The dissolved oxygen concentration in ocean water is the main driver of nutrient and energy flow patterns within marine ecosystems (Diaz & Rosenberg, 2008;Diaz et al., 2009). Oxygen deficiency in ocean water selects for microbial groups capable of utilizing alternative respiratory substrates including nitrate, nitrite, sulfate, or carbon dioxide (Zehnder & Stumm, 1988). Within oxygen-deficient waters, the use of nitrite or nitrate as alternative electron acceptors results in the production of nitrous oxide and nitrogen gas (Lam & Kuypers, 2011). This leads to denitrification or loss of fixed nitrogen.The Arabian Sea (AS) oxygen minimum zone (OMZ) is one of the largest pelagic low-oxygen environments in the open ocean, which is a major part of global ocean-led denitrification, which extends from ~100 to 1,200 m of depth (Jayakumar et al., 2009). Here the oxygen concentration drops to 0.1 ml/L (4.5 μmol/kg) or lower, compared to the average ocean dissolved oxygen concentration that ranges between 6 and 8 ml/L (270-360 μmol/kg). These OMZ regions are of microbiological importance as major biogeochemical processes are catalyzed by the microbial communities which inhabit them