2004
DOI: 10.15381/rpb.v11i2.2459
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Distribución temporal de moluscos y crustáceos tropicales en la Provincia Peruana y su relación con los eventos El Niño

Abstract: RESUMENEn el presente trabajo se analiza la incursión de 25 especies de moluscos y 15 de crustáceos tropicales, registrados entre los años 1972 y 2003, tiempo en el cual ocurrieron cinco eventos El Niño (EN). La presencia de especies tropicales en la Provincia Peruana, se debería al transporte de larvas de especies bentónicas o de juveniles de especies pelágicas, ambas favorecidas por los movimientos de las masas de aguas que caracterizan a los eventos EN. Es posible que algunas especies hayan encontrado «área… Show more

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Cited by 17 publications
(6 citation statements)
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“…The study of latitudinal patterns of rocky shore communities throughout the coast of Peru showed the presence of three biogeographic units: a region with affinity to the Panamic province from 3.5 to 4.5° S; a transitional zone between 5 and 5.5° S; and a region from 6 to 13.5° S matching the Humboldt (Peruvian) province (Fig 8). This biogeographical zonation is consistent with previous classifications based on qualitative single-taxa studies [46, 47, 69, 70]. However, the putative limits of the transitional zone differ.…”
Section: Discussionsupporting
confidence: 91%
“…The study of latitudinal patterns of rocky shore communities throughout the coast of Peru showed the presence of three biogeographic units: a region with affinity to the Panamic province from 3.5 to 4.5° S; a transitional zone between 5 and 5.5° S; and a region from 6 to 13.5° S matching the Humboldt (Peruvian) province (Fig 8). This biogeographical zonation is consistent with previous classifications based on qualitative single-taxa studies [46, 47, 69, 70]. However, the putative limits of the transitional zone differ.…”
Section: Discussionsupporting
confidence: 91%
“…Precisely, it is known that El Niño causes coastal invertebrates’ larval passive displacement. Despite the presence of the northward Humboldt Current, El Niño, by larval advection, is able to temporarily extend southward the distribution range of several mollusk species from the Panamic province, even to the coasts of Chile (Ashton, Riascos, & Pacheco, ; Guzman, Diaz, Ortlieb, & Clarke, ; Paredes, Cardoso, & Tarazona, ; Paredes et al, ; Velez & Zeballos, ). El Niño has the same effect in the vicinity of the California Transition Zone, where it transports larvae in opposite direction to the California Current (Connolly & Roughgarden, ; Glynn, ; Wares et al, ; Zacherl, Gaines, & Lonhart, ).…”
Section: Discussionmentioning
confidence: 99%
“…and El Niño costero events, warming of the eastern Pacific Ocean occurs, which results in a deepening of the thermocline and a rise in sea surface temperatures, causing a marked increase in rainfall and resulting flooding on the South-American continent [11 and references therein]. During such events, temperature anomalies in ocean waters are most significant in the area facing the Sechura Desert [21], leading to the southward migration, along the southeastern Pacific coast, of marine species distributed primarily in the equatorial region [22,23]. The most severe rainfall events lead to significant changes in coastal environments, e.g.…”
Section: Plos Onementioning
confidence: 99%