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Paleoclimatic reconstruction and the response of carbonate minerals during the past 8000 years over the northeast Tibetan Plateau
Han, Li; Li, Yun; Liu, Xingqi; Yang, Huan
第一作者Han, Li
2020-07-10
发表期刊QUATERNARY INTERNATIONAL
ISSN1040-6182
卷号553页码:94-103
摘要The climatic significance of the carbonate content and composition of lake sediments remains unclear. In this study, we analyzed the glycerol dialkyl glycerol tetraethers and mineral contents of Alake Lake sediments to reconstruct temperature and moisture changes over the northeast Tibetan Plateau since 8000 cal yr BP. We identified warm (cold) and wet (dry) conditions during the Roman Warm Period and Holocene Climate Optimum (Early Neoglacial Cooling Period) accompanied by a dominance of aragonite (monohydrocalcite). Based on our results and previous laboratory experiments, we suggest that monohydrocalcite is predominantly deposited in colder, drier, and higher Mg/Ca conditions relative to that of aragonite. The carbonate mineral composition should therefore be fully considered when sediment carbonate contents are used to reconstruct paleo-temperature/moisture changes.
DOI10.1016/j.quaint.2020.06.009
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文献类型期刊论文
条目标识符http://ir.isl.ac.cn/handle/363002/33981
专题盐湖地质与环境实验室
中国科学院青海盐湖研究所
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GB/T 7714
Han, Li,Li, Yun,Liu, Xingqi,et al. Paleoclimatic reconstruction and the response of carbonate minerals during the past 8000 years over the northeast Tibetan Plateau[J]. QUATERNARY INTERNATIONAL,2020,553:94-103.
APA Han, Li,Li, Yun,Liu, Xingqi,&Yang, Huan.(2020).Paleoclimatic reconstruction and the response of carbonate minerals during the past 8000 years over the northeast Tibetan Plateau.QUATERNARY INTERNATIONAL,553,94-103.
MLA Han, Li,et al."Paleoclimatic reconstruction and the response of carbonate minerals during the past 8000 years over the northeast Tibetan Plateau".QUATERNARY INTERNATIONAL 553(2020):94-103.
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