Linked from

The 105 pages that link to Gondwana, each with the reason it gives.

• BiogeographyRelated: Its breakup scattered shared ancestries across South America, Africa, Australia, and Antarctica.

• PangaeaRelated: Pangaea's southern half, whose breakup scattered matching fossils and rocks across southern seas.

• MarsupialRelated: Its breakup shaped the geographic history of several marsupial lineages.

• Continental driftRelated: Fossil and rock matches across Gondwana's fragments were drift's strongest evidence.

• Tethys OceanRelated: Gondwana formed Tethys's southern margin through much of its history.

• PaleobiogeographyRelated: Its breakup reshaped the ranges and later isolation of southern organisms.

• Alfred WegenerRelated: Wegener assembled Gondwana's matches across continents as his strongest case for drift.

• Guiana ShieldRelated: The shield’s crust later became part of Gondwana as continents assembled.

• Indian subcontinentRelated: The Indian landmass separated from Gondwana before drifting north toward Eurasia.

• OrdovicianRelated: Its position over the South Pole made Gondwana central to late Ordovician glaciation.

• Late JurassicRelated: Its land areas hosted distinctive southern Late Jurassic ecosystems.

• Great Rift ValleyRelated: Its breakup established the plate boundaries later reshaped by African rifting.

• Supercontinent cycleRelated: Its assembly at about 550 million years ago completed Pangaea's precursor patchwork.

• Great Dividing RangeRelated: The range’s rocks and landforms developed on the eastern margin of Australia after Gondwana’s breakup.

• Appalachian orogenyRelated: A portion of Gondwana collided with Laurentia during the Alleghanian phase.

• RatiteRelated: Ratite distributions once suggested their ancestors were carried apart as Gondwana broke up.

• AmericasRelated: South America was once joined to the other continents of Gondwana.

• AvaloniaRelated: Avalonia rifted from Gondwana’s northern margin during the Paleozoic.

• TuataraRelated: Tuatara’s deep evolutionary history is often considered alongside New Zealand’s separation from Gondwana.

• AmborellaRelated: Its breakup shaped the region’s geological history, though Amborella’s lineage is much older than the islands’ current geography.

• SauropodomorphaRelated: Sauropodomorph fossils across former Gondwanan continents help reconstruct the lineage's geographic history.

• Alleghanian orogenyRelated: Its approach to Laurentia supplied the continental collision behind the orogeny.

• Afro-EurasiaRelated: Africa was part of Gondwana before its breakup helped shape the modern continent.

• AraucariaceaeRelated: The family’s fossil record and modern range reflect Gondwana’s former connections.

• CeratosauriaRelated: Many Cretaceous ceratosaurs lived on continents that had once formed this southern landmass.

• LauraceaeRelated: The family’s present southern-hemisphere lineages invite comparison with Gondwanan biogeography.

• PalaeognathaeRelated: The southern distribution of many palaeognaths inspired hypotheses tying their history to Gondwana's breakup.

• PodocarpaceaeRelated: The family's distribution reflects the long biogeographic history of southern landmasses.

• Rheic OceanRelated: Gondwana formed the southern margin from which several Rheic-bound terranes departed.

• Southeast Indian RidgeRelated: The ridge’s plate boundary developed as Gondwana fragmented and its constituent plates separated.

• NothofagaceaeRelated: The distribution of southern beeches has long been linked to Gondwana's breakup.

• AbelisauridaeRelated: Abelisaurid fossils occur on several landmasses that were once part of Gondwana.

• Elephant birdRelated: The breakup of Gondwana once seemed to explain ratite distributions, but genetic findings complicate that account.

• MesosaurusRelated: Southern Africa and South America were joined within Gondwana when Mesosaurus lived.

• ProteaceaeRelated: The family's Southern Hemisphere distribution is often considered in light of Gondwanan history.

• RhynchocephaliaRelated: Gondwanan geography provides context for the order’s southern fossil and biogeographic history.

• SarcosuchusRelated: Fossils on both sides of the Atlantic reflect the connected southern landmass of Sarcosuchus's time.

• Tasmanian Wilderness World Heritage AreaRelated: The region’s fossil deposits preserve evidence of plants and animals linked to Gondwanan history.

• Araucaria araucanaRelated: The distribution of Araucariaceae reflects the family’s long history across former Gondwanan lands.

• AsteralesRelated: Southern Hemisphere distributions among some Asterales families invite comparison with Gondwanan history.

• MyrtaceaeRelated: The family’s distribution and history are often interpreted against the breakup of Gondwana.

• NothofagusRelated: The genus’s disjunct southern distribution is often discussed in relation to Gondwanan history.

• BaurusuchidaeRelated: Baurusuchid fossils occur in South America, part of Gondwana during their evolution.

• CarnotaurusRelated: Its fossil record belongs to the South American part of this former southern landmass.

• Continental fragmentRelated: The breakup of Gondwana produced many present-day continental fragments.

• KoolasuchusRelated: Koolasuchus lived in Australia while it remained part of the southern high-latitude world.

• MawsoniaRelated: Mawsonia fossils on both sides of the Atlantic inform reconstructions of Gondwanan connections.

• Okavango RiverRelated: The region’s deep geological history helped shape the broad southern African landscapes through which the river flows.

• Paleo-Tethys OceanRelated: Gondwana bordered the Paleo-Tethys to the south and supplied terranes that later moved north.

• BothriolepisRelated: Bothriolepis fossils occur across regions that were part of or near Gondwana.