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Magnetostratigraphic dating of the Donggutuo and Maliang Paleolithic sites in the Nihewan Basin, North China
Wang, HQ; Deng, CL; Zhu, RX; Wei, Q; Hou, YM; Boeda, E; Wang, HQ (reprint author), Chinese Acad Sci, Inst Geol & Geophys, Paleomagnetism & Geochronol Lab SKL LTE, Beijing 100029, Peoples R China.
2005-07-01
发表期刊QUATERNARY RESEARCH
ISSN0033-5894
卷号64期号:1页码:1-11
文章类型Article
摘要A detailed magnetostratigraphic investigation, coupled with rock-magnetic Studies, was carried out on a lacustrine sequence in the eastern Nihewan Basin, Northern China, which contains the Donggutuo and Maliang Paleolithic sites. Magnetite and hematite were identified as the main carriers for the characteristic remanent magnetizations. Magnetostratigraphic results show that the lacustrine sequence recorded the late Matuyama and Brunhes chrons. Furthermore, the Maliang artifact layer occurs just below the Brunlies/Matuyama boundary, and the Donggutuo artifact layer is just below the Jaramillo onset. Therefore, the age of the Maliang and Donggutuo artifact layers can be definitely estimated to be about 0.78 myr and 1.1 myr, respectively. These two paleomagnetic ages, Coupled with previously obtained paleomagnetic data of the Majuangou, Xiaochangliang, Banshan, Lantian, and Xilioudu Paleolithic sites, suggest an expansion and lengthy flourishing of human groups from northern to north-central China during the entire Early Pleistocene. (c) 2005 University of Washington. All rights reserved.; A detailed magnetostratigraphic investigation, coupled with rock-magnetic Studies, was carried out on a lacustrine sequence in the eastern Nihewan Basin, Northern China, which contains the Donggutuo and Maliang Paleolithic sites. Magnetite and hematite were identified as the main carriers for the characteristic remanent magnetizations. Magnetostratigraphic results show that the lacustrine sequence recorded the late Matuyama and Brunhes chrons. Furthermore, the Maliang artifact layer occurs just below the Brunlies/Matuyama boundary, and the Donggutuo artifact layer is just below the Jaramillo onset. Therefore, the age of the Maliang and Donggutuo artifact layers can be definitely estimated to be about 0.78 myr and 1.1 myr, respectively. These two paleomagnetic ages, Coupled with previously obtained paleomagnetic data of the Majuangou, Xiaochangliang, Banshan, Lantian, and Xilioudu Paleolithic sites, suggest an expansion and lengthy flourishing of human groups from northern to north-central China during the entire Early Pleistocene. (c) 2005 University of Washington. All rights reserved.
关键词Magnetostratigraphy Paleolithic Site Pleistocene Donggutuo Maliang Nihewan Basin North China
WOS标题词Science & Technology ; Physical Sciences
URL查看原文
关键词[WOS]TEMPERATURE-DEPENDENT SUSCEPTIBILITY ; NW-SE TRANSECT ; LOESS PLATEAU ; PALEOMAGNETIC DATES ; EARLY DISPERSALS ; CLIMATE-CHANGE ; EARLY HOMO ; AFRICA ; GEORGIA ; DMANISI
收录类别SCI
语种英语
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000230723100001
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3541
专题古人类及旧石器研究室
通讯作者Wang, HQ (reprint author), Chinese Acad Sci, Inst Geol & Geophys, Paleomagnetism & Geochronol Lab SKL LTE, Beijing 100029, Peoples R China.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Paleomagnetism & Geochronol Lab SKL LTE, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
3.Univ Paris 10, Maison Archeol & Ethnol, F-92023 Nanterre, France
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GB/T 7714
Wang, HQ,Deng, CL,Zhu, RX,et al. Magnetostratigraphic dating of the Donggutuo and Maliang Paleolithic sites in the Nihewan Basin, North China[J]. QUATERNARY RESEARCH,2005,64(1):1-11.
APA Wang, HQ.,Deng, CL.,Zhu, RX.,Wei, Q.,Hou, YM.,...&Wang, HQ .(2005).Magnetostratigraphic dating of the Donggutuo and Maliang Paleolithic sites in the Nihewan Basin, North China.QUATERNARY RESEARCH,64(1),1-11.
MLA Wang, HQ,et al."Magnetostratigraphic dating of the Donggutuo and Maliang Paleolithic sites in the Nihewan Basin, North China".QUATERNARY RESEARCH 64.1(2005):1-11.
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