equatorial Euramerica

E413466

Equatorial Euramerica was a tropical, coal-forming landmass of the late Paleozoic era that hosted extensive rainforests before their widespread decline.

All labels observed (1)

Label Occurrences
equatorial Euramerica canonical 1

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf paleocontinent
paleogeographic landmass
associatedWith glacioeustatic sea-level fluctuations
high atmospheric oxygen levels in the Late Paleozoic
tropical peat accumulation
contributedTo Late Paleozoic coal deposits
major Carboniferous coal basins
documentedBy coal seam stratigraphy
fossil plant assemblages
paleomagnetic data
experienced loss of tropical wetland habitats
widespread rainforest decline
formedFrom collision of Laurentia and Baltica-Avalonia regions
hasEnvironment coal-forming wetlands
humid tropical climate
peat-forming mires
hasEvent Carboniferous rainforest collapse
hasFlora lycopsid-dominated forests
seed ferns
sphenopsids
tree ferns
knownFor coal formation
extensive coal swamps
rainforest ecosystems
linkedTo changes in terrestrial vertebrate faunas
extinctions and turnovers in tropical plant communities
locatedInTimePeriod Carboniferous period
surface form: Carboniferous

Lower Permian Series
surface form: Early Permian

Late Carboniferous
Late Paleozoic
Pennsylvanian
overlapsWith Laurussia
paleobiogeographicSignificance center of Late Paleozoic tropical biodiversity
key region for coal-swamp floras
paleoclimate tropical
paleogeographicPosition equatorial
paleogeographicRelation situated near the paleoequator
partOf Euramerica
precedes assembly of Pangaea as a unified supercontinent
researchField paleobotany
paleoclimatology
paleogeography
stratigraphy
underwent climatic drying during the Late Paleozoic
fragmentation of continuous rainforest belts

How these facts were elicited

Referenced by (1)

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

Carboniferous rainforest collapse tookPlaceIn equatorial Euramerica