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dc.contributor.authorRamp, Christian
dc.contributor.authorDelarue, Julian
dc.contributor.authorPalsbøll, Per J
dc.contributor.authorSears, Richard
dc.contributor.authorHammond, Philip Steven
dc.date.accessioned2015-03-23T15:01:01Z
dc.date.available2015-03-23T15:01:01Z
dc.date.issued2015-03-18
dc.identifier.citationRamp , C , Delarue , J , Palsbøll , P J , Sears , R & Hammond , P S 2015 , ' Adapting to a warmer ocean – seasonal shift of baleen whale movements over three decades ' , PLoS One , vol. 10 , no. 3 , e0121374 . https://doi.org/10.1371/journal.pone.0121374en
dc.identifier.issn1932-6203
dc.identifier.otherPURE: 169909041
dc.identifier.otherPURE UUID: ec386ddc-1141-4c44-8d87-2d07ed5111fe
dc.identifier.otherScopus: 84925428046
dc.identifier.otherORCID: /0000-0002-2381-8302/work/47531650
dc.identifier.otherWOS: 000352138500210
dc.identifier.urihttps://hdl.handle.net/10023/6290
dc.descriptionDate of Acceptance: 11/02/2015en
dc.description.abstractGlobal warming poses particular challenges to migratory species, which face changes to the multiple environments occupied during migration. For many species, the timing of migration between summer and winter grounds and also within-season movements are crucial to maximise exploitation of temporarily abundant prey resources in feeding areas, themselves adapting to the warming planet. We investigated the temporal variation in the occurrence of fin (Balaenoptera physalus) and humpback whales (Megaptera novaeangliae) in a North Atlantic summer feeding ground, the Gulf of St. Lawrence (Canada), from 1984 to 2010 using a long-term study of individually identifiable animals. These two sympatric species both shifted their date of arrival at a previously undocumented rate of more than 1day per year earlier over the study period thus maintaining the approximate 2-week difference in arrival of the two species and enabling the maintenance of temporal niche separation. However, the departure date of both species also shifted earlier but at different rates resulting in increasing temporal overlap over the study period indicating that this separation may be starting to erode. Our analysis revealed that the trend in arrival was strongly related to earlier ice break-up and rising sea surface temperature, likely triggering earlier primary production. The observed changes in phenology in response to ocean warming are a remarkable example of phenotypic plasticity and may partly explain how baleen whales were able to survive a number of changes in climate over the last several million years. However, it is questionable whether the observed rate of change in timing can be maintained. Substantial modification to the distribution or annual life cycle of these species might be required to keep up with the ongoing warming of the oceans.
dc.format.extent15
dc.language.isoeng
dc.relation.ispartofPLoS Oneen
dc.rightsCopyright: © 2015 Ramp et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are crediteden
dc.subjectQH301 Biologyen
dc.subjectDASen
dc.subjectSDG 13 - Climate Actionen
dc.subject.lccQH301en
dc.titleAdapting to a warmer ocean – seasonal shift of baleen whale movements over three decadesen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. School of Biologyen
dc.contributor.institutionUniversity of St Andrews. Sea Mammal Research Uniten
dc.contributor.institutionUniversity of St Andrews. Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews. Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews. Centre for Research into Ecological & Environmental Modellingen
dc.identifier.doihttps://doi.org/10.1371/journal.pone.0121374
dc.description.statusPeer revieweden


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