Eocene–Oligocene climate transition

E49688

The Eocene–Oligocene climate transition was a major global cooling event around 34 million years ago that marked the shift from a greenhouse to an icehouse Earth, including the formation of large Antarctic ice sheets.

All labels observed (6)

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf Cenozoic climate transition
global cooling event
paleoclimatic event
alsoKnownAs EOT
Eocene–Oligocene climate transition
surface form: Eocene–Oligocene boundary event

Eocene–Oligocene climate transition
surface form: Eocene–Oligocene transition
associatedWith Eocene–Oligocene climate transition self-linksurface differs
surface form: Eocene–Oligocene extinction events

expansion of grasslands in some regions
turnover in mammalian faunas
characterizedBy changes in atmospheric CO2 levels
changes in ocean circulation
global cooling
growth of Antarctic ice sheets
rapid temperature drop
shift from greenhouse to icehouse climate state
endTime early Oligocene epoch
followedBy Oligocene icehouse climate state
hasCause Antarctic isolation by circumpolar currents
decline in atmospheric CO2 concentration
opening of Southern Ocean gateways
tectonic reorganization
hasEffect changes in marine biodiversity
changes in terrestrial ecosystems
cooling of deep oceans
expansion of Antarctic ice sheets
onset of large-scale Antarctic glaciation
reorganization of atmospheric circulation
reorganization of ocean circulation patterns
sea-level fall due to ice-sheet growth
strengthening of equator-to-pole temperature gradients
locationOfEffect Antarctica
Southern Ocean
deep ocean basins
global climate system
occursAtTime Eocene–Oligocene boundary
partOf Cenozoic
surface form: Cenozoic Era

Paleogene
surface form: Paleogene Period
precededBy Eocene greenhouse climate state
separates Paleogene
surface form: Eocene Epoch

Oligocene Epoch
significance established persistent polar ice sheets on Earth
major step in long-term Cenozoic cooling trend
startTime approximately 34 million years ago
studiedUsing benthic foraminifera isotopes
deep-sea oxygen isotope records
marine sediment cores
paleobotanical data
terrestrial sedimentary records

How these facts were elicited

Referenced by (7)

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

Paleogene contains Eocene–Oligocene climate transition
Eocene–Oligocene climate transition alsoKnownAs Eocene–Oligocene climate transition
this entity surface form: Eocene–Oligocene transition
Eocene–Oligocene climate transition alsoKnownAs Eocene–Oligocene climate transition
this entity surface form: Eocene–Oligocene boundary event
Eocene–Oligocene climate transition associatedWith Eocene–Oligocene climate transition self-linksurface differs
this entity surface form: Eocene–Oligocene extinction events
Cenozoic glaciations hasPart Eocene–Oligocene climate transition
this entity surface form: Eocene–Oligocene glaciation
Cenozoic glaciations significantEvent Eocene–Oligocene climate transition
Phanerozoic mass extinctions hasPart Eocene–Oligocene climate transition
this entity surface form: Paleogene (Eocene–Oligocene) extinction events