Lystrosaurus and Gondwanaland

  • Edwin H. Colbert


Gondwanaland, that hypothetical supercontinent composed of what are now the continents of Africa, South America, Australia, and Antarctica, and the subcontinent of peninsular India, has been the subject of much lively discussion among geologists, paleontologists, and biologists for more than half a century. Likewise, the inferred phenomenon of continental drift, involving the rifting of Gondwanaland into several large fragments, which are the continents listed above, and the subsequent drifting of those continental blocks to the positions they now occupy, has likewise occupied the attention of many interested authorities, as well as other people, through the past six decades. (It might be added that there has also been a correlative concept of Laurasia, a superconti-nent of what are now the northern hemisphere land masses, with its rifting, and the drifting of its several parts to their present positions. Furthermore, many authorities have envisaged a still larger land mass, Pangaea, embracing both Gondwanaland and Laurasia.) According to most students of the problem, Gondwanaland and Laurasia (or Pangaea) are supposed to have existed during at least the latter part of the Paleozoic and the beginning of the Mesozoic eras, the rifting and drifting having taken place at some time subsequent to the middle or final stages of Triassic history.


Lower Triassic Continental Drift Transantarctic Mountain Raniganj Coal Field Panamanian Isthmus 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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  1. Barrett, P. J. 1971. Stratigraphy and palaeogeography of the Beacon Supergroup in the Transantartic Mountains, Antarctica. Proc. 2nd Gondwana Symposium, South Africa (in press).Google Scholar
  2. Barrett, P. J., R. J. Baillie, and E. H. Colbert. 1968. Triassic amphibian from Antractica. Science, 161:460–462.PubMedCrossRefGoogle Scholar
  3. Bonaparte, J. F. 1966. Chronological survey of the tetrapod-bearing Triassic of Argentina. Breviora (Mus. Comp. Zool.), no. 251:1–13.Google Scholar
  4. Breviora 1967. New vertebrate evidence for a southern transatlantic connexion during the lower or middle Triassic. Palaeont., 10(4):554–563.Google Scholar
  5. Brink, A. S. 1951. On the genus Lystrosaurus Cope. Trans. Roy. Soc. S. Afr., 33(1): 107–120.CrossRefGoogle Scholar
  6. Brink, A. S. 1954. A bibliographical list of reptilia from the Karroo beds of Africa. Palaeont. Afr., 2:1–187.Google Scholar
  7. Brink, A. S. 1959. Note on a new skeleton of Thrinaxodon liorhinus. Palaeont. Afr., 6:15–22.Google Scholar
  8. Bullard, E. 1969. The origin of the oceans. Sci. Amer., 221:66–75.CrossRefGoogle Scholar
  9. Chowdhury, T. R. 1970. Two new dicynodonts from the Triassic Yerrapalli formation of central India. Palaeont., 13(1): 132–144.Google Scholar
  10. Colbert, E. H. 1970. Paleontological investigations at Coalsack Bluff. Antarct. J. U. S., 5:86.Google Scholar
  11. Cox, C. B. 1967. Changes in terrestrial vertebrate faunas during the Mesozoic. The Fossil Record, Geol. Soc, London, p. 77–89.Google Scholar
  12. Crompton, A. W. 1970. Continental drift and a strange fossil reptile. Discovery, 5(2): 105–108.Google Scholar
  13. Darlington, P. J. 1965. Biogeography of the Southern End of the World. Cambridge, Mass., Harvard University Press.Google Scholar
  14. Dietz, R. S. and J. C. Holden. 1970. The breakup of Pangaea. Sci. Amer., 223(4):30–41.CrossRefGoogle Scholar
  15. Dietz, R. S. and W. P. Sproll. 1970. Fit between Africa and Antarctica: a continental drift reconstruction. Science, 167:1612–1614.PubMedCrossRefGoogle Scholar
  16. Du Toit, A. L. 1937. Our Wandering Continents. Edinburgh, Oliver and Boyd.Google Scholar
  17. Du Toit, 1954. Geology of South Africa, 3rd ed., Chaps. 12 and 13, pp. 264–359. Edinburgh, Oliver and Boyd.Google Scholar
  18. Elliot, D. H., E. H. Colbert, W.J. Breed, J. A. Jensen, and J. S. Powell. 1970. Triassic tetrapods from Antarctica: evidence for continental drift. Science, 169:1197–1201.PubMedCrossRefGoogle Scholar
  19. Elliot, D. H., E. H. Colbert, W.J. Breed, J. A. Jensen, and J. S. Powell1971. Antarctic geology and drift reconstructions (in press).Google Scholar
  20. Hallam, A. 1967. The bearing of certain paleozoogeographic data on continental drift. Palaeogeogr. Palaeoclimatol. Palaeoecol., no. 3:201–241.CrossRefGoogle Scholar
  21. Haughton, S. H. 1969. Geological History of South Africa. Capetown, Geological Society of South Africa.Google Scholar
  22. Heirtzler, J. R. 1968. Sea-floor spreading. Sci. Amer., 219(6):60–70.CrossRefGoogle Scholar
  23. Huene, F. von. 1940. Die saurier der Karroo-, Gondwana- und verwandten Ablagerungen in Faunistischer, biologischer und phylogenetischer Hinsicht. N. Jahrb. Mineral. Geol. Paläont., Beil.-Bd., 83 Abt. B:246–347.Google Scholar
  24. Hurley, P. M. 1968. The confirmation of continental drift. Sci. Amer., 218(4):53–64.CrossRefGoogle Scholar
  25. King, L. C. 1965. Geological relationships between South Africa and Antarctica. Geol. Soc. S. Afr. Annex, 68:1–32.Google Scholar
  26. Kitching, J. W. 1968. On the Lystrosaurus zone and its fauna with special reference to some immature Lystrosauridae. Palaeont. Afr., 11:61–76.Google Scholar
  27. Matthew, W. D. 1915. Climate and evolution. Ann. N. Y. Acad. Sci., 24:178–318.Google Scholar
  28. Plumstead, E. P. 1962. Fossil floras of Antarctica. Trans. Antarct. Exped., Scientific Reports, no. 9:1–154.Google Scholar
  29. Robinson, P. L. 1958. Some new vertebrate fossils from the Panchet series of West Bengal. Nature (London). 182:1722–1723.CrossRefGoogle Scholar
  30. Robinson, P. L.1967. The Indian Gondwana formations—a review. First Symposium on Gondwana Stratigraphy, pp. 202–268.Google Scholar
  31. Romer, A. S. 1945. Vertebrate Paleontology. Chicago, University of Chicago Press.Google Scholar
  32. Romer, A. S.1968. Fossils and Gondwanaland. Proc. Amer. Philos. Soc, 112(5):335–343.Google Scholar
  33. Schopf, J. M. 1970. Gondwana Paleobotany. Antarct. J. U. S., 5(3):62–66.Google Scholar
  34. Simpson, G. G. 1940. Mammals and land bridges. J. Washington Acad. Sci., 30(4): 137–162.Google Scholar
  35. Simpson, G. G. 1947. Holarctic mammalian faunas and continental relationships during the Cenozoic. Bull. Geol. Soc. Amer., 58:613–688.CrossRefGoogle Scholar
  36. Simpson, G. G. 1953. Evolution and geography. Condon Lectures, Oregon State System of Higher Education, pp. 1–64.Google Scholar
  37. Smith, A. G., and A. Hallam. 1970. The fit of the southern continents. Nature (London), 225:139–144.CrossRefGoogle Scholar
  38. Sproll, W. P., and R. S. Dietz. 1969. Morphological continental drift fit of Australia and Antarctica. Nature (London), 222:345–348.CrossRefGoogle Scholar
  39. Tripathi, C., and P. P. Satsangi. 1963. Lystrosaurus fauna from the Panchet Series of the Raniganj Coalfields. Palaeont. Indica, (N. S.) 37:1–53.Google Scholar
  40. Wegener, Alfred. 1966. The Origin of Continents and Oceans. New York, Dover Press. (Translated from the 4th revised German edition by John Biram).Google Scholar
  41. Young, Chung-Chien. 1935. On two skeletons of Dicynodontia from Sinkiang. Bull. Geol. Soc. China, 14(4):483–517.CrossRefGoogle Scholar
  42. Young, Chung-Chien.1957. The significance of the lower Triassic reptilian fauna from Wuhsiang of Shansi. Sci. Rec., 1(4):265–270.Google Scholar

Copyright information

© Meredith Corporation 1972

Authors and Affiliations

  • Edwin H. Colbert
    • 1
  1. 1.The Museum of Northern ArizonaFlagstaffUSA

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