Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/55216
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dc.contributor.authorCheal, A.en
dc.contributor.authorDelean, J.en
dc.contributor.authorSweatman, H.en
dc.contributor.authorThompson, A.en
dc.date.issued2007en
dc.identifier.citationEcology, 2007; 88(1):158-169en
dc.identifier.issn0012-9658en
dc.identifier.issn1939-9170en
dc.identifier.urihttp://hdl.handle.net/2440/55216-
dc.description.abstractWe investigated spatial patterns of synchrony among coral reef fish populations and environmental variables over an eight-year period on the Great Barrier Reef, Australia. Our aims were to determine the spatial scale of intra- and interspecific synchrony of fluctuations in abundance of nine damselfish species (genus Pomacentrus) and assess whether environmental factors could have influenced population synchrony. All species showed intraspecific synchrony among populations on reefs separated by ≤100 km, and interspecific synchrony was also common at this scale. At greater spatial scales, only four species showed intraspecific synchrony, over distances ranging from 100–300 km to 500–800 km, and no cases of interspecific synchrony were recorded. The two mechanisms most likely to cause population synchrony are dispersal and environmental forcing through regionally correlated climate (the Moran effect). Dispersal may have influenced population synchrony over distances up to 100 km as this is the expected spatial range for ecologically significant reef fish dispersal. Environmental factors are also likely to have synchronized population fluctuations via the Moran effect for three reasons: (1) dispersal could not have caused interspecific synchrony that was common over distances ≤ 100 km because dispersal cannot link populations of different species, (2) variations in both sea surface temperature and wind speed were synchronized over greater spatial scales (>800 km) than fluctuations in damselfish abundance (800 km) and were correlated with an index of global climate variability, the El Nin˜ o-Southern Oscillation (ENSO), and (3) synchronous population fluctuations of most damselfish species were correlated with ENSO; large population increases often followed ENSO events. We recorded regional variations in the strength of population synchrony that we suspect are due to spatial differences in geophysical, oceanographic, and population characteristics, which act to dilute or enhance the effects of synchronizing mechanisms. We conclude that synchrony is common among Pomacentrus populations separated by tens of kilometers but less prevalent at greater spatial scales, and that environmental variation linked to global climate is likely to be a driving force behind damselfish population synchrony at all spatial scales on the Great Barrier Reef.en
dc.description.statementofresponsibilityA. J. Cheal, S. Delean, H. Sweatman and A. A. Thompsonen
dc.description.urihttp://www.ncbi.nlm.nih.gov/pubmed/17489464?itool=EntrezSystem2.PEntrez.Pubmed.Pubmed_ResultsPanel.Pubmed_RVDocSum&ordinalpos=2en
dc.language.isoenen
dc.publisherEcological Soc Ameren
dc.subjectclimate; coral reef; dispersal; El Nino; ENSO; fish; Moran effect; population; spatial synchrony.en
dc.titleSpatial synchrony in coral reef fish populations and the influence of climateen
dc.typeJournal articleen
dc.identifier.rmid0020092674en
dc.identifier.doi10.1890/0012-9658(2007)88[158:SSICRF]2.0.CO;2en
dc.identifier.pubid37527-
pubs.library.collectionEarth and Environmental Sciences publicationsen
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
Appears in Collections:Earth and Environmental Sciences publications
Environment Institute publications

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