Hadrosaur trackways from the Lower Cretaceous of Canada

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 wer...

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Bibliographic Details
Main Author: Currie, P. J.
Format: Other/Unknown Material
Language:English
Published: 1983
Subjects:
geo
Online Access:https://doi.org/10.7939/R3KK94G1T
https://era.library.ualberta.ca/items/485f400d-213e-44dc-b097-2a8bfe00837c
id fttriple:oai:gotriple.eu:10670/1.vcppu8
record_format openpolar
spelling fttriple:oai:gotriple.eu:10670/1.vcppu8 2023-05-15T17:54:49+02:00 Hadrosaur trackways from the Lower Cretaceous of Canada Currie, P. J. 1983-01-01 https://doi.org/10.7939/R3KK94G1T https://era.library.ualberta.ca/items/485f400d-213e-44dc-b097-2a8bfe00837c en eng doi:10.7939/R3KK94G1T 10670/1.vcppu8 https://era.library.ualberta.ca/items/485f400d-213e-44dc-b097-2a8bfe00837c other ERA : Education and Research Archive geo archeo Other https://vocabularies.coar-repositories.org/resource_types/c_1843/ 1983 fttriple https://doi.org/10.7939/R3KK94G1T 2023-01-22T18:23:16Z 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 make 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. Other/Unknown Material Peace River Unknown Canada Peace River Canyon ENVELOPE(-122.120,-122.120,55.950,55.950)
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
archeo
spellingShingle geo
archeo
Currie, P. J.
Hadrosaur trackways from the Lower Cretaceous of Canada
topic_facet geo
archeo
description 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 make 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.
format Other/Unknown Material
author Currie, P. J.
author_facet Currie, P. J.
author_sort Currie, P. J.
title Hadrosaur trackways from the Lower Cretaceous of Canada
title_short Hadrosaur trackways from the Lower Cretaceous of Canada
title_full Hadrosaur trackways from the Lower Cretaceous of Canada
title_fullStr Hadrosaur trackways from the Lower Cretaceous of Canada
title_full_unstemmed Hadrosaur trackways from the Lower Cretaceous of Canada
title_sort hadrosaur trackways from the lower cretaceous of canada
publishDate 1983
url https://doi.org/10.7939/R3KK94G1T
https://era.library.ualberta.ca/items/485f400d-213e-44dc-b097-2a8bfe00837c
long_lat ENVELOPE(-122.120,-122.120,55.950,55.950)
geographic Canada
Peace River Canyon
geographic_facet Canada
Peace River Canyon
genre Peace River
genre_facet Peace River
op_source ERA : Education and Research Archive
op_relation doi:10.7939/R3KK94G1T
10670/1.vcppu8
https://era.library.ualberta.ca/items/485f400d-213e-44dc-b097-2a8bfe00837c
op_rights other
op_doi https://doi.org/10.7939/R3KK94G1T
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