Eocene

E792421

The Eocene was a geologic epoch, roughly 56 to 34 million years ago, marked by warm global climates and significant diversification of early mammals and modern plant groups.

All labels observed (7)

Label Occurrences
Eocene canonical 21
Eocene Epoch 4
Eocene Series 2

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf geologic epoch
associatedWith active plate tectonics and mountain building
collision of India with Asia
continued opening of the North Atlantic Ocean
development of many modern plant families
diversification of bats
diversification of early horses
diversification of early whales (archaeocetes)
diversification of rodents
early stages of Himalayan uplift
expansion of angiosperm-dominated forests
formation of the Drake Passage region
high sea levels
initial diversification of many modern mammal orders
radiation of early primates
widespread peat and coal formation in some regions
characterizedBy absence of large continental ice sheets for most of epoch
expansion of modern plant groups
greenhouse climate state
high atmospheric CO2 levels
significant diversification of early mammals
warm global climates
warm high-latitude climates
widespread tropical and subtropical forests
chronostratigraphicUnit Eocene Series
linked to: Eocene
endTime Priabonian age close
approximately 34 million years ago
etymology from Greek eos meaning dawn
followedBy Oligocene
linked to: Oligocene Epoch
follows Paleocene
geochronologicUnit Eocene Epoch
linked to: Eocene
hasStratotypeRegion northwestern Europe
hasSubdivision Bartonian
Lutetian
Priabonian
Ypresian
includesEvent Early Eocene Climatic Optimum
Eocene–Oligocene transition cooling
Middle Eocene Climatic Optimum
Paleocene–Eocene Thermal Maximum recovery phase
namedBy Charles Lyell
partOf Paleogene Period
linked to: Paleogene
precededBy Paleocene
precedes Oligocene
linked to: Oligocene Epoch
startTime Ypresian age onset
approximately 56 million years ago
subdivisionOf Cenozoic Era
linked to: Cenozoic

Phanerozoic Eon
usedIn International Commission on Stratigraphy timescale

How these facts were elicited

Referenced by (31)

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

Oromerycidae temporalRange Eocene
Absaroka Range geologicAge Eocene
Oligocene Epoch follows Eocene Epoch
linked to: Eocene
Equidae evolutionaryOrigin Eocene epoch
linked to: Eocene
Tapiridae firstAppearance Eocene
Paleogene climatic optimums occursIn Eocene Epoch
linked to: Eocene
Proboscidea majorRadiation Eocene
Waikato coal measures geologicalAge Late Eocene
linked to: Eocene
Uintah Basin geologicalEra Eocene
Geiseltal region geologicalAgeEvidence Middle Eocene
linked to: Eocene
Fossil Butte National Monument timePeriodRepresented Eocene Epoch
linked to: Eocene
Paenungulata fossilRecord Eocene
Oromeryx extinctionEpoch Eocene
Xiphodon temporalRange Eocene
Eocene chronostratigraphicUnit Eocene Series
linked to: Eocene
Eocene geochronologicUnit Eocene Epoch
linked to: Eocene
Tertiary System historicallyIncluded Eocene Series
linked to: Eocene
Messel Pit geologicalPeriod Eocene
subject linked to: Messel
Hyracotherium livedDuring Eocene
Heptodon geologicalEpoch Early Eocene
linked to: Eocene