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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Detaylı Bibliyografya
Yayımlandı:Ecol Evol
Asıl Yazarlar: Matthews, Cory J. D., Longstaffe, Fred J., Ferguson, Steven H.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: John Wiley and Sons Inc. 2016
Konular:
Original Research
Online Erişim:https://ncbi.nlm.nih.gov/pmc/articles/PMC4979696/
https://ncbi.nlm.nih.gov/pubmed/27547302
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/ece3.2238
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