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Multiphase timing of hominin occupations and the paleoenvironment in Luonan Basin, Central China

Bibliographic Data

ID24088339
AuthorsHuayu Lu (0000-0002-6306-6985, Nanjing University, corresponding author), Hongyan Zhang (0000-0003-3521-532X, Nanjing University), Shejiang Wang (La Trobe University), Richard Cosgrove (0000-0002-9625-3576, La Trobe University), Xuefeng Sun (0000-0002-2688-4663, Nanjing University), Jun Zhao (0000-0001-5132-8012, Nanjing University), Donghuai Sun (Lanzhou University), Cunfa Zhao (Nanjing University), Chen Shen (0000-0002-8714-3340, Royal Ontario Museum), Ming Wei (0000-0003-1605-8218, La Trobe University)
Year2011
Volume76
Issue1
Pages142-147
Publication date2011-07-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueQuaternary Research (JOURNAL)
Journal identifiersISSN: 0033-5894 • E-ISSN: 1096-0287
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1016/j.yqres.2011.04.001
OpenAlexW1977708249
LanguageEN
Citations received26
References cited6

Thousands of Paleolithic artifacts have been recovered from Paleolithic sites in the Luonan Basin, in the upper South Luohe River of central China. Their discovery suggests that the basin was an important area for hominin settlement during the Pleistocene. However, the initial timing of this occupation and the environmental conditions for this period are still largely unknown. In addition, the sediments are not well dated and most of the artifacts lie on the surface. In an attempt to resolve these issues, a new systemic paleomagnetic analysis was carried out on the loess deposits that contain in situ stone tools. Our detailed loess–paleosol analyses of the stratigraphy of different sites in the basin and Chinese Loess Plateau shows the accumulation of the loess since at least 1.1 million years (Ma) ago. Moreover, recently discovered in situ cores, flakes and retouched stone tools in these deposits show that hominins used this region repeatedly from 0.8–0.7 Ma to 0.4–0.3 and 0.2–0.1 Ma. Pedostratigraphic analyses, magnetic susceptibility and carbon isotope analyses also indicate that these hominins lived in a subtropical to warm-temperate climate with broad-needle-leaf forest vegetation mixed with grasses.

Early Pleistocene · Earth science · Geography · Interglacial · Loess · Magnetostratigraphy · Marine isotope stage · Paleomagnetism · Paleosol · Period (music) · Physical geography · Pleistocene · Structural basin · Subtropics · Tectonics · Ecology · Forensic Anthropology and Bioarchaeology Studies · Geology · Geology and Paleoclimatology Research · Paleontology · Pleistocene-Era Hominins and Archaeology · Stratigraphy

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  • TT-OSL dating of Longyadong Middle Paleolithic site and paleoenvironmental implications for hominin occupation in Luonan Basin (central China)

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  • Diverse floodplain deposits of reworked loess in a monsoon climate (Hanzhong Basin, central China)

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  • Consistent C3 plant habitat of hominins during 400–300 ka at the Longyadong Cave site (Luonan Basin, central China) revealed by stable carbon isotope analyses of loess deposits

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Unique citing works26
Citations per year1,86
Citation span2012 - 2026 (15)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 23
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