Lake-Level Oscillation Based on Sediment Strata and Geochemical Proxies Since 11,000 Year From Tengger Nuur, Inner Mongolia, China-Reference-Cited by-同舟云学术

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Lake-Level Oscillation Based on Sediment Strata and Geochemical Proxies Since 11,000 Year From Tengger Nuur, Inner Mongolia, China

Published:2020-08-07 Issue: Volume:8 Page:
ISSN:2296-6463
Container-title:Frontiers in Earth Science
language:
Short-container-title:Front. Earth Sci.

Author:

Chengjun Zhang,Li Zhang,Wanyi Zhang,Yunhan Tao,Yang Liu,Xiangling Wan,Zhen Zhang,Khomid Safarov

Funder

National Natural Science Foundation of China

Publisher

Frontiers Media SA

Subject

General Earth and Planetary Sciences

Reference85 articles.

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2. The history and variability of the East Asian paleomonsoon climate.;An;Quat. Sci.Rev.,2000

3. Consistently large marine reservoir ages in the Norwegian Sea during the Last Deglaciation.;Björck;Quat. Sci. Rev.,2003

4. Persistent solar influence on North Atlantic climate during the Holocene.;Bond;Science,2001

5. The Dry holocene megathermal in inner Mongolia.;Chen;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2003

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1. The late Holocene hydroclimate variability in the Northwest Himalaya: Sedimentary clues from the Wular Lake, Kashmir Valley;Journal of Asian Earth Sciences;2022-05

2. Late Holocene climate variation on the northern Tibetan Plateau inferred from Lake Ayakum;CATENA;2021-12

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