Abrupt changes in the southwest monsoon during Mid-Late Holocene in the western Bay of Bengal

Govil, Pawan; Mazumder, Abhijit; Agrawal, Shailesh; Azharuddin, Syed; Mishra, Ravi; Khan, Hidayatullah; Kumar, Brijesh; Verma, Divya Ratan

doi:10.1016/j.jseaes.2022.105100

Cited by 10 publications

(1 citation statement)

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“…The G. ruber is a symbiont-bearing mixed layer and oligotrophic species of planktic foraminifera that lives in the upper ~ 30 m of the Ocean water column where the environment is composed of high light availability and low turbidity (Feldmeijer et al, 2014;Mulitza et al, 2003;Gast et al, 2000;Govil et al, 2022). The δ 18 O of foraminiferal shells captured the temperature and δ 18 O of seawater at which the oxygen isotope fractionations occurred between the foraminiferal shell and seawater (Emiliani, 1954;Labeyrie et al, 1992).…”

Section: Discussionmentioning

confidence: 99%

Surface hydrodynamic variations and their forcing mechanisms over the past ~412,000 years from the western equatorial Indian Ocean

Kumar,

Govil,

Agrawal

et al. 2024

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Indian Ocean's tropical region receives the most insulation and is influenced by factors such as the intensity of trade winds, global walker circulations, and teleconnections. The western equatorial Indian Ocean (WEIO) is crucial for studying the variability of Indian monsoons in the past. To better understand the changes in mixed layer hydrodynamics and productivity over the past ~ 412 ka, we examined the planktonic foraminifera Globigerinoides ruber (G. ruber) oxygen and carbon isotope record (δ18OG.ruber, δ13CG.ruber) in core VM29045-PC taken from the WEIO (6° 00’ S, 69° 02’ E; 2860 m water depth). The chronology was established using five radiocarbon (14C) dates and δ18OG.ruber compared with global isostack LR04. The values of δ18OG.ruber were lower during Marine isotopic stage (MIS )11, MIS 5, and MIS 1, indicating higher SST, precipitation, and a strong summer monsoon. In contrast, MIS 10 and MIS 2 showed much higher values corresponding to cool and dry periods. The cooling intensities and interstadial cycles in MIS 10 and MIS 2 would be due to the Indian Ocean Dipole (IOD)/ equatorial westerly wind variability. The record (δ18OG.ruber and δ13CG.ruber) was compared globally with the western Pacific warm pool (WPWP), Southern Agulhas Bank (SAB), and southeast Atlantic (SEA), which showed coherency with Indian and other Ocean basins and interstadial warming during the glacial periods MIS 10 and MIS 2. It showed less cooling during MIS 6, MIS 8, and lower productivity. Higher productivity was observed during mid-MIS 10 and 9, and MIS 3 − 1, corresponding to higher δ13CG.ruber values.

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