The Arabian Sea is an important site of biogeochemical ocean-atmosphere tra
nsfers, which play a crucial role in regulating the atmospheric chemical co
mposition and the earth's climate. Widespread denitrification resulting fro
m an intense oxygen-deficiency at mid-depths in this region modulates ocean
ic Combined nitrogen inventory and consequently biological productivity. Du
e to a delicate biogeochemical balance the Arabian Sea is expected to be am
ong the first to react to potential anthropogenic perturbations.