Lomagundi excursion

E843364

The Lomagundi excursion is a major Paleoproterozoic carbon isotope anomaly reflecting a prolonged global increase in organic carbon burial and atmospheric oxygen levels.

All labels observed (1)

Label Occurrences
Lomagundi excursion canonical 1

How this entity was disambiguated

Statements (43)

Predicate Object
instanceOf Paleoproterozoic geological event ⓘ
carbon isotope anomaly ⓘ
carbon isotope excursion ⓘ
affects atmospheric oxygen concentration ⓘ
global carbon cycle ⓘ
redox state of the oceans ⓘ
associatedWith Great Oxidation Event ⓘ
characterizedBy elevated atmospheric oxygen levels ⓘ
global-scale positive δ13C anomaly ⓘ
large positive carbon isotope values in marine carbonates ⓘ
prolonged increase in organic carbon burial ⓘ
duration on the order of 100 million years or more ⓘ
endTime approximately 2.06 billion years ago ⓘ
evidenceType carbon isotope ratios in marine carbonate rocks ⓘ
δ13C measurements of carbonate and organic carbon ⓘ
follows initial rise of atmospheric oxygen in the Great Oxidation Event ⓘ
geologicalAge Paleoproterozoic Eon ⓘ
hasConsequence long-term shift in surface environment redox conditions ⓘ
possible expansion of habitable niches for early life ⓘ
hasMagnitude δ13Ccarb values commonly exceeding +10‰ ⓘ
interpretedAs evidence for large-scale organic carbon sequestration ⓘ
interval of enhanced net oxygen production ⓘ
linkedToProcess enhanced burial of organic carbon in sediments ⓘ
long-term oxygen accumulation in the atmosphere-ocean system ⓘ
oxidation of reduced volcanic and crustal gases ⓘ
namedAfter Lomagundi region in Zimbabwe ⓘ
recordedIn Lomagundi Group of Zimbabwe ⓘ
Paleoproterozoic sedimentary basins ⓘ
relatedConcept Earth oxygenation events ⓘ
carbon isotope stratigraphy ⓘ
organic carbon burial feedbacks ⓘ
relevance constrains timing of atmospheric oxygenation ⓘ
informs models of early Earth habitability ⓘ
used to calibrate Paleoproterozoic stratigraphy ⓘ
spatialExtent global ⓘ
startTime approximately 2.22 billion years ago ⓘ
studiedInDiscipline geochemistry ⓘ
paleoclimatology ⓘ
sedimentary geology ⓘ
temporalRelation postdates onset of the Great Oxidation Event ⓘ
precedes later Paleoproterozoic decline in δ13C values ⓘ
uncertainty exact duration is debated ⓘ
mechanisms driving the anomaly are debated ⓘ

How these facts were elicited

Referenced by (1)

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