Plankton response to weakening of the Iberian coastal upwelling

10 páginas, 4 figuras Coastal upwelling regions, which are affected by equatorward-wind variability, are among the most productive areas of the oceans. It has been suggested that global warming will lead to a general strengthening of coastal upwelling, with important ecological implications and an i...

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Published in:Global Change Biology
Main Authors: Pérez, Fiz F., Padín, X. A., Pazos, Yolanda, Gilcoto, Miguel, Cabanas, Manuel, Pardo, Paula C., Doval, M. Dolores, Farina-Busto, L.
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons 2010
Subjects:
Online Access:http://hdl.handle.net/10261/47957
https://doi.org/10.1111/j.1365-2486.2009.02125.x
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spelling ftcsic:oai:digital.csic.es:10261/47957 2024-02-11T10:06:39+01:00 Plankton response to weakening of the Iberian coastal upwelling Pérez, Fiz F. Padín, X. A. Pazos, Yolanda Gilcoto, Miguel Cabanas, Manuel Pardo, Paula C. Doval, M. Dolores Farina-Busto, L. 2010 http://hdl.handle.net/10261/47957 https://doi.org/10.1111/j.1365-2486.2009.02125.x en eng John Wiley & Sons http://dx.doi.org/10.1111/j.1365-2486.2009.02125.x Global Change Biology 16(4): 1258-1267 (2010) 1354-1013 http://hdl.handle.net/10261/47957 doi:10.1111/j.1365-2486.2009.02125.x 1365-2486 open Climate change Coastal ecosystems Coastal upwelling Plankton succession artículo http://purl.org/coar/resource_type/c_6501 2010 ftcsic https://doi.org/10.1111/j.1365-2486.2009.02125.x 2024-01-16T09:37:04Z 10 páginas, 4 figuras Coastal upwelling regions, which are affected by equatorward-wind variability, are among the most productive areas of the oceans. It has been suggested that global warming will lead to a general strengthening of coastal upwelling, with important ecological implications and an impact on fisheries. However, in the case of the Iberian upwelling, the long-term analysis of climatological variables described here reveals a weakening in coastal upwelling. This is linked to a decrease of zonal sea level pressure gradient, and correlated with an observed increase of sea surface temperature and North Atlantic Oscillation. Weakening of coastal upwelling has led to quantifiable modifications of the ecosystem. In outer shelf waters a drop in new production over the last 40 years is likely related to the reduction of sardine landings at local harbors. On the other hand, in inner shelf and Ria waters, the observed weakening of upwelling has slowed down the residual circulation that introduces nutrients to the euphotic layer, and has increased the stability of the water column. The drop in nutrient levels has been compensated by an increase of organic matter remineralization. The phytoplankton community has responded to those environmental trends with an increase in the percentage of dinoflagellates and Pseudonitzschia spp. and a reduction in total diatoms. The former favors the proliferation of harmful algal blooms and reduces the permitted harvesting period for the mussel aquaculture industry. The demise of the sardine fishery and the potential threat to the mussel culture could have serious socio-economic consequences for the region. This study was partially funded by the European Commission (EU FP6 CARBOOCEAN Integrated Project, Contract no. 511176) and Xunta de Galiza (PGIDIT05PXIC40203PM, PGIDIT08MMA014402PR, PGIDIT07PXIB402153PR and PGIDIT05- MA40201PR). Peer reviewed Article in Journal/Newspaper North Atlantic North Atlantic oscillation Digital.CSIC (Spanish National Research Council) Global Change Biology 16 4 1258 1267
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Climate change
Coastal ecosystems
Coastal upwelling
Plankton succession
spellingShingle Climate change
Coastal ecosystems
Coastal upwelling
Plankton succession
Pérez, Fiz F.
Padín, X. A.
Pazos, Yolanda
Gilcoto, Miguel
Cabanas, Manuel
Pardo, Paula C.
Doval, M. Dolores
Farina-Busto, L.
Plankton response to weakening of the Iberian coastal upwelling
topic_facet Climate change
Coastal ecosystems
Coastal upwelling
Plankton succession
description 10 páginas, 4 figuras Coastal upwelling regions, which are affected by equatorward-wind variability, are among the most productive areas of the oceans. It has been suggested that global warming will lead to a general strengthening of coastal upwelling, with important ecological implications and an impact on fisheries. However, in the case of the Iberian upwelling, the long-term analysis of climatological variables described here reveals a weakening in coastal upwelling. This is linked to a decrease of zonal sea level pressure gradient, and correlated with an observed increase of sea surface temperature and North Atlantic Oscillation. Weakening of coastal upwelling has led to quantifiable modifications of the ecosystem. In outer shelf waters a drop in new production over the last 40 years is likely related to the reduction of sardine landings at local harbors. On the other hand, in inner shelf and Ria waters, the observed weakening of upwelling has slowed down the residual circulation that introduces nutrients to the euphotic layer, and has increased the stability of the water column. The drop in nutrient levels has been compensated by an increase of organic matter remineralization. The phytoplankton community has responded to those environmental trends with an increase in the percentage of dinoflagellates and Pseudonitzschia spp. and a reduction in total diatoms. The former favors the proliferation of harmful algal blooms and reduces the permitted harvesting period for the mussel aquaculture industry. The demise of the sardine fishery and the potential threat to the mussel culture could have serious socio-economic consequences for the region. This study was partially funded by the European Commission (EU FP6 CARBOOCEAN Integrated Project, Contract no. 511176) and Xunta de Galiza (PGIDIT05PXIC40203PM, PGIDIT08MMA014402PR, PGIDIT07PXIB402153PR and PGIDIT05- MA40201PR). Peer reviewed
format Article in Journal/Newspaper
author Pérez, Fiz F.
Padín, X. A.
Pazos, Yolanda
Gilcoto, Miguel
Cabanas, Manuel
Pardo, Paula C.
Doval, M. Dolores
Farina-Busto, L.
author_facet Pérez, Fiz F.
Padín, X. A.
Pazos, Yolanda
Gilcoto, Miguel
Cabanas, Manuel
Pardo, Paula C.
Doval, M. Dolores
Farina-Busto, L.
author_sort Pérez, Fiz F.
title Plankton response to weakening of the Iberian coastal upwelling
title_short Plankton response to weakening of the Iberian coastal upwelling
title_full Plankton response to weakening of the Iberian coastal upwelling
title_fullStr Plankton response to weakening of the Iberian coastal upwelling
title_full_unstemmed Plankton response to weakening of the Iberian coastal upwelling
title_sort plankton response to weakening of the iberian coastal upwelling
publisher John Wiley & Sons
publishDate 2010
url http://hdl.handle.net/10261/47957
https://doi.org/10.1111/j.1365-2486.2009.02125.x
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation http://dx.doi.org/10.1111/j.1365-2486.2009.02125.x
Global Change Biology 16(4): 1258-1267 (2010)
1354-1013
http://hdl.handle.net/10261/47957
doi:10.1111/j.1365-2486.2009.02125.x
1365-2486
op_rights open
op_doi https://doi.org/10.1111/j.1365-2486.2009.02125.x
container_title Global Change Biology
container_volume 16
container_issue 4
container_start_page 1258
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