Phytoplankton biomass cycles in the North Atlantic subpolar gyre: A similar mechanism for two different blooms in the Labrador Sea

• Published in: Geophysical Research Letters
• Main Authors: Lacour, Léo, Claustre, Hervé, Prieur, Louis, D'Ortenzio, Fabrizio
• Other Authors: Laboratoire d'océanographie de Villefranche (LOV), Observatoire océanologique de Villefranche-sur-mer (OOVM), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), This paper represents a contribution to the remOcean (REMotely sensed biogeochemical cycles in the OCEAN, GA 246777) project funded by the European Research Council and to OSS2015 (Ocean strategic services beyond 2015) funded by the seventh framework program (EU) and the ATLANTOS EU project (grant agreement 2014-633211) funded by H2020 program., European Project: 282723,EC:FP7:SPA,FP7-SPACE-2011-1,OSS2015(2011), European Project: 633211,H2020,H2020-BG-2014-2,AtlantOS(2015), European Project: 246777,EC:FP7:ERC,ERC-2009-AdG,REMOCEAN(2010)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2015
• Subjects: bioregions; phytoplankton biomass cycle; light-mixing regime; Labrador Sea; [SDV.EE.BIO]Life Sciences [q-bio]/Ecology; environment/Bioclimatology; [SDV.EE.ECO]Life Sciences [q-bio]/Ecology; environment/Ecosystems; North Atlantic
• Online Access: https://hal.sorbonne-universite.fr/hal-01177050; https://hal.sorbonne-universite.fr/hal-01177050/document; https://hal.sorbonne-universite.fr/hal-01177050/file/grl53105.pdf; https://doi.org/10.1002/2015GL064540

International audience An analysis of seasonal variations in climatological surface chlorophyll points to distinct biogeographical zones in the North Atlantic subpolar gyre. In particular, the Labrador Sea appears well delineated into two regions on either side of the 60°N parallel, with very different climatological phytoplankton biomass cycles. Indeed, north of 60°N, an early and short spring bloom occurs in late April, while south of 60°N, the bloom gradually develops 1 month later and significant biomass persists all summer long. Nevertheless, at climatological scale, the first-order mechanism that controls the bloom is identical for both bioregions. The light-mixing regime can explain the bloom onset in both bioregions. In the Labrador Sea, the blooms seem to rely on a mean community compensation irradiance threshold value of 2.5 mol photon m−2 d−1 over the mixed layer.