Cite
Neodymium isotope ratios and a positive δ13C excursion: interpreting the connection between oceanographic and climate changes during the early Late Ordovician of Laurentia.
MLA
Wright, Zachary A., et al. “Neodymium Isotope Ratios and a Positive Δ13C Excursion: Interpreting the Connection between Oceanographic and Climate Changes during the Early Late Ordovician of Laurentia.” Stratigraphy, vol. 14, no. 1, Nov. 2017, pp. 443–56. EBSCOhost, https://doi.org/10.29041/strat.14.1-4.443-456.
APA
Wright, Z. A., Quinton, P. C., Martin, E. E., Leslie, S. A., MacLeod, K. G., & Herrmann, A. D. (2017). Neodymium isotope ratios and a positive δ13C excursion: interpreting the connection between oceanographic and climate changes during the early Late Ordovician of Laurentia. Stratigraphy, 14(1), 443–456. https://doi.org/10.29041/strat.14.1-4.443-456
Chicago
Wright, Zachary A., Page C. Quinton, Ellen E. Martin, Stephen A. Leslie, Kenneth G. MacLeod, and Achim D. Herrmann. 2017. “Neodymium Isotope Ratios and a Positive Δ13C Excursion: Interpreting the Connection between Oceanographic and Climate Changes during the Early Late Ordovician of Laurentia.” Stratigraphy 14 (1): 443–56. doi:10.29041/strat.14.1-4.443-456.