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dc.contributor.advisorBoyd, Ian
dc.contributor.advisorTodd, Christopher David
dc.contributor.authorHanson, Nora Nell
dc.coverage.spatial172en_US
dc.date.accessioned2012-10-24T14:48:13Z
dc.date.available2012-10-24T14:48:13Z
dc.date.issued2012-11-30
dc.identifieruk.bl.ethos.558145
dc.identifier.urihttps://hdl.handle.net/10023/3221
dc.description.abstractMonitoring the response of upper trophic level animals to ecological change is important to understanding the state and stability of ecosystems. Marine predators integrate information over large geographical scales and are relatively long-lived; furthermore, many of these organisms are restricted to terrestrial or freshwater habitats at certain times during their life history and are accessible to researchers. This thesis investigated the response of marine predators to ecological change at a variety of spatial and temporal scales using stable isotope ratio methods with the aims of developing meaningful proxies, or indices, of variability in marine ecosystems. The first study explored the intrinsic (i.e. ontogenetic) and extrinsic (i.e. environmental) factors important to modulating variation in the stable isotope ratios of C and N in tooth dentin of male Antarctic fur seals (Arctocephalus gazella) in the Southern Ocean. In the second study, long-term records of variation in δ¹⁵N and δ¹³C values of Atlantic salmon (Salmo salar) scales and grey seal (Halichoerus grypus) tooth dentin provided evidence for large-scale climate forcing across the eastern North Atlantic. In the following study, a more detailed examination of intra- and inter-individual stable isotope variation in Atlantic salmon within a single year was undertaken in an attempt to better understand recent declines in somatic condition of these fish. The last two studies were concerned with the development of high resolution sampling of fish otoliths using secondary mass spectrometry (SIMS) and the application of this technique to reconstructing the thermal and metabolic histories of individual Atlantic salmon from intra-otolith δ¹³C and δ¹⁸O values. Stable isotope proxies can be used to document shifts in trophic dynamics and animal movement that may be associated with ecological change. Using multiple tissues, elements and species, such studies provide unique monitoring tools at a range of spatial and temporal scales.en_US
dc.language.isoenen_US
dc.publisherUniversity of St Andrews
dc.subject.lccQH541.5S3H2en_US
dc.subject.lcshMarine ecologyen_US
dc.subject.lcshStable isotopes in ecological researchen_US
dc.subject.lcshPredatory marine animals--Ecologyen_US
dc.subject.lcshTop predators--Ecologyen_US
dc.titleExamining the response of top marine predators to ecological change using stable isotope proxiesen_US
dc.typeThesisen_US
dc.type.qualificationlevelDoctoralen_US
dc.type.qualificationnamePhD Doctor of Philosophyen_US
dc.publisher.institutionThe University of St Andrewsen_US


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