Tracking late jurassic ornithopods in the lusitanian basin of Portugal : Ichnotaxonomic implications
Castanera, Diego (Institut Català de Paleontologia Miquel Crusafont)
Silva, Bruno C. (University of Opole. Institute of Biology. Laboratory of Paleobiology)
dos Santos, Vanda Faria (Universidade de Lisboa. Instituto Dom Luiz)
Malafaia, Elisabete (Universidad Nacional de Educación a Distancia (Espanya). Grupo de Biología Evolutiva)
Belvedere, Matteo (Bournemouth University. Institute for Studies in Landscape and Human Evolution)

Data:	2020
Resum:	The Sociedade de História Natural in Torres Vedras, Portugal houses an extensive collection of as yet undescribed dinosaur tracks with ornithopod affinities. They have been collected from different Late Jurassic (Kimmeridgian-Tithonian) geological formations (Praia de Amoreira-Porto Novo, Alcobaça, Sobral, and Freixial) that outcrop along the Portuguese coast, and belong to two different sub-basins of the Lusitanian Basin (the Consolação and Turcifal sub-basins). Three main morphotypes can be distinguished on the basis of size, mesaxony and the morphology of the metatarsophalangeal pad impression. The minute to small-sized morphotype is similar to the Anomoepus-like tracks identified in other Late Jurassic areas. The small to medium-sized morphotype resembles the Late Jurassic-Early Cretaceous ichnotaxon Dinehichnus, already known in the Lusitanian Basin. Interestingly, these two morphotypes can be distinguished qualitatively (slightly different size, metatarsophalangeal pad impression and digit morphology) but are nevertheless difficult to discriminate by quantitatively analysing their length-width ratio and mesaxony. The third morphotype is considered a large ornithopod footprint belonging to the ichnofamily Iguanodontipodidae. This ichnofamily is typical for Cretaceous tracksites but the new material suggests that it might also be present in the Late Jurassic. The three morphotypes show a negative correlation between size and mesaxony, so the smaller tracks show the stronger mesaxony, and the larger ones weaker mesaxony. The Upper Jurassic ornithopod record from the Lusitanian Basin has yielded both small and medium-sized ornithopod remains, mainly iguanodontians such as dryosaurids and ankylopollexians, which are the main candidates to be the trackmakers.
Ajuts:	Agència de Gestió d'Ajuts Universitaris i de Recerca 2017/BP-00195
Drets:	Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, fins i tot amb finalitats comercials, sempre i quan es reconegui l'autoria de l'obra original.
Llengua:	Anglès
Document:	Article ; recerca ; Versió publicada
Matèria:	Iguanodontipodidae ; Dinehichnus ; Anomoepus-like ; Kimmeridgian ; Tithonian ; Europe
Publicat a:	Acta Palaeontologica Polonica, Vol. 65, Issue 2 (2020) , p. 399-412, ISSN 1732-2421

DOI: 10.4202/APP.00707.2019

Full Text 14 p, 1.2 MB

Supplementary File 2 p, 171.7 KB

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