Macropodosaurus
Macropodosaurus is an ichnogenus of therizinosaurid footprints from the Late Cretaceous of Asia, North America and Poland. The ichnogenus is currently monotypic only including the type ichnospecies M. gravis, described and named in 1964. When first described, "Macropodosaurus" tracks were inferred to have been made by a bipedal, yet indeterminate type of dinosaur. In 2006 it was re-evaluated and concluded to represent footprints of therizinosaurid dinosaurs based on comparisons with skeletal feet remains. History of discovery. In 1963, Russian geologist F.H. Khakimov discovered unusual bipedal trackways at the Shirkent-1 locality of the Shirabad Formation in the Shirkent River  valley (Tajikistan). The material consisted of a series of four-toed footprints found in Cenomanian slabs of hard clayey limestone. They later became the holotype material for the new ichnogenus and ichnospecies "Macropodosaurus gravis", described and named in 1964 by Sergey A. Zakharov. He stated that they were made by a bipedal four-toed dinosaur and not a quadrupedal animal. More later, in 2006 Andrey G. Sennikov re-examined these footprints and concluded that a therizinosaurid dinosaur likely made those tracks. He compared "Macropodosaurus" with the feet of "Erlikosaurus" and "Therizinosaurus" noting that in a plantigrade position they match the  morphology of the tracks. Sennikov considered these tracks to be more associated with therizinosaurids and proposed a plantigrade stance for them. In 2008 two "Macropodosaurus" tracks were discovered in sediments of the Ferron Formation, Utah, in a locality known as the Muddy Creek Canyon. Although these have been in knowledge since their discovery, in 2013 they were described by Gerard Gierlinski and Martin Lockley. "Macropodosaurus" has also been discovered in the Maastrichtian strata of Poland in 2007. This footprint is reminiscent of the tracks described by Zakharov and was assigned to "Macropodosaurus" sp. This discovery may indicate the ancient presence  of therizinosaurids in Europe. In 2017 Masrour with colleagues reported more "Macropodosaurus" footprints in what is now Morocco, further expanding the paleobiogeographical range of therizinosaurids. Sennikov re-analyzed "Macropodosaurus" and the overall foot anatomy of therizinosaurids, concluding that this group had a plantigrade stance. While ancestral therizinosaurs had a gracile and digitigrade stance, therizinosaurids evolved a robust, ponderous body plan and plantigradism. Description. "Macropodosaurus" tracks are relatively large, having average dimensions of long and wide. Individually, they are narrow/long, and have four distinct digits which are set closely together. Each digit ends in moderately pronounced claws. Long trackways are  narrow, running nearly parallel to each other at a distance of ~. Some "Macropodosaurus" tracks are reported with lengths of ~, but this was most likely caused by shifting movement of the animal in loose terrain. Molina-Pérez and Larramendi in 2016 proposed an animal around and for a long "Macropodosaurus" footprint.