Sedimentary Black Carbon Isotope Record of Holocene Climate Changes on the Northeastern Tibetan Plateau-Reference-Cited by-同舟云学术

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Sedimentary Black Carbon Isotope Record of Holocene Climate Changes on the Northeastern Tibetan Plateau

Published:2022-08 Issue:8 Volume:37 Page:
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanog and Paleoclimatol

Author:

Ning Dongliang¹,Jiang Qingfeng¹^ORCID,Ji Ming²^ORCID,Zheng Jianan²³,Kuai Xiang¹,Ge Ying¹,Xu Yuchen¹,Cheng Longjuan¹^ORCID,Zhao Wenwei¹

Affiliation:

1. School of Geographic Science Nantong University Nantong China

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

3. University of Chinese Academy of Science Beijing China

Funder

National Natural Science Foundation of China

Natural Science Research of Jiangsu Higher Education Institutions of China

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022PA004487

Reference105 articles.

1. The 8k event: cause and consequences of a major Holocene abrupt climate change

2. Holocene climatic instability: A prominent, widespread event 8200 yr ago

3. Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka

4. Asynchronous Holocene optimum of the East Asian monsoon

5. The 5400 a BP extreme weakening event of the Asian summer monsoon and cultural evolution

Cited by 3 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Holocene lake response to glacier and catchment changes on the eastern Tibetan Plateau from quantitative conductivity reconstructions based on sedaDNA-derived macrophyte records;Quaternary Science Reviews;2024-08

2. Changes in lake area and water level in response to hydroclimate variations in the source area of the Yellow River: a case study from Lake Ngoring;Frontiers of Earth Science;2023-12

3. Hostile climate during the Last Glacial Maximum caused sparse vegetation on the north-eastern Tibetan Plateau;Quaternary Science Reviews;2023-02

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