Irdin Manha Formation | |
---|---|
Stratigraphic range: Eocene | |
Type | Geological formation |
Location | |
Coordinates | 43°42′N112°00′E / 43.7°N 112.0°E |
Region | Inner Mongolia |
Country | China |
Approximate paleocoordinates | 45°12′N105°42′E / 45.2°N 105.7°E |
The Irdin Manha Formation is a geological formation from the Eocene located in Inner Mongolia, China, a few kilometres south of the Mongolian border. [1]
Color key
| Notes Uncertain or tentative taxa are in small text; |
U.S. paleontologists Henry Fairfield Osborn and Roy C. Andrews discovered two premolars on the site in 1923, and assigned the specimen to the new genus Eudinoceras because he believed it to be related to " Dinoceras " (now known as Uintatherium). Within a decade, however, as more complete specimens were recovered, the animal was identified as a Mongolian relative to the North American pantodont Coryphodon . The expedition also lead to the discovery of the only known skull of Andrewsarchus . [2]
Artiodactyls reported from the Irdin Manha Formation | |||||
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Genus | Species | Presence | Material | Notes | Images |
Achaenodontidae? | An incomplete upper tooth (AMNH 20136). [3] | Doubtfully assigned to the family. | |||
Cf. Archaeomeryx , gen indet. | Fragment of lower jaw (AMNH 20173). [3] | A traguliform. | |||
Andrewsarchus | A. mongoliensis | Around Telegraph Line Camp. [4] | A large skull. [5] | A relative of entelodonts formerly thought to be a mesonychid. | |
Erlianhyus | E. primitivus | Irdin Manha, Erlian Basin, Nei Mongol. [6] | A right upper maxilla with P3–M3 (IVPP V 28275). [6] | A basal artiodactyl. | |
Gobiohyus | G. orientalis | Telegraph Line Camp. [7] | Jaw elements. [3] [7] | A helohyid also found in the Ulan Shireh Formation. | |
G. pressidens | Telegraph Line Camp. [7] | Partial right rami. [3] [7] | A helohyid. | ||
G. robustus | Telegraph Line Camp. [7] | Left ramus (AMNH 20246). [3] [7] | A helohyid. | ||
Obotherium | O. parvum | Irdin Manha, Erlian Basin, Nei Mongol. [8] | Teeth and lower jaws [8] | A tapirulid. | |
Cimolestans reported from the Irdin Manha Formation | |||||
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Genus | Species | Presence | Material | Notes | Images |
Eudinoceras | E. mongoliensis | 2 premolars & jaw elements. [2] [3] [9] | A coryphodontid. | ||
Dinoceratans reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Gobiatherium | G. mirificum | 25 miles southwest from Iren Dabasu. [2] | Skull, jaws & limb elements. [2] | An uintatheriid. | |
Ferae reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Miacis | M. invictus | Isolated upper molar (AMNH 20137). [3] | A miacid. | ||
Propterodon | P. irdinensis | Jaw fragments. [3] | A hyaenodontid. | ||
Sarkastodon | S. mongoliensis | About 25 miles southwest of Iren Dabasu. [10] | Skull & jaws. [10] | An oxyaenid. | |
Glires reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Advenimus | A. burkei | Near Camp Margetts. [11] | Jaw elements. [11] | A ctenodactyloid rodent. | |
Asiomys | A. dawsoni | Huheboerhe. [12] | Fragment of right calcaneus (IVPP V24417). [12] | An ischyromyid rodent. | |
Erenlagus | E. anielae | Huheboerhe. [13] | Teeth. [13] | A stem-lagomorph. | |
Gomphos | G. shevyrevae | Huheboerhe escarpment. [14] | Teeth & foot elements. [14] | A mimotonid. | |
Ischyromyidae genus indet. | Species A | Irdin Manha escarpment. [12] | Right calcaneus (IVPP V24416). [12] | Relatively large ischyromyid rodent, calcaneus comparable in size to that of a coypu or Asiatic brush-tailed porcupine. [12] | |
Species B | Daoteyin Obo. [12] | Right calcaneus (IVPP V24418). [12] | Large ischyromyid rodent with calcaneus matching in length that of a coypu & similar in structure to that of Paramys . [12] | ||
Mimolagus | M. aurorae | Irdin Manha escarpment. [15] | Teeth & foot elements. [15] | A large mimotonid. | |
Pappocricetodon | P. neimongolensis | Huheboerhe. [16] | Teeth. [16] | A cricetid rodent. | |
P. cf. P. zhongtiaensis | Huheboerhe. [16] | A left molar. [16] | A cricetid rodent. | ||
P. sp. | Huheboerhe. [16] | A right molar. [16] | A cricetid rodent. | ||
Paramyidae | Paramyid spp. | Teeth & jaws. [11] | 3 sizes of paramyid rodents, possibly different species. | ||
?Paramyid sp. | Left jaw (AMNH 80801). [11] | Possible small paramyid rodent. | |||
Simplicimys | S. bellus | Huheboerhe. [17] | Teeth. [17] | A ctenodactyloid rodent also known from the Arshanto Formation. | |
Strenulagus | S. solaris | Irdin Manha and Huheboerhe localities. [18] | Isolated cheek teeth, fragmentary upper incisors (dI2) and postcranial elements. [18] | A stem-lagomorph also known from the Khaychin Formation. | |
Tamquammys | T. fractus | Huheboerhe. [17] | Right maxilla (V17798). [17] | A ctenodactyloid rodent. | |
T. wilsoni | Teeth. [17] | A ctenodactyloid rodent also known from the Arshanto & Nomogen formations. | |||
Yongshengomys | Y. extensus | Huheboerhe. [17] | Teeth. [17] | A ctenodactyloid rodent. | |
Yuomys | Y. huheboerhensis | Huheboerhe. [17] | Teeth. [17] | A ctenodactyloid rodent. | |
Y. sp. A | Huheboerhe. [17] | A right molar (V17805). [17] | A ctenodactyloid rodent. | ||
Y. sp. B | Huheboerhe. [17] | A right molar (V17806). [17] | A ctenodactyloid rodent. | ||
Y. sp. C | Huheboerhe. [17] | A right molar (V17807). [17] | A ctenodactyloid rodent. | ||
Mesonychians reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Hapalodectes | ?H. auctus | An upper molar or possibly premolar (AMNH 20130). [3] | A hapalodectid. | ||
H. serus | Around Telegraph Line Camp. [4] | Lower cheek tooth (AMNH 20172). [3] [4] | A hapalodectid. | ||
Harpagolestes | H. leei | Huheboerhe & Daoteyin Obo. [19] | Tooth elements. [19] | A mesonychid. | |
Mesonychidae | Gen. indet. | AMNH 20132. [3] | About the size of Harpagolestes uintensis . | ||
Gen. indet. | Isolated tooth (AMNH 20133). [3] | About the size of Synoplotherium lanius. | |||
Mongolonyx | M. dolichognathus | 7 miles west of Camp Margetts. [4] | Jaw elements. [4] | A large mesonychid. | |
Perissodactyls reported from the Irdin Manha Formation | |||||
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Genus | Species | Presence | Material | Notes | Images |
Caenolophus | C. proficiens | Lower jaw & isolated teeth. [20] | A rhinocerotoid. | ||
Cooperia | C. totadentata | Telegraph Line Camp, 23 miles southeast of Iren Dabasu. [21] | Front of skull (AMNH 20116). [21] | Generic name preoccupied, renamed Forstercooperia . | |
Desmatotherium | D. fissum | Upper jaw fragment. [20] | A helaletid. | ||
D. mongoliense | Irdin Manha escarpment, Duheminboerhe, Huheboerhe & Chaganboerhe. [22] | Parts of 10 individuals. [20] [23] | A helaletid also found in the Mergen Formation. | ||
Forstercooperia | F. totadentata | Telegraph Line Camp, 23 miles southeast of Iren Dabasu. [21] | Front of skull (AMNH 20116). [21] | A paraceratheriid, originally named Cooperia. | |
F. ulanshirehensis | Irdin Manha site. [24] | Jaw elements. [24] | A paraceratheriid also known from the Ulan Shireh Formation. | ||
Gnathotitan | G. berkeyi | Irdin Manha. [25] | Jaw elements. [25] | A brontothere. | |
Lophialetes | L. expeditus | Jaw elements. [20] | A lophialetid. | ||
L. minutus | Upper molar. [20] | A lophialetid. | |||
Metatelmatherium | M. cristatum | Camp Margetts. [25] | Skull & lower jaw (AMNH 26411). [25] | A brontothere. | |
M. parvum | Irdin Manha. [25] | Fragment of left lower jaw (AMNH 20168). [25] | A brontothere. | ||
Microtitan | M. mongoliensis | Jaw elements. [25] | A brontothere. | ||
Pappaceras | P. confluens | Upper gray clays & Camp Margetts area. [26] | Skull & jaw elements. [26] | A paraceratheriid. | |
Paracolodon | P. fissus | Duheminboerhe & Daoteyin Obo. [22] | Skull elements & teeth. [22] | A helaletid. | |
Protitan | P. bellus | Spring Camp, East Mesa, Shara Murun region. [25] | Palatal side of skull (AMNH 26104). [25] | A brontothere. | |
P. grangeri | Skull elements. [25] | A brontothere. | |||
P. minor | Camp Margetts. [25] | Skull elements. [25] | A brontothere. | ||
P. obliquidens | Irdin Manha. [25] | Part of left maxilla (AMNH 20125). [25] | A brontothere. | ||
P. robustus | Irdin Manha. [25] | Jaw elements & teeth. [25] | A brontothere. | ||
Protitanotherium | P. mongoliense | Lower jaw & foot bones (AMNH 18653). [23] | Moved to the genus Rhinotitan . [25] | ||
Rhinotitan | R. mongoliensis | Lower jaw & foot bones (AMNH 18653). [23] | A brontothere originally reported as a species of Protitanotherium . | ||
Rostriamynodon | R. grangeri | East of Camp Margetts. [27] | Complete skull & mandible (AMNH 107635). [27] | An amynodontid. | |
Teleolophus | T. medius | Teeth & jaws. [20] |
Primates reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Tarkops | T. mckennai | Huheboerhe. [28] | Incomplete left lower jaw (IVPP V16424). [28] | An omomyid. | |
Birds reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Buteoninae | Chimney Butte. [29] | Left coracoid (AMNH FR 2941). [29] | Specimen reassigned to Eogrus? sp. | ||
Eogrus | E. aeola | Chimney Butte. [29] | Right metatarsus (AMNH 2936). [29] | An eogruid. | |
E.? sp. | Chimney Butte. [29] | Left coracoid (AMNH FR 2941). [29] | Formerly thought to represent a buteonine, now thought to be an eogruid. [30] | ||
Telecrex | T. grangeri | Chimney Butte, Shara Murun region. [29] [31] | An incomplete right femur (AMNH 2942). [29] [31] | A guineafowl, formerly thought to be a rail. | |
Crocodilians reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Asiatosuchus | A. grangeri | 25 miles southwest of Iren Dabasu. [32] | Portions of at least 2 individuals. [32] | A crocodyloid. | |
Testudines reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
"Adocus" | "A". orientalis | Telegraph Line Camp. [33] [34] | Anterior half of plastron (AMNH 6356). [33] [34] | An adocid. | |
Amyda? | A.? johnsoni | Telegraph Line Camp. [34] | Two-thirds of a carapace (AMNH 6357) & many carapace fragments (AMNH 6359). [34] | A softshell turtle. | |
Trionychidae | Indeterminate | Telegraph Line Camp. [34] | Several kinds of sculptured fragments (AMNH 6360). [34] | Remains of softshell turtles. | |
Fish reported from the Irdin Manha Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Pappichthys | P. mongoliensis | Telegraph Line Camp. [35] | Vertebrae. [36] | Specimens now believed to represent Siluriformes. | |
Siluriformes | Indeterminate | Telegraph Line Camp, Chahar Province. [35] | 5 vertebrae (AMNH 8535). [35] | A catfish likely related to ictalurids. Formerly assigned to Pappichthys mongoliensis. | |
Andrewsarchus, meaning "Andrews' ruler", is an extinct genus of artiodactyl that lived during the Middle Eocene in what is now China. The genus was first described by Henry Fairfield Osborn in 1924 with the type species A. mongoliensis based on a largely complete cranium. A second species, A. crassum, was described in 1977 based on teeth. A mandible, formerly described as Paratriisodon, does probably belong to Andrewsarchus as well. The genus has been historically placed in the families Mesonychidae or Arctocyonidae, or was considered to be a close relative of whales. It is now regarded as the sole member of its own family, Andrewsarchidae, and may have been related to entelodonts. Fossils of Andrewsarchus have been recovered from the Middle Eocene Irdin Manha, Lushi, and Dongjun Formations of Inner Mongolia, each dated to the Irdinmanhan Asian land mammal age.
Simplicidentata is a group of mammals that includes the rodents and their closest extinct relatives. The term has historically been used as an alternative to Rodentia, contrasting the rodents with their close relatives the lagomorphs. However, Simplicidentata is now defined as including all members of Glires that share a more recent common ancestor with living rodents than with living lagomorphs. Thus, Simplicidentata is a total group that is more inclusive than Rodentia, a crown group that includes all living rodents, their last common ancestor, and all its descendants. Under this definition, the loss of the second pair of upper incisors is a synapomorphic feature of Simplicidentata. The loss of the second upper premolar (P2) has also been considered as synapomorphic for Simplicidentata, but the primitive simplicidentate Sinomylus does have a P2.
Mesonyx is a genus of extinct mesonychid mesonychian mammal. Fossils of the various species are found in Early to Late Eocene-age strata in the United States and Early Eocene-aged strata in China, 51.8—51.7 Ma (AEO).
Eurymylidae is a family of extinct simplicidentates. Most authorities consider them to be basal to all modern rodents and may have been the ancestral stock whence the most recent common ancestor of all modern rodents arose. However, the more completely known eurymylids, including Eurymylus, Heomys, Matutinia, and Rhombomylus, appear to represent a monophyletic side branch not directly ancestral to rodents. Huang et al. (2004) have argued that Hanomys, Matutinia, and Rhombomylus form a clade characterized by distinctive features of the skull and dentition that should be recognized as a separate family, Rhombomylidae. Eurymylids are only known from Asia.
Hapalodectidae is an extinct family of relatively small-bodied mesonychian placental mammals from the Paleocene and Eocene of North America and Asia. Hapalodectids differ from the larger and better-known mesonychids by having teeth specialized for cutting, while the teeth of other mesonychids, such as Mesonyx or Sinonyx, are more specialized for crushing bones. Hapalodectids were once considered a subfamily of the Mesonychidae, but the discovery of a skull of Hapalodectes hetangensis showed additional differences justifying placement in a distinct family. In particular, H. hetangensis has a postorbital bar closing the back of the orbit, a feature lacking in mesonychids. The skeleton of hapalodectids is poorly known, and of the postcranial elements, only the humerus has been described. The morphology of this bone indicates less specialization for terrestrial locomotion than in mesonychids.
The Iren Dabasu Formation is a Late Cretaceous geologic formation in the Iren Nor region of Inner Mongolia. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation. The formation was first described and defined by Henry Fairfield Osborn in 1922 and it is located in the Iren Nor region of China.
Gomphos is an extinct genus of early lagomorph from the early Eocene of the China and Mongolia.
Asiavorator is an extinct genus of civet-like carnivoran belonging in the family Stenoplesictidae. It was endemic to Asia and lived during the Eocene and Oligocene epochs.
Ekgmowechashala is an extinct genus of primate belonging to Adapiformes.
This paleomammalogy list records new fossil mammal taxa that were described during the year 2012, as well as notes other significant paleomammalogy discoveries and events which occurred during that year.
Coryphodontidae is an extinct family of pantodont mammals known from the Late Paleocene to the Middle Eocene of Eurasia and North America.
Eggysodontidae is a family of perissodactyls, closely related to rhinoceroses. Fossils have been found in Oligocene deposits in Europe, the Caucasus, Central Asia, China, and Mongolia.
Forstercooperia is an extinct genus of forstercooperiine paraceratheriid rhinocerotoids from the Middle Eocene of Asia.
This paleomammalogy list records new fossil mammal taxa that were described during the year 2011, as well as notes other significant paleomammalogy discoveries and events which occurred during that year.
Paracolodon is an extinct genus of tapiroid perissodactyl belonging to the family Helaletidae. Fossils have been found in Mongolia and the Inner Mongolia region of China.
Deperetella is an extinct genus of deperetellid perissodactyls from Middle to Late Eocene of Asia. The genus was defined in 1925 by W. D. Matthew and Walter W. Granger, who named it after French paleontologist Charles Depéret. The type species is Deperetella cristata.
Pappaceras is an extinct genus of rhinocerotoids from the Early Eocene of Asia belonging to Paraceratheriidae.
Amphicticeps is an extinct genus of small, weasel-like carnivoran mammal. It lived in Mongolia during the Oligocene. The genus was erected in 1924 for the species A. shackelfordi on the basis of a well-preserved skull. Historically, the systematic position of this genus has been problematic until more specimens were described decades later.
Erlianhyus is a genus of cetancodontamorph artiodactyl that lived during the Middle Eocene in China. It is monotypic and known from one species, E. primitivus.
Chakpaktas Formation is a geological formation in eastern Kazakstan, as well as being the lowest fossil-bearing strata of the Zaysan Depression. The formation is aged to the Arshantan Asian Land Animal Age which correlates to between the upper Ypresian and lower Lutetian.