Paleocene

E721105

The Paleocene was an early Cenozoic epoch, roughly 66–56 million years ago, marked by the recovery of life after the dinosaur-extinction event and the rapid diversification of mammals.

All labels observed (3)

Label Occurrences
Paleocene canonical 13
Paleocene Epoch 1
Paleocene Series 1

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf chronostratigraphic unit
geologic epoch
characterizedBy absence of polar ice sheets
decline of non-avian dinosaurs
development of modern coral reefs in some regions
evolution of early carnivorous mammals
evolution of early primate relatives
evolution of early ungulate-like mammals
evolution of large flightless birds in some regions
expansion of angiosperm-dominated forests
high atmospheric CO2 levels
radiation of birds
radiation of mammals
recovery of biodiversity after mass extinction
relatively low diversity of marine plankton compared to later Cenozoic
warm global climate
climateEventNearEnd Paleocene–Eocene Thermal Maximum precursor changes
climateTrend generally warm and equable
contains Danian age
Selandian age
Thanetian age
correlatesWith Danian Stage
Selandian Stage
linked to: Danian Stage

Thanetian Stage
definedBy International Commission on Stratigraphy
end approximately 56 million years ago
follows Cretaceous
lowerBoundaryCoincidesWith iridium-rich clay layer at K–Pg boundary
lowerBoundaryDefinedBy first appearance of the planktonic foraminiferan Globigerina eugubina
marineLife recovery and diversification of teleost fishes
recovery of ammonite-free marine ecosystems
nameCoinedBy Paul Gervais
nameMeaning ancient recent
partOf Cenozoic Era
linked to: Cenozoic

Paleogene Period
linked to: Paleogene
precedes Eocene
start approximately 66 million years ago
startEvent Cretaceous–Paleogene extinction event
stratotypeRegion Danish Basin
terrestrialFauna absence of large non-avian dinosaur megafauna
small-bodied mammals dominant
terrestrialFlora broadleaf evergreen forests at high latitudes
usedIn geologic time scale
paleoclimatology
paleontology
stratigraphy

How these facts were elicited

Referenced by (15)

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

Xenarthra fossilRecordSince Paleocene
Glires hasFossilRecord Paleocene
Paleogene climatic optimums occursIn Paleocene Epoch
linked to: Paleocene
Late Cretaceous precedes Paleocene
Reading Formation geologicEpoch Paleocene
Lambeth Group geologicalPeriod Paleocene
Didelphimorphia firstAppearance Paleocene
Cingulata timeOfOrigin Paleocene
Sokoto Basin geologicalPeriod Paleocene
Eocene precededBy Paleocene
Tertiary System historicallyIncluded Paleocene Series
linked to: Paleocene
Powder River Basin geologicAge Paleocene
Ekofisk oil field geologicalAge Paleocene