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Distribution and abundance of Phyllosoma Larvae (Decapoda, Palinuridae) in the southern Gulf of Mexico and the western Caribbean sea

Por: Manzanilla Domínguez, Heyden Marcos. Maestro [autor].
Gasca, Rebeca [autora].
Tipo de material: Artículo
 impreso(a) 
 
  y electrónico  
  Artículo impreso(a) y electrónico Tipo de contenido: Texto Tipo de medio: Computadora Tipo de portador: Recurso en líneaTema(s): Langostas (Crustáceos) | Langosta espinosa | Scyrillarides aequinoctialis | Scyllarus americanus | Panulirus laevicadua | Justitia longimanus | Larva filosomaDescriptor(es) geográficos: Golfo de México | Banco de Campeche (Campeche, México) | Reserva de la Biosfera Banco Chinchorro (Quintana Roo, México) | Bahía del Espíritu Santo, Felipe Carrillo Puerto (Quintana Roo, México) | Bahía de la Ascensión, Felipe Carrillo Puerto (Quintana Roo, México) Clasificación: AR/595.38409726 / M3 Nota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso En: Crustaceana. Volumen 77, número 1 (2004), páginas 75-93. --ISSN: 0011-216XNúmero de sistema: 46311Resumen:
Inglés

From plankton samples collected during two oceanographic expeditions in the southern Gulf of Mexico (1991) and five in the Mexican Caribbean Sea, we studied the composition, abundance, and distribution of the phyllosoma larvae. A total of 118 phyllosomas belonging to five species of lobster were recorded. Panulirus argus was the most abundant and dominant, it represented 73.9% of the total number of phyllosomas collected, followed by Scyllarides aequinoctialis (18.0%). The phyllosomas were distributed mainly in the coastal areas, with decreasing densities oceanwards. Highest larval concentrations were recorded near the outer border of the Campeche Bank shelf in the southern Gulf of Mexico. In the Mexican Caribbean area, phyllosomas were most abundant around Banco Chinchorro, off Espiritu Santo Bay and Ascension Bay, and near Isla Mujeres; these are well-known spawning areas for the spiny lobster, P. argus and are indicated by the presence of the earliest larval stages. The oldest larvae were concentrated on the Campeche Bank; this was attributed to the effect of a local gyre that retains these larvae. The youngest phyllosomas tended to have an oceanic distribution thus allowing them to enter the oceanic system of mesoscale gyres of the Gulf. In the Mexican Caribbean the coastal shoreward currents seem to act as a retention system for lobster larvae. The distribution of the phyllosoma stages in the Caribbean area suggests a continuous presence of different stages year-round. Some of these larvae, in the northeastern sector, would likely be transported to the Campeche Bank.

Recurso en línea: https://www.jstor.org/stable/20105685
Lista(s) en las que aparece este ítem: Producción Rebeca Gasca
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ECOSUR AR 595.38409726 M3 001 Disponible ECO010017324

Disponible para usuarios de ECOSUR con su clave de acceso

From plankton samples collected during two oceanographic expeditions in the southern Gulf of Mexico (1991) and five in the Mexican Caribbean Sea, we studied the composition, abundance, and distribution of the phyllosoma larvae. A total of 118 phyllosomas belonging to five species of lobster were recorded. Panulirus argus was the most abundant and dominant, it represented 73.9% of the total number of phyllosomas collected, followed by Scyllarides aequinoctialis (18.0%). The phyllosomas were distributed mainly in the coastal areas, with decreasing densities oceanwards. Highest larval concentrations were recorded near the outer border of the Campeche Bank shelf in the southern Gulf of Mexico. In the Mexican Caribbean area, phyllosomas were most abundant around Banco Chinchorro, off Espiritu Santo Bay and Ascension Bay, and near Isla Mujeres; these are well-known spawning areas for the spiny lobster, P. argus and are indicated by the presence of the earliest larval stages. The oldest larvae were concentrated on the Campeche Bank; this was attributed to the effect of a local gyre that retains these larvae. The youngest phyllosomas tended to have an oceanic distribution thus allowing them to enter the oceanic system of mesoscale gyres of the Gulf. In the Mexican Caribbean the coastal shoreward currents seem to act as a retention system for lobster larvae. The distribution of the phyllosoma stages in the Caribbean area suggests a continuous presence of different stages year-round. Some of these larvae, in the northeastern sector, would likely be transported to the Campeche Bank. eng

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