Nitrogen fixation by <i>Trichodesmium</i> spp.: An important source of new nitrogen to the tropical and subtropical North Atlantic Ocean

Douglas G. Capone(University of Southern California), James A. Burns(University of Southern California), Joseph P. Montoya(Georgia Institute of Technology), Ajit Subramaniam(Lamont-Doherty Earth Observatory), Claire Mahaffey(University of Southern California), Troy Gunderson(University of Southern California), Anthony F. Michaels(University of Southern California), Edward J. Carpenter(San Francisco State University)
Global Biogeochemical Cycles
June 1, 2005
Cited by 633

Abstract

The broad distribution and often high densities of the cyanobacterium Trichodesmium spp. in oligotrophic waters imply a substantial role for this one taxon in the oceanic N cycle of the marine tropics and subtropics. New results from 154 stations on six research cruises in the North Atlantic Ocean show depth‐integrated N 2 fixation by Trichodesmium spp. at many stations that equalled or exceeded the estimated vertical flux of NO 3 − into the euphotic zone by diapycnal mixing. Areal rates are consistent with those derived from several indirect geochemical analyses. Direct measurements of N 2 fixation rates by Trichodesmium are also congruent with upper water column N budgets derived from parallel determinations of stable isotope distributions, clearly showing that N 2 fixation by Trichodesmium is a major source of new nitrogen in the tropical North Atlantic. We project a conservative estimate of the annual input of new N into the tropical North Atlantic of at least 1.6 × 10 12 mol N by Trichodesmium N 2 fixation alone. This input can account for a substantial fraction of the N 2 fixation in the North Atlantic inferred by several of the geochemical approaches.


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