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Ridame C., Dekaezemacker J., Guieu C., Bonnet Sophie, L'Helguen S., Malien F. (2014). Contrasted Saharan dust events in LNLC environments : impact on nutrient dynamics and primary production. Biogeosciences, 11 (17), 4783-4800. ISSN 1726-4170

Fichier PDF disponiblehttp://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers17-10/010062557.pdf[ PDF Link ]

Lien direct chez l'éditeur doi:10.5194/bg-11-4783-2014

Titre
Contrasted Saharan dust events in LNLC environments : impact on nutrient dynamics and primary production
Année de publication2014
Type de documentArticle référencé dans le Web of Science WOS:000342116000015
AuteursRidame C., Dekaezemacker J., Guieu C., Bonnet Sophie, L'Helguen S., Malien F.
SourceBiogeosciences, 2014, 11 (17), p. 4783-4800. ISSN 1726-4170
RésuméThe response of the phytoplanktonic community (primary production and algal biomass) to contrasted Saharan dust events (wet and dry deposition) was studied in the framework of the DUNE ("a DUst experiment in a low-Nutrient, low-chlorophyll Ecosystem") project. We simulated realistic dust deposition events (10 gm(-2)) into large mesocosms (52m(3)). Three distinct dust addition experiments 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-R1 and DUNE-2-R2: simulation of two successive wet depositions) in the northwestern oligotrophic Mediterranean Sea. No changes in primary production (PP) and chlorophyll a concentrations (Chl a) were observed after a dry deposition event, while a wet deposition event resulted in a rapid (24 h after dust addition), strong (up to 2.4-fold) and long (at least a week in duration) increase in PP and Chl a. We show that, in addition to being a source of dissolved inorganic phosphorus (DIP), simulated wet deposition events were also a significant source of nitrate (NO3-) (net increases up to +9.8 mu M NO3- at 0.1m in depth) to the nutrient-depleted surface waters, due to cloud processes and mixing with anthropogenic species such as HNO3. The dry deposition event was shown to be a negligible source of NO3-. By transiently increasing DIP and NO3- concentrations in N-P starved surface waters, wet deposition of Saharan dust was able to relieve the potential N or NP co-limitation of the phytoplanktonic activity. Due to the higher input of NO3- relative to DIP, and taking into account the stimulation of the biological activity, a wet deposition event resulted in a strong increase in the NO3-/DIP ratio, from initially less than 6, to over 150 at the end of the DUNE-2-R1 experiment, suggesting a switch from an initial N or NP co-limitation towards a severe P limitation. We also show that the contribution of new production to PP strongly increased after wet dust deposition events, from initially 15% to 60-70% 24 h after seeding, indicating a switch from a regenerated-production based system to a new-production based system. DUNE experiments show that wet and dry dust deposition events induce contrasting responses of the phytoplanktonic community due to differences in the atmospheric supply of bioavailable new nutrients. Our results from original mesocosm experiments demonstrate that atmospheric dust wet deposition greatly influences primary productivity and algal biomass in LNLC environments through changes in the nutrient stocks, and alters the NO3-/DIP ratio, leading to a switch in the nutrient limitation of the phytoplanktonic activity.
Plan de classementEcologie, systèmes aquatiques [036] ; Sciences du milieu [021]
Descr. géo.MEDITERRANEE ; SAHARA
LocalisationFonds IRD [F B010062557]
Identifiant IRDfdi:010062557
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010062557

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