Nemegt Formation

The Nemegt Formation is composed of mudstones and sandstones that were deposited by ancient lakes, streams, and flood plains. The Altan Uul locality was described by Michael Novacek as "a canyon carved out of a very rich series of sedimentary rocks" with "steep cliffs and narrow washes". The climate associated with it was wetter than when preceding formations were deposited; there seems to have existed at least some degree of forest cover as indicated by petrified fossil trunks. When examined, the rock facies of the upper section consist of braided meanders, and oxbow lakes. Alteration of sediment grades indicates frequent hydrodynamic condition changes (seasonal rain). Siltstone pellets indicate desiccation at the channel margins in river low-stand periods. Bank erosion features would form through river channel migration. Generally rivers consisted of low flow regimes with sporadic upper flow regimes indicated by exotic pebbles. The lower sections of the formation may represent lacustrine or palustrine deposition. A study of oxygen-18 isotopes from theropod teeth show seasonal patterns similar to present day continental climates. Mean annual temperatures are estimated to be around with seasonal precipitation patterns compared to meteorological data from Shijiazhuang, China; suggesting a monsoonal, cold semi-arid climate. The groundcover included quillwort like plants as well as sedges (members of the group Cyperaceae). reed grasses (primarily Phragmites) were present. The area also supported Bald Cypress. == Stratigraphy ==

The most recent stratigraphy divides the Nemegt Formation into three informal members. The lower member is dominated by fluvial deposits, while middle and upper members consist of alluvial plain, paludal, lacustrine, and fluvial deposits. The colour of the sediments is usually light grey to tan in colour in comparison to the typically red colour of the underlying Baruungoyot Formation. There has been no absolute dating of the Nemegt Formation. Historically the Nemegt has been considered late Campanian to Maastrichtian, based on comparisons of fossils present, but no exact dating has been performed. U-Pb dating from teeth of Tarbosaurus suggested that the deposition of the middle Nemegt Formation happened before 66.7 ± 2.5 Ma, during the Maastrichtian age, though whether the depositional age of the formation dates back to the late Campanian remains unresolved. While it has been generally assumed that the Djadochta, Baruungoyot, and Nemegt formations were layered in succession, some geological analysis suggested interfingering rather than superposition of these features. Thus these formations could represent different parts of a single interconnected ecosystem, with the Djadochta reflecting arid dune habitats dominated by small animals, the Baruungoyot representing transitional semi-arid zones, and the Nemegt capturing wetter river plains that supported large dinosaurs. ==Paleobiota of the Nemegt Formation==

Stratigraphic positions are based on Eberth (2018) who correlated localities to their approximate position within the formation. Flora Invertebrates Fish Amphibians Mammals Crocodylomorphs Pterosaurs Turtles Dinosaurs Ornithischians Ankylosaurs Hadrosaurs Pachycephalosaurs Sauropods Theropods Alvarezsaurs Birds Dromaeosaurs Ornithomimosaurs Oviraptorosaurs Therizinosaurs Troodontids Tyrannosaurs == See also ==