湖北天门谭家岭遗址全新世中晚期气候变化及其对人类活动的影响

毛欣; 李长安; 张玉芬; 陈旭; 刘辉

doi:10.3799/dqkx.2014.137

Volume 39 Issue 10

Oct. 2014

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Article Navigation > Earth Science > 2014 > 39(10): 1445-1453

Mao Xin, Li Chang'an, Zhang Yufen, Chen Xu, Liu Hui, 2014. Impact of Middle to Late Holocene Climate Changes on Human Activities at Tanjialing Site, Tianmen, Hubei Province. Earth Science, 39(10): 1445-1453. doi: 10.3799/dqkx.2014.137

Citation:

Mao Xin, Li Chang'an, Zhang Yufen, Chen Xu, Liu Hui, 2014. Impact of Middle to Late Holocene Climate Changes on Human Activities at Tanjialing Site, Tianmen, Hubei Province. Earth Science, 39(10): 1445-1453. doi: 10.3799/dqkx.2014.137

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Impact of Middle to Late Holocene Climate Changes on Human Activities at Tanjialing Site, Tianmen, Hubei Province

doi: 10.3799/dqkx.2014.137

Mao Xin^{1, 2
,},
Li Chang'an^{1
,
,},
Zhang Yufen³,
Chen Xu¹,
Liu Hui⁴

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Institute of Hydrogeology and Environmental Geology, Chinese Acdemy of Geological Sciences, Shijiazhuang 050061, China
3.
Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China
4.
Hubei Provincial Institute of Cultural Relics and Archaeology, Wuhan 430077, China

Received Date: 2014-01-03
Publish Date: 2014-10-01

Abstract

Abstract

The Shijiahe culture is a milestone in Chinese civilization development. However, there are still disputes as to the absolute age of the Shijiahe culture and the interaction between climate changes and human activities during this epoch. Sample profile from the Tanjialing site, i.e. a typical site of Shijiahe culture, was analyzed based on AMS ¹⁴C dating and geochemical elements, combined with the methods of principle component analysis (PCA) and ratio of elements (C value). The results show that the absolute age of the Shijiahe culture is around 4 800-4 100 cal. a BP based on three AMS ¹⁴C dating measured in the America NSF-Arizona AMS Laboratory, consistent with the relative age of Shijiahe culture. Between 4 850 and 4 300 cal. a BP, high value of the second principle component (F₂), C value and Mg/Ca ratio indicate that the environment might be relatively warm and wet. Meanwhile, high values of the first and third principle components (F₁ and F₃) reflect strong human disturbances. For the period from 4 300 to 4 124 cal. a BP, low value of F₂, C value and Mg/Ca ratio are indicative of cold and drought conditions. Meanwhile, low values of F₁ and F₃ might be related to weak human disturbances and the collapse of the Shijiahe culture. This study reveals that the flood events in the climate changes from warm and wet to cold and drought background could be one potential trigger of the collapse of the Shijiahe Culture.
- Tanjialing Site,
- absolute age of Shijiahe Culture,
- geochemisty,
- environmental change,
- human activity,
- climate change

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References(75)

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Impact of Middle to Late Holocene Climate Changes on Human Activities at Tanjialing Site, Tianmen, Hubei Province

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