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.

AI illustration

How this image was made

AI-generated illustration of Eocene–Oligocene climate transition

This AI-generated illustration was produced by black-forest-labs/FLUX.2-dev (1024x1024) from a prompt written by openai/gpt-oss-120b from the entity's label + description.

Prompt

Generate an image of the Eocene–Oligocene climate transition (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 (7)

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf Cenozoic climate transition ⓘ
global cooling event ⓘ
paleoclimatic event ⓘ
alsoKnownAs EOT ⓘ
Eocene–Oligocene boundary event ⓘ
Eocene–Oligocene transition ⓘ
associatedWith 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 Era ⓘ
linked to: Cenozoic

Paleogene Period ⓘ
linked to: Paleogene
precededBy Eocene greenhouse climate state ⓘ
separates Eocene Epoch ⓘ
linked to: Paleogene

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 (9)

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 transition ⓘ
linked to: Eocene–Oligocene climate transition
Eocene–Oligocene climate transition → alsoKnownAs → Eocene–Oligocene boundary event ⓘ
linked to: Eocene–Oligocene climate transition
Eocene–Oligocene climate transition → associatedWith → Eocene–Oligocene extinction events ⓘ
linked to: Eocene–Oligocene climate transition
Cenozoic glaciations → hasPart → Eocene–Oligocene glaciation ⓘ
linked to: Eocene–Oligocene climate transition
Cenozoic glaciations → significantEvent → Eocene–Oligocene climate transition ⓘ
Phanerozoic mass extinctions → hasPart → Paleogene (Eocene–Oligocene) extinction events ⓘ
linked to: Eocene–Oligocene climate transition
East Antarctic Ice Sheet → beganForming → Eocene–Oligocene transition ⓘ
linked to: Eocene–Oligocene climate transition
Eocene → includesEvent → Eocene–Oligocene transition cooling ⓘ
linked to: Eocene–Oligocene climate transition