Late Carboniferous-Early Permian Tetrapod Ichnofauna from the Khenifra Basin, Central Morocco

Permian tetrapod footprints from the Spanish Pyrenees

“…This ichnotaxon is well known from many localities with Carboniferous and Permian tetrapod footprints in North America, Europe and Africa (Haubold, 1970(Haubold, , 1996Haubold and Sarjeant, 1973;Gand, 1988;Haubold et al, 1995;Lucas et al, 2005;Voigt et al, 2011aVoigt et al, , 2011bMarchetti et al, 2013). B. salamandroides from the Early Permian of the Czech Republic is the first available ichnospecies of Batrachichnus (Geinitz, 1861;Haubold, 1996).…”

“…Because of the observed difference in manual digit proportions and the remarkable differences in track size we suggest a separation of Batrachichnus and Limnopus from the Peranera Formation. However, it should be stated that the ichnotaxonomic separation of Batrachichnus and Limnopus has been a long lasting and not yet readily resolved issue (Haubold, 1996;Tucker and Smith, 2004;Voigt et al, 2011aVoigt et al, , 2011b.…”

The Gerola Valley site (Orobic Basin, Northern Italy): A key for understanding late Early Permian tetrapod ichnofaunas

“…Since an ichnospecific differentiation was never adequately proposed, we refer to the first named species, Dromopus lacertoides (Geinitz, 1861). It is widely distributed; the material classifiable as D. lacertoides comes from the Permian of Germany (Haubold, 1996;Voigt, 2005), Poland , France (Gand and Haubold, 1984;Gand, 1987), Spain (Voigt and Haubold, 2015), Morocco (Voigt et al, 2011a(Voigt et al, , 2011bHminna et al, 2012), the USA (Haubold et al, 1995;Lucas et al, 2011) andCanada (Van Allen et al, 2005). The trackmakers were probably araeoscelids (Haubold, 1971;Voigt, 2005).…”

A revision of tetrapod footprints from the late Carboniferous of the West Midlands, UK

“…They are also known from the USA (Lucas et al, 2011; Lucas & Dalman, 2013), Canada (Van Allen, Calder & Hunt, 2005), Argentina (Hunt & Lucas, 1998) and Morocco (Voigt et al, 2011a; Voigt et al, 2011b). They appear to range from the middle Moscovian to the middle Kungurian (Tucker & Smith, 2004; Voigt & Lucas, 2015).…”