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.

All labels observed (1)

Label Occurrences
breakup of Rodinia canonical 2

How this entity was disambiguated

Statements (50)

Predicate Object
instanceOf supercontinent breakup ⓘ
tectonic event ⓘ
associatedWith Marinoan glaciation ⓘ
Neoproterozoic glaciations ⓘ
Neoproterozoic oxygenation events ⓘ
Snowball Earth events ⓘ
Sturtian glaciation ⓘ
evolutionary diversification of early eukaryotes ⓘ
followedBy assembly of Gondwana ⓘ
assembly of Pangaea ⓘ
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 ⓘ
partOf Neoproterozoic tectonic evolution ⓘ
produces extensional tectonic structures ⓘ
new ocean basins ⓘ
rift-related sedimentary basins ⓘ
studiedBy geochronology ⓘ
paleomagnetism ⓘ
plate tectonics ⓘ
sedimentology ⓘ
structural geology ⓘ

How these facts were elicited

Referenced by (2)

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

Grenville orogeny → followedBy → breakup of Rodinia ⓘ