Oxygen isotopes data enable researchers to look far back into the geologic past and reconstruct the climate of the past. In ...

Profound environmental and faunal changes are associated with climatic deterioration during the Eocene-Oligocene transition (EOT) roughly 34 million years ago. Primates are among the most ...

Examination of middle Eocene through Oligocene samples from the Gay's Cove, Bath Cliffs, and Codrington College sections (Oceanic Formation, Barbados) demonstrates the presence of two major benthic ...

Oxygen isotopes data enable researchers to look far back into the geologic past and reconstruct the climate of the past. In doing so, they consider several factors such as ocean temperature and ice ...

Thirty-nine macrofossil taxa are recorded from the late Oligocene (Duntroonian to mid Waitakian) Torehina Formation at Waitete Bay, northern Coromandel Peninsula. A rich fauna dominated by infaunal ...

The climate change that occurred about 34 million years ago may hold the reason as to why humans originated in Africa and not in Asia. More specifically, the deterioration of climate marking the ...