Changes in Intermediate Circulation in the Bay of Bengal Since the Last Glacial Maximum as Inferred From Benthic Foraminifera Assemblages and Geochemical Proxies
文献类型：期刊论文
| 作者 | Ma, Ruifang1; Sepulcre, Sophie1; Licari, Laetitia2; Bassinot, Franck3; Liu, Zhifei4; Tisnerat-Laborde, Nadine3; Kallel, Nejib5; Yu, Zhaojie6; Colin, Christophe1 |
| 刊名 | GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
 |
| 出版日期 | 2019-03-01 |
| 卷号 | 20期号:3页码:1592-1608 |
| 关键词 | Bay of Bengal intermediate water masses glacial Holocene benthic foraminiferal assemblages carbon and oxygen stable isotopes B-P C-14 age |
| ISSN号 | 1525-2027 |
| DOI | 10.1029/2018GC008179 |
| 通讯作者 | Ma, Ruifang(rui-fang.ma@u-psud.fr) |
| 英文摘要 | Benthic foraminiferal assemblages and geochemical tracers (delta O-18, delta C-13 and C-14) have been analyzed on benthic and planktonic foraminifera from core MD77-176, located in the northern Bay of Bengal, in order to reconstruct the evolution of intermediate circulation in the northern Indian Ocean since the last glaciation. Results indicate that during the Last Glacial Maximum (LGM), Southern Sourced Water masses were dominant at the core site. A high relative abundance of intermediate and deep infaunal species during the LGM reflects low oxygen concentration and/or mesotropic to eutrophic deep water conditions, associated with depleted benthic delta C-13 values. During the Holocene, benthic foraminiferal assemblages indicate an oligotropic to mesotrophic environment with well-ventilated bottom water conditions compared with LGM. Higher values for benthic foraminifera delta C-13 and B-P C-14 age offsets suggest an increased contribution of North Atlantic Deep Water to the northern Bay of Bengal during the Late Holocene compared to the LGM. Millennial-scale events punctuated the last deglaciation, with a shift in the delta C-13 and the epsilon(Nd) values coincident with low B-P C-14 age offsets, providing strong evidence for an increased contribution of Antarctic Intermediate Water at the studied site. This was associated with enhanced upwelling in the Southern Ocean, reflecting a strong sea-atmospheric CO2 exchange through Southern Ocean ventilation during the last deglaciation. |
| 资助项目 | National Natural Science Foundation of China[41806060] ; China Scholarship Council ; INSU-LEFE-IMAGO-CITRON GLACE program |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000464647100018 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/161059]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 通讯作者 | Ma, Ruifang |
| 作者单位 | 1.Univ Paris Saclay, Univ Paris Sud, CNRS, GEOPS, Orsay, France 2.Aix Marseille Univ, Europole Arbois, CEREGE, BP80, Aix En Provence, France 3.CNRS, CEA, UVSQ, LSCE,IPSL,UMR 8212, Gif Sur Yvette, France 4.Tongji Univ, State Key Lab Marine Geol, Shanghai, Peoples R China 5.Univ Sfax, Fac Sci Sfax, Lab Georessources Mat Environnem & Changements Gl, LR13ES23, Sfax, Tunisia 6.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Shandong, Peoples R China |
| 推荐引用方式 GB/T 7714 | Ma, Ruifang,Sepulcre, Sophie,Licari, Laetitia,et al. Changes in Intermediate Circulation in the Bay of Bengal Since the Last Glacial Maximum as Inferred From Benthic Foraminifera Assemblages and Geochemical Proxies[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2019,20(3):1592-1608. |
| APA | Ma, Ruifang.,Sepulcre, Sophie.,Licari, Laetitia.,Bassinot, Franck.,Liu, Zhifei.,...&Colin, Christophe.(2019).Changes in Intermediate Circulation in the Bay of Bengal Since the Last Glacial Maximum as Inferred From Benthic Foraminifera Assemblages and Geochemical Proxies.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,20(3),1592-1608. |
| MLA | Ma, Ruifang,et al."Changes in Intermediate Circulation in the Bay of Bengal Since the Last Glacial Maximum as Inferred From Benthic Foraminifera Assemblages and Geochemical Proxies".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 20.3(2019):1592-1608. |
入库方式： OAI收割
来源：海洋研究所
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