Pleistocene climate change inferred from multi-proxy analyses of a loess-paleosol sequence in China-Reference-Cited by-同舟云学术

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Pleistocene climate change inferred from multi-proxy analyses of a loess-paleosol sequence in China

Published:2018-04 Issue: Volume:154 Page:428-434
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Wu Yi^ORCID,Qiu Shifan,Fu Shuqing,Rao Zhiguo,Zhu Zhaoyu

Funder

National Natural Science Foundation of China

State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS

Science and Technology Planning Project of Guangdong Province, China

China Scholarship Council

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference56 articles.

1. Multiple expansions of C4 plant biomass in East Asia since 7 Ma coupled with strengthened monsoon circulation;An;Geology,2005

2. Mineral-magnetic signal of long-term climatic variation in Pleistocene fluvio-lacustrine sediments, Nihewan Basin (North China);Ao;J. Asian Earth Sci.,2010

3. Climatic interpretation of the Luochuan and Lingtai loess sections, China, based on changing iron oxide mineralogy and magnetic susceptibility;Balsam;Earth Planet. Sci. Lett.,2004

4. Sediment dispersal in the Atlantic-Ocean-evaluation by visible-light spectra;Balsam;Rev. Aquat. Sci.,1991

5. Rock magnetism and geochemistry of two Plio-Pleistocene Chinese loess–palaeosol sequences—implications for quantitative palaeoprecipitation reconstruction;Bloemendal;Palaeogeog. Palaeoclimat. Palaeoecol.,2005

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