Niche construction by non-diazotrophs for N 2 fixers in the eastern tropical North Atlantic Ocean

Diazotrophic dinitrogen (N 2 ) fixation contributes ~76% to new nitrogen inputs to the sunlit open ocean, but environmental factors determining N 2 fixation rates are not well constrained. Excess phosphate (phosphatenitrate/16>0) and iron availability control N 2 fixation rates in the eastern tro...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Singh, A, Bach, LT, Fischer, T, Hauss, H, Kiko, R, Paul, AJ, Stange, P, Vandromme, P, Riebesell, U
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2017
Subjects:
Earth Sciences
Oceanography
Biological Oceanography
North Atlantic
Online Access:https://doi.org/10.1002/2017GL074218
http://ecite.utas.edu.au/133666
Description
Summary:Diazotrophic dinitrogen (N 2 ) fixation contributes ~76% to new nitrogen inputs to the sunlit open ocean, but environmental factors determining N 2 fixation rates are not well constrained. Excess phosphate (phosphatenitrate/16>0) and iron availability control N 2 fixation rates in the eastern tropical North Atlantic (ETNA), but it remains an open question how excess phosphate is generated within or supplied to the phosphate‐depleted sunlit layer. Our observations in the ETNA region (8N15N, 19W23W) suggest that Prochlorococcus and Synechococcus , the two ubiquitous non‐diazotrophic cyanobacteria with cellular N:P ratios higher than the Redfield ratio, create an environment of excess phosphate, which cannot be explained by diapycnal mixing, atmospheric, and riverine inputs. Thus, our results unveil a new biogeochemical niche construction mechanism by non‐diazotrophic cyanobacteria for their diazotrophic phylum group members (N 2 fixers). Our observations may help to understand the prevalence of diazotrophy in low‐phosphate, oligotrophic regions.

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