catopsaloides - Synonyms for catopsaloides

Examples of "catopsaloides"
The species "Catopsbaatar catopsaloides" has also been known as "Catopsalis catopsaloides" and "Djadochtatherium catopsaloides" (Kielan-Jaworowska 1974). Fossil remains were found in the Campanian (Upper Cretaceous)-age strata of Hermiin Tsav (Khermeen Tsav) in Mongolia. This was originally regarded as a species of "Djadochtatherium". It also spent a while assigned to the North American genus "Catopsalis" (Cope 1882), courtesy of an interpretation in 1979 by Kielan-Jaworowska and Sloan. The original material consisted of three skulls, the most complete of which was juvenile. Subsequently, a fourth specimen was identified and then an even more complete example came to light in 1999, along with some postcranial skeleton. This belonged to an elderly animal. It has been provisionally considered by Kielan-Jaworowska but has yet to be fully described. With a skull length of around 6 cm, this was a pretty large multituberculate.
The region that is preserved in the Barun Goyot Formation was home to the maniraptoran "Hulsanpes perlei", the oviraptorids "Conchoraptor gracilis" and "Ajancingenia yanshini", the alvarezsaurids "Ceratonykus oculatus", "Mononykus" and "Parvicursor remotus", the pachycephalosaur "Tylocephale gilmorei", the ankylosaurs "Saichania chulsanensis" and "Tarchia gigantea", and the ceratopsians "Bagaceratops rozhdestvenskyi", "Breviceratops kozlowskii", "Lamaceratops tereschenkoi" and "Platyceratops tatarinovi". The largest dinosaur among them was the titanosaur "Quaesitosaurus orientalis". It was observed that many of the same genera were present at the Barun Goyot and Djadochta Formations, though there was variation at the species level. Vertebrates present in the Barun Goyot Formation included the primitive birds "Gobipteryx minuta" and "Hollanda luceria" and the lizards "Estesia mongoliensis", "Ovoo gurvel", "Proplatynotia longirostrata" and "Gobiderma pulchrum". The early mammals that were present in this region during the time of "Avimimus" were the placental mammals "Asioryctes nemegetensis" and "Barunlestes butleri", the amphibian "Gobiates khermeentsavi", the multituberculate mammals "Catopsbaatar catopsaloides", "Chulsanbaatar vulgaris" and "Nemegtbaatar gobiensis", and the marsupial mammal "Asiatherium reshetovi" and "Deltatheridium pretrituberculare". Numerous dinosaurs eggshells found in this region support the presence of sauropods and maniraptors.
"Conchoraptor" shared its paleoenvironment with the maniraptoran "Hulsanpes perlei", the oviraptorid "Ajancingenia yanshini", the avimimid "Avimimus", the alvarezsaurids "Ceratonykus oculatus", "Mononykus" and "Parvicursor remotus", the pachycephalosaur "Tylocephale gilmorei", the ankylosaurs "Saichania chulsanensis" and "Tarchia gigantea", and the ceratopsians "Bagaceratops rozhdestvenskyi", "Breviceratops kozlowskii", "Lamaceratops tereschenkoi" and "Platyceratops tatarinovi". The largest dinosaur among them was the titanosaur "Quaesitosaurus orientalis". It was observed that many of the same genera were present at the Barun Goyot and Djadochta Formations, though there was variation at the species level. Vertebrates present in the Barun Goyot Formation included the primitive birds "Gobipteryx minuta" and "Hollanda luceria" and the lizards "Estesia mongoliensis", "Ovoo gurvel", "Proplatynotia longirostrata" and "Gobiderma pulchrum". The early mammals that were present in this region during the time of "Conchoraptor" were the placental mammals "Asioryctes nemegetensis" and "Barunlestes butleri", the amphibian "Gobiates khermeentsavi", the multituberculate mammals "Catopsbaatar catopsaloides", "Chulsanbaatar vulgaris" and "Nemegtbaatar gobiensis", and the marsupial mammal "Asiatherium reshetovi" and "Deltatheridium pretrituberculare". Numerous dinosaurs eggshells found in this region support the presence of sauropods and maniraptors.