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Rates of dinitrogen fixation and the abundance of diazotrophs in North American coastal waters between Cape Hatteras and Georges Bank
Author(s) -
Mulholland M. R.,
Bernhardt P. W.,
Blanco-Garcia J. L.,
Mannino A.,
Hyde K.,
Mondragon E.,
Turk K.,
Moisander P. H.,
Zehr J. P.
Publication year - 2012
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.2012.57.4.1067
Subject(s) - continental shelf , diazotroph , oceanography , temperate climate , pelagic zone , abundance (ecology) , trichodesmium , geology , environmental science , ecology , biology , nitrogen fixation , paleontology , bacteria
We coupled dinitrogen (N 2 ) fixation rate estimates with molecular biological methods to determine the activity and abundance of diazotrophs in coastal waters along the temperate North American Mid‐Atlantic continental shelf during multiple seasons and cruises. Volumetric rates of N 2 fixation were as high as 49.8 nmol N L −1 d −1 and areal rates as high as 837.9 µmol N m −2 d −1 in our study area. Our results suggest that N 2 fixation occurs at high rates in coastal shelf waters that were previously thought to be unimportant sites of N 2 fixation and so were excluded from calculations of pelagic marine N 2 fixation. Unicellular N 2 ‐fixing group A cyanobacteria were the most abundant diazotrophs in the Atlantic coastal waters and their abundance was comparable to, or higher than, that measured in oceanic regimes where they were discovered. High rates of N 2 fixation and the high abundance of diazotrophs along the North American Mid‐Atlantic continental shelf highlight the need to revise marine N budgets to include coastal N 2 fixation. Integrating areal rates of N 2 fixation over the continental shelf area between Cape Hatteras and Nova Scotia, the estimated N 2 fixation in this temperate shelf system is about 0.02 Tmol N yr −1 , the amount previously calculated for the entire North Atlantic continental shelf. Additional studies should provide spatially, temporally, and seasonally resolved rate estimates from coastal systems to better constrain N inputs via N 2 fixation from the neritic zone.