Eccentricity-paced geomagnetic field and monsoon rainfall variations over the last 870 kyr

Author:

Zhou Weijian123,Kong Xianghui12ORCID,Paterson Greig A.4ORCID,Sun Youbin15,Wu Yubin26,Ao Hong1,Xian Feng12,Du Yajuan12,Tang Ling7,Zhou Jie7,Shi Zhengguo1ORCID,Jull A. J. Timothy89ORCID,Zhao Guoqing12,An Zhisheng13ORCID

Affiliation:

1. State Key Laboratory of Loess, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China

2. Shaanxi Key Laboratory of Accelerator Mass Spectrometry and Application, Xi’an Accelerator Mass Spectrometry Center, Xi’an 710061, China

3. Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China

4. Department of Earth, Ocean and Ecological Sciences, Geomagnetism Laboratory, University of Liverpool, Liverpool L69 3GP, UK

5. School of Human Settlements and Civil Engineering, Xi’an Jiaotong University, Xi’an 710049, China

6. University of Chinese Academy of Sciences, Beijing 100049, China

7. Xi’an Institute for Innovative Earth Environment Research, Xi’an 710061, China

8. Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen H-4026, Hungary

9. University of Arizona, Tucson, AZ 85721

Abstract

Whether there are links between geomagnetic field and Earth’s orbital parameters remains unclear. Synchronous reconstructions of parallel long-term quantitative geomagnetic field and climate change records are rare. Here, we present 10 Be-derived changes of both geomagnetic field and Asian monsoon (AM) rainfall over the last 870 kyr from the Xifeng loess–paleosol sequence on the central Chinese Loess Plateau. The  10 Be GM flux (a proxy for geomagnetic field-induced 10 Be production rate) reveals 13 consecutive geomagnetic excursions in the Brunhes chron, which are synchronized with the global records, providing key time markers for Chinese loess–paleosol sequences. The  10 Be-derived rainfall exhibits distinct ~100 kyr glacial–interglacial cycles, and superimposed precessional (~23 kyr) cycles that match with those in Chinese speleothem δ 18 O record. We find that changes in the geomagnetic field and AM rainfall share a common ~100 kyr cyclicity, implying a likely eccentricity modulation of both the geomagnetic field and climate.

Funder

Chinese Academy of Sciences

National Natural Science Foundation of China

UKRI | Natural Environment Research Council

EC | European Regional Development Fund

Publisher

Proceedings of the National Academy of Sciences

Subject

Multidisciplinary

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