Ontology type: schema:ScholarlyArticle Open Access: True
2018-12
AUTHORSKe Yin, Hanlie Hong, Thomas J. Algeo, Gordon Jock Churchman, Zhaohui Li, Zongmin Zhu, Qian Fang, Lulu Zhao, Chaowen Wang, Kaipeng Ji, Weidong Lei, Zhenggang Duan
ABSTRACTDiffuse reflectance spectrophotometry (DRS) is a new, fast, and reliable method to characterize Fe-oxides in soils. The Fe-oxide mineralogy of the Jiujiang red earth sediments was investigated using DRS to investigate the climate evolution of southern China since the mid-Pleistocene. The DRS results show that hematite/(hematite + goethite) ratios [Hm/(Hm + Gt)] exhibit an upward decreasing trend within the Jiujiang section, suggesting a gradual climate change from warm and humid in the middle Pleistocene to cooler and drier in the late Pleistocene. Upsection trends toward higher (orthoclase + plagioclase)/quartz ratios [(Or + Pl)/Q] and magnetic susceptibility values (χlf) support this inference, which accords with global climate trends at that time. However, higher-frequency climatic subcycles observed in loess sections of northern China are not evident in the Jiujiang records, indicating a relatively lower climate sensitivity of the red earth sediments in southern China. More... »
PAGES3610
http://scigraph.springernature.com/pub.10.1038/s41598-018-20119-4
DOIhttp://dx.doi.org/10.1038/s41598-018-20119-4
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PUBMEDhttps://www.ncbi.nlm.nih.gov/pubmed/29483522
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"description": "Diffuse reflectance spectrophotometry (DRS) is a new, fast, and reliable method to characterize Fe-oxides in soils. The Fe-oxide mineralogy of the Jiujiang red earth sediments was investigated using DRS to investigate the climate evolution of southern China since the mid-Pleistocene. The DRS results show that hematite/(hematite\u2009+\u2009goethite) ratios [Hm/(Hm\u2009+\u2009Gt)] exhibit an upward decreasing trend within the Jiujiang section, suggesting a gradual climate change from warm and humid in the middle Pleistocene to cooler and drier in the late Pleistocene. Upsection trends toward higher (orthoclase\u2009+\u2009plagioclase)/quartz ratios [(Or\u2009+\u2009Pl)/Q] and magnetic susceptibility values (\u03c7lf) support this inference, which accords with global climate trends at that time. However, higher-frequency climatic subcycles observed in loess sections of northern China are not evident in the Jiujiang records, indicating a relatively lower climate sensitivity of the red earth sediments in southern China.",
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"name": "Fe-oxide mineralogy of the Jiujiang red earth sediments and implications for Quaternary climate change, southern China",
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