Spatial variation in N 2 -fixation rate and diazotroph activity in the Tropical Atlantic

• Main Authors: Montoya, J. P., Voss, M., Capone, D. G.
• Other Authors: Georgia Institute of Technology Atlanta, Leibniz-Institut für Ostseeforschung Warnemünde (IOW), Leibniz Association, University of Southern California (USC)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2007
• Subjects: [PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]; [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]; [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces; environment; [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; [SDU.STU]Sciences of the Universe [physics]/Earth Sciences; North Atlantic
• Online Access: https://hal.science/hal-00297619; https://hal.science/hal-00297619/document; https://hal.science/hal-00297619/file/bg-4-369-2007.pdf

International audience A variety of N 2 -fixers occur in oligotrophic waters and these diazotrophs make a substantial contribution to the nitrogen budget of the upper water column. A synthesis of previously published and new rate measurements for the North Atlantic provides insight into the role of two different groups of N 2 -fixers ( Trichodesmium and small diazotrophs) in supporting N 2 fixation in the tropical Atlantic. The highest rates of N 2 fixation occurred in the western part of the basin, but the full data set showed no significant difference between the eastern and western parts of the basin in overall rates of N 2 -fixation by the two groups of diazotrophs. N 2 -fixation by Trichodesmium was strongly dominant in the western part of the basin while small diazotrophs played a much larger role to the east of 40° W. The reasons for this shift in dominance are unclear, as is the identity of the small organisms fixing N 2 in the water column.