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Dentine oxygen isotopes (δ (18)O) as a proxy for odontocete distributions and movements

Spatial variation in marine oxygen isotope ratios (δ (18)O) resulting from differential evaporation rates and precipitation inputs is potentially useful for characterizing marine mammal distributions and tracking movements across δ (18)O gradients. Dentine hydroxyapatite contains carbonate and phosp...

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Detalles Bibliográficos
Autores principales:	Matthews, Cory J. D., Longstaffe, Fred J., Ferguson, Steven H.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	John Wiley and Sons Inc. 2016
Materias:	Original Research
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4979696/ https://www.ncbi.nlm.nih.gov/pubmed/27547302 http://dx.doi.org/10.1002/ece3.2238

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