Statements (61)
| Predicate | Object |
|---|---|
| gptkbp:instance_of |
gptkb:geological_formation
|
| gptkbp:associated_with |
ice ages
fossil records glacial deposits climate models climate change theories marine sedimentation patterns paleontological evidence cap carbonates glacial-interglacial cycles mass extinction paleoclimatic reconstructions |
| gptkbp:caused_by |
plate tectonics
reduced solar output |
| gptkbp:exhibited_at |
geological records
|
| gptkbp:followed_by |
Ediacaran period
|
| gptkbp:historical_debate |
gptkb:Research_Institute
|
| https://www.w3.org/2000/01/rdf-schema#label |
Snowball Earth events
|
| gptkbp:impact |
gptkb:physicist
biodiversity |
| gptkbp:influenced_by |
gptkb:volcanic_activity
gptkb:volcano biogeochemical cycles solar radiation changes climate feedback loops ocean circulation changes tectonic uplift oceanic currents atmospheric composition changes |
| gptkbp:is_characterized_by |
global glaciation
|
| gptkbp:is_described_as |
climate feedback mechanisms
|
| gptkbp:is_discussed_in |
gptkb:literary_work
|
| gptkbp:is_linked_to |
gptkb:Snowball_Earth_hypothesis
Cambrian explosion Earth's geological history biological evolution paleobiology Earth's climate history geological time scale Earth's albedo effect |
| gptkbp:is_studied_in |
geologists
geological surveys paleoclimatologists |
| gptkbp:occurs_in |
gptkb:Cryogenian_period
approximately 635 million years ago approximately 720 million years ago |
| gptkbp:related_to |
Rodinia supercontinent
|
| gptkbp:resulted_in |
algal blooms
increased carbon dioxide levels extensive ice coverage changes in ocean chemistry changes in biodiversity patterns changes in terrestrial ecosystems extinction of certain species |
| gptkbp:theory |
gptkb:Joseph_Kirschvink
geological processes geochemical evidence paleomagnetic data alternative climate models |
| gptkbp:bfsParent |
gptkb:Proterozoic_Eon
|
| gptkbp:bfsLayer |
4
|