The paleosol complex S5 in the China Loess Plateau - A record of climatic optimum during the last 1.2 Ma

An Zhisheng; Liu Tungsheng; Zhou Yizhi; Sun Fuqing; Ding Zhongly

doi:10.1007/BF00157939

The paleosol complex S₅ in the China Loess Plateau - A record of climatic optimum during the last 1.2 Ma

An Zhisheng
, Liu Tungsheng
, Zhou Yizhi
, Sun Fuqing
, Ding Zhongly

Chinese Academy of Sciences

Research output: Contribution to journal › Article › peer-review

24 Scopus citations

Abstract

Having investigated the loess-paleosol sequence in various loess deposition basins in the China Loess Plateau, authors have found that the paleosol complex S₅ is of special significance in terms of Pleistocene paleoclimate. Paleopedological, micromorphological, palynological and paleomagnetic evidences indicate that this paleosol complex formed in the interval of 460,000 to at least 560,000 years BP, which was a climatic optimum.

Original language	English
Pages (from-to)	141-143
Number of pages	3
Journal	GeoJournal
Volume	15
Issue number	2
DOIs	https://doi.org/10.1007/BF00157939
State	Published - Sep 1987
Externally published	Yes

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title = "The paleosol complex S5 in the China Loess Plateau - A record of climatic optimum during the last 1.2 Ma",

abstract = "Having investigated the loess-paleosol sequence in various loess deposition basins in the China Loess Plateau, authors have found that the paleosol complex S5 is of special significance in terms of Pleistocene paleoclimate. Paleopedological, micromorphological, palynological and paleomagnetic evidences indicate that this paleosol complex formed in the interval of 460,000 to at least 560,000 years BP, which was a climatic optimum.",

author = "An Zhisheng and Liu Tungsheng and Zhou Yizhi and Sun Fuqing and Ding Zhongly",

year = "1987",

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AU - Zhisheng, An

AU - Tungsheng, Liu

AU - Yizhi, Zhou

AU - Fuqing, Sun

AU - Zhongly, Ding

PY - 1987/9

Y1 - 1987/9

N2 - Having investigated the loess-paleosol sequence in various loess deposition basins in the China Loess Plateau, authors have found that the paleosol complex S5 is of special significance in terms of Pleistocene paleoclimate. Paleopedological, micromorphological, palynological and paleomagnetic evidences indicate that this paleosol complex formed in the interval of 460,000 to at least 560,000 years BP, which was a climatic optimum.

AB - Having investigated the loess-paleosol sequence in various loess deposition basins in the China Loess Plateau, authors have found that the paleosol complex S5 is of special significance in terms of Pleistocene paleoclimate. Paleopedological, micromorphological, palynological and paleomagnetic evidences indicate that this paleosol complex formed in the interval of 460,000 to at least 560,000 years BP, which was a climatic optimum.

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DO - 10.1007/BF00157939

M3 - 文章

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SN - 0343-2521

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ER -

The paleosol complex S₅ in the China Loess Plateau - A record of climatic optimum during the last 1.2 Ma

Abstract

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