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Late Middle Pleistocene climate in southwestern China: inferences from the stratigraphic record of Panxian Dadong Cave, Guizhou
Karkanas, Panagiotis1; Schepartz, Lynne A.2; Miller-Antonio, Sari3; Wei, Wang4; Huang Weiwen5; Karkanas, P (reprint author), Ephoreia Polaeoanthropol Speleol So Greece, Ardittou 34B, Athens 11636, Greece.
2008-08-01
发表期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
卷号27期号:15-16页码:1555-1570
文章类型Article
摘要Panxian Dadong Cave, situated in the subtropical zone of southwestern China, preserves a fan-like sedimentary sequence close to its entrance that spans the period between MIS 8 and 5 (300-130 ka). The frequent alternation of flowstone formation, cementation, clastic deposition, and frost activity in the depositional sequence makes it ideal for reconstructing the environmental conditions prevailing during the later Middle Pleistocene on the Guizhou Plateau. Macroscopic and microscopic sedimentary analyses determine that clastic deposits were entering the cave in the form of intermittent cohesive debris flows and sheetflows during cold and relatively city climatic conditions when vegetation cover was reduced. Interlayered impure flowstones were forming during wetter phases but still under glacial conditions. Seasonally freezing temperatures are deduced from the frequent occurrence of cycles of well-developed freeze-thaw features affecting both the clastic parts of the sequence and the flowstones as they were deposited. The described depositional processes were responsible for lateral redistribution on the fan surface of bone remains and lithic artifacts that were accumulating on the surface as a result of hominid activities. During the intervening interglacial stages (MIS 7 and possibly MIS 5) clastic deposition was considerably reduced and only thin flowstone caps and weathering manganese-iron crusts were forming. It is suggested that precipitation was much higher during glacial intervals than interglacials under a predominantly cold climate. Dadong Cave provides a good example of very cold and wet climatic conditions during glacials in the subtropics of East Asia. (C) 2008 Elsevier Ltd. All rights reserved.; Panxian Dadong Cave, situated in the subtropical zone of southwestern China, preserves a fan-like sedimentary sequence close to its entrance that spans the period between MIS 8 and 5 (300-130 ka). The frequent alternation of flowstone formation, cementation, clastic deposition, and frost activity in the depositional sequence makes it ideal for reconstructing the environmental conditions prevailing during the later Middle Pleistocene on the Guizhou Plateau.
WOS标题词Science & Technology ; Physical Sciences
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关键词[WOS]ISOTOPIC RECORDS ; ASIAN MONSOON ; SEDIMENTS ; QINGHAI ; MODEL ; PALEOCLIMATE ; ROCKSHELTERS ; SPELEOTHEMS ; PERSPECTIVE ; SIMULATION
收录类别SCI ; AHCI
语种英语
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000259017900007
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文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3227
专题中科院古脊椎所(2000年以后)
古人类及旧石器研究室
通讯作者Karkanas, P (reprint author), Ephoreia Polaeoanthropol Speleol So Greece, Ardittou 34B, Athens 11636, Greece.
作者单位1.Ephoreia Polaeoanthropol Speleol So Greece, Athens 11636, Greece
2.Florida State Univ, Dept Anthropol, Tallahassee, FL 32306 USA
3.Calif State Univ Stanislaus, Dept Anthropol Geog, Turlock, CA 95382 USA
4.Nat Hist Museum Guangxi, Nanning 530012, Peoples R China
5.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing, Peoples R China
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Karkanas, Panagiotis,Schepartz, Lynne A.,Miller-Antonio, Sari,et al. Late Middle Pleistocene climate in southwestern China: inferences from the stratigraphic record of Panxian Dadong Cave, Guizhou[J]. QUATERNARY SCIENCE REVIEWS,2008,27(15-16):1555-1570.
APA Karkanas, Panagiotis,Schepartz, Lynne A.,Miller-Antonio, Sari,Wei, Wang,Huang Weiwen,&Karkanas, P .(2008).Late Middle Pleistocene climate in southwestern China: inferences from the stratigraphic record of Panxian Dadong Cave, Guizhou.QUATERNARY SCIENCE REVIEWS,27(15-16),1555-1570.
MLA Karkanas, Panagiotis,et al."Late Middle Pleistocene climate in southwestern China: inferences from the stratigraphic record of Panxian Dadong Cave, Guizhou".QUATERNARY SCIENCE REVIEWS 27.15-16(2008):1555-1570.
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