Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska.

MLA

Gaglioti, Benjamin V., et al. “Younger-Dryas Cooling and Sea-Ice Feedbacks Were Prominent Features of the Pleistocene-Holocene Transition in Arctic Alaska.” Quaternary Science Reviews, vol. 169, Aug. 2017, pp. 330–43. EBSCOhost, https://doi.org/10.1016/j.quascirev.2017.05.012.

APA

Gaglioti, B. V., Mann, D. H., Wooller, M. J., Jones, B. M., Wiles, G. C., Groves, P., Kunz, M. L., Baughman, C. A., & Reanier, R. E. (2017). Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska. Quaternary Science Reviews, 169, 330–343. https://doi.org/10.1016/j.quascirev.2017.05.012

Chicago

Gaglioti, Benjamin V., Daniel H. Mann, Matthew J. Wooller, Benjamin M. Jones, Gregory C. Wiles, Pamela Groves, Michael L. Kunz, Carson A. Baughman, and Richard E. Reanier. 2017. “Younger-Dryas Cooling and Sea-Ice Feedbacks Were Prominent Features of the Pleistocene-Holocene Transition in Arctic Alaska.” Quaternary Science Reviews 169 (August): 330–43. doi:10.1016/j.quascirev.2017.05.012.