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Paleoclimatic Studies from Sediments in the Bay of Bengal

The Bay of Bengal receives large volume of sediments discharged through seven major rivers, the largest of them being the Ganga and the Brahmaputra river system (G-B). These sediments preserve records of the sediment discharged from these rivers. Sediment composition of the Bay appears to be mainly governed by three processes viz. detrital, biogenic and diagenetic, with detrital being the dominant in this region. Their input reveals physical and chemical erosion of the terrain over which they flow and is strongly dependent on the monsoon intensity, especially the southwest or summer monsoon (Sarin et al., 1979). This study reports results from the two gravity cores (4032; ~13.36 o N; 88.9 o E and 4040; 6.03 o N; 89.94 o E) collected from the central and southern Bay of Bengal respectively.