Pridoli Epoch

E147845

The Pridoli Epoch is the final epoch of the Silurian Period, marking a transitional interval in Earth’s history just before the onset of the Devonian.

All labels observed (3)

Label Occurrences
Pridoli 4
Pridoli Series 2
Pridoli Epoch canonical 1

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf chronostratigraphic unit
geologic epoch
biota diverse marine invertebrate faunas
early terrestrial plant communities
jawless and jawed fishes
boundaryAboveDefinedBy base of the Lochkovian at the Silurian–Devonian boundary
boundaryBelowDefinedBy top of the Ludfordian Stage
characterizedBy continued diversification of early jawed fishes
development of early vascular land plants
stabilization of post-Late Ordovician extinction ecosystems
chronologicalPosition late Silurian
climate generally warm greenhouse conditions
conodontFaunas used for high-resolution stratigraphic subdivision
contains Pridoli Epoch self-linksurface differs
surface form: Pridoli Series
correlatesWith uppermost Silurian strata worldwide
definedBy International Commission on Stratigraphy
duration about 4 million years
end approximately 419 million years ago
endUncertainty about ±2 million years
fishEvolutionSignificance radiation of early jawed vertebrates (gnathostomes)
follows Ludfordian Age
graptoliteFaunas important for global biostratigraphic correlation
GSSPDefinedBy first appearance of the graptolite Monograptus parultimus
GSSPLocation Pridoli section near Prague, Czech Republic
ICSStatus ratified unit on the International Chronostratigraphic Chart
importance key interval for studying Silurian–Devonian transition
isEquivalentChronostratigraphicUnitOf Pridoli Epoch self-linksurface differs
surface form: Pridoli Series
lithostratigraphicAssociations shallow-marine carbonates and shales in many regions
namedAfter Pridoli Epoch self-linksurface differs
surface form: Pridoli

Pridoli area near Prague in the Czech Republic
paleoclimate low-latitude tropical seas over many continental shelves
paleogeography dominance of Gondwana and Laurentia as major landmasses
partOf Silurian
surface form: Silurian Period
plantEvolutionSignificance expansion of simple vascular plants onto land
positionInPeriod final epoch of the Silurian Period
positionInSystem fourth and youngest epoch of the Silurian System
precedes Devonian Period
Lochkovian Epoch
seaLevelTrend relatively high global sea levels
standardAbbreviation Pridoli Epoch self-linksurface differs
surface form: Pridoli
start approximately 423 million years ago
startUncertainty about ±2 million years
stratigraphicUsage international chronostratigraphic standard
timeScale Paleozoic Era
Phanerozoic Eon
transitionRole transitional interval between Silurian and Devonian biotas
usedIn geologic time scale
stratigraphic correlation

How these facts were elicited

Referenced by (7)

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

Early Devonian follows Pridoli Epoch
Silurian subdivision Pridoli Epoch
this entity surface form: Pridoli
Pridoli Epoch namedAfter Pridoli Epoch self-linksurface differs
this entity surface form: Pridoli
Pridoli Epoch contains Pridoli Epoch self-linksurface differs
this entity surface form: Pridoli Series
Pridoli Epoch isEquivalentChronostratigraphicUnitOf Pridoli Epoch self-linksurface differs
this entity surface form: Pridoli Series
Pridoli Epoch standardAbbreviation Pridoli Epoch self-linksurface differs
this entity surface form: Pridoli
Lochkovian follows Pridoli Epoch
this entity surface form: Pridoli