In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 20, No. 3 ( 2019-03), p. 1592-1608
Abstract:
We produced high‐resolution records of benthic foraminiferal assemblages, 14 C ages, oxygen, and carbon stable isotopes since 40 kyr BP Hydrological changes of the intermediate water in Bay of Bengal since LGM, were influenced by SSW during the LGM and NADW during the Holocene During the last deglaciation, geochemical records indicate increased northward flow of AAIW and enhanced upwelling in the Southern Ocean
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2018GC008179
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2027201-7
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