Morphological trends in reticulate Nummulites across the Eocene–Oligocene transition
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DOI: 10.1111/pala.70003
Abstract: At the Eocene–Oligocene transition (EOT), c. 34.44–33.65 Ma, the Earth's climate shifted from ‘greenhouse’ to ‘icehouse’ conditions. This change coincides with the first continental ice growth on Antarctica, global cooling, and widespread overturning of faunal and… read more here.
Keywords: reticulate nummulites; oligocene transition; morphological trends; eocene oligocene ... See more keywords