Cite
Late Pleistocene environmental change interpreted from δ 13C and δ 18O of tooth enamel from the Black Creek Swamp Megafauna site, Kangaroo Island, South Australia
MLA
Forbes, M. S., et al. “Late Pleistocene Environmental Change Interpreted from δ 13C and δ 18O of Tooth Enamel from the Black Creek Swamp Megafauna Site, Kangaroo Island, South Australia.” Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 291, no. 3/4, May 2010, pp. 319–27. EBSCOhost, https://doi.org/10.1016/j.palaeo.2010.03.003.
APA
Forbes, M. S., Kohn, M. J., Bestland, E. A., & Wells, R. T. (2010). Late Pleistocene environmental change interpreted from δ 13C and δ 18O of tooth enamel from the Black Creek Swamp Megafauna site, Kangaroo Island, South Australia. Palaeogeography, Palaeoclimatology, Palaeoecology, 291(3/4), 319–327. https://doi.org/10.1016/j.palaeo.2010.03.003
Chicago
Forbes, M.S., M.J. Kohn, E.A. Bestland, and R.T. Wells. 2010. “Late Pleistocene Environmental Change Interpreted from δ 13C and δ 18O of Tooth Enamel from the Black Creek Swamp Megafauna Site, Kangaroo Island, South Australia.” Palaeogeography, Palaeoclimatology, Palaeoecology 291 (3/4): 319–27. doi:10.1016/j.palaeo.2010.03.003.