Fixed nitrogen (N) limits productivity across much of the low-latitude ocean. The magnitude of its inventory results from the balance of N input and N loss, the latter largely occurring in regionally well-defined low-oxygen waters and sediments (denitrification and anammox). The rate and distribution of N input by biotic N fixation, the dominant N source, is not well known. Here we compile N fixation estimates from experimental measurements, tracer-based geochemical and modeling approaches, and discuss their limitations and uncertainties. The lack of adequate experimental data coverage and the insufficient understanding of the controls of marine N fixation result in high uncertainties, which make the assessment of the current N-balance a challenge. We suggest that a more comprehensive understanding of the environmental and ecological interaction of marine N fixers is required to advance the field toward robust N fixation rates estimates and predictions.
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6157310 | PMC |
http://dx.doi.org/10.3389/fmicb.2018.02112 | DOI Listing |
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