Journal of Geographical Sciences ›› 2022, Vol. 32 ›› Issue (2): 358-374.doi: 10.1007/s11442-022-1951-3
• Special Issue: Climate Change and Its Regional Response • Previous Articles
LIU Dengke1(), SUN Xuefeng1,*(
), HU Xuzhi2, YI Liang3, GUO Xiaoqi1, WANG Yichao1, WANG Shejiang4,5, LU Huayu1
Received:
2020-12-17
Accepted:
2021-08-11
Online:
2022-02-25
Published:
2022-04-25
Contact:
SUN Xuefeng
E-mail:mg1927010@smail.nju.edu.cn;xuefeng@nju.edu.cn
About author:
Liu Dengke, Master Candidate, specialized in physical geography. E-mail: mg1927010@smail.nju.edu.cn
Supported by:
LIU Dengke, SUN Xuefeng, HU Xuzhi, YI Liang, GUO Xiaoqi, WANG Yichao, WANG Shejiang, LU Huayu. Evidence of Middle Pleistocene hominin migration in the Qinling Mountains (central China) from the Miaokou Paleolithic site[J].Journal of Geographical Sciences, 2022, 32(2): 358-374.
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Figure 1
Location of the Miaokou Paleolithic site. The small red triangles mark the sites of Danjiang River Valley; the small black triangles mark the sites of other river valleys; the red dots mark the newly discovered sites in Danjiang River Valley; and the red pentacle marks the Miaokou site.
Figure 5
Composite orthogonal projections ((a1)-(f1)) and residual magnetization intensity decay curves ((a2)-(f2)) of the representative progressive thermal demagnetization of the samples of the Miaokou profile. The solid (hollow) circles represent the horizontal (vertical) component projections; NRM is the natural remanent magnetization; and the highest temperature is 680℃.
Table 1
Summary of sample codes, depth information, water contents, radionuclide concentrations, calculated dose rates, De values, and luminescence ages; “wc” means water contents, with an absolute uncertainty of ± 5%
Lab No. | Sample No. | Depth (cm) | wc (%) | U (ppm) | Th (ppm) | K (%) | Dose rate (Gy/ka) | De (Gy) | Age (ka) |
---|---|---|---|---|---|---|---|---|---|
NJU2889 | MK-1 | 160 | 4 | 2.197±0.04 | 13.214±0.15 | 1.765±0.02 | 3.43±0.19 | 486±25 | 141±11 |
NJU2890 | MK-2 | 240 | 6 | 2.137±0.03 | 12.427±0.13 | 1.760±0.01 | 3.24±0.17 | 550±27 | 169±17 |
Figure 6
Lithostratigraphy, magnetic susceptibility, magnetic polarity stratigraphy of the Miaokou profile and its comparison with the magnetic susceptibility of Luochuan, and geomagnetic polarity time scale (Hilgen et al., 2012). MS, magnetic susceptibility; Dec., magnetic declination; Inc., magnetic inclination; a and b, OSL age; VGP Lat., virtual geomagnetic pole latitude; MAD, maximum angular difference; GPTS, geomagnetic polarity time scale; N, normal polarity; B, Brunhes normal polarity; M, Matuyama reversed polarity.
Figure 7
Distribution of Paleolithic sites older than 0.6 Ma in the QMR according to standard loess-paleosol stratigraphic sequence (Ding et al., 2002) and δ18O stack (Lisiecki and Raymo, 2005). The sites marked with blue symbols were previously studied by our team; purple symbols indicate the research by other workers; red symbols mark the present study.
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