Statistics for Coiling direction of the planktic foraminifer Globorotalia truncatulinoides as a proxy for reconstructing upper ocean hydrography in the North Atlantic during the mid-Pleistocene climate transition
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Coiling direction of the planktic foraminifer Globorotalia truncatulinoides as a proxy for reconstructing upper ocean hydrography in the North Atlantic during the mid-Pleistocene climate transition | 2 |
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Caldwell_udel_0060M_13321.pdf | 7 |