Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosms

The response of N<sub>2</sub> (dinitrogen) fixation to contrasted (wet and dry) Saharan dust deposition was studied in the framework of the DUNE project (a DUst experiment in a low-Nutrient, low-chlorophyll Ecosystem) during which realistic simulations of dust deposition (10 g m<sup&g...

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Main Authors: C. Ridame, C. Guieu, S. L'Helguen
Format: Article
Language:English
Published: Copernicus Publications 2013-11-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/10/7333/2013/bg-10-7333-2013.pdf
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author C. Ridame
C. Guieu
S. L'Helguen
author_facet C. Ridame
C. Guieu
S. L'Helguen
author_sort C. Ridame
collection DOAJ
description The response of N<sub>2</sub> (dinitrogen) fixation to contrasted (wet and dry) Saharan dust deposition was studied in the framework of the DUNE project (a DUst experiment in a low-Nutrient, low-chlorophyll Ecosystem) during which realistic simulations of dust deposition (10 g m<sup>&minus;2</sup>) into large mesocosms (52 m<sup>3</sup>) were performed. Three distinct experimental dust additions were conducted in June 2008 (DUNE-1-P: simulation of a wet deposition, DUNE-1-Q: simulation of a dry deposition) and 2010 (DUNE-2-R: simulation of 2 successive wet depositions) in the northwestern oligotrophic Mediterranean Sea. Here we show that wet and dry dust deposition induced a rapid (24 h or 48 h after dust additions), strong (from 2- to 5.3-fold) and long (at least 4–6 days duration) increase in N<sub>2</sub> fixation, indicating that both wet and dry Saharan dust deposition was able to relieve efficiently the nutrient limitation(s) of N<sub>2</sub> fixation. This means in particular that N<sub>2</sub> fixation activity was not inhibited by the significant input of nitrate associated with the simulated wet deposition (~ 9 mmol NO<sub>3</sub><sup>&minus;</sup> m<sup>&minus;2</sup>). The input of new nitrogen associated with N<sub>2</sub> fixation was negligible relative to the atmospheric NO<sub>3</sub><sup>&minus;</sup> input associated with the dust. The contribution of N<sub>2</sub> fixation to primary production was negligible (&le; 1%) before and after dust addition in all experiments, indicating that N<sub>2</sub> fixation was a poor contributor to the nitrogen demand for primary production. Despite the stimulation of N<sub>2</sub> fixation by dust addition, the rates remained low, and did not significantly change the contribution of N<sub>2</sub> fixation to new production since only a maximum contribution of 10% was observed. The response of N<sub>2</sub> fixation by diazotrophs and CO<sub>2</sub> fixation by the whole phytoplankton community suggests that these metabolic processes were limited or co-limited by different nutrients. With this novel approach, which allows us to study processes as a function of time while atmospheric particles are sinking, we show that new atmospheric nutrients associated with Saharan dust pulses do significantly stimulate N<sub>2</sub> fixation in the Mediterranean Sea and that N<sub>2</sub> fixation is not a key process in the carbon cycle in such oligotrophic environments.
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spelling doaj.art-ea3b1bee0dee467b9b05cad4dc568b902022-12-21T19:26:39ZengCopernicus PublicationsBiogeosciences1726-41701726-41892013-11-0110117333734610.5194/bg-10-7333-2013Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosmsC. Ridame0C. Guieu1S. L'Helguen2CNRS-INSU/IRD/MNHN/UPMC, LOCEAN: Laboratoire d'Océanographie et du Climat: Expérimentation et Approches Numériques, UMR7159, 4 Place Jussieu &ndash; 75252 Paris Cedex 05, FranceLOV: Laboratoire d'Océanographie de Villefranche/Mer, CNRS-INSU UMR7093, Observatoire Océanologique, 06230 Villefranche-sur-Mer, FranceUniversité de Brest, CNRS/IRD, UMR6539, Laboratoire des Sciences de l'Environnement Marin, OSU-IUEM, 29280 Plouzané, FranceThe response of N<sub>2</sub> (dinitrogen) fixation to contrasted (wet and dry) Saharan dust deposition was studied in the framework of the DUNE project (a DUst experiment in a low-Nutrient, low-chlorophyll Ecosystem) during which realistic simulations of dust deposition (10 g m<sup>&minus;2</sup>) into large mesocosms (52 m<sup>3</sup>) were performed. Three distinct experimental dust additions were conducted in June 2008 (DUNE-1-P: simulation of a wet deposition, DUNE-1-Q: simulation of a dry deposition) and 2010 (DUNE-2-R: simulation of 2 successive wet depositions) in the northwestern oligotrophic Mediterranean Sea. Here we show that wet and dry dust deposition induced a rapid (24 h or 48 h after dust additions), strong (from 2- to 5.3-fold) and long (at least 4–6 days duration) increase in N<sub>2</sub> fixation, indicating that both wet and dry Saharan dust deposition was able to relieve efficiently the nutrient limitation(s) of N<sub>2</sub> fixation. This means in particular that N<sub>2</sub> fixation activity was not inhibited by the significant input of nitrate associated with the simulated wet deposition (~ 9 mmol NO<sub>3</sub><sup>&minus;</sup> m<sup>&minus;2</sup>). The input of new nitrogen associated with N<sub>2</sub> fixation was negligible relative to the atmospheric NO<sub>3</sub><sup>&minus;</sup> input associated with the dust. The contribution of N<sub>2</sub> fixation to primary production was negligible (&le; 1%) before and after dust addition in all experiments, indicating that N<sub>2</sub> fixation was a poor contributor to the nitrogen demand for primary production. Despite the stimulation of N<sub>2</sub> fixation by dust addition, the rates remained low, and did not significantly change the contribution of N<sub>2</sub> fixation to new production since only a maximum contribution of 10% was observed. The response of N<sub>2</sub> fixation by diazotrophs and CO<sub>2</sub> fixation by the whole phytoplankton community suggests that these metabolic processes were limited or co-limited by different nutrients. With this novel approach, which allows us to study processes as a function of time while atmospheric particles are sinking, we show that new atmospheric nutrients associated with Saharan dust pulses do significantly stimulate N<sub>2</sub> fixation in the Mediterranean Sea and that N<sub>2</sub> fixation is not a key process in the carbon cycle in such oligotrophic environments.http://www.biogeosciences.net/10/7333/2013/bg-10-7333-2013.pdf
spellingShingle C. Ridame
C. Guieu
S. L'Helguen
Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosms
Biogeosciences
title Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosms
title_full Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosms
title_fullStr Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosms
title_full_unstemmed Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosms
title_short Strong stimulation of N<sub>2</sub> fixation in oligotrophic Mediterranean Sea: results from dust addition in large in situ mesocosms
title_sort strong stimulation of n sub 2 sub fixation in oligotrophic mediterranean sea results from dust addition in large in situ mesocosms
url http://www.biogeosciences.net/10/7333/2013/bg-10-7333-2013.pdf
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AT cguieu strongstimulationofnsub2subfixationinoligotrophicmediterraneansearesultsfromdustadditioninlargeinsitumesocosms
AT slhelguen strongstimulationofnsub2subfixationinoligotrophicmediterraneansearesultsfromdustadditioninlargeinsitumesocosms