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1983 | 28 | 1-2 |

Tytuł artykułu

Hadrosaur trackways from the Lower Cretaceous of Canada

Autorzy

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
The most common ichnogenus in the Peace River Canyon is Amblydactylus, a large bipedal herbivore. The morphology of the hand and footprints suggest that the tracks and trackways were made by hadrosaurs, and the ichnites might represent the earliest record of these dinosaurs. Amblydactylus tracks were made in a wide variety of depositional environments, including the mud beneath several metres of water. Juveniles were gregarious and stayed together after hatching until they were large enough to join herds of more mature animals. Hadrosaur herds appear to have walked side by side, seldom crossing paths, although there was little structure to the herds when they were in the water and/or feeding. Calculation of the walking speeds indicate that the herbivores were generally slower than the carnivores.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

28

Numer

1-2

Opis fizyczny

p.63-73,fig.,ref.

Twórcy

autor
  • Tyrell Museum of Palaeontology, P.D.Box 7500, Drumheller, Alberta , TOJ OYO, Canada

Bibliografia

  • ALEXANDER, R. McN. 1976. Estimates of the speeds of dinosaurs. — Nature, 261, 129.
  • BECKLES, S. H. 1862. On some natural casts of reptilian footprints in the Wealden Beds of the Isle of Wight and Swanage. — Q. J. Geol. Soc., London, 18, 443—447.
  • BIRD, R. T. 1954. We captured a “live” Brontosaurus. — Nat. Geogr., 105 (5).
  • COOMBS, W. P. 1980. Swimming ability of carnivorous dinosaurs. — Science, 207, 1198—1199.
  • CURRIE, P. J. 1980. Palaeontological expedition to the Peace River Canyon, between Hudson’s Hope and the W. A. C. Bennett Dam, 1979. — Unpublished report to Heritage Conservation Branch, B. C. Provincial Government.
  • CURRIE, P. J. 1981. Bird footprints from the Gething Formation (Aptian, Lower Cretaceous) of northeastern British Columbia, Canada. — J. Vert. Paleont., 1, 3—4, 257—264.
  • CURRIE, P. J. and SARJEANT, W. A. S. 1979. Lower Cretaceous dinosaur footprints from the Peace River Canyon, British Columbia, Canada — Palaeogeogr., Palaeoclimatol., Palaeoecol., 28, 103—115.
  • DUTUIT, J. M. and OUAZZOU, A. 1980, Découverte d’une piste de Dinosaure Sauropode sur le site ďempreintes de Demnat (Haut-Atlas marocain). — Mém. Soc. Géol. France, N. S., 1980 (139), 95—102.
  • HITCHCOCK, E. 1858. Ichnology of New England, report on the sandstone of the Connecticut Valley, especially its fossil footmarks, 199 pp. W. White, Printer to the State, Boston.
  • KAYE, J. M. and RUSSELL, D. A. 1973. The oldest record of hadrosaurian dinosaurs in North America. — J. Paleont., 47, 91—93.
  • KOOL, R. 1981. The walking speed of dinosaurs from the Peace River Canyon, British Columbia, Canada. — Can. J. Earth Sci., 18, 823—825.
  • LANGSTON, W. 1960. A hadrosaurian ichnite. — Nat. Hist. Pap., Nat. Mus. Can., 4, 1—9.
  • McLEARN, F. H. 1923. Peace River Canyon coal area, B. C. — Geol. Survey Canada, Sum. Rept. 1922, pt. B, 1—46.
  • OSBORN, H. F. 1912. The integument of the iguanodont dinosaur Trachodon. — Am. Mus. Nat. Hist., Mem. 1, 33—54.
  • OSTROM, J. H. 1972. Were some dinosaurs gregarious? — Palaeogeogr., Palaeoclimatol., Palaeoecol., 11, 287—301.
  • RUSSELL, D. A. and BÉLAND, P. 1976. Running dinosaurs. — Nature, 264, 486.
  • STERNBERG, C. M. 1932. Dinosaur tracks from Peace River, British Columbia. — Nat. Mus. Can., Ann. Rep. 1930, 59—85.
  • STOTT, D. F. 1975. The Cretaceous system in northeastern B. C. — Geol. Assoc. Can., Spec. Pap. 13, 441—467.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

bwmeta1.element.agro-07836419-61e9-45a9-aca5-4eb66a16484c
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