Home > Articles > Published articles > Intra-trackway morphological variations due to substrate consistency: the el frontal dinosaur tracksite (lower Cretaceous, Spain) |
Date: | 2014 |
Abstract: | An ichnological and sedimentological study of the El Frontal dinosaur tracksite (Early Cretaceous, Cameros basin, Soria, Spain) highlights the pronounced intra-trackway variation found in track morphologies of four theropod trackways. Photogrammetric 3D digital models revealed various and distinct intra-trackway morphotypes, which reflect changes in footprint parameters such as the pace length, the track length, depth, and height of displacement rims. Sedimentological analyses suggest that the original substrate was non-homogenous due to lateral changes in adjoining microfacies. Multidata analyses indicate that morphological differences in these deep and shallow tracks represent a part of a continuum of track morphologies and geometries produced by a gradient of substrate consistencies across the site. This implies that the large range of track morphologies at this site resulted from similar trackmakers crossing variable facies. The trackways at the El Frontal site present an exemplary case of how track morphology, and consequently potential ichnotaxa, can vary, even when produced by a single trackmaker. |
Grants: | Ministerio de Economía y Competitividad CGL2011/30069-C02-01 Ministerio de Economía y Competitividad CGL2010/16447 Ministerio de Economía y Competitividad BES2012-051847 Ministerio de Ciencia e Innovación JDC-2011 Ministerio de Educación y Ciencia AP2008-01340 |
Rights: | 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. |
Language: | Anglès |
Document: | Article ; recerca ; Versió publicada |
Published in: | PloS one, Vol. 9, Issue 4 (April 2014) , art. e0093708, ISSN 1932-6203 |
14 p, 10.0 MB |