breakup of Rodinia

E790078

The breakup of Rodinia was a major Neoproterozoic tectonic event in which the ancient supercontinent fragmented into separate landmasses, profoundly influencing global climate, ocean circulation, and the subsequent assembly of later supercontinents.

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All labels observed (1)

Label Occurrences
breakup of Rodinia canonical 2

Statements (50)

Predicate Object
instanceOf supercontinent breakup
tectonic event
associatedWith Marinoan glaciation NERFINISHED
Neoproterozoic glaciations NERFINISHED
Neoproterozoic oxygenation events
Snowball Earth events NERFINISHED
Sturtian glaciation NERFINISHED
evolutionary diversification of early eukaryotes
followedBy assembly of Gondwana
assembly of Pangaea NERFINISHED
assembly of Pannotia
hasConsequence assembly of later supercontinents
changes in global climate
changes in global ocean circulation
development of new ocean gateways
formation of separate continental blocks
fragmentation of the supercontinent Rodinia
initiation of new subduction zones
reorganization of global plate motions
hasEffectOn continental weathering rates
global carbon cycle
marine sedimentation patterns
nutrient flux to oceans
paleogeography of Neoproterozoic Earth
hasEndTime approximately 600 million years ago
hasPhase development of passive continental margins
initial rifting of continental margins
ocean basin opening
hasPrimaryEvidence paleomagnetic data from continental blocks
passive margin sedimentary sequences
rift-related volcanic rocks
hasStartTime approximately 800 million years ago
hasUncertainty exact configuration of Rodinia prior to breakup
exact timing of rifting events on different margins
involves development of passive margins
formation of new oceanic crust
large igneous province magmatism
mantle upwelling
rifting of continental lithosphere
seafloor spreading
occursIn Neoproterozoic Era NERFINISHED
partOf Neoproterozoic tectonic evolution NERFINISHED
produces extensional tectonic structures
new ocean basins
rift-related sedimentary basins
studiedBy geochronology
paleomagnetism
plate tectonics
sedimentology
structural geology

Referenced by (2)

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

Grenville orogeny followedBy breakup of Rodinia