Latitudinal δ13C and δ15N variations in particulate organic matter (POM) in surface waters from the Indian ocean sector of Southern Ocean and the Tropical Indian Ocean in 2012. (August 2015)

• Record Type: Journal Article
• Authors: Soares, Melena A.; Bhaskar, Parli V.; Naik, Ravidas K.; Dessai, Deepti; George, Jenson; Tiwari, Manish; Anilkumar, N.
• Is Part Of: Deep sea research. Volume 118(2015)Part B
• Page Start: 186
• Page End: 196
• Publication Date: 2015-08
• Subjects: Carbon isotope -- Nitrogen isotope -- Particulate organic matter -- Southern Ocean -- Indian Ocean; Oceanography -- Periodicals; Ocean bottom -- Periodicals; Marine biology -- Periodicals; 551.46
• DOI: 10.1016/j.dsr2.2015.06.009
• Languages: English
• ISSNs: 0967-0645

Abstract

Abstract: Surface water samples were collected onboard ORV Sagar Nidhi from 11 stations in the Tropical Indian Ocean (TIO) and 9 stations in the Indian Ocean sector of Southern Ocean (IOSO) (between 3°N and 53°S) during the austral summer 2012 to understand δ 13 C and δ 15 N signatures of particulate organic matter (POM) in the two different oceanic regimes. Organic carbon and nitrogen concentrations (%C and %N) and δ 13 C and δ 15 N values (δ 13 C(POM) and δ 15 N(POM) ) of POM were analysed along with a suite of supporting oceanographic parameters. Overall, large-scale variations in %C, %N, δ 13 C(POM) and δ 15 N(POM) values were observed in surface waters, which may be influenced by physical and biological processes. The δ 13 C(POM) values ranged from −26.82‰ to −21.40‰ and were higher in the subtropical waters (40–43°S), with an increase of approximately 3‰. δ 15 N(POM) values varied over a wide range, from −5.09‰ to 4.09‰, with higher δ 15 N(POM) in the nitrate-depleted subtropical waters. δ 13 C(POM) had a significant relation with temperature and an inverse relation with total CO2 (tCO2 ) beyond 40°S. The elemental C:N ratio ranged from 4.4 to 10.8 in the tropical waters, with higher ratios in equatorial waters (1°N–3°S). The biological community structure and diverse biological processes influence the spatial variations of δ 13 C(POM) and δ 15 N(POM) values in the study area. The selective enrichment of carbon of POM in tropical surface waters may be due to the dominance of picoplankton and associated biological processes. Beyond 40°S, a combination of physical factors including SST, eddies along with the changing biological community, especially the dominance of dinoflagellates in the subtropical front and diatoms in the polar front appears to control the latitudinal variability of POM characteristics.