On a basin and global scale, iron (Fe) and P are thought to be primary chemical factors limiting N 2 fixation. The climatological and biological forcings, which individually or cumulatively promote diazotroph growth or trigger blooms, are still poorly understood. Improvements in coupled biological-physical and ecosystem models have allowed for the explicit representation of diazotrophs and, in particular, Trichodesmium and thus hold great potential for unraveling the factors that constrain diazotroph distribution and growth.The role of N 2 fixation in both the global N and C cycle, through both the inter-glacial and glacial cycles as well in the present day ocean, remains an open question. The emerging body of data on global rates of denitrification implies that the oceans are losing nitrate rapidly and, if true, either the rates of N 2 fixation are even higher than we currently estimate or, on some time-scale, the total stock of nitrate in the oceans is more variable than expected. Each of these outcomes has direct implications for the air-sea partitioning of CO 2 on climate time-scales. The question remains: does the importance of marine N 2 fixation relative to denitrification oscillate over various timescales in response to climate forcing or is the N cycle in a homeostatic steady state?