Great Ordovician Biodiversification Event

E87794

The Great Ordovician Biodiversification Event was a profound evolutionary radiation during the Ordovician Period that saw a dramatic increase in marine biodiversity and the establishment of many major animal groups in Paleozoic oceans.

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AI-generated illustration of Great Ordovician Biodiversification Event

This AI-generated illustration was produced by black-forest-labs/FLUX.2-dev (1024x1024) from a prompt written by openai/gpt-oss-120b from the entity's label + description.

Prompt

Generate an image of the Great Ordovician Biodiversification Event (The Great Ordovician Biodiversification Event was a profound evolutionary radiation during the Ordovician Period that saw a dramatic increase in marine biodiversity and the establishment of many major animal groups in Paleozoic oceans.)

All labels observed (1)

Label Occurrences
Great Ordovician Biodiversification Event canonical 7

How this entity was disambiguated

Statements (55)

Predicate Object
instanceOf Ordovician event ⓘ
biodiversification event ⓘ
evolutionary radiation ⓘ
paleontological event ⓘ
affects brachiopods ⓘ
bryozoans ⓘ
conodonts ⓘ
corals ⓘ
echinoderms ⓘ
graptolites ⓘ
mollusks ⓘ
ostracods ⓘ
trilobites ⓘ
alsoKnownAs GOBE ⓘ
associatedWith development of complex food webs ⓘ
expansion of carbonate platforms ⓘ
increase in alpha diversity ⓘ
increase in beta diversity ⓘ
increase in gamma diversity ⓘ
increase in plankton diversity ⓘ
characterizedBy dramatic increase in marine biodiversity ⓘ
expansion of ecological niches ⓘ
increase in bioturbation ⓘ
increase in ecological complexity ⓘ
increase in predation pressure ⓘ
increase in reef-building activity ⓘ
increase in taxonomic richness ⓘ
increase in tiering within seafloor communities ⓘ
endApproximateMa 444 ⓘ
follows Cambrian explosion ⓘ
hasDomain benthic communities ⓘ
marine ecosystems ⓘ
planktonic communities ⓘ
hasSignificance important benchmark for Phanerozoic biodiversity patterns ⓘ
key event in the history of marine life ⓘ
major step in the establishment of the Paleozoic marine fauna ⓘ
occursIn Paleozoic Era ⓘ
partOf Ordovician Period ⓘ
peakApproximateMa 470 ⓘ
possibleDriver changes in ocean chemistry ⓘ
climatic cooling from greenhouse to icehouse conditions ⓘ
increased nutrient input to oceans ⓘ
plate tectonics and continental reconfiguration ⓘ
sea-level rise and expansion of shallow seas ⓘ
precedes Late Ordovician mass extinction ⓘ
resultsIn differentiation of marine faunal provinces ⓘ
establishment of many major animal groups in Paleozoic oceans ⓘ
long-term rise in marine diversity above Cambrian levels ⓘ
startApproximateMa 485 ⓘ
studiedIn paleobiology ⓘ
paleoecology ⓘ
stratigraphy ⓘ
temporalLocation Early Ordovician ⓘ
linked to: Middle Ordovician

Late Ordovician ⓘ
Middle Ordovician ⓘ

How these facts were elicited

Referenced by (7)

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

Paleozoic Era → majorEvent → Great Ordovician Biodiversification Event ⓘ
Ordovician Period → characterizedBy → Great Ordovician Biodiversification Event ⓘ
Cambrian Period → followedByEvent → Great Ordovician Biodiversification Event ⓘ
Late Ordovician mass extinction → precededBy → Great Ordovician Biodiversification Event ⓘ
Middle Ordovician → associatedWith → Great Ordovician Biodiversification Event ⓘ
GOBE → fullName → Great Ordovician Biodiversification Event ⓘ
GOBE → abbreviationOf → Great Ordovician Biodiversification Event ⓘ