Publicación:
Changes in rocky intertidal communities after the 2015 and 2017 El Niño events along the Peruvian coast

dc.contributor.author Valqui J. es_PE
dc.contributor.author Ibañez-Erquiaga B. es_PE
dc.contributor.author Pacheco A.S. es_PE
dc.contributor.author Wilbur L. es_PE
dc.contributor.author Ochoa D. es_PE
dc.contributor.author Cardich J. es_PE
dc.contributor.author Pérez-Huaranga M. es_PE
dc.contributor.author Salas-Gismondi R. es_PE
dc.contributor.author Pérez A. es_PE
dc.contributor.author Indacochea A. es_PE
dc.contributor.author Avila-Peltroche J. es_PE
dc.contributor.author Ch M.R. es_PE
dc.contributor.author Carré M. es_PE
dc.date.accessioned 2024-05-30T23:13:38Z
dc.date.available 2024-05-30T23:13:38Z
dc.date.issued 2021
dc.description.abstract The Peruvian coast experiences the largest interannual variability of sea surface temperature in the world due to the combined influence of the coastal upwelling and El Niño Southern Oscillation (ENSO). Although biological impacts of El Niño events have been widely reported, their effects on rocky intertidal communities remains largely unknown in Peru. Herein, we analyze the results of two biological surveys of rocky intertidal communities, conducted along 1400 km of the Peruvian coast. The first survey was conducted in 2015 yielding a snapshot of the distribution of rocky intertidal communities after 17 years of stable La Niña-like conditions. The second survey was carried in October 2017, after the 2015-16 and the 2017 El Niño events, which produced warm sea surface temperature (SST) anomalies up to 6 °C on the Peruvian coast. We find no changes throughout the latitudinal transect in taxonomic richness but an important turnover of species, especially marked in the transition zone (~4–8°S) between the Panamic and the Humboldt provinces. Temperature-related southward migration of species was evidenced in a few sites but did not explain the large-scale change in communities observed from 2015 to 2017, primarily driven by large changes in the distribution of a few ecologically important species across the Panamic and Humboldt provinces. A primary environmental impact on some ecologically key species likely triggered a chain of secondary impacts through ecological relationships which lead to a complex change independent from SST gradients. Further studies are needed to better characterize and disentangle the seasonal and interannual variability of the rocky intertidal communities and their drivers. When this interannual variability is integrated, the nine study sites show a highly persistent community structure determined by the latitudinal SST gradient along the Peruvian coast. © 2020 Elsevier Ltd
dc.description.sponsorship Consejo Nacional de Ciencia, Tecnología e Innovación Tecnológica - Concytec
dc.identifier.doi https://doi.org/10.1016/j.ecss.2020.107142
dc.identifier.scopus 2-s2.0-85098596325
dc.identifier.uri https://hdl.handle.net/20.500.12390/2372
dc.language.iso eng
dc.publisher Academic Press
dc.relation.ispartof Estuarine, Coastal and Shelf Science
dc.rights info:eu-repo/semantics/openAccess
dc.subject Thermal anomaly
dc.subject Biogeography es_PE
dc.subject Community structure es_PE
dc.subject Humboldt current ecosystem es_PE
dc.subject Latitudinal pattern es_PE
dc.subject Macrobenthos es_PE
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#5.08.04
dc.title Changes in rocky intertidal communities after the 2015 and 2017 El Niño events along the Peruvian coast
dc.type info:eu-repo/semantics/article
dspace.entity.type Publication
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