The Ulan Gochu Formation is a geologic formation in Inner Mongolia, northern China. The deposits of the Ulan Gochu Formation date to the late Middle Eocene or Late Eocene, and preserve fossils of a diverse, perissodactyl-dominated mammal fauna. The fossil fauna of the Ulan Gochu Formation is the type fauna of the Ulangochuian, one of the Asian land mammal ages (ALMAs).
Research history The deposits of the Ulan Gochu Formations are situated in the Erlian Basin, a structural basin located in central Inner Mongolia in northern China, close to the border between China and Mongolia. The first study on the Erlian Basin was published by the Russian geologist Vladimir Obruchev in 1892. It was later extensively studied by the Central Asiatic Expeditions of the American Museum of Natural History, over the course of five field seasons in the 1920s. The researchers of the Central Asiatic Expeditions were responsible for naming most of the formations in the basin, including the Ulan Gochu Formations. Later studies and field expeditions in the Erlian Basin were conducted by the Sino-Soviet Paleontological Expedition in 1959–1960, the Regional Geological Survey of the Nei Mongol Autonomous Region in the 1960s and 1970s, and the Institute of Vertebrate Paleontology and Paleoanthropology, American Museum of Natural History, and Carnegie Museum of Natural History since the 1980s. The Erlian Basin preserves near-continuous sedimentary layers from the late Paleocene to the early Oligocene. The Ulan Gochu Formation preserves strata of late Middle Eocene or Late Eocene age. It overlies the Shara Murun Formation and underlies the Baron Sog Formation. Because the Eocene sediments in the Erlian Basin are near-continuous, there has been much debate historically over where certain stratigraphic units end and others begin. The Asian land mammal ages (ALMA) of the Eocene are mainly based on the different fossil faunas found in the Erlian Basin; the fauna of the Ulan Gochu Formation is the type fauna of the Ulangochuian ALMA. Debate on the stratigraphy have complicated reconstructions of the Asian Eocene, since definitions and interpretations of the stratigraphic units impact the definitions of the land mammal ages. In some cases, different researchers have used entirely different frameworks and stratigraphic unit names. Much work has been done in the 21st century to establish a functional framework, though some stratigraphic issues still remain.
Depositional environment The Erlian Basin experienced a subtropical and humid climate during the Eocene. The vegetation was highly diverse and dominated by deciduous trees and shrubs.
Fossil fauna
Mammals
Anagaloidea
Artiodactyla
Didymoconidae
Hyaenodontia
Lagomorpha
Mesonychia
Perissodactyla
Pholidota
Rodentia
Reptiles
References





