Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic Ocean
We have determined the latitudinal distribution of <i>Trichodesmium</i> spp. abundance and community N<sub>2</sub> fixation in the Atlantic Ocean along a meridional transect from ca. 30° N to 30° S in November–December 2007 and April–May 2008. The observations from both cruis...
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doaj-e8d0930214bd4b8cb7e8946f47fc71072020-11-25T01:21:38ZengCopernicus PublicationsBiogeosciences1726-41701726-41892010-10-017103167317610.5194/bg-7-3167-2010Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic OceanE. MarañónM. VarelaA. BodeB. Mouriño-CarballidoA. FernándezWe have determined the latitudinal distribution of <i>Trichodesmium</i> spp. abundance and community N<sub>2</sub> fixation in the Atlantic Ocean along a meridional transect from ca. 30° N to 30° S in November–December 2007 and April–May 2008. The observations from both cruises were highly consistent in terms of absolute magnitude and latitudinal distribution, showing a strong association between <i>Trichodesmium</i> abundance and community N<sub>2</sub> fixation. The highest <i>Trichodesmium</i> abundances (mean = 220 trichomes L<sup>−1,</sup>) and community N<sub>2</sub> fixation rates (mean = 60 μmol m<sup>−2</sup> d<sup>−1</sup>) occurred in the Equatorial region between 5° S–15° N. In the South Atlantic gyre, <i>Trichodesmium</i> abundance was very low (ca. 1 trichome L<sup>−1</sup>) but N<sub>2</sub> fixation was always measurable, averaging 3 and 10 μmol m<sup>2</sup> d<sup>−1</sup> in 2007 and 2008, respectively. We suggest that N<sub>2</sub> fixation in the South Atlantic was sustained by other, presumably unicellular, diazotrophs. Comparing these distributions with the geographical pattern in atmospheric dust deposition points to iron supply as the main factor determining the large scale latitudinal variability of <i>Trichodesmium</i> spp. abundance and N<sub>2</sub> fixation in the Atlantic Ocean. We observed a marked South to North decrease in surface phosphate concentration, which argues against a role for phosphorus availability in controlling the large scale distribution of N<sub>2</sub> fixation. Scaling up from all our measurements (42 stations) results in conservative estimates for total N<sub>2</sub> fixation of ∼6 TgN yr<sup>−1</sup> in the North Atlantic (0–40° N) and ~1.2 TgN yr<sup>−1</sup> in the South Atlantic (0–40° S). http://www.biogeosciences.net/7/3167/2010/bg-7-3167-2010.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
E. Marañón M. Varela A. Bode B. Mouriño-Carballido A. Fernández |
spellingShingle |
E. Marañón M. Varela A. Bode B. Mouriño-Carballido A. Fernández Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic Ocean Biogeosciences |
author_facet |
E. Marañón M. Varela A. Bode B. Mouriño-Carballido A. Fernández |
author_sort |
E. Marañón |
title |
Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic Ocean |
title_short |
Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic Ocean |
title_full |
Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic Ocean |
title_fullStr |
Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic Ocean |
title_full_unstemmed |
Latitudinal distribution of <i>Trichodesmium</i> spp. and N<sub>2</sub> fixation in the Atlantic Ocean |
title_sort |
latitudinal distribution of <i>trichodesmium</i> spp. and n<sub>2</sub> fixation in the atlantic ocean |
publisher |
Copernicus Publications |
series |
Biogeosciences |
issn |
1726-4170 1726-4189 |
publishDate |
2010-10-01 |
description |
We have determined the latitudinal distribution of <i>Trichodesmium</i> spp. abundance and community N<sub>2</sub> fixation in the Atlantic Ocean along a meridional transect from ca. 30° N to 30° S in November–December 2007 and April–May 2008. The observations from both cruises were highly consistent in terms of absolute magnitude and latitudinal distribution, showing a strong association between <i>Trichodesmium</i> abundance and community N<sub>2</sub> fixation. The highest <i>Trichodesmium</i> abundances (mean = 220 trichomes L<sup>−1,</sup>) and community N<sub>2</sub> fixation rates (mean = 60 μmol m<sup>−2</sup> d<sup>−1</sup>) occurred in the Equatorial region between 5° S–15° N. In the South Atlantic gyre, <i>Trichodesmium</i> abundance was very low (ca. 1 trichome L<sup>−1</sup>) but N<sub>2</sub> fixation was always measurable, averaging 3 and 10 μmol m<sup>2</sup> d<sup>−1</sup> in 2007 and 2008, respectively. We suggest that N<sub>2</sub> fixation in the South Atlantic was sustained by other, presumably unicellular, diazotrophs. Comparing these distributions with the geographical pattern in atmospheric dust deposition points to iron supply as the main factor determining the large scale latitudinal variability of <i>Trichodesmium</i> spp. abundance and N<sub>2</sub> fixation in the Atlantic Ocean. We observed a marked South to North decrease in surface phosphate concentration, which argues against a role for phosphorus availability in controlling the large scale distribution of N<sub>2</sub> fixation. Scaling up from all our measurements (42 stations) results in conservative estimates for total N<sub>2</sub> fixation of ∼6 TgN yr<sup>−1</sup> in the North Atlantic (0–40° N) and ~1.2 TgN yr<sup>−1</sup> in the South Atlantic (0–40° S). |
url |
http://www.biogeosciences.net/7/3167/2010/bg-7-3167-2010.pdf |
work_keys_str_mv |
AT emaranon latitudinaldistributionofitrichodesmiumisppandnsub2subfixationintheatlanticocean AT mvarela latitudinaldistributionofitrichodesmiumisppandnsub2subfixationintheatlanticocean AT abode latitudinaldistributionofitrichodesmiumisppandnsub2subfixationintheatlanticocean AT bmourinocarballido latitudinaldistributionofitrichodesmiumisppandnsub2subfixationintheatlanticocean AT afernandez latitudinaldistributionofitrichodesmiumisppandnsub2subfixationintheatlanticocean |
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1725129355048255488 |