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Great American Interchange information


Examples of migrant species in both Americas. Olive green silhouettes denote North American species with South American ancestors; blue silhouettes denote South American species with North American ancestors.

The Great American Biotic Interchange (commonly abbreviated as GABI), also known as the Great American Interchange and the Great American Faunal Interchange, was an important late Cenozoic paleozoogeographic biotic interchange event in which land and freshwater fauna migrated from North America to South America via Central America and vice versa, as the volcanic Isthmus of Panama rose up from the sea floor and bridged the formerly separated continents. Although earlier dispersals had occurred, probably over water, the migration accelerated dramatically about 2.7 million years (Ma) ago during the Piacenzian age.[1] It resulted in the joining of the Neotropic (roughly South American) and Nearctic (roughly North American) biogeographic realms definitively to form the Americas. The interchange is visible from observation of both biostratigraphy and nature (neontology). Its most dramatic effect is on the zoogeography of mammals, but it also gave an opportunity for reptiles, amphibians, arthropods, weak-flying or flightless birds, and even freshwater fish to migrate. Coastal and marine biota, however, were affected in the opposite manner; the formation of the Central American Isthmus caused what has been termed the Great American Schism, with significant diversification and extinction occurring as a result of the isolation of the Caribbean from the Pacific.[2]

The occurrence of the interchange was first discussed in 1876 by the "father of biogeography", Alfred Russel Wallace.[3][4] Wallace had spent five years exploring and collecting specimens in the Amazon basin. Others who made significant contributions to understanding the event in the century that followed include Florentino Ameghino, W. D. Matthew, W. B. Scott, Bryan Patterson, George Gaylord Simpson and S. David Webb.[5] The Pliocene timing of the formation of the connection between North and South America was discussed in 1910 by Henry Fairfield Osborn.[6]

Analogous interchanges occurred earlier in the Cenozoic, when the formerly isolated land masses of India and Africa made contact with Eurasia about 56 and 30 Ma ago, respectively.[7][8][9][10][11][12][13][14][15][16][17][excessive citations]

  1. ^ O'Dea, A.; Lessios, H. A.; Coates, A. G.; et al. (2016). "Formation of the Isthmus of Panama". Science Advances. 2 (8): e1600883. Bibcode:2016SciA....2E0883O. doi:10.1126/sciadv.1600883. PMC 4988774. PMID 27540590.
  2. ^ Cite error: The named reference Lessios was invoked but never defined (see the help page).
  3. ^ Wallace, Alfred Russel (1876). The Geographical Distribution of Animals. With a Study of the Relations of Living and Extinct Faunas as Elucidating the Past Changes of the Earth's Surface. Vol. 1. New York: Harper and Brothers. OCLC 556393.
  4. ^ Wallace, Alfred Russel (1876). Ibid.. Vol. 2. New York: Harper and Brothers. OCLC 556393.
  5. ^ Marshall, L. G. (July–August 1988). "Land Mammals and the Great American Interchange" (PDF). American Scientist. 76 (4): 380–388. Bibcode:1988AmSci..76..380M. Archived (PDF) from the original on 2013-03-02. Retrieved 2014-04-22.
  6. ^ Osborn, H. (1910). The Age Of Mammals In Europe, Asia, And North America. New York, EEUU: The Macmillan Company. pp. 80–81.
  7. ^ Karanth, K. Praveen (2006-03-25). "Out-of-India Gondwanan origin of some tropical Asian biota" (PDF). Current Science. 90 (6): 789–792. Retrieved 2008-12-29.
  8. ^ Clementz, Mark; Bajpai, S.; Ravikant, V.; Thewissen, J. G. M.; Saravanan, N.; Singh, I. B.; Prasad, V. (1 January 2011). "Early Eocene warming events and the timing of terrestrial faunal exchange between India and Asia". Geology. 39 (1): 15–18. Bibcode:2011Geo....39...15C. doi:10.1130/G31585.1. Retrieved 28 August 2022.
  9. ^ Rose, Kenneth D.; Rana, Rajendra S.; Sahni, Ashok; Kumar, Kishor; Singh, Lachham; Smith, Thierry (1 June 2009). "First Tillodont from India: Additional Evidence for an Early Eocene Faunal Connection between Europe and India?". Acta Palaeontologica Polonica. 54 (2): 351–355. doi:10.4202/app.2008.0067. S2CID 129644411.
  10. ^ Das, Debasis P.; Carolin, Nora; Bajpai, Sunil (22 Aug 2021). "A nyctitheriid insectivore (Eulipotyphla, Mammalia) of Asian affinity from the early Eocene of India". Historical Biology. 34 (7): 1157–1165. doi:10.1080/08912963.2021.1966002. S2CID 238735010. Retrieved 28 August 2022.
  11. ^ Rana, Rajendra S.; Kumar, Kishor; Escarguel, Gilles; Sahni, Ashok; Rose, Kenneth D.; Smith, Thierry; Singh, Hukam; Singh, Lachham (1 March 2008). "An Ailuravine Rodent from the Lower Eocene Cambay Formation at Vastan, Western India, and Its Palaeobiogeographic Implications". Acta Palaeontologica Polonica. 53 (1): 1–14. doi:10.4202/app.2008.0101. S2CID 56382943.
  12. ^ Li, Fengyuan; Shao, Lili; Li, Shuqiang (3 February 2020). "Tropical Niche Conservatism Explains the Eocene Migration from India to Southeast Asia in Ochyroceratid Spiders". Systematic Biology. 69 (5): 987–998. doi:10.1093/sysbio/syaa006. PMID 32011715. Retrieved 28 August 2022.
  13. ^ Ali, Jason R.; Aitchison, Jonathan C. (June 2008). "Gondwana to Asia: Plate tectonics, paleogeography and the biological connectivity of the Indian sub-continent from the Middle Jurassic through latest Eocene (166–35 Ma)". Earth-Science Reviews. 88 (3–4): 145–166. Bibcode:2008ESRv...88..145A. doi:10.1016/j.earscirev.2008.01.007. Retrieved 28 August 2022.
  14. ^ Dutta, Suryendu; Tripathi, Suryakant M.; Mallick, Monalisa; Mathews, Runcie P.; Greenwood, Paul F.; Rao, Mulagalapalli R.; Summons, Roger E. (July 2011). "Eocene out-of-India dispersal of Asian dipterocarps". Review of Palaeobotany and Palynology. 166 (1–2): 63–68. Bibcode:2011RPaPa.166...63D. doi:10.1016/j.revpalbo.2011.05.002. Retrieved 28 August 2022.
  15. ^ Kapur, Vivesh V.; Carolin, N.; Bajpai, S. (2022). "Early Paleogene mammal faunas of India: a review of recent advances with implications for the timing of initial India-Asia contact". Himalayan Geology. 47 (1B): 337–356. Retrieved 28 August 2022.
  16. ^ Hedges, S. Blair (2001-01-02). "Afrotheria: Plate tectonics meets genomics". Proceedings of the National Academy of Sciences. 98 (1): 1–2. Bibcode:2001PNAS...98....1H. doi:10.1073/pnas.98.1.1. PMC 33345. PMID 11136239.
  17. ^ Kappelman, John; Rasmussen, D. Tab; Sanders, William J.; Feseha, Mulugeta; Bown, Thomas; Copeland, Peter; Crabaugh, Jeff; Fleagle, John; Glantz, Michelle; Gordon, Adam; Jacobs, Bonnie; Maga, Murat; Muldoon, Kathleen; Pan, Aaron; Pyne, Lydia; Richmond, Brian; Ryan, Timothy; Seiffert, Erik R.; Sen, Sevket; Todd, Lawrence; Wiemann, Michael C.; Winkler, Alisa C. (4 December 2003). "Oligocene mammals from Ethiopia and faunal exchange between Afro-Arabia and Eurasia". Nature. 426 (6966): 549–552. Bibcode:2003Natur.426..549K. doi:10.1038/nature02102. hdl:2027.42/62496. PMID 14654838. S2CID 4336007. Retrieved 28 August 2022.

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Great American Interchange

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it is the only one known from North America, crossing over from South America during the Great American Interchange. The earliest discovery of Titanis...

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Tapir

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Interchange

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Look up interchange in Wiktionary, the free dictionary. Interchange may refer to: Interchange (road), a collection of ramps, exits, and entrances between...

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Central American Seaway

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submarine deposits in Central America. The second is the Great American Interchange of vertebrates between North and South America which required a continuous...

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Great American

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North America Great American Insurance Group and Great American Financial Resources, divisions of American Financial Group Great American Interchange, a...

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Llama

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camelids to spread to South America as part of the Great American Interchange, where they evolved further. Meanwhile, North American camelids died out at the...

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Peccary

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in North America during the Miocene and migrated into South America during the Pliocene–Pleistocene as part of the Great American Interchange. They are...

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Phorusrhacidae

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in North America. This makes the phorusrhacids the only known large South American predator to migrate north in the Great American Interchange that followed...

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Cingulata

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to migrate to southern North America during the Pliocene or early Pleistocene as part of the Great American Interchange. After surviving for tens of millions...

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Tremarctinae

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Americas. The group is thought to have originated in eastern North America, and then invaded South America as part of the Great American Interchange....

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Xenarthra

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3 million years ago, spread to Central and North America as part of the Great American Interchange. Nearly all of the formerly abundant megafaunal xenarthrans...

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North American porcupine

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Brazil 30 million years ago, and then migrated to North America during the Great American Interchange after the Isthmus of Panama rose 3 million years ago...

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Human migration Great Upheaval Early human migrations Pre-modern human migration Indo-European migrations Great American Interchange This disambiguation...

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Procyonidae

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Central America (where their diversity is greatest); they entered the formerly isolated South America as part of the Great American Interchange, beginning...

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Gomphothere

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North America during the Miocene and Pliocene epochs and dispersed into South America during the Pleistocene as part of the Great American Interchange. Gomphotheres...

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Doedicurus

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Panama allowed North American fauna to invade South America in the Great American Interchange, including big cats, bears, proboscideans, camelids, and horses...

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Arctotherium

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endemic to Central and South America. Arctotherium migrated from North America to South America during the Great American Interchange, following the formation...

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Shrew

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New Zealand, and South America have no native shrews. However, as a result of the Great American Interchange, South America does have a relatively recently...

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Rodent

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years later. Rodents participated in the Great American Interchange that resulted from the joining of the Americas by formation of the Isthmus of Panama...

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Pampatheriidae

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Pleistocene after the formation of the Isthmus of Panama as part of the Great American Interchange. They became extinct as part of the end-Pleistocene extinctions...

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Pliocene

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South America became linked to North America through the Isthmus of Panama during the Pliocene, making possible the Great American Interchange and bringing...

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Geography of South America

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Isthmus of Panama some 3 million years ago, which resulted in the Great American Interchange. The Andes, likewise a comparatively young and seismically restless...

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Armadillo

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migrate northward into southern North America by the early Pleistocene, as part of the Great American Interchange. (Some of their much larger cingulate...

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