The holotype was first discovered and collected in 2002 during the field expedition conducted by the Mongolian Academy of Sciences and the American Museum of Natural History, the specimen only preserved a partial left dentary. It was discovered on the outcrops at the Tsagan Tsonj locality in the Bayan Shireh Formation,[1] the age is estimated to be around 102 million to 86 million years ago, between the Cenomanian and Santonianstages of the Late Cretaceous epoch.[2] The generic name, Tsagandelta, is derived from the Mongolianцагаан (tsagaan, meaning white) and the Greekδέλτᾰ (delta, meaning crest or point-shaped) in reference to the withish sediments at the Tsagan Tsonj locality and the prominent dentition of the Deltatheroida. The specific name, dashzevegi, is in honor to the Mongolian paleontologist Demberlyin Dashzeveg who did notable research on early mammals.[1]
Description
Tsagandelta is currently known from one specimen, the holotypePSS-MAE 629. This specimen is composed of a left dentary fragment containing an almost intact second molar, the base of the third molar and the roots of the first premolar; various other tooth sockets are empty, and the dental formula is probably similar to that of Deltatheridium.[1] Based on comparisons with the related Lotheridium, the preserved dentary indicates that Tsagandelta was slightly smaller than the former; Lotheridium is about the size of a modern marten.[3]
Classification
Tsagandelta was classified within the Deltatheridiidae, being more derived than Sulestes and Oklatheridium but less so than the rest of the family. This phylogenetic position has been argued to suggest an Asian origin for Deltatheroida.[1]
Paleobiology
Like most deltatheroideans, Tsagandelta was a carnivore, its molar anatomy similar to the carnassials of other carnivorous therians. Tsagandelta and its relatives (as well as the unrelated eutriconodonts) are among the Mesozoic mammals most clearly specialised to meat-eating.[1][3]
Paleoecology
Tsagandelta hails from the Bayan Shireh Formation, dating from the Cenomanian to the Santonian.[1][2] It is adjacent to the Iren Dabasu Formation, these formations bear a very similar fauna.[4] A great diversity of reptiles are known from the Bayan Shireh Formation, mainly compromising dinosaur and non-dinosaur taxa that likely preyed on Tsagandelta, mammals however, are pooly known from this formation.[5][6][7][8]
^Tsuihiji, T.; Watabe, M.; Barsbold, R.; Tsogtbaatar, K. (2015). "A gigantic caenagnathid oviraptorosaurian (Dinosauria: Theropoda) from the Upper Cretaceous of the Gobi Desert, Mongolia". Cretaceous Research. 56: 60–65. Bibcode:2015CrRes..56...60T. doi:10.1016/j.cretres.2015.03.007.
^Park, J. Y.; Lee, Y. N.; Currie, P. J.; Kobayashi, Y.; Koppelhus, E.; Barsbold, R.; Mateus, O.; Lee, S.; Kim, S. H. (2019). "Additional skulls of Talarurus plicatospineus (Dinosauria: Ankylosauridae) and implications for paleobiogeography and paleoecology of armored dinosaurs". Cretaceous Research. 108: 104340. doi:10.1016/j.cretres.2019.104340. S2CID212423361.
^Lee, Y. M.; Lee, H. J.; Kobayashi, Y.; Carabajal, A. P.; Barsbold, R.; Fiorillo, A. R.; Tsogtbaatar, K. (2019). "Unusual locomotion behaviour preserved within a crocodyliform trackway from the Upper Cretaceous Bayanshiree Formation of Mongolia and its palaeobiological implications". Palaeogeography, Palaeoclimatology, Palaeoecology. 533 (109353): 2. Bibcode:2019PPP...53309239L. doi:10.1016/j.palaeo.2019.109239. S2CID197584839.