Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …

In environmental magnetism, rock and mineral magnetic techniques are used to investigate
the formation, transportation, deposition, and postdepositional alterations of magnetic …

Abstract The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …

Since the recognition in the mid-19th century that glaciers had been considerably more
extensive than at present, the Quaternary (Pleistocene and Holocene series) has been …

About 34 million years ago, Earth's climate shifted from a relatively ice-free world to one with
glacial conditions on Antarctica characterized by substantial ice sheets. How Earth's …

Arctic sea-ice extent and volume are declining rapidly. Several studies project that the Arctic
Ocean may become seasonally ice-free by the year 2040 or even earlier. Putting this into …

The long-standing view of Earth's Cenozoic glacial history calls for the first continental-scale
glaciation of Antarctica in the earliest Oligocene epoch (∼ 33.6 million years ago), followed …

The origin of third-order eustatic sequences is reviewed by comparing recent sequence
stratigraphic data to the latest, best-constrained astronomical model. Middle Eocene to …

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 (EO) climate transition (ca. 34 Ma) marks a period of
Antarctic ice growth and a major step from early Cenozoic greenhouse conditions toward …