breakup of Gondwana

E55394

The breakup of Gondwana was a major tectonic event during the Mesozoic era in which the ancient southern supercontinent fragmented into the continents and oceanic plates of the Southern Hemisphere, reshaping global geography and climate.


Statements (58)
Predicate Object
instanceOf geological process
plate tectonic event
tectonic event
endTime Cenozoic era
evidencedBy fossil distributions
matching geological structures on now-separated continents
paleomagnetic data
stratigraphic correlations
follows assembly of Gondwana supercontinent
breakup of Laurasia
hasCause mantle convection
plate tectonics
rifting
hasConsequence formation of circum-Antarctic current
onset of Antarctic glaciation
hasEffect biogeographic isolation of southern landmasses
changes in global climate
divergent evolution of Southern Hemisphere biotas
formation of modern Southern Hemisphere continents
fragmentation of Gondwana supercontinent
opening of the Indian Ocean
opening of the South Atlantic Ocean
opening of the Southern Ocean
reorganization of global ocean circulation
hasPhase initial rifting between East and West Gondwana
isolation of Antarctica
northward drift of India
separation of Africa and South America
involves continental rifting
formation of mid-ocean ridges
seafloor spreading
transform faulting
occursIn Mesozoic era
partOf breakup of Pangaea
precededBy late Paleozoic orogenies
resultsIn African Plate
Antarctic Plate
Australian Plate
Indian Plate
Indo-Australian Plate
Nazca Plate
Scotia Plate
South American Plate
microplates in the Indian Ocean
separates Africa from Antarctica
Africa from Australia
Africa from India
Africa from South America
Australia from Antarctica
India from Antarctica
India from Australia
Madagascar from Africa
New Zealand from Antarctica
South America from Antarctica
startTime Early Jurassic
studiedBy geologists
paleoclimatologists
paleomagnetists

Referenced by (3)

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