中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Distribution and isotopic composition of foraminifera at cold-seep Site 973-4 in the Dongsha area, northeastern South China Sea

文献类型:期刊论文

作者Zhang, Bidong3,4; Pan, Mengdi3,4; Wu, Daidai3,4; Wu, Nengyou1,2
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2018-12-01
卷号168页码:145-154
关键词Foraminifera Assemblage Stable isotopes Cold seep The South China Sea
ISSN号1367-9120
DOI10.1016/j.jseaes.2018.05.007
通讯作者Wu, Daidai(wudd@ms.giec.ac.cn)
英文摘要A 1375-cm-long gravity core (Site 973-4) was acquired from the Dongsha cold seep area of the northeastern South China Sea (SCS). We measured its stable isotopes of planktonic foraminifera and investigated benthic foraminiferal assemblage compositions. Accelerator mass spectrometry C-14 analysis of planktonic foraminifera shows that some intervals are dated to Marine Isotope Stage (MIS) 3. Pulleniatina obliquiloculata has positive delta C-13 (0.25-1.25 parts per thousand) except for a negative carbon isotopic excursion (up to delta C-13 = 1.15 parts per thousand), but its light -carbon sources remain elusive. The benthic delta C-13 values (Uvigerina) of non -seep and cold-seep boreholes from the SCS have no systematic difference. Therefore, the benthic delta C-13 at Site 973-4 did not record the enhanced seepage activities (if occurred) during the last sea-level lowstand in the Dongsha area. In the pre-Holocene sediments, the foraminiferal assemblages have lower diversities, Shannon-Wiener indices, evenness indices, Simpson indices and higher calcareous proportions like typical cold-seep settings. The changes in oxygen levels (lower in the glacial period than those in the Holocene) indicated by foraminiferal indices reflect either bottom-water oxygen variations on the glacial-interglacial scale or enhanced seepage activities during the last glacial period.
WOS关键词ORGANIC-CARBON FLUX ; LIVING BENTHIC FORAMINIFERA ; DEEP-WATER PALEOCEANOGRAPHY ; MODERN METHANE SEEPS ; CONTINENTAL-SLOPE ; COMMUNITY STRUCTURE ; DISSOLVED-OXYGEN ; HYDROCARBON-SEEP ; ADRIATIC SEA ; INDIAN-OCEAN
资助项目National Natural Science Foundation of China[41273022] ; CNPC-CAS science and technology cooperation project[2015A-4813] ; China Geological Survey[GHZ2012006003]
WOS研究方向Geology
语种英语
WOS记录号WOS:000452945000015
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China ; CNPC-CAS science and technology cooperation project ; China Geological Survey
源URL[http://ir.giec.ac.cn/handle/344007/29801]  
专题中国科学院广州能源研究所
通讯作者Wu, Daidai
作者单位1.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266071, Peoples R China
2.Minist Land & Resources, Key Lab Gas Hydrate, Qingdao Inst Marine Geol, Qingdao 266071, Peoples R China
3.Chinese Acad Sci, Key Lab Gas Hydrate, Guangzhou 510640, Guangdong, Peoples R China
4.Chinese Acad Sci, Guangzhou Inst Energy Convers, Guangzhou 510640, Guangdong, Peoples R China
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Zhang, Bidong,Pan, Mengdi,Wu, Daidai,et al. Distribution and isotopic composition of foraminifera at cold-seep Site 973-4 in the Dongsha area, northeastern South China Sea[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,168:145-154.
APA Zhang, Bidong,Pan, Mengdi,Wu, Daidai,&Wu, Nengyou.(2018).Distribution and isotopic composition of foraminifera at cold-seep Site 973-4 in the Dongsha area, northeastern South China Sea.JOURNAL OF ASIAN EARTH SCIENCES,168,145-154.
MLA Zhang, Bidong,et al."Distribution and isotopic composition of foraminifera at cold-seep Site 973-4 in the Dongsha area, northeastern South China Sea".JOURNAL OF ASIAN EARTH SCIENCES 168(2018):145-154.

入库方式: OAI收割

来源:广州能源研究所

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