Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary

Hong Ao; Eelco J. Rohling; Ran Zhang; Andrew P. Roberts; Ann E. Holbourn; Jean Baptiste Ladant; Guillaume Dupont-Nivet; Wolfgang Kuhnt; Peng Zhang; Feng Wu; Mark J. Dekkers; Qingsong Liu; Zhonghui Liu; Yong Xu; Christopher J. Poulsen; Alexis Licht; Qiang Sun; John C.H. Chiang; Xiaodong Liu; Guoxiong Wu; Chao Ma; Weijian Zhou; Zhangdong Jin; Xinxia Li; Xinzhou Li; Xianzhe Peng; Xiaoke Qiang; Zhisheng An

doi:10.1038/s41467-021-27054-5

Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary

Hong Ao
, Eelco J. Rohling
, Ran Zhang
, Andrew P. Roberts
, Ann E. Holbourn
, Jean Baptiste Ladant
, Guillaume Dupont-Nivet
, Wolfgang Kuhnt
, Peng Zhang
, Feng Wu
, Mark J. Dekkers
, Qingsong Liu
, Zhonghui Liu
, Yong Xu
, Christopher J. Poulsen
, Alexis Licht
, Qiang Sun
, John C.H. Chiang
, Xiaodong Liu
, Guoxiong Wu

Chao Ma, Weijian Zhou, Zhangdong Jin, Xinxia Li, Xinzhou Li, Xianzhe Peng, Xiaoke Qiang, Zhisheng An

CAS - Institute of Earth Environment
Pilot National Laboratory for Marine Science and Technology
Australian National University
University of Southampton
CAS - Institute of Atmospheric Physics
Kiel University
University of Michigan, Ann Arbor
Université Paris-Saclay
Géosciences Rennes
University of Potsdam
Utrecht University
Southern University of Science and Technology
The University of Hong Kong
China Geological Survey
University of Washington
Xi'an University of Science and Technology
University of California at Berkeley
Chengdu University of Technology
China University of Geosciences, Wuhan
Nanjing University

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83 引用（Scopus）

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.

源语言	英语
文章编号	6935
期刊	Nature Communications
卷	12
期	1
DOI	https://doi.org/10.1038/s41467-021-27054-5
出版状态	已出版 - 12月 2021
已对外发布	是

联合国可持续发展目标

此成果有助于实现下列可持续发展目标：

可持续发展目标 13 气候行动

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10.1038/s41467-021-27054-5

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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., ... An, Z. (2021). Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary. Nature Communications, 12(1), 文章 6935. https://doi.org/10.1038/s41467-021-27054-5

@article{fcd1166e228a4d12bfedcad6c70338cc,

title = "Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary",

abstract = "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{\textquoteright}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 \textasciitilde{}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 {\textquoteleft}wet-gets-wetter and dry-gets-drier{\textquoteright} 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 \textasciitilde{}100-kyr periodicities between 8.1 and 3.4 Ma.",

author = "Hong Ao and Rohling, \{Eelco J.\} and Ran Zhang and Roberts, \{Andrew P.\} and Holbourn, \{Ann E.\} and Ladant, \{Jean Baptiste\} and Guillaume Dupont-Nivet and Wolfgang Kuhnt and Peng Zhang and Feng Wu and Dekkers, \{Mark J.\} and Qingsong Liu and Zhonghui Liu and Yong Xu and Poulsen, \{Christopher J.\} and Alexis Licht and Qiang Sun and Chiang, \{John C.H.\} and Xiaodong Liu and Guoxiong Wu and Chao Ma and Weijian Zhou and Zhangdong Jin and Xinxia Li and Xinzhou Li and Xianzhe Peng and Xiaoke Qiang and Zhisheng An",

note = "Publisher Copyright: {\textcopyright} 2021, The Author(s).",

year = "2021",

month = dec,

doi = "10.1038/s41467-021-27054-5",

language = "英语",

volume = "12",

journal = "Nature Communications",

issn = "2041-1723",

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number = "1",

}

Ao, H, Rohling, EJ, Zhang, R, Roberts, AP, Holbourn, AE, Ladant, JB, Dupont-Nivet, G, Kuhnt, W, Zhang, P, Wu, F, Dekkers, MJ, Liu, Q, Liu, Z, Xu, Y, Poulsen, CJ, Licht, A, Sun, Q, Chiang, JCH, Liu, X, Wu, G, Ma, C, Zhou, W , Jin, Z, Li, X, Li, X, Peng, X, Qiang, X & An, Z 2021, 'Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary', Nature Communications, 卷 12, 号码 1, 6935. https://doi.org/10.1038/s41467-021-27054-5

TY - JOUR

T1 - Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary

AU - Ao, Hong

AU - Rohling, Eelco J.

AU - Zhang, Ran

AU - Roberts, Andrew P.

AU - Holbourn, Ann E.

AU - Ladant, Jean Baptiste

AU - Dupont-Nivet, Guillaume

AU - Kuhnt, Wolfgang

AU - Zhang, Peng

AU - Wu, Feng

AU - Dekkers, Mark J.

AU - Liu, Qingsong

AU - Liu, Zhonghui

AU - Xu, Yong

AU - Poulsen, Christopher J.

AU - Licht, Alexis

AU - Sun, Qiang

AU - Chiang, John C.H.

AU - Liu, Xiaodong

AU - Wu, Guoxiong

AU - Ma, Chao

AU - Zhou, Weijian

AU - Jin, Zhangdong

AU - Li, Xinxia

AU - Li, Xinzhou

AU - Peng, Xianzhe

AU - Qiang, Xiaoke

AU - An, Zhisheng

PY - 2021/12

Y1 - 2021/12

N2 - 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.

AB - 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.

UR - https://www.scopus.com/pages/publications/85119957827

U2 - 10.1038/s41467-021-27054-5

DO - 10.1038/s41467-021-27054-5

M3 - 文章

C2 - 34836960

AN - SCOPUS:85119957827

SN - 2041-1723

VL - 12

JO - Nature Communications

JF - Nature Communications

IS - 1

M1 - 6935

ER -

Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary

摘要

联合国可持续发展目标

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