Sources of new nitrogen in the Indian Ocean

作者：Raes Eric J^*; Thompson Peter A; McInnes Allison S; Hoang Minh Nguyen; Hardman Mountford Nick; Waite Anya M

来源：Global Biogeochemical Cycles, 2015, 29(8): 1283-1297.

DOI：10.1002/2015GB005194

Quantifying the different sources of nitrogen (N) within the N cycle is crucial to gain insights in oceanic phytoplankton production. To understand the controls of primary productivity and the associated capture of CO2 through photosynthesis in the southeastern Indian Ocean, we compiled the physical and biogeochemical data from four voyages conducted in 2010, 2011, 2012, and 2013. Overall, higher NH4+ assimilation rates (similar to 530 mu molm(-2) h(-1)) relative to NO3- assimilation rates (similar to 375 mu molm(-2) h(-1)) suggest that the assimilation dynamics of C are primarily regulated by microbial regeneration in our region. N-2 fixation rates did not decline when other source of dissolved inorganic nitrogen were available, although the assimilation of N-2 is a highly energetic process. Our data showed that the diazotrophic community assimilated(-2) nmol N L-1 h(-1) at relative elevated NH4+ assimilation rates similar to 12 nmol L-1 h(-1) and NO3- assimilation rates similar to 6 nmol L-1 h(-1). The small diffusive deep water NO3- fluxes could not support the measured NO3- assimilation rates and consequently point toward another source of dissolved inorganic NO3-. Highest NO2- values coincided consistently with shallow lower dissolved O-2 layers (100-200m; 100-180 mu mol L-1). These results suggest that nitrification above the pycnocline could be a significant component of the N cycle in the eastern Indian Ocean. In our analysis we provide a conceptual understanding of how NO3- in the photic zone could be derived from new N through N-2 fixation. We conclude with the hypothesis that N injected through N-2 fixation can be recycled within the photic zone as NH4+ and sequentially oxidized to NO2- and NO3- in shallow lower dissolved oxygen layers.

• 出版日期2015-8
• 单位CSIRO