Abelichnus

Abelichnus is an extinct ichnogenus of dinosaur footprint from the Candeleros Formation and the Rio Limay Formation. The type ichnospecies, Abelichnus astigerrae, was first discovered in Argentina in 1987 and was recorded as the biggest known dinosaur footprint ever discovered. "Abelichnus" probably grew to a size of 12.5-13 meters (41-42 ft) long. 
Description.
In 1999 Calvo suggested that some theropod trackways and isolated tracks (which he made the basis of the ichnotaxon "Abelichnus astigarrae" in 1991) belonged to "Giganotosaurus", based on their large size - these were discovered at Lake Ezequiel Ramos Mexia in 1987 by A. Delgado. The largest tracks are long with a pace of , and the smallest is long with a pace of . The tracks are tridactyl (three-toed) and have large and coarse digits, with prominent claw impressions. Impressions of the digits occupy most of the track-length, and one track has a thin heel. Though the tracks were found in a higher stratigraphic level than the main fossils of "Giganotosaurus", they were from the same strata as the "Giganotosaurus" tooth MUCPv-52 and some sauropod dinosaurs that are also known from the same strata as "Giganotosaurus".
Taxonomy.
Possible trackmakers of "Abelichnus" could have been "Abelisaurus" or "Carnotaurus", although according to Calvo (1999), "Giganotosaurus" was the track maker.