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Articles

Comparative analysis of Late Jurassic sauropod trackways from the Jura Mountains (NW Switzerland) and the central High Atlas Mountains (Morocco): implications for sauropod ichnotaxonomy

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Pages 109-133 | Received 02 Oct 2009, Accepted 22 Nov 2009, Published online: 19 Apr 2010
 

Abstract

Late Jurassic sauropod trackways from the Jura Mountains (NW Switzerland) and the central High Atlas Mountains (Morocco) are described and compared. Emphasis is put on track preservation and trackway configuration. The trackways are similar with respect to preservation and the pes and manus track outlines, but they show a large range of trackway configuration. Only one of the trackways reveals digit and claw impressions, and thus differences in trackway gauge and the position of pes and manus tracks are the most explicit characters for their distinction. The Late Jurassic to Early Cretaceous ichnotaxa Brontopodus, Parabrontopodus and Breviparopus are reviewed and a differential diagnosis is given for the trackways studied. The reference trackway of Breviparopus corresponds to one of the studied trackways of Morocco. Parabrontopodus and Breviparopus are considered to be both valid ichnotaxa, even though we recommend the latter to be formally erected based on better-preserved tracks than those currently exposed. The analysed trackways and ichnotaxa suggest that trackway configuration, notably trackway gauge (width), is not decisively influenced by extrinsic factors such as ontogenetic stage, locomotion speed and substrate properties. However, it cannot be excluded that it is related to other factors such as individual behaviour or even sexual dimorphism.

Acknowledgements

A part of this research was carried out during the PhD theses of DM and MB and therefore the Swiss National Science Foundation (grant no. 20-109214.05) and the Università degli Studi di Padova, respectively, are acknowledged. We thank all the authorities of the Demnat region, from the community chief to the governor of the Azilal Province, for permissions for the fieldwork. We also warmly thank the AESVT of Demnat, especially M. Chaouki and M. Essoufi, and to Simohamed Benhimou from Taghbalout, for support with the logistics and contact with the local authorities and people. N.-E. Jalil (University Cadi Ayyad, Marrakech) is thanked for the organisation of the field trips, the relationships with the M'Goun Geopark direction and the invitation to contribute to this special volume. S. Ishigaki (Hayashibara Museum of Natural Sciences, Okayama) is thanked for kindly sharing his huge amount of unpublished sketches of the Iouaridène tracksites. G. Dyke and N.-E. Jalil are thanked for editorial work and for accepting us to contribute to this special volume on north African vertebrate paleontology.

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