Djadochta Formation

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Djadochta Formation
Stratigraphic range: Campanian,
~75–71  Ma
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Sunset (20373858488).jpg
Bayn Dzak (Flaming Cliffs), the type locality of the Djadochta Formation
Type Geological formation
Unit of Shamo Group
Sub-unitsBayn Dzak Member, Tugrugyin Member
Underlies Barun Goyot Formation
Overlies Alagteeg Formation
Area Nemegt Basin, Ulan Nur Basin
Thicknessover 90 m (300 ft)
Lithology
Primary Sandstone
Other Mudstone
Type section
Named forShabarakh Usu (Bayn Dzak)
Named byBerkey & Morris
Location Flaming Cliffs
Year defined1927
Coordinates 44°08′19″N103°43′40″E / 44.13861°N 103.72778°E / 44.13861; 103.72778
Approximate paleocoordinates 30°42′N9°12′E / 30.7°N 9.2°E / 30.7; 9.2
Region Ömnögov
CountryFlag of Mongolia.svg  Mongolia
Thickness at type sectionabout 90 m (300 ft)

The Djadochta Formation (sometimes transcribed and also known as Djadokhta, Djadokata, or Dzhadokhtskaya) is a highly fossiliferous geological formation situated in Central Asia, Gobi Desert, dating from the Late Cretaceous period, about 75 million to 71 million years ago. The type locality is the Bayn Dzak locality, famously known as the Flaming Cliffs. Reptile (including dinosaur) and mammal remains are among the fossils recovered from the formation.

Contents

Excavation history

Cretaceous-aged dinosaur fossil localities of Mongolia. Djadochta localities at area B. Cretaceous-aged dinosaur fossil localities of Mongolia.PNG
Cretaceous-aged dinosaur fossil localities of Mongolia. Djadochta localities at area B.

The Djadochta Formation was first documented and explored—though only a single locality—during paleontological expeditions of the American Museum of Natural History in 1922–1925, which were part of the Central Asiatic Expeditions. The expeditions were led by Roy Chapman Andrews, in company of Walter Willis Granger as chief paleontologist and field team. The team did extensive exploration at the Bayn Dzak (formerly Shabarakh Usu) region, which they nicknamed Flaming Cliffs given that at sunset the sediments of this locality had a characteristic reddish color. Notable finds included the first known fossils of Oviraptor , Protoceratops , Saurornithoides , and Velociraptor , the first confirmed dinosaur eggs (a partial nest of Oviraptor), as well as fossil mammals. Some of these were briefly described by Henry Fairfield Osborn during the ongoing years of the expeditions. In 1927 the formation was formally described and established by Berkey and Morris, with Bayn Dzak as the type locality. [1] [2]

In 1963, the Mongolian paleontologist Demberelyin Dashzeveg reported the discovery of a new fossiliferous locality of the Djadochta Formation: Tugriken Shireh. [3] During the 1960s to 1970s, Polish-Mongolian and Russian-Mongolian paleontological expeditions collected new, partial to complete specimens of Protoceratops and Velociraptor at this locality, making these dinosaur species a common occurrence in Tugriken Shireh. [4] Some of the most notable excavations made at Tugriken Shireh include the Fighting Dinosaurs (Protoceratops and Velociraptor locked in combat), [5] [6] and abundant articulated, in situ (in the original pose), and sometimes complete skeletons of Protoceratops. [7] [8]

During the 1980s, a joint Soviet-Mongolian paleontological expedition discovered several Mesozoic fossil-rich localities in the Gobi Desert of Mongolia. Among these sites, Udyn Sayr was discovered and examined by the expedition, regarding its age as Late Cretaceous. This new locality was predominantly rich in avimimid fossils, with a lesser abundance of mammal and other dinosaur fossils. [4]

In 1993 teams of a collaborative Mongolian-North American expedition (supported by the Mongolian Academy of Sciences and American Museum of Natural History) discovered a new fossil locality of the Djadochta Formation called Ukhaa Tolgod (meaning "Brown Hills"). Like previous localities, Ukhaa Tolgod has yielded a prominent abundance of well-preserved fossils, including high concentrations of mammal, dinosaur, lizard, and egg remains. A vast majority of specimens from this locality are usually found in near-complete articulation. Overall, when compared to other Mesozoic fossil sites, the diversity of fossils in Ukhaa Tolgod is unusually high. [9] [10]

Description

The modern-day Djadochta Formation is set in an arid habitat of sand dunes with little freshwater apart from oases and arroyos, in the Gobi Desert. The dominant lithology of the Djadochta Formation is represented by non-marine, cemented reddish-orange and pale orange to light gray, medium to fine-grained sands and sandstones, which include minor deposits of calcareous concretions and orange-brown silty clay. Less abundant sedimentation comprises conglomerates, siltstones, fluvial (water-deposited) sandstones, and mudstones. The entire thickness of the formation in the Ulan Nur Basin is at least 80 m (260 ft). Several aeolian processes (wind works) indicate the presence of large straight-crested dune-like structures, and smaller barchan (crescent-shaped) and parabolic (poorly U-shaped) dunes across the formation. [11] [12] [10] Reddish sandstones are observed in numerous localities. [12] [10]

Exposures at the Flaming Cliffs Bayanzag4.JPG
Exposures at the Flaming Cliffs

Stratigraphy and age

The Djadochta Formation occurs in the Late Cretaceous period of the Campanian stage. Magnetostratigraphic datings from the Bayn Dzak and Tugriken Shireh localities suggest that the Djadochta Formation was deposited during a time of rapidly changing polarity at about 75 million to 71 million years ago. [12]

The Djadochta Formation is separated into a lower Bayn Dzak Member and an upper Turgrugyin Member, which represent very similar depositional environments. [12] Further strata from the Bayn Dzak Member includes that of the Ukhaa Tolgod locality, and its overall age is regarded also within the Campanian. [10]

Based on the superposition of the members, the Tugrugyin Member overlies the Bayn Dzak Member making it somewhat younger, which indicates that the Bayn Dzak paleofauna lived somewhat earlier than that from Tugriken Shireh. However, it is not yet understood the precise temporal difference: [12] Localities within the Djadochta Formation are considered to represent a sequence of progressively younger sediments and thereby paleofaunas. Ukhaa Tolgod may be younger than both Bayn Dzak and Tugriken Shireh. [18] Based on their fossil record and strata, Udyn Sayr and Zamyn Khondt have been correlated with other Djadokhta localities, though fossils of Udyn Sayr may indicate that this locality is younger than Bayn Dzak and Tugriken Shireh. [19]

Examinations on the strata of the Alag Teg (also spelled Alag Teeg or Alag Teer) locality, once considered part of this formation, indicates that it belongs to a different geological formation: the Alagteeg Formation, which is slightly older than the overlying Djadochta Formation. Based on sediments and stratigraphic relationships, the lower part of the Bayn Dzak locality is correlated with the Alag Teg locality, making both sections part of the Alagteeg Formation. The upper or main part of the former locality is considered part of the Djadochta Formation itself, as it shares similar lithology and stratigraphic relationships with Tugriken Shireh. [14]

Stratigraphy of the Djadochta Formation [12] [14]
FormationTime periodMemberLithologyThicknessImage
Barun Goyot Early Maastrichtian Poorly cemented, fine and medium-grained red to reddish-brown sandstones.~110 m (360 ft)
Djadochta Campanian
TurgrugyinPale orange to light gray (sometimes yellowish-white) sands and sandstones.30 m (98 ft)
Aepyornithomimus (MPC-D 100 130) in field.png
Bayn DzakReddish-orange, crossbedded, and structureless sandstones, with minor deposits of brown siltstones and mudstones.90 m (300 ft)
Bayanzag.JPG
Alagteeg Early Campanian
Santonian
"lower Bayn Dzak"Alternating reddish brown mudstone and horizontally laminated sandstone, with ripple cross laminations and rhizoliths.~15 m (49 ft)

Depositional environment

Based on strata and rock facies (such as sandstones and caliche) of the formation and coeval units (Bayan Mandahu) it is currently agreed that sediments of the Djadochta Formation were deposited by wind activity in arid paleoenvironments comprising sand dunes with a warm semi-arid climate. [20] [12] [14] Fluvial sedimentation at the Ukhaa Tolgod locality indicates the presence of short-lived water bodies during the times of the formation, which also contributed to its deposition. [10]

Taphonomy

Citipati IGM 100 979 (2).jpg
Protoceratops specimen MPC-D 100 534.png
Examples of the Djadochta Formation preservation: articulated Citipati (top) and Protoceratops (bottom) specimens

A vast majority of articulated specimens from the Djadochta Formation are found in unstructured sandstones, indicating burial in situ by high-energy sand-bearing events. Some buried Protoceratops individuals are preserved in distinctive postures involving the body and head arched upwards, suggesting that the animals died in the process of trying to free themselves from the body of sand, where they eventually fossilized. As they were unable to escape burial, the sandy mass prevented carcasses from being scavenged by vertebrates. Most of these "buried" specimens are found with bite traces and large borings (tunnel-like holes made by small invertebrates) on bone joints areas and other surfaces, indicating that after death they were largely scavenged by invertebrates, such as skin beetles. [21] [22] [23]

It has been suggested that the repeated occurrence of these feeding traces at limb joints may reflect that the responsible scavengers focused on collagen at the joint cartilage of dried dinosaur carcasses as a source of nitrogen, which was very low in the arid Djadochta Formation environments. [24]

Examinations at the fossil preservation and sediments of Ukhaa Tolgod indicates that preserved animals were buried alive by catastrophic dune collapses. It is thought to have occurred when sand dunes became oversaturated with water resulting in their sudden downfall; heavy rainfall events likely acted as the triggering mechanism for this collapse. [9] [25] [10] Examples from the Ukhaa Tolgod preservation include Citipati (brooding adults entombed atop nests and eggs); [26] [27] Khaan (a pair in close proximity likely killed by a single collapse event); [28] and Saichangurvel (individual buried alive by a muddy dune). [29]

Paleobiota of the Djadochta Formation

Articulated Protoceratops from Tugriken Shireh. This dinosaur is one of the most common occurrences in the Djadochta Formation Protoceratops specimen MPC-D 100 519.jpg
Articulated Protoceratops from Tugriken Shireh. This dinosaur is one of the most common occurrences in the Djadochta Formation

Among fossils, Protoceratops is extremely common in Djadochta localities. Bayn Dzak is reported as one of the localities with the highest concentration of Protoceratops fossils and has been noted as the "Protoceratops fauna". [30] Adjacent to Bayn Dzak, at Tugriken Shireh, Protoceratops is also abundant. [15] Other common dinosaur components of the paleofauna include Pinacosaurus and Velociraptor . [11] Small vertebrates like lizards and mammals are rather abundant and diverse, with Adamisaurus and Kryptobaatar being the most abundant representatives. [29] [31] [30] The paleofauna of the Djadochta Formation is very similar in composition to the nearby and coeval-regarded Bayan Mandahu Formation of Inner Mongolia. The two formations share many of the same genera, but differ in species. For instance, the most common mammal in Djadochta is Kryptobaatar dashzevegi, while in Bayan Mandahu it is the closely related K. mandahuensis. Similarly, the dinosaur fauna of Djadochta includes Protoceratops andrewsi and Velociraptor mongoliensis, which Bayan Mandahu yields P. hellenikorhinus and V. osmolskae. [20] [32]

Although fossil plants are extremely rare in the Djadochta Formation, the great abundancy of herbivorous Protoceratops at the arid-deposited Tugriken Shireh locality indicates that it had a moderate coverage of bushes or other low-growing plants. [15]

The relatively low paleobiodiversity and climate settings of the Djadochta suggest that these conditions contributed to stressed paleoenvironments. Most of the fossil occurrences in the formation are occupied by Protoceratops, and small to medium-sized ankylosaurs, oviraptorids, and dromaeosaurids make much of the overall paleofauna. Large-bodied animals are absent or extremely rare in the formation. Comparisons with the Nemegt Formation further reflects stressed paleoenvironments. In contrast to Djadochta, Nemegt has yielded an extensive diversity of large dinosaur taxa, such as Deinocheirus , Nemegtosaurus , Saurolophus , Tarbosaurus , or Therizinosaurus . Most of these taxa are herbivorous, which combined with the mesic (well-watered) settings of the Nemegt Formation allowed the development of giant herbivores, in contrast to the stressed Djadochta Formation. Another indicative of stressed paleoenvironments is the almost non-existent amount of fully aquatic animals. Turtles are rarely recovered, and most are terrestrial such as Zangerlia . [30]

Tyrannosaurids found in the formation may belong to an indeterminate species of Tarbosaurus , possibly extending the time range of the genus. [33] It is suggested that most of the fragmented hadrosaur, tyrannosaur and sauropod remains across the formation likely belong to non-endemic, passing by species. [30]

Color key
Taxon Reclassified taxonTaxon falsely reported as presentDubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Flora

GenusSpeciesLocationMaterialNotesImages
Radicites R. gobiensisBayn Dzak"Twenty plant roots." [34] A tracheophyte, likely conifer.

Amphibians

GenusSpeciesLocationMaterialNotesImages
Gobiates IndeterminateUdyn Sayr"Partial skeleton with partial urostyle." [35] A frog.

Crocodylomorphs

GenusSpeciesLocationMaterialNotesImages
Artzosuchus A. brachicephalusUdyn Sayr"Partial skull." [36] A crocodylomorph.
Gobiosuchus G. kielanaeBayn Dzak"Multiple specimens with partial skulls and skeletons." [37] [38] A gobisuchid. Gobiosuchus restoration (2004).png
G.? parvusUdyn Sayr"Partial skull and skeleton." [39] [40] A gobisuchid.
Shamosuchus S. djadochtaensisBayn Dzak, Ukhaa Tolgod"Two skulls and partial skeleton." [41] [42] A paralligatorid.

Lizards

GenusSpeciesLocationMaterialNotesImages
Adamisaurus A. magnidentatusBayn Dzak, Tugriken Shireh, Ukhaa Tolgod"Skulls and skeletons from multiple specimens." [43] [29] A teiid. Also present in the Barun Goyot Formation and Bayan Mandahu Formation.
Aiolosaurus A. oriensUkhaa Tolgod"Incomplete skull and partial skeleton." [29] A varanoid.
Carusia C. intermediaBayn Dzak, Ukhaa Tolgod"Skulls from multiple specimens." [29] A carusiid. Also present in the Barun Goyot Formation and Bayan Mandahu Formation.
Cherminotus C. longifronsTugriken Shireh, Ukhaa Tolgod"Skulls and partial skeleton." [29] A varanoid. Also present in the Barun Goyot Formation.
Ctenomastax C. parvaZos"Incomplete skull." [29] An iguanid. Also present in the Barun Goyot Formation.
Dzhadochtosaurus D. giganteusTugriken Shireh"Partially complete skull." [44] A macrocephalosaur.
Eoxanta E. lacertifronsUkhaa Tolgod"Incomplete skull." [29] A scincomorph. Also present in the Barun Goyot Formation.
Estesia E. mongoliensisBayn Dzak, Ukhaa Tolgod"Partial skulls and teeth." [29] A monstersaur. Also present in the Barun Goyot Formation.
Flaviagama F. dzerzhinskiiTugriken Shireh"Skull and two vertebrae." [45] A priscagamid.
Globaura G. venustaBayn Dzak, Ukhaa Tolgod"Partial skulls." [29] A scincomorph. Also present in the Barun Goyot Formation.
Gobiderma G. pulchrumUdyn Sayr, Ukhaa Tolgod"Skulls and skin impressions." [29] A monstersaur. Also present in the Barun Goyot Formation.
Gobinatus G. arenosusUkhaa Tolgod"Partial skull." [29] A teiid. Also present in the Barun Goyot Formation.
Hymenosaurus H. clarkiUkhaa Tolgod"Partial skull." [29] A scincomorph.
Isodontosaurus I. gracilisBayn Dzak, Tugriken Shireh, Ukhaa Tolgod, Zos"Numerous skulls and a partial skeleton." [29] An iguanian. Also present in the Bayan Mandahu Formation.
Macrocephalosaurus IndeterminateUkhaa Tolgod"Partial skull and skeleton." [29] A teiid. Also present in the Barun Goyot Formation.
Mimeosaurus M. crassusBayn Dzak, Ukhaa Tolgod, Zos Wash"Partially complete skulls." [29] An acrodont. Also present in the Bayan Mandahu Formation.
Myrmecodaptria M. microphagosaUkhaa Tolgod"Single skull." [29] A gekkotan.
Ovoo O. gurvalLittle Ukhaa Tolgod"Partial skull." [46] A varanid.
Parmeosaurus P. scutatusUkhaa Tolgod"Articulated skull and skeleton." [29] A scincomorph.
Phrynosomimus P. asperUkhaa Tolgod"Two partial skulls." [29] An acrodont. Also present in the Barun Goyot Formation.
Priscagama P. gobiensisBayn Dzak, Ukhaa Tolgod"Incomplete skulls." [29] An priscagamid. Also present in the Barun Goyot Formation.
Saichangurvel S. davidsoniUkhaa Tolgod"Complete skull and skeleton in articulation." [47] An iguanian.
Slavoia S. darevskiiUkhaa Tolgod"Skulls and skeleton." [29] A scincomorph. Also present in the Barun Goyot Formation.
Telmasaurus T. grangeriBayn Dzak"Partial skull and skeleton." [48] [29] A varanid.
Temujinia T. ellisoniTugriken Shireh, Ukhaa Tolgod"Several partial skulls." [29] An iguanid.
Tchingisaurus T. multivagusUkhaa Tolgod"Partial skull." [29] A teiid.
Unnamed scincomorph IndeterminateUkhaa Tolgod"Partial skull." [29] A scincomorph.
Varanoidea indet.IndeterminateUkhaa Tolgod"Partial maxilla and vertebra." [29] A varanoid.
Zapsosaurus Z. sceliphrosTugriken Shireh"Two partial skulls." [29] An iguanid.

Mammals

GenusSpeciesLocationMaterialNotesImages
Asiatherium A. reshetoviUdyn Sayr"Articulated skull and skeleton." [49] A metatherian. Asiatherium reshetovi 78784.jpg
Bulganbaatar B. nemegtbaataroidesBayn Dzak, Ukhaa Tolgod"Partial skull, and other remains." [50] [9] A multituberculate.
Catopsbaatar C. catopsaloidesUkhaa TolgodNot specified. [9] A djadochtatheriid. Also present in the Barun Goyot Formation. Catopsbaatar.jpg
Chulsanbaatar C. vulgarisUkhaa Tolgod"Skull and partial skeleton." [9] A multituberculate. Also present in the Barun Goyot Formation.
Deltatheridium D. pretrituberculareBayn Dzak, Ukhaa Tolgod"Partial skull and skeleton remains." [51] [52] A tribosphenid.
Deltatheroides D. cretacicusBayn Dzak"Partial skull." [51] A djadochtatheriid.
Djadochtatherium D. matthewiBayn Dzak, Tugriken Shireh"Partial skulls." [53] [54] A djadochtatheriid.
Hyotheridium H. dobsoniBayn Dzak"Partial skull." [51] A therian.
IndeterminateUkhaa TolgodNot specified. [9] A therian.
Kamptobaatar K. kuczynskiiBayn Dzak, Ukhaa Tolgod"Partial skull, and other remains." [55] [9] A multituberculate.
Kennalestes K. gobiensisBayn Dzak, Ukhaa Tolgod"Nearly complete skull, and other remains." [56] [9] An eutherian.
Kryptobaatar K. dashzevegiBayn Dzak, Tugriken Shireh, Ukhaa Tolgod"Skulls and skeleton remains from several specimens." [55] [31] A djadochtatheriid. Gobibaatar and Tugrigbaatar are considered synonyms of this taxon. [57]
Maelestes M. gobiensisUkhaa Tolgod"Partial skull with skeleton." [58] A cimolestid.
Mangasbaatar M. udaniiUdyn Sayr"Skulls and partial skeleton from two specimens." [59] A djadochtatheriid.
Nemegtbaatar N. gobiensisUkhaa TolgodNot specified. [9] A multituberculate. Also present in the Barun Goyot Formation.
Nemegtbaatar restoration.jpg
Sloanbaatar S. mirabilisBayn Dzak, Ukhaa Tolgod"Complete skull, and other remains." [55] [9] A multituberculate.
Tombaatar T. sabuliUkhaa Tolgod"Partial skull." [60] A djadochtatheriid.
Ukhaatherium U. nessoviUkhaa Tolgod"Partial to nearly complete skeletons from several specimens." [61] [62] [63] An eutherian.
Zalambdalestes Z. lecheiBayn Dzak, Tugriken Shireh"Skulls and skeletons from several specimens." [51] [64] An eutherian.
Zalambdalestes.jpg

Pterosaurs

GenusSpeciesLocationMaterialNotesImages
Azhdarchidae indet.IndeterminateTugriken Shireh"Indeterminate bone inside the gut cavity of a Velociraptor." [65] An azhdarchid.

Turtles

GenusSpeciesLocationMaterialNotesImages
Nanhsiungchelyidae indet.IndeterminateAbdrant Nuru"Three shell fragments." [66] A nanhsiungchelyid.
IndeterminateBayn Dzak"Partial shells." [66] A nanhsiungchelyid.
IndeterminateUdyn Sayr"Two shell fragments." [66] A nanhsiungchelyid.
Zangerlia Z. dzamynchondiZamyn Khondt"Partial shell." [67] A nanhsiungchelyid.
Z. ukhaachelysUkhaa Tolgod"Partial skull and skeleton." [68] A nanhsiungchelyid.

Dinosaurs

Alvarezsaurs

GenusSpeciesLocationMaterialNotesImages
Alvarezsauridae indet.IndeterminateTugriken Shireh"Partial skull, braincase, and skeleton elements of two specimens." [69] [70] An alvarezsaurid also known as the Tugriken Shireh alvarezsaur. Uncertainly referred as Parvicursor sp. [70]
Kol K. ghuvaUkhaa Tolgod"A well-preserved right foot." [71] A large alvarezsaurid. Its classification has been criticized. [72] Kol ghuva.jpg
Shuvuuia S. desertiUkhaa Tolgod"Multiple specimens with skull and skeletons." [73] [74] [75] [76] [77] An alvarezsaurid. Shuvuuia.jpg
Undescribed Alvarezsauridae IndeterminateBayn Dzak"Partial pelvic girdle and hindlimb." [78] An alvarezsaurid.
IndeterminateGilvent WashNot given. [76] An alvarezsaurid.

Ankylosaurids

GenusSpeciesLocationMaterialNotesImages
Minotaurasaurus M. ramachandraniUkhaa Tolgod[Two] complete skulls, mandibles, and first cervical half-ring. [79] [80] An ankylosaurid previously thought to be a junior synonym of Tarchia, but is now considered to be a valid and distinct taxon. Minotaurasaurus skull cast.jpg
Pinacosaurus P. grangeriBayn Dzak, Ukhaa Tolgod[Three] skulls, mandibles, predentary, cervical vertebrae, dorsal vertebrae, caudal vertebrae, ribs, scapula, coracoids, humerus, radius, ulna, ilium, femora, tibia, fibula, pelvis, manus, tail club handles, cervical half-rings, osteoderms, and a nearly complete skeleton lacking a skull. [81] [82] [83] An ankylosaurid also known from the Alagteeg Formation and Bayan Mandahu Formation. Pinacosaurus.jpg
Ankylosauridae indet.IndeterminateZamyn KhondtPartially complete postcranial skeleton with in situ osteoderms. [84] Previously referred to Saichania, but is now referred to as Ankylosauridae indet., or cf. Pinacosaurus . [84] Saichania skeleton.jpg

Birds

GenusSpeciesLocationMaterialNotesImages
Apsaravis A. ukhaanaUkhaa Tolgod"Partial postcranial skeleton." [85] A basal ornithurine bird.
Elsornis E. keniTugriken Shireh"Partial articulated skeleton lacking the skull." [86] An enantiornithe.
Gobipteryx G. minutaUkhaa Tolgod"Partial skull." [87] An enantiornithine. Also present in the Barun Goyot Formation.
Protoceratopsidovum'P. fluxuosumBayn Dzak"Partial eggs." [88] Eggs probably laid by a bird. [89]
P. minimumBaga Tariach, Tugriken Shireh"Clutch of four eggs and one pole of egg." [88] Eggs probably laid by a bird. [89]
P. sincerumBayn Dzak, Tugriken Shireh"Multiple eggs and shells." [88] Eggs probably laid by a bird. [89]
Styloolithus S. sabathiBayn Dzak"Partial to complete eggs." [89] Eggs probably laid by a bird.

Ceratopsians

GenusSpeciesLocationMaterialNotesImages
Bainoceratops B. efremoviBayn Dzak"Partial vertebrae." [90] A protoceratopsid. May be synonymous with Protoceratops. [91]
Bagaceratops IndeterminateUdyn Sayr"Skull with partial skeleton." [19] A protoceratopsid. Indeterminate between Bagaceratops and Protoceratops. [19] Bagaceratops specimen MPC-D 100 551B (cropped).png
Protoceratops P. andrewsiBayn Dzak, Tugriken Shireh, Udyn Sayr, Zamyn Khondt"Multiple partial to complete specimens." [92] [7] [93] [8] [19] A protoceratopsid. Protoceratops andrewsi Restoration.png
P. hellenikorhinusBor Tolgoi, Udyn Sayr"Partial cranial remains." [94] A protoceratopsid. Protoceratops hellenikorhinus Restoration.png
Protoceratopsidae indet.IndeterminateUkhaa Tolgod"Numerous skulls and remains." [95] [96] A protoceratopsid. Ukhaa Tolgod protoceratopsid skull.png
Udanoceratops U. tschizhoviUdyn Sayr"Skull and fragmented skeleton elements." [97] A giant leptoceratopsid. Udanoceratops Restoration.png

Dromaeosaurs

GenusSpeciesLocationMaterialNotesImages
Tsaagan T. mangasUkhaa Tolgod"Skull and partial skeleton." [98] A dromaeosaurid Tsaagan.png
Velociraptor V. mongoliensisBayn Dzak, Chimney Buttes, Gilvent Wash, Tugriken Shireh, Udyn Sayr, Ukhaa Tolgod"Multiple partial to complete specimens." [99] [100] [101] [102] [103] [104] A dromaeosaurid. Velociraptor Restoration.png
Undescribed Dromaeosauridae IndeterminateAbdrant Nuru"Claw." [105] A dromaeosaurid.
IndeterminateZos Wash"Frontal region." [98] A dromaeosaurid. Differs from Tsaagan . [98]

Hadrosaurs

GenusSpeciesLocationMaterialNotesImages
Hadrosauroidea indet.IndeterminateTugriken Shireh"Fragmented remains from juveniles." [106] [107] A hadrosauroid.
Plesiohadros P. djadokhtaensisAlag Teeg"Skull and partial body elements." [107] A hadrosauroid. Actually hails from the Alagteeg Formation. [108]

Halszkaraptorines

GenusSpeciesLocationMaterialNotesImages
Halszkaraptor H. escuillieiUkhaa Tolgod"Partial skeleton with complete skull." [109] A halszkaraptorine. Halszkaraptor 2.jpg
Mahakala M. omnogovaeTugriken Shireh"Fragmented skull and skeleton." [110] A halszkaraptorine. Mahakala omnogovae 1st pass.png

Ornithomimosaurs

GenusSpeciesLocationMaterialNotesImages
Aepyornithomimus A. tugrikinensisTugriken Shireh"Nearly complete foot." [111] An ornithomimid. Aepyornithomimus.jpg
Ornithomimosauria indet.IndeterminateUkhaa Tolgod"Partial braincase, jaw tips, ribs, and vertebral fragments". [112] [113] An ornithomimid.

Oviraptorosaurs

GenusSpeciesLocationMaterialNotesImages
Avimimus A. portentonsusUdyn Sayr"Partial skull and skeleton." [114] [115] An avimimid. Its locality origin has been disputed and may hail from the Nemegt Formation. [116] Avimimus mmartyniuk wiki.png
Citipati C. osmolskaeUkhaa Tolgod"Multiple specimens with partial to nearly complete skeletons, an embryo, eggs and nesting individuals." [117] [118] [119] [27] An oviraptorid. Citipati osmolskae Restoration.png
Elongatoolithus E. frustrabilis
E. subtitectorius
Khaan K. mckennaiUkhaa Tolgod"Several specimens with partial to complete skeletons and skulls." [118] [120] [28] An oviraptorid. Khaan mckennai profile1.jpg
Macroolithus M. mutabilis"Eggs."Eggs probably laid by an oviraptorid
Oviraptor O. philoceratopsBayn Dzak"Partial skeleton with skull, associated with a nest and juvenile." [121] [119] [27] An oviraptorid. Oviraptor Restoration.png
Oviraptoridae indet.IndeterminateZamyn Khondt"Nearly complete skeleton with skull." [122] An oviraptorid also known as the Zamyn Khondt oviraptorid. Uncertainly referred to Citipati . [118] [119] Zamyn Khond oviraptorid Restoration.png
IndeterminateZamyn Khondt"Nearly complete skull with atlas and axis." [123] An oviraptorid. Unnamed oviraptorid 100 79.jpg
IndeterminateUdyn Sayr"Assemblage of individuals." [27] An oviraptorid.
IndeterminateNot specified."Two skulls with characteristic high crest." [124] [125] [126] An oviraptorid. The Childrens Museum of Indianapolis - Cast of Oviraptor skull.jpg

Pachycephalosaurs

GenusSpeciesLocationMaterialNotesImages
Goyocephale G. lattimoreiBoro Khovil"Partial skull and skeleton." [127] A pachycephalosaurid. Locality sediments may belong to this formation. [127] [128] Goyocephale restoration.jpg
Prenocephale P. prenesBayn Dzak"Complete skull and partial postcranium of several specimens."A pachycephalosaurid also known from the Nemegt Formation. Prenocephale bickering.jpg

Troodontids

GenusSpeciesLocationMaterialNotesImages
Almas A. ukhaaUkhaa Tolgod"Skull with partial skeleton." [129] A troodontid. Almas.png
Archaeornithoides A. deinosauriscusBayn Dzak"Partial skull." [130] A troodontid? Uncertain relationships among coelurosaurs. [130] [131]
Byronosaurus B. jaffeiUkhaa Tolgod"Skull and fragmentary skeleton." [132] A troodontid. Byronosaurus.jpg
Gobivenator G. mongoliensisZamyn Khondt"Almost complete skeleton." [133] A troodontid. Gobivenator Restoration.jpg
Saurornithoides S. mongoliensisBayn Dzak"Skull with fragmentary skeleton." [134] A troodontid. Saurornithoides restoration.png
Troodontidae indet.IndeterminateUkhaa Tolgod"Partial skeleton." [135] A troodontid.
IndeterminateUkhaa Tolgod"Juvenile skulls, skeleton, and one nest." [136] [131] A troodontid. Referred to either Almas, [137] [129] or Byronosaurus. [131] Dromaeosaurid juvenile AMNH 28506 cast.jpg
IndeterminateUkhaa Tolgod"Fragmented skull and skeleton remains." [138] A troodontid. Provisionally referred to Saurornithoides, [138] but now excluded. [134]
IndeterminateUkhaa Tolgod"Partial skull and skeletons from two specimens." [74] A troodontid.

Tyrannosaurids

GenusSpeciesLocationMaterialNotesImages

Tyrannosauridae indet.

IndeterminateBayn DzakNot specified. [32] A tyrannosaurid.
IndeterminateKhongil"Supraorbital, vertebra, rib, femur and metatarsals." [139] A tyrannosaurid.
IndeterminateNot specified."Partial right ilium." [140] A tyrannosaurid.
IndeterminateNot specified."Teeth." [20] A tyrannosaurid.

Sauropods

GenusSpeciesLocationMaterialNotesImages
Sauropoda indet.IndeterminateNot specified. [141] Not specified. [141] A sauropod.
Resized pan-flaming-cropped2.jpg
Panoramic view of the Flaming Cliffs (Bayn Dzak), type locality of the Djadochta Formation

See also

Related Research Articles

<i>Velociraptor</i> Dromaeosaurid dinosaur genus from the Late Cretaceous

Velociraptor is a genus of small dromaeosaurid dinosaurs that lived in Asia during the Late Cretaceous epoch, about 75 million to 71 million years ago. Two species are currently recognized, although others have been assigned in the past. The type species is V. mongoliensis, named and described in 1924. Fossils of this species have been discovered in the Djadochta Formation, Mongolia. A second species, V. osmolskae, was named in 2008 for skull material from the Bayan Mandahu Formation, China.

<i>Oviraptor</i> Extinct genus of dinosaurs

Oviraptor is a genus of oviraptorid dinosaur that lived in Asia during the Late Cretaceous period. The first remains were collected from the Djadokhta Formation of Mongolia in 1923 during a paleontological expedition led by Roy Chapman Andrews, and in the following year the genus and type species Oviraptor philoceratops were named by Henry Fairfield Osborn. The genus name refers to the initial thought of egg-stealing habits, and the specific name was intended to reinforce this view indicating a preference over ceratopsian eggs. Despite the fact that numerous specimens have been referred to the genus, Oviraptor is only known from a single partial skeleton regarded as the holotype, as well as a nest of about fifteen eggs and several small fragments from a juvenile.

<i>Protoceratops</i> Genus of reptiles (fossil)

Protoceratops is a genus of small protoceratopsid dinosaurs that lived in Asia during the Late Cretaceous, around 75 to 71 million years ago. The genus Protoceratops includes two species: P. andrewsi and the larger P. hellenikorhinus. The former was described in 1923 with fossils from the Mongolian Djadokhta Formation, and the latter in 2001 with fossils from the Chinese Bayan Mandahu Formation. Protoceratops was initially believed to be an ancestor of ankylosaurians and larger ceratopsians, such as Triceratops and relatives, until the discoveries of other protoceratopsids. Populations of P. andrewsi may have evolved into Bagaceratops through anagenesis.

<i>Enigmosaurus</i> Extinct genus of reptiles

Enigmosaurus is a genus of therizinosauroid that lived in Asia during the Late Cretaceous period. It was a medium-sized, ground-dwelling, bipedal herbivore that represents the third therizinosaur taxon from the Bayan Shireh Formation, although it is known from the lower part. The genus is monotypic, including only the type species E. mongoliensis, known from a well preserved pelvis and other tentative body remains.

<i>Byronosaurus</i> Extinct genus of dinosaurs

Byronosaurus is a genus of troodontid dinosaur from the Late Cretaceous Period of Mongolia.

<i>Bagaceratops</i> Protoceratopsid dinosaur genus from the Late Cretaceous

Bagaceratops is a genus of small protoceratopsid dinosaurs that lived in Asia during the Late Cretaceous, around 72 to 71 million years ago. Bagaceratops remains have been reported from the Barun Goyot Formation and Bayan Mandahu Formation. One specimen may argue the possible presence of Bagaceratops in the Djadochta Formation.

<span class="mw-page-title-main">Bayan Shireh Formation</span> Geological formation in Mongolia

The Bayan Shireh Formation is a geological formation in Mongolia, that dates to the Cretaceous period. It was first described and established by Vasiliev et al. 1959.

Bainoceratops is a genus of ceratopsian dinosaur from the late Campanian in the Late Cretaceous. The type species is B. efremovi. Its fossils were found in southern Mongolia in the Djadochta Formation.

<i>Citipati</i> Genus of oviraptorid dinosaur

Citipati is a genus of oviraptorid dinosaur that lived in Asia during the Late Cretaceous period, about 75 million to 71 million years ago. It is mainly known from the Ukhaa Tolgod locality at the Djadochta Formation, where the first remains were collected during the 1990s. The genus and type species Citipati osmolskae were named and described in 2001. A second species from the adjacent Zamyn Khondt locality may also exist. Citipati is one of the best-known oviraptorids thanks to a number of well-preserved specimens, including individuals found in brooding positions atop nests of eggs, though most of them were initially referred to the related Oviraptor. These nesting specimens have helped to solidify the link between non-avian dinosaurs and birds.

<span class="mw-page-title-main">Barun Goyot Formation</span>

The Barun Goyot Formation is a geological formation dating to the Late Cretaceous Period. It is located within and is widely represented in the Gobi Desert Basin, in the Ömnögovi Province of Mongolia.

<span class="mw-page-title-main">Nemegt Formation</span> Geological formation in Mongolia

The Nemegt Formation is a geological formation in the Gobi Desert of Mongolia, dating to the Late Cretaceous. The formation consists of river channel sediments and contains fossils of fish, turtles, crocodilians, and a diverse fauna of dinosaurs, including birds.

<i>Tsaagan</i> Extinct genus of dinosaurs

Tsaagan is a genus of dromaeosaurid dinosaur from the Djadokhta Formation of the Late Cretaceous of Mongolia.

<i>Minotaurasaurus</i> Extinct genus of dinosaurs

Minotaurasaurus is a monospecific genus of ankylosaurid dinosaur that lived in Mongolia during the Late Cretaceous in what is now the Djadochta Formation. The type and only species, Minotaurasaurus ramachandrani, is known from two skulls, a cervical vertebra and a cervical half ring. It was named and described in 2009 by Clifford Miles and Clark Miles. The first fossils of Minotaurasaurus were illegally exported out of Mongolia.It has been suggested to be a synonym of Tarchia but more recent publications consider it as a distinct genus.

<i>Kol ghuva</i> Extinct species of dinosaur

Kol is an extinct genus of coelurosaurian theropod dinosaur from the Late Cretaceous of Mongolia. The type and only species is Kol ghuva. The type specimen was excavated from the Ukhaa Tolgod locality of the Djadochta Formation, dating to about 75 million years ago. It is believed to have been about twice the size of the contemporaneous Shuvuuia. However, unlike Shuvuuia, which is known from many well preserved specimens, and although Ukhaa Tolgod has been thoroughly explored, Kol is known only from one complete foot, suggesting that it must have been relatively rare in that ecosystem.

Aiolosaurus is an extinct genus of monitor lizard from the Late Cretaceous of Mongolia. The type and only species, Aiolosaurus oriens, was named in 2000 from Ukhaa Tolgod, a rich fossil site in the Campanian-age Djadochta Formation.

Saichangurvel is an extinct genus of iguanian lizards from the Late Cretaceous of Mongolia. It is a member of a clade called Gobiguania, an exclusively Late Cretaceous group of iguanian lizards that was likely endemic to the Gobi Desert. The type species, Saichangurvel davidsoni, was named by paleontologists Jack Conrad and Mark Norell of the American Museum of Natural History in 2007. It is known from a single nearly complete and fully articulated skeleton called IGM 3/858, which was found eroding from a block of sandstone during a thunderstorm at a fossil locality called Ukhaa Tolgod. IGM 3/858 comes from the Djadochta Formation, which is between 75 and 71 million years in age. Just as it is today, the Gobi was a desert during the Cretaceous. IGM 3/858 may have died in a collapsing sand dune, the rapid burial preserving its skeleton in pristine condition.

Priscagama is an extinct genus of iguanian lizard from the Late Cretaceous of Mongolia and China. It belongs to an extinct family of iguanians called Priscagamidae. Several incomplete skulls have been found in the Barun Goyot and Djadochta formations, and were originally referred to the genus Mimeosaurus; the type species Priscagama gobiensis was named in 1984 when it was recognized that these skulls belonged to a distinct species. Priscagama differs from most other priscagamids in having a more elongate, lightly built skull. It is very similar in appearance to another priscagamid called Pleurodontagama, as the two can only be distinguished by the shape of their teeth.

<i>Almas ukhaa</i> Genus of reptiles (fossil)

Almas is a genus of troodontid theropod dinosaur from the Late Cretaceous of Mongolia. It contains a single species, Almas ukhaa, named in 2017 by Pei Rui and colleagues, based on a partial articulated skeleton. The only known specimen was found in the Djadochta Formation, which is late Campanian in age.

<span class="mw-page-title-main">Javkhlant Formation</span> Geological formation in Mongolia

The Javkhlant Formation is a geological formation in Mongolia whose strata date back to the Late Cretaceous possibly Santonian to Campanian. Ceratopsian, ornithopod and theropod remains been found in the formation. A prominent fossilized therizinosauroid nesting site is also known from the formation.

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