T-OAE

E727678

T-OAE is a major Early Jurassic global oceanic anoxic event marked by widespread marine oxygen depletion, carbon cycle disruption, and significant biotic turnover.

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Statements (47)

Predicate Object
instanceOf climatic perturbation
oceanic anoxic event
abbreviationOf Toarcian Oceanic Anoxic Event NERFINISHED
affects global oceans
marine ecosystems
approximateAgeMa 183
associatedWith black shale deposition
carbon cycle instability
changes in seawater chemistry
enhanced greenhouse conditions
expanded oxygen minimum zones
extinction of ammonites
extinction of benthic invertebrates
extinction of brachiopods
global warming
increased weathering rates
mass extinction of marine taxa
nutrient enrichment of oceans
ocean acidification
turnover in marine plankton
characterizedBy enhanced organic carbon burial
global carbon cycle disruption
negative carbon isotope excursion
significant biotic turnover
widespread marine oxygen depletion
consequence collapse of some marine food webs
long-term changes in carbon reservoirs
restructuring of marine biodiversity
duration hundreds of thousands of years
fullName Toarcian Oceanic Anoxic Event NERFINISHED
geologicTimePosition early Toarcian
hasEvidenceIn carbon isotope records
marine stratigraphic sections
organic-rich sedimentary rocks
paleontological records
linkedTo Karoo-Ferrar large igneous province NERFINISHED
large igneous province volcanism
occursIn Early Jurassic NERFINISHED
Toarcian Age NERFINISHED
recordedIn European epicontinental seas
Panthalassa Ocean margins
Tethys Ocean margins
triggerHypothesis climate warming-induced stratification
massive volcanic CO2 emissions
methane release from marine sediments
usedAs chemostratigraphic marker
paleoenvironmental analog for modern deoxygenation

Referenced by (1)

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