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.
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.
this entity surface form:
Lomagundi–Jatuli event