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作 者:HOU ShuGui WANG YeTang PANG HongXi
机构地区:[1]Key Laboratory for Coast and Island Development(Ministry of Education),School of Geographic and Oceanographic Sciences,Nanjing University [2]State Key Laboratory of Cryospheric Science,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences [3]Shandong Provincial Key Laboratory of Marine Ecological Restoration,Shandong Marine Fisheries Research Institute
出 处:《Chinese Science Bulletin》2013年第10期1095-1106,共12页
基 金:supported by the National Natural Science Foundation of China (41171052,40825017,41206175 and 41176165);the State Oceanic Administration (CHINARE2012-02-02);Ministry of Education (20110091110025 and 1082020904)
摘 要:Stable isotopic composition in Antarctic snow and ice is commonly regarded as one of invaluable palaeoclimate proxies and plays a critically important role in reconstructing past climate change.In this paper we summarized the spatial distribution and the controlling factors of δD,δ18O,d-excess and 17O-excess in Antarctic snow and ice,and discussed their reliability and applicability as palaeoclimate proxies.Recent progress in the stable isotopic records from Antarctic deep ice cores was reviewed,and perspectives on bridging the current understanding gaps were suggested.Stable isotopic composition in Antarctic snow and ice is commonly regarded as one of invaluable palaeoclimate proxies and plays a critically important role in reconstructing past climate change. In this paper we summarized the spatial distribution and the con- trolling factors of bD, 80, d-excess and 170-excess in Antarctic snow and ice, and discussed their reliability and applicability as palaeoclimate proxies. Recent progress in the stable isotopic records from Antarctic deep ice cores was reviewed, and perspectives on bridging the current understanding gaps were suggested.
关 键 词:稳定同位素 气候变化 南极 冰雪 气候代用指标 同位素组成 同位素记录 控制因素
分 类 号:P467[天文地球—大气科学及气象学]
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