Continuous aridification since the mid‐Holocene as the main cause of C 3 / C 4 dynamics in the grasslands of northeastern China-Reference-Cited by-同舟云学术

Continuous aridification since the mid‐Holocene as the main cause of C 3 / C 4 dynamics in the grasslands of northeastern China

Published:2020-04-22 Issue:1 Volume:72 Page:356-371
ISSN:1351-0754
Container-title:European Journal of Soil Science
language:en
Short-container-title:Eur J Soil Sci

Author:

Li Nannan¹²³⁴^ORCID,Xie Manman⁵,Sack Dorothy⁶,Dubois Nathalie⁴⁷,Yang Xiuyun⁸,Gao Guizai¹,Li Dehui¹,Liu Lidan⁹,Liu Hongyan¹⁰,Leng Chengcheng¹,Wang Jiangyong¹,Liu Baojian¹¹,Jie Dongmei¹²¹²^ORCID

Affiliation:

1. Institute for Peat and Mire Research, State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration Northeast Normal University Changchun China

2. School of Geographical Sciences Northeast Normal University Changchun China

3. CEREGE, CNRS, IRD, INRA Aix‐Marseille University, Europôle de l'Arbois Aix‐en‐Provence France

4. Surface Waters – Research and Management, Eawag, Swiss Federal Institute of Aquatic Science and Technology Dübendorf Switzerland

5. National Research Center for Geoanalysis Chinese Academy of Geological Sciences Beijing China

6. Department of Geography Ohio University Athens Ohio USA

7. Department of Earth Sciences ETH Zürich Zürich Switzerland

8. College of Urban and Environmental Science Peking University Beijing China

9. College of Resource and Environment Science Hunan Normal University Changsha China

10. School of Resources Environment and Tourism Anyang Normal University Anyang China

11. School of Life Science Jilin Normal University Siping China

12. Key Laboratory of Vegetation Ecology Ministry of Education Changchun China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Soil Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/ejss.12960

Reference82 articles.

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4. Phytoliths as paleoenvironmental indicators, West Side Middle Awash Valley, Ethiopia

5. Insolation values for the climate of the last 10 million years

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