Mathematics – Logic
Scientific paper
Jun 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30k..42s&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 11, pp. 42-1, CiteID 1588, DOI 10.1029/2002GL016541
Mathematics
Logic
3
Geochemistry: Isotopic Composition/Chemistry, Geochemistry: Geochemical Cycles (0330), Oceanography: General: Paleoceanography, Oceanography: Biological And Chemical: Carbon Cycling, Oceanography: Biological And Chemical: Biogeochemical Cycles (1615)
Scientific paper
Analyses of foraminiferal δ18O (δ18Ocarb), δ13C (δ13Ccarb) and bulk organic matter (δ13Corg) across a tropical Eocene/Oligocene boundary (EOB) section from Kutch basin, western India show that the ocean cooling (at least ~3°C) is coincident with a rapid enrichment (~3‰) in δ13Corg but depletion (~1.5‰) in δ13Ccarb. The decrease in pCO2 in ocean-atmosphere system across the boundary, possibly resulting from enhanced silicate weathering in rising Himalayas and accompanied organic carbon burial in ocean, caused the cooling and δ13Corg enrichment. The end-Eocene climatic stress decreased the oceanic productivity (and δ13Ccarb) eventually causing extinction of larger benthic foraminiferal community. The data suggest a critical role of tropical ocean and direct forcing of CO2 on global climate change at least for this crucial Cenozoic transition.
Bhattacharya Somesh Kr.
Ray Arnab K.
Sarangi Sash
Sarkar Abhijit
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