Lianmuqin Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Unit of | Tugulu Group |
Underlies | Donggou & Kumutake Formations |
Overlies | Shengjinkou Formation |
Thickness | 213–360 m (699–1,181 ft) |
Lithology | |
Primary | Mudstone, siltstone |
Location | |
Coordinates | 46°00′N85°48′E / 46.0°N 85.8°E |
Approximate paleocoordinates | 45°00′N81°54′E / 45.0°N 81.9°E |
Region | Xinjiang |
Country | China |
Extent | Junggar Basin |
Type section | |
Named for | Lianmuqin |
The Lianmuqin Formation, [2] also transcribed as Lianmugin Formation, [3] and Lianmuxin Formation, [4] is an Early Cretaceous geologic formation composed of "interbedded red green and yellow variegated mudstones and siltstones". [5] [6] Dinosaur remains have been recovered from it. [7]
The formation is named after Lianmuqin Town in Shanshan County, Xinjiang.
Dinosaurs of the Lianmuqin Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Asiatosaurus [8] | A. mongoliensis [8] | NW Junggar Basin | ||||
Kelmayisaurus [8] [9] | K. petrolicus [8] | NW Junggar Basin | "Maxilla and dentary." [10] | |||
Xinjiangovenator | X. parvus | NW Junggar Basin | "Tibia [and] phalanges." [11] | Formerly thought to be a representative of Phaedrolosaurus ilikensis. [8] | ||
Phaedrolosaurus | P. ilikensis | NW Junggar Basin | "tooth" [12] | |||
Psittacosaurus [8] | P. xinjiangensis [8] | NW Junggar Basin | ||||
Tugulusaurus [8] | T. faciles [8] | NW Junggar Basin | "Hindlimb, rib, [and a] vertebral centrum." [13] | |||
Wuerhosaurus [8] | W. homheni [8] | NW Junggar Basin | "Partial skeleton." [14] | |||
Pterosaurs of the Lianmuqin Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Dsungaripteridae indet. [15] | indeterminate [15] | Southern Junggar Basin | Not referable to Lonchognathosaurus or Dsungaripterus ; likely a new taxon. [15] | |||
Dsungaripterus | D. weii [16] | NW Junggar Basin | ||||
Noripterus | N. complicidens [17] | NW Junggar Basin | ||||
Lonchognathosaurus | L. acutirostris [17] | Southern Junggar Basin | Possible junior synonym of Dsungaripterus weii. [18] | |||
Ornithocheiromorpha Indet. [19] | Indeterminate | |||||
Name | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
Sinopliosaurus | S. weiyuanensis | NW Junggar Basin | Three vertebrae and a tooth. [20] [21] | Dubious genus of plesiosaur. | ||
Name | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
Edentosuchus | E. tienshanensis [22] | NW Junggar Basin | ||||
Name | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
Dracochelys | D. bicuspis | Southern Junggar Basin | [23] | |||
Ordosemys | O. brinkmania | NW Junggar Basin | [23] | |||
Wuguia | W. efremovi | Southern Junggar Basin | [23] | |||
Xinjiangchelys | X. sp. | NW Junggar Basin | [23] | |||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Dsungaripterus is a genus of dsungaripterid pterosaur which lived during the Early Cretaceous in what is now China and possibly South Korea. Its fossils come from the Wuerho Pterosaur Fauna group (WPF) of the Tugulu Group, comprising sections of the of the Junggar Basin. Both formations have seen various age estimates, with data suggest at least some of the WPF dates to the middle Valanginian, but the upper and lower bounds of these pterosaur bearing deposits remains unclear.
Wuerhosaurus is a genus of stegosaurid dinosaur from the Early Cretaceous Period of China and Mongolia. As such, it was one of the last genera of stegosaurians known to have existed.
Xinjiangovenator is a genus of coelurosaurian dinosaurs, possibly part of the group Maniraptora, which lived during the Early Cretaceous period, sometime between the Valanginian and Albian stages. The remains of Xinjiangovenator were found in the Lianmuqin Formation of Wuerho, Xinjiang, China, and were first described by Dong Zhiming in 1973. The genus is based on a single specimen, an articulated partial right lower leg, containing the tibia, three pieces of the fibula, the calcaneum and the astragalus. This specimen, IVPP V4024-2, is the holotype of the genus.
Phaedrolosaurus is a genus of dubious coelurosaurian theropod dinosaur, based on a single isolated and non-diagnostic tooth possibly from the Valanginian-Albian-aged Lianmuqin Formation of Wuerho, in the autonomous region of Xinjiang, China.
Asiatosaurus is an extinct genus of herbivorous sauropod dinosaur which lived during the Early Cretaceous in Mongolia and China. The type species is known only from teeth, making it difficult to rely on information until more specimens are found to expand our knowledge, and another species is known, also based on scant remains; both are now classified as nomina dubia.
Tugulusaurus is a genus of coelurosaurian theropod dinosaur that belongs to the Alvarezsauroidea. It is known from the Early Cretaceous Tugulu Group in the Urhe area of the People's Republic of China. It was one of the first members of Alvarezsauria ever discovered.
Kelmayisaurus is an extinct genus of allosauroid theropod dinosaur from the Early Cretaceous. It was roughly 10–12 meters long and its name refers to the petroleum-producing city of Karamay in the Xinjiang province of western China near where it was found.
Noripterus is a genus of dsungaripterid pterodactyloid pterosaur from Lower Cretaceous-age Wuerho Pterosaur Fauna (WPF) of the Lianmuqin Formation and Shengjinkou Formation in the Junggar Basin of Xinjiang, China. Both formations have seen various age estimates, with data suggest at least some of the WPF dates to the middle Valanginian, but the upper and lower bounds of these pterosaur bearing deposits remains unclear. It was first named by Yang Zhongjian in 1973. Additional fossil remains have been recovered from Tsagaantsav Svita, Mongolia.
Lonchognathosaurus is a genus of dsungaripterid pterodactyloid pterosaur from the Aptian-Albian-age Lower Cretaceous Lianmuqin Formation of Xinjiang, China.
The Subashi Formation is a Late Cretaceous formation from the Xinjiang Autonomous Region of western China. Initially described by Dong Zhiming in 1977, the formation contains remains of Tarbosaurus which were initially described as a separate taxon Shanshanosaurus huoyanshanensis. Remains of a sauropod, likely Nemegtosaurus, and a hadrosaurid, likely Jaxartosaurus, have also been found.
Paleontology or palaeontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilised feces (coprolites), palynomorphs and chemical residues. Because humans have encountered fossils for millennia, paleontology has a long history both before and after becoming formalized as a science. This article records significant discoveries and events related to paleontology that occurred or were published in the year 1973.
The Tuchengzi Formation is a geological formation in China whose strata span the Tithonian to Berriasian ages. Dinosaur fossils, particularly footprints, have been found from the formation.
The Shishugou Formation is a geological formation in Xinjiang, China.
The Kalaza Formation is a geological formation in Xinjiang, China whose strata date back to the Late Jurassic. There is some confusion with the stratigraphy of this unit, as the term is used for sediments of equivalent age in both the Junggar Basin and the Turpan Basin. Dinosaur remains are among the fossils that have been recovered from formation.
The Tugulu Group is a geological Group in Xinjiang, China whose strata date back to the Early Cretaceous. Dinosaur skeletal remains and footprints are among the fossils that have been recovered from the formation.
Sinopliosaurus is a dubious genus of pliosauroid plesiosaur. It lived during the Aptian and Albian stages of the Early Cretaceous of the People's Republic of China - its exact age is unknown. The type species, Sinopliosaurus weiyuanensis, was named and described in 1944 by Yang Zhongjian. One species, "S." fusuiensis, was later shown to be based on teeth from a spinosaurid theropod dinosaur which is now known as Siamosaurus. S. weiyuanensis was considered as a freshwater plesiosaur.
Edentosuchus is a genus of protosuchian crocodyliform. It is known from fossils found in rocks of the Early Cretaceous-age Tugulu Group from the Junggar Basin, Xinjiang, China. Two partial skulls and several neck vertebrae are known to date. An articulated partial postcranial skeleton may also belong to this genus, but there is no overlapping material between it and known Edentosuchus specimens.
Dsungaripteridae is a group of pterosaurs within the suborder Pterodactyloidea. They were robust pterosaurs with good terrestrial abilities and flight honed for inland settings, and were commonly interpreted as durophagous and possibly piscivorous pterosaurs. Fossils have been discovered from Early Cretaceous deposits in Asia, South America and possibly Europe.
Silutitan is a genus of euhelopodid sauropod dinosaur from the Shengjinkou Formation of Xinjiang, China. It contains only the type species, Silutitan sinensis.
The Shengjinkou Formation is an Early Cretaceous (Valanginian)-aged Konservat-Lagerstätte composed of "interbedded red green and yellow variegated mudstones and siltstones" that is part of the larger Tugulu Group of China. Dinosaur and pterosaur remains have been recovered from the formation.