Changes in the content of eolian iron during the past 900 ka and the implications
Wei, JJ; Guo, ZT
2003-09
发表期刊CHINESE SCIENCE BULLETIN
卷号48期号:17页码:1882-1886
文章类型Article
摘要In this study, total Fe2O3 content (Fe-t) in two parallel sections from the central Loess Plateau (Xifeng and Changwu) is analyzed to address the variations of eolian iron in the past 900 ka. The obtained timeseries indicate that Fet values in some glacial intervals are comparable to that of interglacial periods and its oscillations do not generally correspond to the long-term glacial-interglacial changes. Rather, it exhibits higher frequency fluctuations without detectable 100 ka period, but with a strong 20 ka period and a clear 40 ka period. The combination of 20 ka and 40 ka periods suggest that eolian iron content was relatively independent of glacial-interglacial changes, but more strongly influenced by the insolation changes in the northern hemisphere. Higher iron content was observed for the S5-1 soil that is correlative to marine delta(18)O stage 13. In marine records, this stage is characterized by higher delta(13)C values, suggesting that the event is of global significance.
关键词loess-paleosol sequences eolian iron paleoclimate spectral analysis
学科领域Science & Technology - Other Topics
DOI10.1360/03wd0184
关键词[WOS]MAGNETIC-SUSCEPTIBILITY RECORD ; CHINESE LOESS ; MONSOON VARIATIONS ; CLIMATE ; STRATIGRAPHY ; SEQUENCES ; EVENTS
收录类别SCI ; SCIE
语种英语
WOS研究方向Multidisciplinary Sciences
WOS记录号WOS:000185748300020
出版者SCIENCE CHINA PRESS
引用统计
被引频次:3[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/361006/12098
专题黄土与第四纪地质国家重点实验室(1985-2004)
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Wei, JJ,Guo, ZT. Changes in the content of eolian iron during the past 900 ka and the implications[J]. CHINESE SCIENCE BULLETIN,2003,48(17):1882-1886.
APA Wei, JJ,&Guo, ZT.(2003).Changes in the content of eolian iron during the past 900 ka and the implications.CHINESE SCIENCE BULLETIN,48(17),1882-1886.
MLA Wei, JJ,et al."Changes in the content of eolian iron during the past 900 ka and the implications".CHINESE SCIENCE BULLETIN 48.17(2003):1882-1886.
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