Paleozoic Era

E14994

The Paleozoic Era was an ancient geologic time interval, spanning roughly 541 to 252 million years ago, marked by the emergence and diversification of complex life in the seas and on land and the assembly of major continental landmasses.

All labels observed (8)

Label Occurrences
Paleozoic Era canonical 37
Paleozoic 21
Paleozoic era 9

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf geologic era
alternativeName Paleozoic Era
surface form: Palaeozoic Era
characterizedBy assembly of supercontinent Pangaea
colonization of land by arthropods
colonization of land by plants
diversification of marine invertebrates
emergence of complex animal life
evolution of vertebrates on land
formation of extensive coal swamps
major orogenies
multiple mass extinctions
climate generally variable climate
periods of extensive glaciation
contains Cambrian Period
Carboniferous period
surface form: Carboniferous Period

Devonian Period
Ordovician Period
Permian Period
Silurian
surface form: Silurian Period
duration approximately 289 million years
endsWith Permian–Triassic mass extinction
surface form: Permian–Triassic extinction event
endTime 252 million years ago
fieldOfStudy geology
paleontology
follows Neoproterozoic Era
majorEvent Cambrian explosion
Carboniferous rainforest collapse
Great Ordovician Biodiversification Event
Late Devonian extinction
Permian–Triassic mass extinction
partOf Phanerozoic Eon
precedes Mesozoic Era
significance development of complex terrestrial ecosystems
first appearance of most major animal phyla in fossil record
major diversification of vertebrates
transition of life from sea to land
startTime 541 million years ago
tectonicActivity closure of Iapetus Ocean
closure of Rheic Ocean
formation of Appalachian orogenies
formation of Ural orogeny
typicalLifeForms ammonoids
brachiopods
early amphibians
early fishes
early reptiles
trilobites
vascular land plants

How these facts were elicited

Referenced by (74)

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

Cambrian biota geologicalContext Paleozoic Era
Wenlock partOf Paleozoic Era
Nashville Basin geologicAge Paleozoic Era
this entity surface form: Paleozoic
Helderberg geologicalPeriod Paleozoic Era
this entity surface form: Palaeozoic
Pennyrile region geologicEraOfFormation Paleozoic Era
this entity surface form: Paleozoic
Pertnjara Group geologicAge Paleozoic Era
this entity surface form: Paleozoic
Sudetes mountains geologicalPeriod Paleozoic Era
subject surface form: Sudetes
this entity surface form: Paleozoic
Swartberg Mountains geologicalPeriod Paleozoic Era
this entity surface form: Paleozoic
Age of Fishes appliesTo Paleozoic Era
Age of Fishes partOf Paleozoic Era
Laurussia continent geologicEra Paleozoic Era
subject surface form: Laurussia
Cisuralian Epoch partOf Paleozoic Era
Cisuralian Epoch era Paleozoic Era
Asselian partOf Paleozoic Era
Sakmarian era Paleozoic Era
Wordian era Paleozoic Era
Guadalupian Epoch partOf Paleozoic Era
Late Ordovician mass extinction occursIn Paleozoic Era
this entity surface form: Paleozoic era
Middle Ordovician partOf Paleozoic Era
Late Ordovician positionInEra Paleozoic Era
Arkoma Basin geologicAge Paleozoic Era
this entity surface form: Paleozoic
Qinling–Dabie orogeny startEra Paleozoic Era
Blountian tectophase geologicTime Paleozoic Era
Terreneuvian belongsToEra Paleozoic Era