Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approach
Two phytoplankton succession events (September-October 1993 and March 1994) in the Ría de Vigo were studied in relation to their hydrodynamic context. By means of a circulation box model we calculated horizontal and vertical residual fluxes as well as budgets of phytoplankton associated with them. T...
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Consejo Superior de Investigaciones Científicas
2001-07-01
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doaj-ae83d49b77a24e96948bea596ba8c7562021-05-05T13:49:49ZengConsejo Superior de Investigaciones CientíficasScientia Marina0214-83581886-81342001-07-0165S1657610.3989/scimar.2001.65s165695Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approachBelén Martín Miguez0L. Fariña-Busto1F. G. Figueiras2F. F. Pérez3Universidade de Vigo, Facultad de CienciasUniversidade de Vigo, Facultad de CienciasInstituto de Investigacións Mariñas, C.S.I.C.Instituto de Investigacións Mariñas, C.S.I.C.Two phytoplankton succession events (September-October 1993 and March 1994) in the Ría de Vigo were studied in relation to their hydrodynamic context. By means of a circulation box model we calculated horizontal and vertical residual fluxes as well as budgets of phytoplankton associated with them. This allowed us to assess the importance of the two factors involved in the selection processes: one hydrodynamic (dependent upon physical dispersion) and one biogeochemical (involving all other processes such as growth, mortality and grazing). The first period was characterised by a downwelling event which produced a reversal of the estuarine circulation pattern (horizontal velocity = 4 km d-1 and downward velocities up to 9 m d-1). This provided suitable conditions for the blooming of Gymnodinium catenatum favoured by its capacity to swim, while the diatom community almost disappeared. The second period corresponded to an upwelling Æ relaxation sequence. During upwelling (horizontal velocity = 6 km d-1; upward velocities up to 12 m d-1), Thalassiosira spp. was dominant. It is suggested that the less energetic conditions associated with the relaxation event (horizontal velocity=1 km d-1; upward velocities < 1 m d-1) favoured the selection of Chatoceros spp. due to its lower sinking rate.http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/701estuarine circulationsuccessionbox modelgymnodinium catenatumchaetoceros spp.thalassiosira spp.ría de vigo |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Belén Martín Miguez L. Fariña-Busto F. G. Figueiras F. F. Pérez |
spellingShingle |
Belén Martín Miguez L. Fariña-Busto F. G. Figueiras F. F. Pérez Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approach Scientia Marina estuarine circulation succession box model gymnodinium catenatum chaetoceros spp. thalassiosira spp. ría de vigo |
author_facet |
Belén Martín Miguez L. Fariña-Busto F. G. Figueiras F. F. Pérez |
author_sort |
Belén Martín Miguez |
title |
Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approach |
title_short |
Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approach |
title_full |
Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approach |
title_fullStr |
Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approach |
title_full_unstemmed |
Succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the Ría de Vigo: a box-model approach |
title_sort |
succession of phytoplankton assemblages in relation to estuarine hydrodynamics in the ría de vigo: a box-model approach |
publisher |
Consejo Superior de Investigaciones Científicas |
series |
Scientia Marina |
issn |
0214-8358 1886-8134 |
publishDate |
2001-07-01 |
description |
Two phytoplankton succession events (September-October 1993 and March 1994) in the Ría de Vigo were studied in relation to their hydrodynamic context. By means of a circulation box model we calculated horizontal and vertical residual fluxes as well as budgets of phytoplankton associated with them. This allowed us to assess the importance of the two factors involved in the selection processes: one hydrodynamic (dependent upon physical dispersion) and one biogeochemical (involving all other processes such as growth, mortality and grazing). The first period was characterised by a downwelling event which produced a reversal of the estuarine circulation pattern (horizontal velocity = 4 km d-1 and downward velocities up to 9 m d-1). This provided suitable conditions for the blooming of Gymnodinium catenatum favoured by its capacity to swim, while the diatom community almost disappeared. The second period corresponded to an upwelling Æ relaxation sequence. During upwelling (horizontal velocity = 6 km d-1; upward velocities up to 12 m d-1), Thalassiosira spp. was dominant. It is suggested that the less energetic conditions associated with the relaxation event (horizontal velocity=1 km d-1; upward velocities < 1 m d-1) favoured the selection of Chatoceros spp. due to its lower sinking rate. |
topic |
estuarine circulation succession box model gymnodinium catenatum chaetoceros spp. thalassiosira spp. ría de vigo |
url |
http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/701 |
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1721460748675186688 |