Dentine oxygen isotopes (δ 18O) as a proxy for odontocete distributions and movements
Spatial variation in marine oxygen isotope ratios (δ 18O) resulting from differential evaporation rates and precipitation inputs is potentially useful for characterizing marine mammal distributions and tracking movements across δ 18O gradients. Dentine hydroxyapatite contains carbonate and phosphate...
| Main Authors: | , , |
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| Format: | Online |
| Language: | English |
| Published: |
John Wiley and Sons Inc.
2016
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| Online Access: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4979696/ |