Evidence for a Relatively Warm Mid‐to Late Holocene on the Southeastern Tibetan Plateau-Reference-Cited by-同舟云学术

Evidence for a Relatively Warm Mid‐to Late Holocene on the Southeastern Tibetan Plateau

Published:2022-08-12 Issue:15 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Feng Xiaoping¹²^ORCID,Zhao Cheng³^ORCID,D'Andrea William J.⁴,Hou Juzhi¹²^ORCID,Yang Xiangdong⁵^ORCID,Xiao Xiayun⁵,Shen Ji³,Duan Yanwu¹²,Chen Fahu¹²

Affiliation:

1. State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE) Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing China

2. Alpine Paleoecology and Human Adaptation Group (ALPHA) Institute of Tibetan Plateau Research CAS Beijing China

3. School of Geography and Ocean Science Nanjing University Nanjing China

4. Lamont‐Doherty Earth Observatory of Columbia University Palisades NY USA

5. State Key Laboratory of Lake Science and Environment Nanjing Institute of Geography and Limnology Chinese Academy of Science Nanjing China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL098740

Reference75 articles.

1. Holocene warming in western continental Eurasia driven by glacial retreat and greenhouse forcing

2. Persistent Solar Influence on North Atlantic Climate During the Holocene

3. Seasonal origin of the thermal maxima at the Holocene and the last interglacial

4. Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode

5. Holocene volcanic history as recorded in the sulfate stratigraphy of the European Project for Ice Coring in Antarctica Dome C (EDC96) ice core

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