中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Stratigraphic distribution of the radiolarian Spongodiscus biconcavus Haeckel at IODP Site U1340 in the Bering Sea and its paleoceanographic significance

文献类型:期刊论文

作者Chen, MH ; Zhang, Q ; Zhang, LL ; Zarikian, CA ; Wang, RJ
刊名PALAEOWORLD
出版日期2014
卷号23期号:1页码:90-104
关键词Radiolarian Spongodiscus biconcavus Paleoceanography NHG Bering Sea Integrated Ocean Drilling Program (IODP) Site U1340
ISSN号1871-174X
通讯作者mhchen@scsio.ac.cn ; zhang_qiang6142@yahoo.com.cn ; llzhang@scsio.ac.cn ; zarikian@iodp.tamu.edu ; rjwangk@online.sh.cn
中文摘要The temporal and spatial distributions of the radiolarian species Spongodiscus biconcavus Haeckel are investigated to understand the paleoceanographic evolution of the Bering Sea region during the last 4.3 Myr based on extensive study of samples collected at Site U1340 during the IODP Expedition 323. The biostratigraphic resolution for the region is also improved by multidisciplinary studies of radiolarians, diatoms, dinoflagellates, ebridians, and silicoflagellates. The results demonstrate that the abundance variation of S. biconcavus during the last 4.3 Myr is closely related to global climate changes, and the species can be used as a warm water and climate proxy in the Bering Sea. Based on the downhole profiles of S. biconcavus and other parameters, we conclude that the southern Bering Sea was associated with a warm water mass prior to 3.147 Ma but it gradually cooled thereafter. From 2.793 Ma to 0.889 Ma, a cold water mass and sea-ice predominated in the Bering Sea, in response to the early Northern Hemisphere glaciation (NHG). Furthermore, the climate suddenly became much cooler post 0.889 Ma. Nevertheless, a reversal of this cooling trend occurred after the Mid-Pleistocene Climatic Transition (-1.2 Ma), marked by reoccurrence of warm water and reduced sea-ice in the Bering Sea until the final retreat of warm water mass from the Bering Sea after 0.239 Ma. These processes are correlated with biogeographic expansion and retreat of warm water planktonic species. (C) 2013 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
学科主题Paleontology
收录类别SCI
资助信息NSFC [41076026, 40906030, 41030859]; National Key Project for Basic Research of China [2013CB956102]
原文出处ELSEVIER SCIENCE BV
WOS记录号WOS:000332271400007
公开日期2014-12-11
源URL[http://ir.scsio.ac.cn/handle/344004/10642]  
专题南海海洋研究所_中科院边缘海地质重点实验室
推荐引用方式
GB/T 7714
Chen, MH,Zhang, Q,Zhang, LL,et al. Stratigraphic distribution of the radiolarian Spongodiscus biconcavus Haeckel at IODP Site U1340 in the Bering Sea and its paleoceanographic significance[J]. PALAEOWORLD,2014,23(1):90-104.
APA Chen, MH,Zhang, Q,Zhang, LL,Zarikian, CA,&Wang, RJ.(2014).Stratigraphic distribution of the radiolarian Spongodiscus biconcavus Haeckel at IODP Site U1340 in the Bering Sea and its paleoceanographic significance.PALAEOWORLD,23(1),90-104.
MLA Chen, MH,et al."Stratigraphic distribution of the radiolarian Spongodiscus biconcavus Haeckel at IODP Site U1340 in the Bering Sea and its paleoceanographic significance".PALAEOWORLD 23.1(2014):90-104.

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来源:南海海洋研究所

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