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对中国中部白龙洞古人类居住遗址的磁性地层年代测定。

Magnetostratigraphic dating of the hominin occupation of Bailong Cave, central China.

机构信息

State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China.

Institutions of Earth Science, Chinese Academy of Sciences, Beijing, 100029, China.

出版信息

Sci Rep. 2018 Jun 26;8(1):9699. doi: 10.1038/s41598-018-28065-x.

DOI:10.1038/s41598-018-28065-x
PMID:29946102
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6018768/
Abstract

Intermontane basins in the southern piedmont of the Qinling Mountains are important sources of information on hominin occupation and settlement, and provide an excellent opportunity to study early human evolution and behavioral adaptation. Here, we present the results of a detailed magnetostratigraphic investigation of the sedimentary sequence of hominin-bearing Bailong Cave in Yunxi Basin, central China. Correlation to the geomagnetic polarity time scale was achieved using previously published biostratigraphy, Al/Be burial dating, and coupled electron spin resonance (ESR) and U-series dating. The Bailong Cave hominin-bearing layer is dated to the early Brunhes Chron, close to the Matuyama-Brunhes geomagnetic reversal at 0.78 Ma. Our findings, coupled with other records, indicate the flourishing of early humans in mainland East Asia during the Mid-Pleistocene climate transition (MPT). This suggests that early humans were adapted to diverse and variable environments over a broad latitudinal range during the MPT, from temperate northern China to subtropical southern China.

摘要

秦岭南麓山间盆地是古人类居住和活动的重要信息来源,为研究早期人类进化和行为适应提供了绝佳机会。本研究详细报道了中国中部云溪盆地含人类化石的白龙洞沉积序列的磁性地层学研究结果。通过已发表的生物地层学、Al/Be 埋藏测年、电子自旋共振(ESR)与铀系测年的综合研究,实现了与地磁场极性时间尺度的对比。白龙洞含人类化石层的年代被确定为早布容正向极性时期,接近 0.78 Ma 的马修斯-布容地磁反转。我们的发现与其他记录一起表明,中更新世气候转型期间(MPT),古人类在东亚大陆大量繁衍。这表明在 MPT 期间,早期人类已经适应了从中国温带北部到亚热带南部的广泛纬度范围内多样且多变的环境。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/b43c04662659/41598_2018_28065_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/8c9e151748f3/41598_2018_28065_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/28eed0e3e64c/41598_2018_28065_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/40939c532133/41598_2018_28065_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/a36cd5325cc1/41598_2018_28065_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/2206360d7302/41598_2018_28065_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/e29092092847/41598_2018_28065_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/f5111da4699e/41598_2018_28065_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/d9ca6593fd95/41598_2018_28065_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/b43c04662659/41598_2018_28065_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/8c9e151748f3/41598_2018_28065_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/28eed0e3e64c/41598_2018_28065_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/40939c532133/41598_2018_28065_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/a36cd5325cc1/41598_2018_28065_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/2206360d7302/41598_2018_28065_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/e29092092847/41598_2018_28065_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/f5111da4699e/41598_2018_28065_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/d9ca6593fd95/41598_2018_28065_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1835/6018768/b43c04662659/41598_2018_28065_Fig9_HTML.jpg

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