Cisuralian Epoch

E392438

The Cisuralian Epoch is the earliest subdivision of the Permian, marking a time of significant diversification of terrestrial life and continued development of early amniotes following the late Paleozoic ice age.

All labels observed (3)

Label Occurrences
Cisuralian Epoch canonical 4
Cisuralian Series 1
Cisuralian epoch 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf geologic epoch ⓘ
subdivision of the Permian Period ⓘ
alsoKnownAs Lower Permian Series ⓘ
associatedWith post-glacial isostatic and eustatic sea-level changes ⓘ
characterizedBy abundant coal-bearing and red-bed continental deposits in some regions ⓘ
continued radiation of early amniotes ⓘ
development of early synapsid-dominated faunas ⓘ
diversification of terrestrial ecosystems ⓘ
expansion of arid and seasonally dry continental interiors ⓘ
retreat of late Paleozoic continental ice sheets ⓘ
chronostratigraphicRank series ⓘ
climate transition from late Paleozoic ice age to generally warmer and drier conditions ⓘ
containsAge Artinskian Age ⓘ
Asselian Age ⓘ
Kungurian Age ⓘ
linked to: Artinskian Age

Sakmarian Age ⓘ
earliestEpochOf Permian Period ⓘ
end approximately 272.3 million years ago ⓘ
eon Phanerozoic Eon ⓘ
era Paleozoic Era ⓘ
followedBy Guadalupian Epoch ⓘ
follows Late Carboniferous ⓘ
Pennsylvanian Subperiod ⓘ
geochronologicRank epoch ⓘ
lowerBoundaryDefinedBy first appearance datum of the conodont Streptognathodus isolatus ⓘ
lowerBoundaryStratotype Global Stratotype Section and Point at Aidaralash Creek near Aqtöbe, Kazakhstan ⓘ
marineLife abundant brachiopods ⓘ
ammonoids and other cephalopods ⓘ
diverse crinoids and other echinoderms ⓘ
diverse fusulinid foraminifera ⓘ
namedAfter western slope of the Ural Mountains (Cis-Uralian region) ⓘ
notableFor shift from coal-swamp ecosystems to more xeric terrestrial biomes ⓘ
paleogeography assembly and early evolution of the supercontinent Pangea ⓘ
extensive interior continental basins ⓘ
partOf Paleozoic Era ⓘ
Permian Period ⓘ
plantLife expansion of seed ferns and conifers in drier habitats ⓘ
positionInPermian lower (earliest) series of the Permian ⓘ
recognizedBy International Commission on Stratigraphy ⓘ
standardGlobalUse international chronostratigraphic chart ⓘ
start approximately 298.9 million years ago ⓘ
system Permian System ⓘ
linked to: Permian Period
terrestrialLife decline of many Carboniferous lycopsid swamp floras ⓘ
diverse early reptiles (sauropsid amniotes) ⓘ
early pelycosaur-grade synapsids ⓘ
early therapsid precursors ⓘ
timeSpan about 26.6 million years ⓘ
upperBoundaryApproximateEvent significant faunal turnover in marine invertebrates ⓘ
upperBoundaryDefinedBy base of the Guadalupian Epoch ⓘ

How these facts were elicited

Referenced by (6)

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

Permian Period → hasSubdivision → Cisuralian Epoch ⓘ
Asselian → marksBeginningOf → Cisuralian Epoch ⓘ
Asselian → partOf → Cisuralian Epoch ⓘ
Sakmarian → partOf → Cisuralian Series ⓘ
linked to: Cisuralian Epoch
Guadalupian Epoch → follows → Cisuralian Epoch ⓘ
Edaphosaurus → livedDuring → Cisuralian epoch ⓘ
linked to: Cisuralian Epoch