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Longitudinal variability of the biogeochemical role of Mediterranean aerosols in the Mediterranean Sea
Ternon E., Guieu C., Ridame C., L'Helguen S., Catala P.
Biogeosciences 8 (2011) 1067-1080 - http://hal.univ-brest.fr/hal-00671170
Articles dans des revues avec comité de lecture
Sciences de l'environnement
Longitudinal variability of the biogeochemical role of Mediterranean aerosols in the Mediterranean Sea
E. Ternon 1, Cécile Guieu () 1, C. Ridame 2, Stéphane L'Helguen () 3, P. Catala 4
1 :  Laboratoire d'océanographie de Villefranche (LOV)
http://www.obs-vlfr.fr
CNRS : UMR7093 – INSU – Université Pierre et Marie Curie [UPMC] - Paris VI
BP 28 06234 VILLEFRANCHE SUR MER CEDEX
France
2 :  Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Institut de recherche pour le développement [IRD] – INSU – CNRS : UMR7159 – Université Pierre et Marie Curie [UPMC] - Paris VI – Muséum National d'Histoire Naturelle (MNHN)
case 100 4 place jussieu 75252 PARIS CEDEX 05
France
3 :  Laboratoire des Sciences de l'Environnement Marin (LEMAR)
http://www-iuem.univ-brest.fr/UMR6539/
Institut Universitaire Européen de la Mer (IUEM) – Université de Bretagne Occidentale [UBO] – CNRS : UMR6539 – Institut de Recherche pour le Développement
Technopôle Brest-Iroise, Place Nicolas Copernic, 29280 Plouzané
France
4 :  Laboratoire d'Océanographie Microbienne (LOMIC)
Université Pierre et Marie Curie [UPMC] - Paris VI – CNRS : UMR7621
Observatoire Océanologique, Banyuls/mer
France
The Mediterranean Sea is a semi-enclosed basin characterized by a strong thermal stratification during summer during which the atmosphere is the main source of new nutrients to the nutrient-depleted surface layer. From aerosol sampling and microcosm experiments performed during the TransMed BOUM cruise (June-July 2008) we showed that: (i) the Mediterranean atmosphere composition (Al, Fe, P) was homogeneous over ~28° of longitude and was a mixture with a constant proportion of anthropogenic contribution and a variable but modest contribution of crustal aerosols. This quite stable composition over a one month period and a long transect (~2500 km) allowed to define the Mediterranean atmospheric "background" that characterizes the summer season in the absence of major Saharan event and forest fires, (ii) primary production significantly increased at all tested stations after aerosols addition collected on-board and after Saharan dust analog addition, indicating that both additions relieved on-going (co)-limitations. Although both additions significantly increased the N2 fixation rates at the western station, diazotrophic activity remained very low (~0.2 nmol N L−1 d−1), (iii) due to the presence of anthropogenic particles, the probable higher solubility of nutrients associated with mixed aerosols (crustal + anthropogenic contribution), conferred a higher fertilizing potential to on-board collected aerosol as compared to Saharan dust analog. Finally, those experiments showed that atmospheric inputs from a mixed atmospheric event ("summer rain" type) or from a high-intensity Saharan event would induce comparable response by the biota in the stratified Mediterranean SML, during summer.
Anglais

Biogeosciences
Publisher European Geosciences Union (EGU)
ISSN 1726-4170 (eISSN : 1726-4189)
internationale
17/11/2011
8
1067-1080

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