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Climate indexes of phytoliths from Homo erectus' cave deposits in Nanjing

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A study on phytoliths and their climate indexes is carried out from Homo erectus' cave deposits in Hulu Cave, Nanjing. Evidence shows that phytolith assemblages of the cave deposits are dominated by the cold resistant types with a lower warm index, reflecting an overall cold inclined climate. This possibly connects the cave deposits with glacial climate to a great extent, which is in accordance with the northern fauna revealed by fossil mammals and temperate climate indicated by pollen assemblages. According to the distributional state of the phytoliths and their climate indexes on 4 profiles in the cave, it is revealed that profiles Ⅰ and Ⅱ display certain cold/warm, and dry/wet fluctuations; profile Ⅲ shows a humid and cold condition with the highest humility in the cave deposits; while profile Ⅳ indicates a possible quick accumulating process because of its stable climate indexes except for its bottom and top.

climate indexesphytolithsNanjing Homo erectuscave deposits

WANG Weiming、Liu Jinling、ZHOU Xiaodan

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Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China

Nanjing Geological Museum, Nanjing 210018, China

国家自然科学基金国家重点基础研究发展计划(973计划)

49971076G2000077700

2003

科学通报(英文版)
中国科学院

科学通报(英文版)

SCI
ISSN:1001-6538
年,卷(期):2003.48(18)
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