Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of California

ABSTRACT Larval fish composition and abundance were analyzed during February-March (winter) and November-December (autumn) of 2005 to investigate which environmental conditions and mesoscale oceanographic processes affect the distribution of larval fish assemblages in the Gulf of California, and if...

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Autores principales: Urias-Leyva,Homero, Aceves-Medina,Gerardo, Avendaño-Ibarra,Raymundo, Saldierna-Martínez,Ricardo J., Gómez-Gutiérrez,Jaime, Robinson,Carlos J.
Lenguaje:English
Publicado: Pontificia Universidad Católica de Valparaíso. Facultad de Recursos Naturales. Escuela de Ciencias del Mar 2018
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Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-560X2018000100020
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spelling oai:scielo:S0718-560X20180001000202018-04-17Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of CaliforniaUrias-Leyva,HomeroAceves-Medina,GerardoAvendaño-Ibarra,RaymundoSaldierna-Martínez,Ricardo J.Gómez-Gutiérrez,JaimeRobinson,Carlos J. fish larvae assemblage upwelling eddies Gulf of California ABSTRACT Larval fish composition and abundance were analyzed during February-March (winter) and November-December (autumn) of 2005 to investigate which environmental conditions and mesoscale oceanographic processes affect the distribution of larval fish assemblages in the Gulf of California, and if these variables and processes are useful to delimit specific regions of ichthyofaunal distribution. The overall pattern was mostly a latitudinal gradient of the abundance of two faunistic complexes of larval fish assemblages (temperate northern and tropical southern complexes) strongly associated with the spatial distribution of sea surface temperature. The integration of these results, with previous investigations in the region, lets us confirm that the northern and southern larval fish assemblages extend and contract their distribution ranges according to the latitudinal displacement of the 21°C sea surface isotherm. We identified this to be a valuable criterion to establish the southern distribution limit of the temperate larval fish assemblage, and the 18°C as the northern limit of the tropical larval fish assemblage. However, this general pattern is maintained only in absence of mesoscale oceanographic features (upwelling and eddies) that increase larval drift from the coast to the central region of the Gulf, particularly during the November-December period when longitudinal gradients were stronger than in February-March.info:eu-repo/semantics/openAccessPontificia Universidad Católica de Valparaíso. Facultad de Recursos Naturales. Escuela de Ciencias del MarLatin american journal of aquatic research v.46 n.1 20182018-03-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-560X2018000100020en10.3856/vol46-issue1-fulltext-4
institution Scielo Chile
collection Scielo Chile
language English
topic fish larvae
assemblage
upwelling
eddies
Gulf of California
spellingShingle fish larvae
assemblage
upwelling
eddies
Gulf of California
Urias-Leyva,Homero
Aceves-Medina,Gerardo
Avendaño-Ibarra,Raymundo
Saldierna-Martínez,Ricardo J.
Gómez-Gutiérrez,Jaime
Robinson,Carlos J.
Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of California
description ABSTRACT Larval fish composition and abundance were analyzed during February-March (winter) and November-December (autumn) of 2005 to investigate which environmental conditions and mesoscale oceanographic processes affect the distribution of larval fish assemblages in the Gulf of California, and if these variables and processes are useful to delimit specific regions of ichthyofaunal distribution. The overall pattern was mostly a latitudinal gradient of the abundance of two faunistic complexes of larval fish assemblages (temperate northern and tropical southern complexes) strongly associated with the spatial distribution of sea surface temperature. The integration of these results, with previous investigations in the region, lets us confirm that the northern and southern larval fish assemblages extend and contract their distribution ranges according to the latitudinal displacement of the 21°C sea surface isotherm. We identified this to be a valuable criterion to establish the southern distribution limit of the temperate larval fish assemblage, and the 18°C as the northern limit of the tropical larval fish assemblage. However, this general pattern is maintained only in absence of mesoscale oceanographic features (upwelling and eddies) that increase larval drift from the coast to the central region of the Gulf, particularly during the November-December period when longitudinal gradients were stronger than in February-March.
author Urias-Leyva,Homero
Aceves-Medina,Gerardo
Avendaño-Ibarra,Raymundo
Saldierna-Martínez,Ricardo J.
Gómez-Gutiérrez,Jaime
Robinson,Carlos J.
author_facet Urias-Leyva,Homero
Aceves-Medina,Gerardo
Avendaño-Ibarra,Raymundo
Saldierna-Martínez,Ricardo J.
Gómez-Gutiérrez,Jaime
Robinson,Carlos J.
author_sort Urias-Leyva,Homero
title Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of California
title_short Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of California
title_full Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of California
title_fullStr Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of California
title_full_unstemmed Regionalization in the distribution of larval fish assemblages during winter and autumn in the Gulf of California
title_sort regionalization in the distribution of larval fish assemblages during winter and autumn in the gulf of california
publisher Pontificia Universidad Católica de Valparaíso. Facultad de Recursos Naturales. Escuela de Ciencias del Mar
publishDate 2018
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-560X2018000100020
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