Demise of the Planktic Foraminifer Genus Morozovella during the Early Eocene Climatic Optimum: New Records from ODP Site 1258 (Demerara Rise, Western Equatorial Atlantic) and Site 1263 (Walvis Ridge, South Atlantic)
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D’Onofrio, R.; Luciani, V.; Dickens, G.R.; Wade, B.S.; Kirtland Turner, S. Demise of the Planktic Foraminifer Genus Morozovella during the Early Eocene Climatic Optimum: New Records from ODP Site 1258 (Demerara Rise, Western Equatorial Atlantic) and Site 1263 (Walvis Ridge, South Atlantic). Geosciences 2020, 10, 88. https://doi.org/10.3390/geosciences10030088
D’Onofrio R, Luciani V, Dickens GR, Wade BS, Kirtland Turner S. Demise of the Planktic Foraminifer Genus Morozovella during the Early Eocene Climatic Optimum: New Records from ODP Site 1258 (Demerara Rise, Western Equatorial Atlantic) and Site 1263 (Walvis Ridge, South Atlantic). Geosciences. 2020; 10(3):88. https://doi.org/10.3390/geosciences10030088
Chicago/Turabian StyleD’Onofrio, Roberta, Valeria Luciani, Gerald R. Dickens, Bridget S. Wade, and Sandra Kirtland Turner. 2020. "Demise of the Planktic Foraminifer Genus Morozovella during the Early Eocene Climatic Optimum: New Records from ODP Site 1258 (Demerara Rise, Western Equatorial Atlantic) and Site 1263 (Walvis Ridge, South Atlantic)" Geosciences 10, no. 3: 88. https://doi.org/10.3390/geosciences10030088