Linked from

The 71 pages that link to Pangaea, each with the reason it gives.

• Plate tectonicsRelated: Plate reconstructions turned Pangaea from hypothesis into a mapped episode of Earth history.

• CretaceousRelated: Its breakup set the continental arrangement inherited by Cretaceous ecosystems.

• PermianRelated: Its vast interior and surrounding coastlines shaped Permian climates and habitats.

• TriassicRelated: Its vast interior helped produce the Triassic's strongly seasonal, arid climate.

• Continental driftRelated: The ancestral configuration drift was supposed to explain breaking apart.

• CarboniferousRelated: Its assembly reshaped Carboniferous geography and contributed to regional climate change.

• MesozoicRelated: Its breakup changed coastlines, climates, and routes for animal dispersal.

• PaleozoicRelated: Its assembly changed ocean circulation and habitats toward the era’s close.

• Tethys OceanRelated: Tethys occupied the eastern region of Pangaea before the supercontinent fragmented.

• North American PlateRelated: The plate’s later separation from other continental blocks followed Pangaea’s breakup.

• JurassicRelated: Its fragmentation shaped Jurassic oceans, climates, and biogeographic barriers.

• Wilson cycleRelated: Its assembly closed earlier oceans; its breakup opened the Atlantic.

• Late TriassicRelated: Its vast interior shaped Late Triassic climates and connected terrestrial ecosystems.

• LaurentiaRelated: Laurentia became part of Pangaea through Paleozoic collisions with other continents.

• Ural MountainsRelated: The Uralian collision helped join landmasses that became part of Pangaea.

• Rift valleyRelated: Its breakup produced rifts that later opened into the Atlantic Ocean.

• Alpine orogenyRelated: Its breakup initiated the plate rearrangements that eventually opened and closed the Tethys realm.

• Carboniferous rainforest collapseRelated: Its continental interiors and changing geography influenced tropical climate patterns.

• Karoo SupergroupRelated: Karoo deposition took place while southern Africa lay within Pangaea.

• Caledonian orogenyRelated: The collisions that built the belt contributed to the assembly of this later supercontinent.

• GlossopterisRelated: Glossopteris spread across southern regions within the larger Pangaean landmass.

• CoelophysisRelated: Coelophysis lived when its North American habitat was part of this connected landmass.

• Central Atlantic Magmatic ProvinceRelated: CAMP erupted across the interior of this supercontinent before its breakup.

• Afar DepressionRelated: Its breakup set the long-term plate motions that shaped the Red Sea and Gulf of Aden.

• DimetrodonRelated: Dimetrodon fossils come from regions that lay within Pangaea's tropical belt.

• Alleghanian orogenyRelated: Its assembly culminated in the continental collision that drove this mountain-building episode.

• PannotiaRelated: Pangaea formed much later, making it a distinct stage in the supercontinent cycle.

• Continental riftRelated: Its breakup began with rifting that opened the Atlantic Ocean.

• Early PermianRelated: Its vast interior and geography influenced Early Permian environments.

• Middle TriassicRelated: Its geography shaped the climates and habitats represented in Middle Triassic rocks.

• Monte San GiorgioRelated: Its breakup reshaped the marine geography in which the site’s Triassic ecosystems developed.

• Central Asian Orogenic BeltRelated: The belt’s late Paleozoic accretion contributed to the continental framework incorporated into Pangea.

• MesosaurusRelated: Its geography explains how Mesosaurus fossils occur on both sides of the South Atlantic.

• PanthalassaRelated: Its assembly brought the continents together within Panthalassa; its breakup reshaped the ocean.

• RhynchosauriaRelated: Its connected landmasses help explain rhynchosaur fossils across multiple continents.

• DiadectesRelated: Permian North America formed part of this connected landmass.

• EuropasaurusRelated: Its breakup shaped the coastal and island geography of Jurassic Europe.

• Late Paleozoic icehouseRelated: Its vast interiors and geography influenced rainfall, weathering, and climate during the icehouse.

• PareiasauriaRelated: Pareiasaur fossils occur across regions that were joined within this Permian landmass.

• CotylorhynchusRelated: Its habitat lay within the continental interior of Pangaea.

• Geology of the AppalachiansRelated: The Appalachians formed along Pangaea’s collisional interior before rifting separated the continents.

• MegazostrodonRelated: Its Early Jurassic setting belongs to a world still shaped by the breakup of Pangaea.

• Triassic–Jurassic extinctionRelated: The supercontinent was beginning to rift as CAMP volcanism and the extinction unfolded.