Deep circulation in the Late Cretaceous: Oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores

MLA

Saltzman, Es, and Ej Barron. Deep Circulation in the Late Cretaceous: Oxygen Isotope Paleotemperatures from Inoceramus Remains in D.S.D.P. Cores. Nov. 1982. EBSCOhost, https://doi.org/10.1016/0031-0182(82)90088-8.

APA

Saltzman, E., & Barron, E. (1982). Deep circulation in the Late Cretaceous: Oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores. https://doi.org/10.1016/0031-0182(82)90088-8.

Chicago

Saltzman, Es, and Ej Barron. 1982. “Deep Circulation in the Late Cretaceous: Oxygen Isotope Paleotemperatures from Inoceramus Remains in D.S.D.P. Cores,” November. doi:10.1016/0031-0182(82)90088-8.