Lomagundi event

E843363

The Lomagundi event was a prolonged Paleoproterozoic episode of unusually high carbon isotope ratios in marine carbonates, interpreted as evidence for a major global increase in oxygen production and organic carbon burial.

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All labels observed (2)

Label Occurrences
Lomagundi event canonical 1
Lomagundi–Jatuli event 1

Statements (39)

Predicate Object
instanceOf carbon isotope excursion
geological event
paleoclimatic event
affects marine carbonates
associatedWith changes in global carbon cycle
long-term oxygenation of Earth’s surface environments
rise of atmospheric oxygen
duration on the order of 100 million years or more
endTime approximately 2.1 billion years ago
fieldOfStudy Earth system science
geochemistry
geology
paleoclimatology
follows Great Oxidation Event NERFINISHED
geologicTimePeriod Paleoproterozoic
hasCharacteristic large positive δ13C excursion
unusually high carbon isotope ratios in marine carbonates
hasConsequence changes in ocean redox conditions
drawdown of volcanic and metamorphic CO2
possible climatic cooling
interpretedAsEvidenceFor enhanced organic carbon burial
major global increase in oxygen production
involvesProcess burial of organic carbon in sediments
oxygenic photosynthesis
linkedTo changes in sulfur and iron cycling
evolution of early aerobic ecosystems
namedAfter Lomagundi district in Zimbabwe NERFINISHED
Lomagundi region NERFINISHED
recordedIn carbonate rock sequences
marine sedimentary basins
relatedTo Great Oxidation Event NERFINISHED
scale global
startTime approximately 2.3 billion years ago
studiedUsing stable carbon isotope geochemistry
stratigraphic correlations
temporalRelation occurs after initial rise of atmospheric O2 in the Paleoproterozoic
precedes later Proterozoic oxygenation events
uncertainty exact duration and global synchronicity remain debated
magnitude of associated atmospheric O2 increase is uncertain

Referenced by (2)

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

Lomagundi–Jatuli carbon isotope excursion alsoKnownAs Lomagundi event
this entity surface form: Lomagundi–Jatuli event