateau and general drying of the Asian interior. The possible influence of dust iron on oceanic biogeochemical cycle is modified from Martínez-García & Winckler (2014). Note the significant role of iron fertilization in the carbon cycle through stimulating oceanic primary productivity, CO2 uptake and burial of organic carbon in deep-sea sediments.