Changes in Intermediate Circulation in the Bay of Bengal Since the Last Glacial Maximum as Inferred From Benthic Foraminifera Assemblages and Geochemical Proxies

• Published in: Geochemistry, Geophysics, Geosystems
• Main Authors: Ma, Ruifang, Sepulcre, Sophie, Licari, Laetitia, Bassinot, Franck, Liu, Zhifei, Tisnerat-Laborde, Nadine, Kallel, Nejib, Yu, Zhaojie, Colin, Christophe
• Format: Report
• Language: English
• Published: AMER GEOPHYSICAL UNION 2019
• Subjects: Bay of Bengal; intermediate water masses; glacial Holocene; benthic foraminiferal assemblages; carbon and oxygen stable isotopes; B-P C-14 age; Geochemistry & Geophysics; MERIDIONAL OVERTURNING CIRCULATION; NORTHEAST INDIAN-OCEAN; DEEP-WATER; ATMOSPHERIC CO2; SOUTHERN-OCEAN; ISOTOPE COMPOSITION; ATLANTIC CLIMATE; OXYGEN ISOTOPES; ORGANIC-CARBON; SEA; Antarctic; Indian; Southern Ocean; Antarc*; North Atlantic Deep Water; North Atlantic; Planktonic foraminifera
• Online Access: http://ir.qdio.ac.cn/handle/337002/161058; https://doi.org/10.1029/2018GC008179

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.