An estimation of annual new production and carbon fluxes in the northeast Atlantic Ocean during 2001

A dual 13C/15N isotopic technique was used to estimate carbon and nitrogen uptake rates during the 1‐year‐long Programme Océan Multidisciplinaire Méso Echelle (POMME) experiment in the northeast basin of the Atlantic Ocean (16°–22°W, 38°–45°N). Rates of primary production ranged from 2.26 μmoles L−1...

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Veröffentlicht in:Journal of Geophysical Research 2005-07, Vol.110 (C7), p.n/a
Hauptverfasser: Fernández I., Camila, Raimbault, Patrick, Garcia, Nicole, Rimmelin, Peggy, Caniaux, Guy
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Raimbault, Patrick
Garcia, Nicole
Rimmelin, Peggy
Caniaux, Guy
description A dual 13C/15N isotopic technique was used to estimate carbon and nitrogen uptake rates during the 1‐year‐long Programme Océan Multidisciplinaire Méso Echelle (POMME) experiment in the northeast basin of the Atlantic Ocean (16°–22°W, 38°–45°N). Rates of primary production ranged from 2.26 μmoles L−1 d−1 in winter to maximum surface values of 7.8 μmoles L−1 d−1 during the spring season. Nitrate assimilation was intense since the beginning of winter and accounted for 3–7 mmoles m−2 d−1 in the first 80 m depth of the water column. Rates increased to 5–9 mmoles m−2 d−1 during the spring season. NO3− uptake rates during the late summer season were close to winter values. Ammonium assimilation activity balanced the uptake of nitrate for all seasons. The seasonal f ratio was close to 0.28 in winter, increased to 0.34 in spring, and, finally, decreased to 0.25 in late summer. Annual carbon uptake rates for the entire POMME area accounted for 16.9 moles C m−2 yr−1. From this result, annual new production could be estimated to 5.7 moles C m−2 yr−1.
doi_str_mv 10.1029/2004JC002616
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Geophys. Res</addtitle><description>A dual 13C/15N isotopic technique was used to estimate carbon and nitrogen uptake rates during the 1‐year‐long Programme Océan Multidisciplinaire Méso Echelle (POMME) experiment in the northeast basin of the Atlantic Ocean (16°–22°W, 38°–45°N). Rates of primary production ranged from 2.26 μmoles L−1 d−1 in winter to maximum surface values of 7.8 μmoles L−1 d−1 during the spring season. Nitrate assimilation was intense since the beginning of winter and accounted for 3–7 mmoles m−2 d−1 in the first 80 m depth of the water column. Rates increased to 5–9 mmoles m−2 d−1 during the spring season. NO3− uptake rates during the late summer season were close to winter values. Ammonium assimilation activity balanced the uptake of nitrate for all seasons. The seasonal f ratio was close to 0.28 in winter, increased to 0.34 in spring, and, finally, decreased to 0.25 in late summer. 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source Wiley Online Library - AutoHoldings Journals; Wiley-Blackwell AGU Digital Library; Wiley Online Library (Open Access Collection); Alma/SFX Local Collection
subjects Marine
mesoscale features
nitrogen cycling
North Atlantic Ocean
Ocean, Atmosphere
primary production
Sciences of the Universe
title An estimation of annual new production and carbon fluxes in the northeast Atlantic Ocean during 2001
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