dc.contributorSuárez-Morales, E., El Colegio de la Frontera Sur, Unidad Chetumal, Apdo. Postal 424, Chetumal, Quintana Roo 77000, Mexico; Franco-Gordo, C., Centro de Ecología Costera, Universidad de Guadalajara, Gómez Farías, 82, San Patricio Melaque, Jalisco 48980, Mexico; Saucedo-Lozano, M., Centro de Ecología Costera, Universidad de Guadalajara, Gómez Farías, 82, San Patricio Melaque, Jalisco 48980, Mexico
dc.creatorSuarez-Morales, E.
dc.creatorFranco-Gordo, C.
dc.creatorSaucedo-Lozano, M.
dc.date.accessioned2015-09-15T18:33:16Z
dc.date.accessioned2022-11-02T14:08:24Z
dc.date.available2015-09-15T18:33:16Z
dc.date.available2022-11-02T14:08:24Z
dc.date.created2015-09-15T18:33:16Z
dc.date.issued2000
dc.identifierhttp://hdl.handle.net/20.500.12104/43339
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-0034485772&partnerID=40&md5=b6a7967e075c214e1a94b6e87ffa1e33
dc.identifier10.1163/156854000504778
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4991379
dc.description.abstractZooplankton samples were collected during autumn (September, 1990) off the coasts of the Mexican state of Jalisco, northwestern Mexico, in the eastern tropical Pacific. Taxonomic analysis of the pelagic Copepoda yielded 44 species, Subeucalanus subcrassus, Temora discaudata, Undinula vulgaris, Euchaeta marina, Centropages furcatus, and Candacia catula being the overall dominant forms. Together they represented almost 75% of total copepod numbers. The influence of the North Equatorial Current, related to tropical conditions, is clear in the local community structure. Shannon-Wiener diversity was homogeneously high (over 3.2 bits/ind.) in most samples. Highest densities were recorded in the neritic zone. Overall copepod density values suggest a moderate to high productivity in the surveyed area. Station clustering showed a neritic and an oceanic facies, their limits roughly determined by the outer border of the narrow shelf. However, the coast-ocean gradient is moderate, with abundant neritic-oceanic forms, and oceanic representatives over the continental shelf. These effects may result from across-shelf mixing of neritic and oceanic water due to (1) the effect of inshore-wards wind-driven advective processes, and (2) the narrowness of the continental shelf. It is suggested that these processes favour a degree of homogeneity of the copepod community along this and other parts of the Mexican tropical Pacific.
dc.relationScopus
dc.relationWOS
dc.relationCrustaceana
dc.relation73
dc.relation6
dc.relation751
dc.relation761
dc.titleOn the pelagic copepod community of the central mexican tropical pacific (autumn, 1990)
dc.typeArticle


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