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Phytoplankton size structure and primary production in a highly dynamic. coastal ecosystem (Ria de Vigo, NW-Spain): Seasonal and short-time scale variability

Authors :
Pedro Cermeño
Emilio Fernández
Carmen G. Castro
Emilio Marañón
Pablo Serret
Valesca Pérez
Laboratoire d'océanographie de Villefranche (LOV)
Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de la Mer de Villefranche (IMEV)
Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Source :
ESTUARINE COASTAL AND SHELF SCIENCE, ESTUARINE COASTAL AND SHELF SCIENCE, 2006, 67 (1-2), pp.251-266. ⟨10.1016/j.ecss.2005.11.027⟩
Publication Year :
2006
Publisher :
HAL CCSD, 2006.

Abstract

Size-fractionated phytoplankton biomass and primary production, together with net community metabolism, were measured in a coastal ecosystem (Ria de Vigo, NW-Spain) during a full annual cycle (July 2001-July 2002). On a seasonal scale, this ecosystem was characterized by two distinct oceanographic conditions, namely upwelling and downwelling favourable seasons. During the upwelling season, total chlorophyll a (Chl a) and particulate organic carbon production rates (POC-pr) were in the range 36-129 mg Chl a m(-2) and 89-834 mg C m(-2) h(-1), respectively, and were mainly accounted for (> 80%) by the microphytoplankton size fraction (> 20 pm). During the downwelling season, total Chl a and POC-pr were much lower (< 27 mg Chl a m(-2) and < 97 mg C m(-2) h(-1), respectively), and the pico- (< 2 mu m) and nano-(2-20 mu m) phytoplankton size fractions significantly increased their contribution to total Chl a (46-87%) and POC-pr (30-86%). The seasonal and short-time scale variability in the hydrographic conditions, in particular upwelling intermittency, provides a feasible explanation for the continuous dominance of large-sized phytoplankton during the upwelling period. Shelf water intrusions, continuous vertical mixing and the size-dependent limitation in light acquisition (package effect), suffered in a higher degree by larger phytoplankton, were likely to account for the shift in phytoplankton size structure during the downwelling period. During the upwelling season, community respiration represented a minor fraction of gross primary production (15-30%), which highlights the large export potential of organic matter by this ecosystem. On the contrary, community respiration accounted for a major fraction of primary production (85%) during the downwelling period, which suggests that most of the photosynthesised organic matter was remineralised within the ecosystem. Although the microbial plankton community of the Rfa de Vigo exhibits a net autotrophic functioning throughout the year, the magnitude of the carbon flows and budgets seems to be dependent on phytoplankton size structure. (c) 2005 Elsevier Ltd. All rights reserved.

Details

Language :
English
Database :
OpenAIRE
Journal :
ESTUARINE COASTAL AND SHELF SCIENCE, ESTUARINE COASTAL AND SHELF SCIENCE, 2006, 67 (1-2), pp.251-266. ⟨10.1016/j.ecss.2005.11.027⟩
Accession number :
edsair.doi.dedup.....8e57964c6c37a86e7ed408c7e61f64b9
Full Text :
https://doi.org/10.1016/j.ecss.2005.11.027⟩