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DOI | 10.1038/s41467-021-27054-5 |
Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary | |
Ao H.; Rohling E.J.; Zhang R.; Roberts A.P.; Holbourn A.E.; Ladant J.-B.; Dupont-Nivet G.; Kuhnt W.; Zhang P.; Wu F.; Dekkers M.J.; Liu Q.; Liu Z.; Xu Y.; Poulsen C.J.; Licht A.; Sun Q.; Chiang J.C.H.; Liu X.; Wu G.; Ma C.; Zhou W.; Jin Z.; Li X.; Li X.; Peng X.; Qiang X.; An Z. | |
发表日期 | 2021 |
ISSN | 2041-1723 |
卷号 | 12期号:1 |
英文摘要 | Across the Miocene–Pliocene boundary (MPB; 5.3 million years ago, Ma), late Miocene cooling gave way to the early-to-middle Pliocene Warm Period. This transition, across which atmospheric CO2 concentrations increased to levels similar to present, holds potential for deciphering regional climate responses in Asia—currently home to more than half of the world’s population— to global climate change. Here we find that CO2-induced MPB warming both increased summer monsoon moisture transport over East Asia, and enhanced aridification over large parts of Central Asia by increasing evaporation, based on integration of our ~1–2-thousand-year (kyr) resolution summer monsoon records from the Chinese Loess Plateau aeolian red clay with existing terrestrial records, land-sea correlations, and climate model simulations. Our results offer palaeoclimate-based support for ‘wet-gets-wetter and dry-gets-drier’ projections of future regional hydroclimate responses to sustained anthropogenic forcing. Moreover, our high-resolution monsoon records reveal a dynamic response to eccentricity modulation of solar insolation, with predominant 405-kyr and ~100-kyr periodicities between 8.1 and 3.4 Ma. © 2021, The Author(s). |
语种 | 英语 |
scopus关键词 | aridification; global warming; human activity; hydrology; Miocene; paleoclimate; Pliocene; Central Asia; China; Far East; Loess Plateau |
来源期刊 | Nature Communications
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/250565 |
作者单位 | State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China; Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China; Research School of Earth Sciences, Australian National University, Canberra, ACT, Australia; Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton, United Kingdom; Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; Institute of Geosciences, Christian-Albrechts-University, Kiel, Germany; Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI, United States; Laboratoire des Sciences du Climat et de l’Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, 91191, France; Géosciences Rennes, UMR-CNRS 6118, University Rennes, Rennes, France; Department of Geosciences, Potsdam University, Potsdam, Germany; Pa... |
推荐引用方式 GB/T 7714 | Ao H.,Rohling E.J.,Zhang R.,等. Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary[J],2021,12(1). |
APA | Ao H..,Rohling E.J..,Zhang R..,Roberts A.P..,Holbourn A.E..,...&An Z..(2021).Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary.Nature Communications,12(1). |
MLA | Ao H.,et al."Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary".Nature Communications 12.1(2021). |
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