Marinoan glaciation

E231931

The Marinoan glaciation was a major Neoproterozoic ice age, likely a global or near-global “Snowball Earth” event that occurred around 650–635 million years ago.

All labels observed (2)

Label Occurrences
Marinoan glaciation canonical 9
Elatina glaciation 1

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf Neoproterozoic ice age ⓘ
Snowball Earth event ⓘ
glaciation event ⓘ
alsoKnownAs Elatina glaciation ⓘ
linked to: Marinoan glaciation
associatedWith changes in ocean chemistry ⓘ
large negative carbon isotope excursions ⓘ
perturbations of the global carbon cycle ⓘ
rise in atmospheric oxygen levels (hypothesized) ⓘ
causedBy continental configuration favoring ice growth (hypothesized) ⓘ
long-term drawdown of atmospheric CO₂ (hypothesized) ⓘ
characterizedBy extensive continental ice sheets ⓘ
low-latitude glaciation ⓘ
climateExtent global or near-global ⓘ
climateModel Snowball Earth hypothesis ⓘ
duration on the order of several million years ⓘ
endMarkedBy deposition of cap carbonates ⓘ
endTime approximately 635 million years ago ⓘ
evidenceFrom cap carbonates ⓘ
dropstones in marine sediments ⓘ
glacial diamictites ⓘ
paleomagnetic data indicating low-latitude ice ⓘ
fieldOfStudy Neoproterozoic geology ⓘ
linked to: Neoproterozoic Era

paleoclimatology ⓘ
stratigraphy ⓘ
followedBy Ediacaran Period ⓘ
follows Sturtian glaciation ⓘ
geologicalAge late Cryogenian, ca. 650–635 Ma ⓘ
geologicalPeriod Neoproterozoic ⓘ
linked to: Neoproterozoic Era
impactOn subsequent Ediacaran biotic diversification (hypothesized) ⓘ
locationEvidence Canada ⓘ
China ⓘ
Namibia ⓘ
Northwest Canada ⓘ
linked to: Northern Canada

South Australia ⓘ
Svalbard ⓘ
namedAfter Marino, South Australia ⓘ
partOf Cryogenian glaciations ⓘ
Neoproterozoic Snowball Earth episodes ⓘ
precededBy Sturtian glaciation ⓘ
precedes Ediacaran Period ⓘ
relatedConcept Ediacaran biota ⓘ
Snowball Earth ⓘ
Sturtian glaciation ⓘ
significance key constraint on Cryogenian–Ediacaran boundary ⓘ
one of the most severe ice ages in Earth history ⓘ
startTime approximately 650 million years ago ⓘ
terminationMechanism accumulation of volcanic CO₂ leading to greenhouse warming (hypothesized) ⓘ
timeSpan late Cryogenian Period ⓘ
linked to: Cryogenian Period

How these facts were elicited

Referenced by (10)

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

Neoproterozoic Era → includesEvent → Marinoan glaciation ⓘ
Snowball Earth glaciations → hasPart → Marinoan glaciation ⓘ
Sturtian glaciation → followedBy → Marinoan glaciation ⓘ
Marinoan glaciation → alsoKnownAs → Elatina glaciation ⓘ
linked to: Marinoan glaciation
Gaskiers glaciation → precededBy → Marinoan glaciation ⓘ
Neoproterozoic Oxygenation Event → linkedTo → Marinoan glaciation ⓘ
Cryogenian Period → hasMajorGlaciation → Marinoan glaciation ⓘ
Slushball Earth → relatesTo → Marinoan glaciation ⓘ
subject linked to: slushball Earth
breakup of Rodinia → associatedWith → Marinoan glaciation ⓘ