Data from: Endothermic mosasaurs? Possible thermoregulation of Late Cretaceous mosasaurs (Reptilia, Squamata) indicated by stable oxygen isotopes in fossil bioapatite in comparison with coeval marine fish and pelagic seabirds

Harrell Jr TL, Pérez-Huerta A, Suarez CA

Date Published: April 11, 2016

DOI: http://dx.doi.org/10.5061/dryad.5vv55

 

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Title Harrell et al Supplemental Oxygen Isotope Data
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Description Supplemental Table 1 – Oxygen isotope (δ18O) results for all fossil samples reported in this study. Mooreville Chalk specimens are plotted in Figure 2. Results are relative to Vienna Standard Mean Ocean Water (V-SMOW).
Download Harrell et al Supplemental Data.xlsx (13.59 Kb)
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When using this data, please cite the original publication:

Harrell Jr TL, Pérez-Huerta A, Suarez CA (2016) Endothermic mosasaurs? Possible thermoregulation of Late Cretaceous mosasaurs (Reptilia, Squamata) indicated by stable oxygen isotopes in fossil bioapatite in comparison with coeval marine fish and pelagic seabirds. Palaeontology 59(3): 351–363. http://dx.doi.org/10.1111/pala.12240

Additionally, please cite the Dryad data package:

Harrell Jr TL, Pérez-Huerta A, Suarez CA (2016) Data from: Endothermic mosasaurs? Possible thermoregulation of Late Cretaceous mosasaurs (Reptilia, Squamata) indicated by stable oxygen isotopes in fossil bioapatite in comparison with coeval marine fish and pelagic seabirds. Dryad Digital Repository. http://dx.doi.org/10.5061/dryad.5vv55
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