A new dinosaur tracksite with small footprints in the Urbión Group (Cameros Basin, Lower Cretaceous, La Rioja, Spain)

  1. Díaz Martínez, Ignacio 1
  2. García Ortiz de Landaluce, Esperanza
  3. Pérez Lorente, Félix 2
  1. 1 Universidad de La Rioja, c/Madre de Dios 51-53, Logroño La Rioja, Spain, CONICET, Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, c/ General Roca 1242, Fisque Menuco-General Roca Río Negro, Argentina
  2. 2 Universidad de La Rioja
    info

    Universidad de La Rioja

    Logroño, España

    ROR https://ror.org/0553yr311

Revue:
Journal of iberian geology: an international publication of earth sciences

ISSN: 1886-7995 1698-6180

Année de publication: 2015

Titre de la publication: Dinosaur palaeontology and environment

Volumen: 41

Número: 1

Pages: 167-175

Type: Article

DOI: 10.5209/REV_JIGE.2015.V41.N1.48661 DIALNET GOOGLE SCHOLAR lock_openAccès ouvert editor

D'autres publications dans: Journal of iberian geology: an international publication of earth sciences

Dépôt institutionnel: lock_openAccès ouvert Editor

Résumé

A new dinosaur tracksite (La Rueda) with ten small tridactyl footprints (the length ranges between 9 and 15 cm) from the Urbión Group (Cameros Basin, Lower Cretaceous, La Rioja, Spain) is described. The footprints are approximately as long as wide and have high divarication angles between digits II-IV (~80º), some pad impressions on each digit, claw marks, a medial notch and a circular heel pad impression. They are here classified as indeterminate ornithopod footprints and contribute to the increase in the dinosaur ichnodiversity of the Urbión Group. Small dinosaur footprints are scarce in the worldwide fossil record. In the Urbión Group, large dinosaur tracks are much more frequent than small ones. This scarcity could be explained as ecological biases (dearth of small individuals in an area). Nevertheless, the number of small footprints in the Urbión Group is instead the product of by preservation biases (coarse grain sediments and fluvial erosive bases) and the weathering and erosion processes (brittle nature of the rock) that affect especially to small tracks than large ones identified in this Group