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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/367
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dc.contributor.authorYoshinaga, Marcos Y.-
dc.contributor.authorSumida, Paulo Y. G.-
dc.contributor.authorSilveira, Ilson C. A.-
dc.contributor.authorCiotti, Aurea M.-
dc.contributor.authorGaeta, Salvador A.-
dc.contributor.authorPacheco, Luiz F. C. M.-
dc.contributor.authorKoettker, Andrea G.-
dc.date.accessioned2014-05-20T13:12:23Z-
dc.date.accessioned2016-10-25T16:32:53Z-
dc.date.available2014-05-20T13:12:23Z-
dc.date.available2016-10-25T16:32:53Z-
dc.date.issued2010-01-01-
dc.identifierhttp://dx.doi.org/10.1016/j.jmarsys.2009.07.007-
dc.identifier.citationJournal of Marine Systems. Amsterdam: Elsevier B.V., v. 79, n. 1-2, p. 124-133, 2010.-
dc.identifier.issn0924-7963-
dc.identifier.urihttp://hdl.handle.net/11449/367-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/367-
dc.description.abstractAbundance and composition of marine benthic communities have been relatively well studied in the SE Brazilian coast, but little is known on patterns controlling the distribution of their planktonic larval stages. A survey of larval abundance in the continental margin, using a Multi-Plankton Sampler, was conducted in a cross-shelf transect off Cabo Frio (23 degrees S and 42 degrees W) during a costal upwelling event. Hydrographic conditions were monitored through discrete CDT casts. Chlorophyll-a in the top 100 m of the water column was determined and changes in surface chlorophyll-a was estimated using SeaWiFS images. Based on the larval abundances and the meso-scale hydrodynamics scenario, our results suggest two different processes affecting larval distributions. High larval densities were found nearshore due to the upwelling event associated with high chlorophyll a and strong along shore current. on the continental slope, high larval abundance was associated with a clockwise rotating meander, which may have entrapped larvae from a region located further north (Cabo de Sao Tome, 22 degrees S and 41 degrees W). In mid-shelf areas, our data suggests that vertical migration may likely occur as a response to avoid offshore transport by upwelling plumes and/or cyclonic meanders. The hydrodynamic scenario observed in the study area has two distinct yet extremely important consequences: larval retention on food-rich upwelling areas and the broadening of the tropical domain to southernmost subtropical areas. (C) 2009 Elsevier B.V. All rights reserved.en
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)-
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)-
dc.format.extent124-133-
dc.language.isoeng-
dc.publisherElsevier B.V.-
dc.sourceWeb of Science-
dc.subjectSE Brazilian coast (23 degrees S and 42 degrees W)en
dc.subjectShelf dynamicsen
dc.subjectCoastal upwellingen
dc.subjectZooplanktonen
dc.subjectInvertebrate larvaeen
dc.titleVertical distribution of benthic invertebrate larvae during an upwelling event along a transect off the tropical Brazilian continental marginen
dc.typeoutro-
dc.contributor.institutionUniversidade de São Paulo (USP)-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.description.affiliationUniv São Paulo, Inst Oceanog, BR-05508120 São Paulo, Brazil-
dc.description.affiliationUNESP, BR-11330900 Sao Vicente, SP, Brazil-
dc.description.affiliationUnespUNESP, BR-11330900 Sao Vicente, SP, Brazil-
dc.description.sponsorshipIdFAPESP: 01/00165-2-
dc.description.sponsorshipIdFAPESP: 04/06369-7-
dc.identifier.doi10.1016/j.jmarsys.2009.07.007-
dc.identifier.wosWOS:000272761400010-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofJournal of Marine Systems-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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