Drivers of the Late Ordovician Mass Extinction: redox, volcanism, atmospheric oxygen/carbon dioxide and/or glaciation.

MLA

Morrison, Audrey, et al. “Drivers of the Late Ordovician Mass Extinction: Redox, Volcanism, Atmospheric Oxygen/Carbon Dioxide and/or Glaciation.” Estonian Journal of Earth Sciences, vol. 72, no. 1, Jan. 2023, p. 150. EBSCOhost, https://doi.org/10.3176/earth.2023.27.

APA

Morrison, A., Lefebvre, A., Patter, A. V., Davis, A., Oelschlagel, M., Blamey, N., Jin, J., Riechelmann, S., & Brand, U. (2023). Drivers of the Late Ordovician Mass Extinction: redox, volcanism, atmospheric oxygen/carbon dioxide and/or glaciation. Estonian Journal of Earth Sciences, 72(1), 150. https://doi.org/10.3176/earth.2023.27

Chicago

Morrison, Audrey, Amy Lefebvre, Ariel Van Patter, Alyssa Davis, Matthew Oelschlagel, Nigel Blamey, Jisuo Jin, Sylvia Riechelmann, and Uwe Brand. 2023. “Drivers of the Late Ordovician Mass Extinction: Redox, Volcanism, Atmospheric Oxygen/Carbon Dioxide and/or Glaciation.” Estonian Journal of Earth Sciences 72 (1): 150. doi:10.3176/earth.2023.27.