Major climatic transitions and aberrations accompanied by global carbon cycle perturbations
are known to have occurred during the Eocene epoch, between 56-34 Ma. The warmest …

Major climate transitions and perturbations in global carbon cycle are known to have
occurred during the Eocene, between 56 and 34 million years ago (Ma). A series of carbon …

The Middle Eocene Climatic Optimum (MECO) is an enigmatic warming event that
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …

Abstract The Eocene‐Oligocene transition (EOT),~ 34 Ma, marks a tipping point in the long‐
term Cenozoic greenhouse to icehouse climate transition. Paleorecords reveal stepwise …

Abstract The Miocene Climatic Optimum (MCO;~ 16.9 to 14.7 Ma) provides an outstanding
opportunity to investigate climate‐carbon cycle dynamics during a geologically recent …

Abstract The Paleocene‐Eocene Thermal Maximum was a transient, carbon‐induced global
warming event, considered the closest analog to ongoing climate change. Impacts of a …

Abstract The Middle Eocene Climatic Optimum (MECO;~ 40.1 Ma) is a transient global
warming event that abruptly reversed the long-term Eocene cooling trend. The primary …

Sedimentary records show that calcium carbonate (CaCO3) preservation fluctuated during
the Eocene. These fluctuations are well documented for the equatorial Pacific. However …

The late Paleocene to early Eocene warming trend was punctuated by a series of orbitally
paced transient warming events, associated with the release of isotopically light carbon into …

The carbonate saturation profile of the oceans shoaled markedly during a transient global
warming event known as the Paleocene‐Eocene thermal maximum (PETM)(circa 55 Ma) …