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Stable isotope and minor element proxies for Eocene climate of Seymour Island, Antarctica Cite as Lohmann, K. (2001) "Stable isotope and minor element proxies for Eocene climate of Seymour Island, Antarctica" U.S. Antarctic Program (USAP) Data Center. doi: https://doi.org/. AMD - DIF Record(s) EOCENE_CLIMATE_SEYMOUR_IS Abstract Geochemical composition of shells of the bivalve, Cucullaea from the La Meseta Formation, Seymour Island, Antarctica. Creator(s): Lohmann, Kyger Date Created: 2001-06-11 Repository: USAP-DC (current) - AMD-RESCUE (original) License: Creative Commons Attribution-NonCommercial v4.0 Generic [CC BY-NC 4.0] Award(s) NSF 9980538 Version: 1 Related Project(s) Evolution of Sea Surface Temperatures in the Coastal Antarctic Paleoenvironment During the Late Cretaceous and Paleogene References Dutton, A.L., Lohmann, K.C, and Zinsmeister, W., 2002, Stable isotope and elemental proxies of Eocene climate of Seymour Island, Antarctica. Paleoceanography, v.17, no.2. (doi:10.1029/2000PA000593)