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过去 870 千年来的偏心率调谐地磁场所和季风降水变化。

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

机构信息

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

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

出版信息

Proc Natl Acad Sci U S A. 2023 Apr 25;120(17):e2211495120. doi: 10.1073/pnas.2211495120. Epub 2023 Apr 17.

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 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 Be flux (a proxy for geomagnetic field-induced 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 Be-derived rainfall exhibits distinct 100 kyr glacial-interglacial cycles, and superimposed precessional (23 kyr) cycles that match with those in Chinese speleothem δO 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.

摘要

地磁场与地球轨道参数之间是否存在联系尚不清楚。对并行的长期定量地磁场和气候变化记录进行同步重建的情况很少。在这里,我们从中国黄土高原西部风尘序列中展示了过去 870 千年来的地磁场和亚洲季风(AM)降雨的 Be 衍生变化。Be 通量(地磁场诱导的 Be 产生率的代理)揭示了 Brunhes 时期间的 13 个连续地磁激扰,这些激扰与全球记录同步,为中国黄土-古土壤序列提供了关键的时间标记。Be 衍生的降雨量显示出明显的约 100 千禧年冰期-间冰期循环,并叠加了岁差(~23 千禧年)循环,与中国洞穴石笋 δO 记录中的循环相匹配。我们发现地磁场和 AM 降雨量的变化具有共同的约 100 千禧年周期性,这表明地磁场和气候的偏心率调制可能存在联系。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0c1c/10151570/d808b309010e/pnas.2211495120fig01.jpg

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