Oligocene Epoch

E252484

The Oligocene Epoch was a geologic time interval roughly 34 to 23 million years ago marked by global cooling, the expansion of grasslands, and significant evolution and diversification of mammals.

All labels observed (3)

Label Occurrences
Oligocene 7
Oligocene Epoch canonical 1
Oligocene Series 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf chronostratigraphic unit
geologic epoch
baseDefinedBy extinction of planktonic foraminifer Hantkenina
characterizedBy continued breakup of Gondwana-derived landmasses
development of modern-type ecosystems
diversification of mammals
expansion of grasslands
global cooling
climate generally cooler and drier than Eocene
climateEvent Antarctic glaciation expansion
strengthening of latitudinal temperature gradients
climateTrend cooling relative to Eocene
duration about 11 million years
end approximately 23.03 million years ago
fauna decline of many archaic mammal groups
diversification of early cetaceans
diversification of early primates
diversification of early rodents
diversification of marine invertebrates
evolution of early ruminants
evolution of more modern-type horses
presence of large browsing mammals
radiation of early carnivorans
flora decline of some tropical forests at mid-latitudes
early spread of grasses
expansion of open woodlands
followedBy Miocene Epoch
linked to: Miocene
follows Eocene Epoch
linked to: Eocene
geochronologicEquivalent Oligocene Series
linked to: Oligocene Epoch
GSSPDefinedBy base at Massignano, Italy
nameCoined 1854
namedBy Heinrich Ernst Beyrich
nameEtymology from Greek words meaning "few" and "recent"
oceanography development of Antarctic Circumpolar Current
paleogeography continued opening of the North Atlantic
development of more modern continental configurations
increasing isolation of Antarctica
partOf Paleogene Period
linked to: Paleogene
positionInCenozoic third epoch of the Cenozoic Era
positionInPaleogene final epoch of the Paleogene Period
seaLevel generally lower than in Eocene
significance important stage in evolution of modern mammal faunas
transition toward modern Cenozoic climates
start approximately 33.9 million years ago
subdivision Early Oligocene
Late Oligocene
tectonics continued uplift of the Alps
continued uplift of the Himalayas
rifting and volcanism in East Africa

How these facts were elicited

Referenced by (9)

Full triples — surface form annotated when it differs from this entity's canonical label.

Alpine orogeny mainPhase Oligocene
linked to: Oligocene Epoch
Western Cascades geologicPeriod Oligocene
linked to: Oligocene Epoch
Badlands National Park geologicalPeriodRepresented Oligocene
linked to: Oligocene Epoch
Procyonidae firstAppearance Oligocene
linked to: Oligocene Epoch
Poebrotherium temporalRange Oligocene
linked to: Oligocene Epoch
Mysticeti timeOfOrigin Oligocene
linked to: Oligocene Epoch
Oligocene Epoch geochronologicEquivalent Oligocene Series
linked to: Oligocene Epoch
Miocene follows Oligocene
linked to: Oligocene Epoch