Stokesosaurus
Stokesosaurus (meaning "Stokes' lizard") is a genus of small (around in length), carnivorous early tyrannosauroid theropod dinosaurs from the late Jurassic period of Utah, United States. History. From 1960 onwards Utah geologist William Lee Stokes and his assistant James H. Madsen excavated thousands of disarticulated "Allosaurus" bones at the Cleveland-Lloyd Dinosaur Quarry in Emery County, Utah. During the early 1970s, Madsen began to catalogue these finds in detail, discovering that some remains represented species new to science. In 1974 Madsen named and described the type species "Stokesosaurus clevelandi". Its generic name honours Stokes. The specific name refers to  the town of Cleveland, Utah. The holotype (UMNH 2938, also known as UMNH VP 7473 and formerly known as UUVP 2938) was uncovered in the Brushy Basin Member of the Morrison Formation dating from the early Tithonian stage, about 150 million years old. It consists of a left ilium or hip bone, belonging to a juvenile individual. Madsen also assigned a paratype, UUVP 2320, a 50% larger right ilium. Additionally he referred a right premaxilla, UUVP 2999. However, this was in 2005 referred to "Tanycolagreus". "Stokesosaurus" and "Tanycolagreus" are about the same size, and it is possible that the latter  is a junior synonym of the former. However, the ilium (the best and perhaps only known element of "Stokesosaurus") of "Tanycolagreus" has never been recovered, making direct comparison difficult. In 1976 Peter Malcolm Galton considered "Stokesosaurus" to be a second species of the British possible early tyrannosauroid "Iliosuchus", that he named as "Iliosuchus clevelandi". This has found no acceptance among other researchers; in 1980 Galton himself withdrew his opinion. Some later finds were referred to "Stokesosaurus". This included some ischia and tail vertebrae in 1991, and a partial braincase in 1998. Another, very small ilium referred to "Stokesosaurus", found in  South Dakota, is lost but may actually belong to the related "Aviatyrannis". More fragmentary remains possibly referable to "Stokesosaurus" have been recovered from stratigraphic zone 2 of the Morrison Formation, dated to the late Kimmeridgian age, about 152 million years ago. A second species, "Stokesosaurus langhami", was described by Roger Benson in 2008 based on a partial skeleton from England. However, further study showed that this species should be referred to a new genus, which was named "Juratyrant" in 2012. Benson and Stephen Brusatte concluded that not a single bone had been justifiably referred to "Stokesosaurus", and that not even  the paratype could be safely assigned, leaving the holotype ilium as the only known fossil of the taxon. In addition, many traits initially believed to unite "Stokesosaurus clevelandi" and "Juratyrant langhami" under one genus could not be conclusively disproven to exist on other tyrannosauroids. In fact, one of the traits, a posterodorsally inclined ridge on the lateral side of the ilium, was found on the undescribed left ilium of the holotype of "Eotyrannus". This leaves only a single autapomorphy of "Stokesosaurus" which is not present in "Juratyrant" or other tyrannosauroids: a swollen rim around the articular surface of the pubic  peduncle. The holotype ilium is long, indicating a small individual. Madsen in 1974 estimated that the adult body length was about . In 2010, Gregory S. Paul estimated the length at and the weight at . Classification. In 1974 Madsen assigned "Stokesosaurus" to the Tyrannosauridae. However, modern cladistic analyses indicate a more basal position. In 2012 the study by Brusatte and Benson recovered "Stokesosaurus" as a basal member of the Tyrannosauroidea, and closely related to "Eotyrannus" and "Juratyrant". Below is a 2013 cladogram by Loewen "et al." that places "Stokesosaurus" and "Juratyrant" as derived members of Proceratosauridae, due to sharing with "Sinotyrannus  a narrow preacetabular notch. Many basal tyrannosauroids have incomplete or unknown ilia and this trait may be more widespread than currently known. Various traits support the argument that Sinotyrannus" is a proceratosaurid. However, a 2016 analysis utilizing both parsimonious and Bayesian phylogeny placed "Stokesosaurus" and "Juratyrant" as tyrannosauroids slightly more advanced than Proceratosauridae and "Dilong". In addition, "Eotyrannus" is recovered as a sister taxon of these genera in the parsimonious phylogeny. Paleoecology. Habitat. The Morrison Formation is a sequence of shallow marine and alluvial sediments which, according to radiometric dating, ranges between 156.3 million years old (Ma) at its base , to 146.8 million years old at the top, which places it in the late Oxfordian, Kimmeridgian, and early Tithonian stages of the Late Jurassic period. This formation is interpreted as a semiarid environment with distinct wet and dry seasons. The Morrison Basin where dinosaurs lived, stretched from New Mexico to Alberta and Saskatchewan, and was formed when the precursors to the Front Range of the Rocky Mountains started pushing up to the west. The deposits from their east-facing drainage basins were carried by streams and rivers and deposited in swampy lowlands, lakes, river channels and floodplains. This formation is  similar in age to the Solnhofen Limestone Formation in Germany and the Tendaguru Formation in Tanzania. In 1877 this formation became the center of the Bone Wars, a fossil-collecting rivalry between early paleontologists Othniel Charles Marsh and Edward Drinker Cope. Paleofauna. The Morrison Formation records an environment and time dominated by gigantic sauropod dinosaurs such as "Camarasaurus", "Barosaurus", "Diplodocus", "Apatosaurus" and "Brachiosaurus". Dinosaurs that lived alongside "Stokesosaurus" included the herbivorous ornithischians "Camptosaurus", "Dryosaurus", "Stegosaurus" and "Othnielosaurus". Predators in this paleoenvironment included the theropods "Saurophaganax", "Torvosaurus", "Ceratosaurus", "Marshosaurus", "Ornitholestes" and "Allosaurus", which accounted for 70 to 75% of theropod specimens  and was at the top trophic level of the Morrison food web. Other animals that shared this paleoenvironment included bivalves, snails, ray-finned fishes, frogs, salamanders, turtles, sphenodonts, lizards, terrestrial and aquatic crocodylomorphans, and several species of pterosaur. Examples of early mammals present in this region, were docodonts, multituberculates, symmetrodonts, and triconodonts. The flora of the period has been revealed by fossils of green algae, fungi, mosses, horsetails, cycads, ginkgoes, and several families of conifers. Vegetation varied from river-lining forests of tree ferns, and ferns (gallery forests), to fern savannas with occasional trees such as the "Araucaria"-like conifer "Brachyphyllum