Quaternary period

E33564

The Quaternary period is the most recent division of geologic time, characterized by repeated ice ages, the evolution and global spread of modern humans, and significant climatic fluctuations over the last 2.6 million years.

All labels observed (6)

How this entity was disambiguated

Statements (51)

Predicate Object
instanceOf geologic period
associatedWith Antarctic ice sheet expansion
Northern Hemisphere ice sheets
formation of modern river systems
human-induced environmental change in late Holocene
loess deposition
permafrost development
baseDefinedBy Gauss–Matuyama geomagnetic reversal
marine isotope stage 103
characterizedBy development of modern ecosystems
evolution of Homo sapiens
global climatic fluctuations
global spread of modern humans
major ice ages
megafaunal extinctions
orbital forcing of climate
repeated glacial–interglacial cycles
sea level fluctuations
climateDriver Milankovitch cycles
greenhouse gas concentration changes
ice sheet dynamics
contains Holocene climatic optimum
Last Glacial Maximum
Pleistocene epoch
surface form: Last Interglacial (Eemian)

Little Ice Age
Younger Dryas cold event
current interglacial
definedBy International Commission on Stratigraphy
duration about 2.58 million years
endTime present
follows Neogene
surface form: Neogene period
hasEpoch Holocene
surface form: Holocene epoch

Pleistocene epoch
includesTaxonEvent Denisovan extinction
Late Quaternary megafaunal extinction
Neanderthal extinction
domestication of plants and animals
emergence of genus Homo
evolution of anatomically modern humans
rise of human civilizations
partOf Cenozoic
surface form: Cenozoic Era
precedes Holocene
surface form: Holocene epoch
startTime Pleistocene epoch onset
approximately 2.58 million years ago
stratotypeSection Vrica section, Calabria, Italy
subdividedInto Holocene
surface form: Early Holocene

Pleistocene epoch
surface form: Early Pleistocene

Holocene
surface form: Late Holocene

Pleistocene epoch
surface form: Late Pleistocene

Holocene climatic optimum
surface form: Middle Holocene

Pleistocene epoch
surface form: Middle Pleistocene

How these facts were elicited

Referenced by (58)

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

Kishimadake geologicalAge Quaternary period
this entity surface form: Quaternary
Nekodake geologicalAge Quaternary period
this entity surface form: Quaternary
Chihsing Mountain hasGeologicalAge Quaternary period
this entity surface form: Quaternary
Estancia Basin geologicalAge Quaternary period
this entity surface form: Quaternary
Ajusco mountain geologicalAge Quaternary period
subject surface form: Ajusco
this entity surface form: Quaternary
Telica geologicalAge Quaternary period
this entity surface form: Quaternary
Quaternary science studies Quaternary period
Kerinci Volcano geologicalAge Quaternary period
this entity surface form: Quaternary