supercontinent Pangaea
E200224
Pangaea was a massive supercontinent that existed during the late Paleozoic and early Mesozoic eras, when nearly all of Earth's landmasses were joined together before breaking apart into the continents we know today.
All labels observed (10)
| Label | Occurrences |
|---|---|
| Pangaea | 15 |
| Mesozoic supercontinent Pangaea | 1 |
| Pangaea assembly | 1 |
| Pangaea supercontinent | 1 |
| Pangaea supercontinent configuration | 1 |
| Pangea assembly | 1 |
| assembly of Pangaea | 1 |
| breakup of Pangaea | 1 |
| supercontinent Pangaea canonical | 1 |
| supercontinent Pangea | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T1772733 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
Target entity: supercontinent Pangaea Context triple: [Triassic, associatedWith, supercontinent Pangaea]
-
A.
supercontinent Pannotia
Supercontinent Pannotia was a short-lived late Proterozoic landmass that assembled near the end of the Precambrian and preceded the formation of the better-known supercontinent Pangaea.
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B.
supercontinent Rodinia
Rodinia was an ancient supercontinent that assembled during the Proterozoic Eon and existed before the later supercontinent Pangaea, profoundly influencing Earth’s early tectonic and climatic evolution.
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C.
supercontinent Columbia (Nuna)
Supercontinent Columbia (also known as Nuna) was an ancient landmass that assembled in the Paleoproterozoic and represents one of Earth’s earliest known supercontinents, predating Rodinia and Pangaea.
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D.
Gondwana
Gondwana was a vast ancient supercontinent in the Southern Hemisphere that included present-day South America, Africa, Antarctica, Australia, the Indian subcontinent, and the Arabian Peninsula.
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E.
Laurentia
Laurentia is an ancient Precambrian craton that forms the geological core of present-day North America and parts of Greenland and Scotland.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: supercontinent Pangaea Target entity description: Pangaea was a massive supercontinent that existed during the late Paleozoic and early Mesozoic eras, when nearly all of Earth's landmasses were joined together before breaking apart into the continents we know today.
-
A.
supercontinent Pannotia
Supercontinent Pannotia was a short-lived late Proterozoic landmass that assembled near the end of the Precambrian and preceded the formation of the better-known supercontinent Pangaea.
-
B.
supercontinent Rodinia
Rodinia was an ancient supercontinent that assembled during the Proterozoic Eon and existed before the later supercontinent Pangaea, profoundly influencing Earth’s early tectonic and climatic evolution.
-
C.
supercontinent Columbia (Nuna)
Supercontinent Columbia (also known as Nuna) was an ancient landmass that assembled in the Paleoproterozoic and represents one of Earth’s earliest known supercontinents, predating Rodinia and Pangaea.
-
D.
Gondwana
Gondwana was a vast ancient supercontinent in the Southern Hemisphere that included present-day South America, Africa, Antarctica, Australia, the Indian subcontinent, and the Arabian Peninsula.
-
E.
Laurentia
Laurentia is an ancient Precambrian craton that forms the geological core of present-day North America and parts of Greenland and Scotland.
- F. None of above. chosen
Statements (50)
| Predicate | Object |
|---|---|
| instanceOf |
prehistoric landmass
ⓘ
supercontinent ⓘ |
| associatedWith |
Permian period
ⓘ
Triassic ⓘ
surface form:
Triassic period
early Jurassic period ⓘ |
| beganBreakingApartApproximately | 200 million years ago ⓘ |
| breakupProcess |
rifting
ⓘ
seafloor spreading ⓘ |
| breakupProduced |
Atlantic Ocean
ⓘ
Indian Ocean ⓘ Southern Ocean margins ⓘ |
| climateCharacteristic |
extensive arid regions
ⓘ
large continental interior ⓘ strong seasonal contrasts ⓘ |
| comprised |
Gondwana
ⓘ
Laurasia ⓘ |
| containedPresentDay |
Africa
ⓘ
Antarctica ⓘ Asia ⓘ Australia ⓘ Europe ⓘ North America ⓘ South America ⓘ |
| continentType | supercontinent ⓘ |
| evidenceFrom |
fossil distribution
ⓘ
geological fit of continental margins ⓘ glacial deposits ⓘ paleomagnetism ⓘ |
| existedDuring |
early Mesozoic era
ⓘ
late Paleozoic era ⓘ |
| followedBy | supercontinent cycle leading to future possible supercontinents ⓘ |
| formedApproximately | 335 million years ago ⓘ |
| fullyFragmentedBy | about 175 million years ago ⓘ |
| hadInteriorSea |
Paleo-Tethys Ocean
ⓘ
Tethys Ocean ⓘ |
| influenced |
global biodiversity patterns
ⓘ
global climate ⓘ ocean circulation ⓘ |
| nameLanguage | Greek ⓘ |
| nameMeaning | "all Earth" ⓘ |
| paleogeographicReconstructionBy |
Alfred Wegener
ⓘ
subsequent geologists and geophysicists ⓘ |
| partOf | supercontinent cycle ⓘ |
| precededBy |
supercontinent Pannotia
ⓘ
supercontinent Rodinia ⓘ |
| proposalYear | 1912 ⓘ |
| proposedBy | Alfred Wegener ⓘ |
| supportsTheory |
continental drift
ⓘ
plate tectonics ⓘ |
| surroundedBy | Panthalassa Ocean ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Subject: supercontinent Pangaea Description of subject: Pangaea was a massive supercontinent that existed during the late Paleozoic and early Mesozoic eras, when nearly all of Earth's landmasses were joined together before breaking apart into the continents we know today.
Referenced by (24)
Full triples — surface form annotated when it differs from this entity's canonical label.