Vegetation and climate changes since the middle MIS 3 inferred from a Wulagai Lake pollen record, Inner Mongolia, Northeastern China-Reference-Cited by-同舟云学术

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Vegetation and climate changes since the middle MIS 3 inferred from a Wulagai Lake pollen record, Inner Mongolia, Northeastern China

Published:2019-03 Issue: Volume:262 Page:44-51
ISSN:0034-6667
Container-title:Review of Palaeobotany and Palynology
language:en
Short-container-title:Review of Palaeobotany and Palynology

Author:

Li Huashu,Liu Xingqi,Herzschuh Ulrike,Cao Xianyong,Yu Zhitong,Wang Yong

Funder

National Natural Science Foundation of China

German Research Foundation

NSFC

Publisher

Elsevier BV

Subject

Paleontology,Ecology, Evolution, Behavior and Systematics

Reference70 articles.

1. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130,000 years;An;Quat. Res.,1991

2. Agriculture and environmental change at Qingpu, Yangtze delta region, China: a biomarker, stable isotope and palynological approach;Atahan;The Holocene,2007

3. Insolation values for the climate of the last 10 million years;Berger;Quat. Sci. Rev.,1991

4. Flexible paleoclimate age-depth models using an autoregressive gamma process;Blaauw;Bayesian Anal.,2011

5. Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum–Part 1: experiments and large-scale features;Braconnot;Clim. Past,2007

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5. Pollen-based climate changes since the middle MIS 3 in Jilantai Salt Lake in the marginal region of the Asian summer monsoon domain, Inner Mongolia, China;Journal of Asian Earth Sciences;2022-08

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