Ilek Formation | |
---|---|
Stratigraphic range: Lower Cretaceous, Barremian–Aptian | |
Type | Geological formation |
Unit of | Kiya River Basin |
Underlies | Kiya Formation |
Overlies | Tyazhin Formation |
Thickness | Up to 746 metres (2,450 ft) |
Lithology | |
Primary | Clay, siltstone |
Other | Marl, sandstone |
Location | |
Coordinates | 55°54′N88°00′E / 55.9°N 88.0°E |
Approximate paleocoordinates | 54°12′N84°36′E / 54.2°N 84.6°E |
Region | Western Siberia |
Country | Russia |
Extent | Kemerovo Oblast |
Type section | |
Named by | L. A. Ragozin |
Year defined | 1935 |
The Ilek Formation is a Lower Cretaceous geologic formation in Western Siberia. Many different fossils have been recovered from the formation. It overlies the Late Jurassic Tyazhin Formation and underlies the Albian Kiya Formation. [1]
The formation was described by L. A. Ragozin in 1935. It consists of sands with sandstone concretions, layers of silts, clays and marls. [2] Age of the formation, according to a crude 1962 estimate, is Valanginian(?) - Hauterivian - Barremian. Its thickness varies greatly, reaching 746 m in Teguldet borehole. [3] A more recent 2024 estimate based on invertebrate and vertebrate fossils placed the age of the formation at Barremian–Aptian. [4]
The Ilek Formation conformably overlies the Upper Jurassic Tyazhin Formation. [1] Gastropods and bivalves of Valanginian age have been recovered from the lower part of the formation, and gastropods and bivalves of Hauterivian to Barremian age have been found in the upper part, as well as Barremian ostracods. The age of the Shestakovo 1 locality is poorly constrained. [5] Palynological samples from the Shestakovo 3 locality are characteristic of the Aptian. No angiosperm pollen has been found at this locality, indicating that it is older than the Albian. [6] The upper layers of the formation do contain angiosperm pollen, indicating that part of the formation may extend into the Albian. The overlying Kiya Formation is upper Albian based on plant biostratigraphy. [1]
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Kiyatriton | K. leshchinskiyi [7] |
| Atlas, trunk vertebrae, fragmentary dentaries, femora, humerus, and nearly complete ilium | A crown-group salamander | |
Kuzbassia | K. sola [8] |
| Two atlantal centra and a trunk vertebral centrum | A karaurid |
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Acinacodus | A. tagaricus [9] | Right dentary fragment | An amphidontid mammal | ||
Baidabatyr | B. clivosus [10] |
| Upper premolar | A multituberculate | |
Gobiconodon | G. borissiaki [11] | 21 upper and lower jaws. | A gobiconodont | ||
G. hoburensis [12] | A fragmentary lower jaw. | ||||
Kemchugia | K. magna [13] | A tooth | An amphilestid mammal | ||
Kiyatherium | K. cardiodens [14] | A maxilla | A zhangheotheriid mammal | ||
Sibirotherium | S. rossicum [15] |
| M1 tooth; [15] mandibular fragments [16] | A docodontan mammaliaform | |
Xenocretosuchus | X. sibiricus [17] | Dental elements | A tritylodontid mammaliamorph | ||
Yermakia | Y. domitor [13] |
| A mandible | A tinodontid mammal |
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
cf. Khurendukhosaurus [18] | K. cf. sp |
| Dorsal vertebra, sacral vertebra | A non-neochoristodere choristodere | |
"Shestakovo choristodere" [18] |
| Fragmentary dentaries, several vertebrae, rib fragments | A possible neochoristodere | ||
Choristodera [18] | Indeterminate |
| Cervical centrum | May represent a taxon distinct from both Khurendukhosaurus and the "Shestakovo choristodere" |
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Paramacellodidae | Indeterminate [4] |
| |||
Platynota | Indeterminate [4] |
| |||
Xenosauridae | Indeterminate [4] |
| A knob-scaled lizard |
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Kirgizemys | A macrobaenid |
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Kyasuchus | K. saevi [19] |
| A partial skull | A shartegosuchid crocodyliform | |
Tagarosuchus | T. kulemzini [20] |
| Nearly complete skull | A crocodyliform |
Genus | Species | Locality | Material | Notes | Image |
---|---|---|---|---|---|
?Ctenochasmatidae | Indeterminate [13] |
| |||
Lonchognathosaurus | L. cf. sp. [21] |
| Wing metacarpal fragment | A dsungaripterid | |
Ornithocheiridae | Indeterminate [22] |
| |||
Pterodactyloidea | Indeterminate [13] |
|
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Lithostrotia | Indeterminate [23] | Caudal vertebrae | Potentially three distinct taxa of titanosaur | ||
Sibirotitan | S. astrosacralis [5] |
| Vertebrae, sacrum, and pedal elements | A somphospondylan sauropod |
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Ornithischia | Indeterminate [4] |
| Isolated teeth | Originally identified as two distinct "hypsilophodontid" taxa [25] | |
Psittacosaurus | P. sibiricus [26] |
| Several skeletons | A ceratopsian | |
Stegosauria | Indeterminate [13] |
| Isolated teeth [25] |
Genus | Species | Locality | Material | Notes | Images |
---|---|---|---|---|---|
Evgenavis | E. nobilis [27] | A set of limb elements | A confuciusornithiform | ||
Kiyacursor | K. longipes [28] |
| Partial skeleton including cervical and caudal vertebrae, cervical and dorsal ribs, a left scapulocoracoid, humeri, and much of both hind limbs [28] | A noasaurid theropod | |
Paraves | Indeterminate [29] | Teeth | May belong to either Microraptorinae or Troodontidae | ||
Mystiornis | M. cyrili [30] |
| Isolated metatarsus | An avisaurid enantiornithean | |
Paraves | Indeterminate [29] | Teeth | May belong to either Microraptorinae or Troodontidae | ||
Tyrannosauroidea | Indeterminate [29] | Teeth | |||
Urbacodon | U. cf. sp. [29] | Teeth | A troodontid with unserrated teeth |
Lonchognathosaurus is a genus of dsungaripterid pterodactyloid pterosaur from the Aptian-Albian-age Lower Cretaceous Lianmuqin Formation of Xinjiang, China.
Gobiconodon is an extinct genus of carnivorous mammals belonging to the family Gobiconodontidae. Undisputed records of Gobiconodon are restricted to the Early Cretaceous of Asia and North America, but isolated teeth attributed to the genus have also been described from formations in England and Morocco dating as far back as the Middle Jurassic. Species of Gobiconodon varied considerably in size, with G. ostromi, one of the larger species, being around the size of a modern Virginia opossum. Like other gobiconodontids, it possessed several speciations towards carnivory, such as shearing molariform teeth, large canine-like incisors and powerful jaw and forelimb musculature, indicating that it probably fed on vertebrate prey. Unusually among predatory mammals and other eutriconodonts, the lower canines were vestigial, with the first lower incisor pair having become massive and canine-like. Like the larger Repenomamus there might be some evidence of scavenging.
Kyasuchus is an extinct genus of shartegosuchid crocodyliform. Fossils have been found from the Ilek Formation outcropping in the Kemerovo Oblast of Russia, deposited during the Aptian and Albian stages of the Early Cretaceous. The localities from which specimens of this genus have been found have also yielded many other vertebrate remains such as those of palaeonisciform fishes, turtles, various lizards, troodontids, triconodonts, the ceratopsian Psittacosaurus, and the protosuchian-grade crocodylomorph Tagarosuchus.
The Murtoi Formation is a geologic formation in vicinity of Lake Gusinoye in Russia. The Murtoi Fm's sedimentation age. It was deposited in the late Valanginian to Early Hauterivian of the Early Cretaceous.
The Itat Formation is a geologic formation in western Siberia. It was deposited in the Bajocian to Bathonian ages of the Middle Jurassic. Dinosaur remains are among the fossils that have been recovered from the formation, including the proceratosaurid Kileskus, as well as fish, amphibians, mammals and many other vertebrates. The formation is noted for bearing significant coal reserves, with large open pit coal mines extracting lignite from the unit currently in operation.
Juchilestes is an amphidontid mammal genus from the early Cretaceous. It lived in what is now the Beipiao of western Liaoning, eastern China. It is known from the holotype D2607, which consists of three-dimensionally preserved, partial skull with mandibles and some teeth. It was found in 2004 from the Lujiatun Site of the Yixian Formation. It was first named by Chun-Ling Gao, Gregory P. Wilson, Zhe-Xi Luo, A. Murat Maga, Qingjin Meng and Xuri Wang in 2010 and the type species is Juchilestes liaoningensis.
Acinacodus is an extinct genus of amphidontid "eutriconodont" which existed in Shestakovo 1 locality in Western Siberia, Russia during the early Cretaceous period. It was described by A. V. Lopatin, E. N. Maschenko and A. O. Averianov in 2010, and the type species is Acinacodus tagaricus.
The Amphidontidae are a family of extinct mammals from the Early Jurassic to the Early Cretaceous, belonging to the eutriconodonts. It contains most of the species previously belonged to Amphilestidae.
Tagarosuchus is an extinct genus of Early Cretaceous protosuchian-grade crocodyliform. Fossils of Tagarosuchus have been found from southern Siberia, including a nearly complete skull found near the village of Shestakovo in Kemerovo Oblast. Tagarosuchus was named in 1999, with the type species being T. kulemzini. Remains have been recovered from the Aptian-Albian Ilek Formation.
Sineleutherus is an extinct genus of euharamiyids which existed in Asia during the Jurassic period. The type species is Sineleutherus uyguricus, which was described by Thomas Martin, Alexander O. Averianov and Hans-Ulrich Pfretzschner in 2010; it lived in what is now China during the late Jurassic Qigu Formation. A second species, Sineleutherus issedonicus, was described by A. O. Averianov, A. V. Lopatin and S. A. Krasnolutskii in 2011. It lived in what is now Sharypovsky District during the middle Jurassic ; its fossils were collected from the upper part of the Itat Formation. However, this is now believed to represent several euharamiyid taxa not closely related to Sineleutherus.
Mystiornis is an extinct genus of bird which existed in what is now western Siberia, Russia during the early Cretaceous period. It is known from an isolated metatarsus found in the Shestakovo-1 locality of southern Western Siberia. It was named by Evgeny N. Kurochkin, Nikita V. Zelenkov, Alexandr O. Averianov and Sergei V. Leshchinskiy in 2011, and the type species is Mystiornis cyrili. While most recent studies place it as an Enantiornithine, specifically an Avisaurid, the authors note that the placement in both groups is tentative and further material will be required to make a firm decision on placement due to the unusual features of the existing material.
The Karauridae are a family of stem-group salamanders (Caudata) that are known from the Middle Jurassic to Early Cretaceous in Central Asia, Northern Asia and Western Europe. The family includes four members: Karaurus from the Middle-Late Jurassic Karabastau Formation of Kazakhstan, Kokartus from the Middle Jurassic Balabansai Formation of Kyrgyzstan, Marmorerpeton from the Middle Jurassic Forest Marble Formation of England and Kilmaluag Formation of Scotland, and Kuzbassia from the Early Cretaceous (Aptian) Ilek Formation. The members are some of the oldest known salamanders. The family is united by several morphological characters, including sculptured skull roof bones. Like some modern salamanders, karaurids were neotenic. Members of the family likely fed via suction feeding on small fish and invertebrates. The Early Cretaceous Siberian Kulgeriherpeton has been suggested to be a karaurid by some authors.
Xenocretosuchus is an extinct genus of tritylodont therapsids from the Aptian Ilek Formation of Siberia, in the Russian Federation. The type species, X. sibiricus, is known only from dental elements, as is X. kolossovi, described from the Batylykh Formation in 2008. Some authors have treated these species as part of the genus Stereognathus, otherwise known from the Middle Jurassic of Britain, but this is rejected by other authors.
Tengrisaurus is a genus of lithostrotian sauropod, from the Early Cretaceous (Valanginian-Hauterivian) Murtoi Formation, Russia. It was described in 2017 by Averianov & Skutschas. The type species is T. starkovi. New remains were described in 2021 by Averianov, Sizov & Skutschas.
Sibirotitan is a genus of somphospondyl sauropod from the Ilek Formation of Russia. The type and only species is S. astrosacralis.
Evgenavis is a genus of pygostylian dinosaurs that lived from the Barremian to the Aptian. The type specimen ZIN PH 1/154 is an isolated tarsometatarsus found in the Ilek Formation, Western Siberia. Evgenavis may have been the only confuciusornithiform known outside the Jehol Biota, although there is also the possibility that it could have been a different type of avialan, such as an enantiornithean or a relative of Vorona. A cladogram within a 2019 study involving a wide range of theropods included Evgenavis as a longipterygid.
The Batylykh Formation is a geological formation in Yakutia, Russia. It is of an uncertain Early Cretaceous age, probably dating between the Berriasian and the Barremian. It is the oldest unit of the 1,500 metres (4,900 ft) thick Sangar Series within the Vilyuy syneclise. The mudstones, sandstones and shales of the formation were deposited in a fluvial to lacustrine environment.
Fossiomanus is an extinct genus of tritylodontid mammaliamorphs from the Early Cretaceous of China. It includes one species, F. sinensis, which is known from a single nearly complete skeleton from the Aptian Jiufotang Formation. Features of its limbs and vertebrae indicate that Fossiomanus was adapted towards a fossorial lifestyle.
Sibirotherium is an extinct genus of docodont mammaliaform. It is known from only a single named species, Sibirotherium rossicum, known from jaw fragments and teeth found in the Early Cretaceous (Aptian) aged Ilek Formation in western Siberia, alongside Khorotherium also from Siberia, it is one of the youngest docodonts.
Kiyacursor is an extinct genus of noasaurid theropod dinosaur from the Early Cretaceous Ilek Formation of Russia. The genus contains a single species, K. longipes, known from a partial skeleton. Kiyacursor represents the first Early Cretaceous ceratosaur discovered in Asia, as well as the second non-avian theropod named from Russia, after Kileskus in 2010.