Late Ordovician

E402491

The Late Ordovician was the final subdivision of the Ordovician Period, marked by extensive marine biodiversity followed by one of the largest mass extinction events in Earth's history.

All labels observed (1)

Label Occurrences
Late Ordovician canonical 2

How this entity was disambiguated

Statements (51)

Predicate Object
instanceOf geologic epoch ⓘ
subdivision of the Ordovician Period ⓘ
associatedWith changes in ocean chemistry ⓘ
changes in ocean circulation ⓘ
continental configurations dominated by Gondwana ⓘ
major reorganization of marine ecosystems ⓘ
bioticEffect collapse of many shallow-marine communities ⓘ
selective extinction among warm-water taxa ⓘ
turnover in reef-building organisms ⓘ
characterizedBy Late Ordovician mass extinction ⓘ
diverse marine invertebrate faunas ⓘ
extensive shallow epicontinental seas ⓘ
global cooling ⓘ
high marine biodiversity ⓘ
large sea-level fall ⓘ
major glaciation event ⓘ
widespread carbonate platforms ⓘ
climateTrend transition from greenhouse to icehouse conditions ⓘ
commonFossilGroup brachiopods ⓘ
bryozoans ⓘ
corals ⓘ
crinoids ⓘ
graptolites ⓘ
nautiloid cephalopods ⓘ
trilobites ⓘ
containsStage Hirnantian ⓘ
Katian ⓘ
Sandbian ⓘ
dominantLifeForm marine invertebrates ⓘ
endTime approximately 443.8 million years ago ⓘ
follows Middle Ordovician ⓘ
glaciationCenter present-day North Africa ⓘ
present-day South America ⓘ
linked to: South America
glaciationLocation Gondwana supercontinent ⓘ
linked to: Gondwana
GSSPDefinedBy first appearance of the graptite Normalograptus extraordinarius (Hirnantian base) ⓘ
first appearance of the graptolite Diplacanthograptus caudatus (Katian base) ⓘ
first appearance of the graptolite Nemagraptus gracilis (Sandbian base) ⓘ
hasMajorEvent Gondwanan glaciation ⓘ
Hirnantian glaciation ⓘ
Late Ordovician mass extinction ⓘ
massExtinctionRank one of the five largest Phanerozoic mass extinctions ⓘ
massExtinctionSeverity eliminated an estimated 85 percent of marine species ⓘ
partOf Ordovician Period ⓘ
positionInEon Phanerozoic Eon ⓘ
positionInEra Paleozoic Era ⓘ
positionInSystem third and final series of the Ordovician System ⓘ
precedes Silurian Period ⓘ
linked to: Silurian
seaLevelChange major regression during glacial maximum ⓘ
subsequent transgression during deglaciation ⓘ
startTime approximately 458.4 million years ago ⓘ
timeSpan about 14.6 million years ⓘ

How these facts were elicited

Referenced by (2)

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