Transition from a warm and dry to a cold and wet climate in NE China across the Holocene-Reference-Cited by-同舟云学术

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Transition from a warm and dry to a cold and wet climate in NE China across the Holocene

Published:2018-07 Issue: Volume:493 Page:36-46
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Zheng Yanhong^ORCID,Pancost Richard D.,Naafs B. David A.^ORCID,Li Qiyuan,Liu Zhao,Yang Huan^ORCID

Funder

National Natural Science Foundation of China

Outstanding Youth Foundation of Shaanxi Province

Marie Curie International Incoming Fellowship

State Key Laboratory of Loess and Quatenary Geology

MOST

ERC

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference107 articles.

1. Asynchronous Holocene optimum of the East Asian monsoon;An;Quat. Sci. Rev.,2000

2. Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka;An;Sci. Rep.,2012

3. Replicated proxy-climate signals over the last 2000 years from two distant peat bogs: new evidence for regional palaeoclimate teleconnections;Barber;Quat. Sci. Rev.,2000

4. Holocene palaeoclimates from peat stratigraphy: macrofossil proxy-climate records from three oceanic raised peat bogs in England and Ireland;Barber;Quat. Sci. Rev.,2003

5. Examining the global distribution of dominant archaeal populations in soil;Bates;ISME J.,2011

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