An improved comparison of Chinese loess with deep-sea delta O-18 record over the interval 1.6-2.6 Ma
Sun, YB; An, ZS
2004-07-10
发表期刊GEOPHYSICAL RESEARCH LETTERS
卷号31期号:13
文章类型Article
摘要Based on a refined orbital timescale for the lower portion of Pleistocene loess-paleosol sequence at Lingtai section, we present an improved comparison of Chinese loess with deep-sea delta(18)O record over the interval 1.6-2.6 Ma. Unlike previous land-ocean comparison, our result suggests that each paleosol unit from S-25 to S-32 is approximately including two interglacial oxygen isotope stages. The rationality of our revised comparison is supported by the well-constrained ages of geomagnetic reversal boundaries in Chinese loess, and the almost cycle-to-cycle correlation between the grain size and deep-sea delta(18)O record. Spectral analyses demonstrate that variations of the magnetic susceptibility and grain size in the interval 1.6-2.6 Ma were dominated by a prominent 410-ka periodicity, implying a possible response of the East Asian monsoon evolution to orbital eccentricity forcing.
关键词Chinese loess East Asian monsoon deep-sea delta O-18 land-ocean comparison
学科领域Geology
DOI10.1029/2004GL019716
关键词[WOS]OXYGEN-ISOTOPE RECORD ; ASTRONOMICAL CALIBRATION ; PALEOCLIMATE RECORDS ; NORTH-ATLANTIC ; GRAIN-SIZE ; PLATEAU ; CLIMATE ; DEPOSITS ; VARIABILITY ; TIMESCALE
收录类别SCI ; SCIE
语种英语
WOS研究方向Geosciences, Multidisciplinary
WOS记录号WOS:000222654400001
出版者AMER GEOPHYSICAL UNION
引用统计
被引频次:9[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/12062
专题黄土与第四纪地质国家重点实验室(1985-2004)
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GB/T 7714
Sun, YB,An, ZS. An improved comparison of Chinese loess with deep-sea delta O-18 record over the interval 1.6-2.6 Ma[J]. GEOPHYSICAL RESEARCH LETTERS,2004,31(13).
APA Sun, YB,&An, ZS.(2004).An improved comparison of Chinese loess with deep-sea delta O-18 record over the interval 1.6-2.6 Ma.GEOPHYSICAL RESEARCH LETTERS,31(13).
MLA Sun, YB,et al."An improved comparison of Chinese loess with deep-sea delta O-18 record over the interval 1.6-2.6 Ma".GEOPHYSICAL RESEARCH LETTERS 31.13(2004).
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