GOBE

E413465

GOBE refers to the Great Ordovician Biodiversification Event, a major evolutionary radiation during the Ordovician period when marine life rapidly diversified and global biodiversity dramatically increased.

All labels observed (1)

Label Occurrences
GOBE canonical 1

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf biodiversification event ⓘ
evolutionary radiation ⓘ
paleontological event ⓘ
abbreviationOf Great Ordovician Biodiversification Event ⓘ
affects benthic communities ⓘ
marine ecosystems ⓘ
planktonic communities ⓘ
associatedWith changes in ocean circulation ⓘ
cooling global climate ⓘ
expansion of shallow marine habitats ⓘ
increased nutrient availability ⓘ
plate tectonic reconfigurations ⓘ
sea-level fluctuations ⓘ
characterizedBy ecological diversification of marine communities ⓘ
rapid increase in marine biodiversity ⓘ
taxonomic diversification of marine animals ⓘ
comparedTo Cambrian Explosion ⓘ
linked to: Cambrian explosion
considered one of the most significant biodiversification events of the Phanerozoic ⓘ
evidenceType paleoecological community analyses ⓘ
taxonomic diversity curves ⓘ
followsEvent Cambrian Explosion ⓘ
linked to: Cambrian explosion
fullName Great Ordovician Biodiversification Event ⓘ
hasTemporalPosition after Cambrian Explosion ⓘ
before end-Ordovician mass extinction ⓘ
impactOnBiodiversity long-term increase in global marine diversity ⓘ
impactOnBiota establishment of many modern marine clades ⓘ
majorlyInvolves brachiopods ⓘ
bryozoans ⓘ
conodonts ⓘ
echinoderms ⓘ
graptolites ⓘ
mollusks ⓘ
trilobites ⓘ
occursInGeologicPeriod Ordovician period ⓘ
linked to: Ordovician Period
precedesEvent end-Ordovician mass extinction ⓘ
recognizedBy fossil record of Ordovician strata ⓘ
resultsIn development of more complex food webs ⓘ
expansion of ecological niches ⓘ
increase in ecosystem complexity ⓘ
increase in number of marine families ⓘ
increase in number of marine genera ⓘ
studiedInDiscipline evolutionary biology ⓘ
paleobiology ⓘ
paleoecology ⓘ
paleontology ⓘ
stratigraphy ⓘ
timeSpan Early Late Ordovician ⓘ
Middle Ordovician ⓘ

How these facts were elicited

Referenced by (1)

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