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The White River Fauna are fossil animals found in the White River Group of South Dakota, North Dakota, Wyoming, Colorado and Nebraska in the United States. In southwest South Dakota and northwest Nebraska, these fossils are characteristic of the White River Badlands (including Badlands National Park), though they can be found far beyond the limits of the White River watershed. [1]
In Wyoming, the White River Group is undifferentiated, and is more commonly known as the White River Formation. Further east in Nebraska and South Dakota, the group is divided into the Chadron Formation (lower part) and Brule Formation (upper part). Exposures are less well-investigated in northeast Colorado and scattered sites across western North Dakota. The White River Group is overlain by the Sharps Formation in Badlands National Park and the Arikaree Group in northwest Nebraska.
Animals from the White River Group date from the Eocene and Oligocene epochs. The fauna is representative of four North American Land Mammal Ages (NALMAs):
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Bathornis |
| †Bathornithidae | Eocene-Miocene | The type genus of the Bathornithidae, large predatory birds related to seriemas. [2] | |
† Paracrax | †Bathornithidae | Closely related and similar to the conspecific Bathornis; however, it seems to have occupied more arid environments. [3] |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Bothriodon |
| †Anthracotheriidae | |||
† Elomeryx |
| †Anthracotheriidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Poebrotherium |
| Camelidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Archaeotherium |
| †Entelodontidae | Oligocene | ||
† Daeodon |
| †Entelodontidae | Miocene |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Leptomeryx | †Leptomerycidae | The most common fossil found in the area. [4] |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
†Eporeodon |
| †Merycoidodontidae | Oligocene | ||
† Leptauchenia | †Merycoidodontidae | ||||
† Merycoidodon | †Merycoidodontidae | ||||
† Miniochoerus | †Merycoidodontidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Protoceras | †Protoceratidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Hypertragulus | †Hypertragulidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Hyaenodon |
| †Hyaenodontidae | Eocene - Miocene |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Daphoneus |
| †Amphicyonidae | Eocene-Miocene | ||
† Parictis | †Amphicynodontinae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Archaeocyon |
| †Borophaginae | Oligocene | ||
†Osbornodon | Canidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Dinictis |
| †Nimravidae | Eocene-Miocene | ||
† Hoplophoneus |
| †Nimravidae | Eocene-Oligocene | ||
† Nimravus | †Nimravidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Xenocranium |
| †Epoicotheriidae | Oligocene |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Palaeolagus | Leporidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Megacerops | †Brontotheriidae | Eocene - Oligocene |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Mesohippus | Equidae | ||||
† Miohippus | Equidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Metamynodon | †Amynodontidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Hyracodon | †Hyracodontidae | Eocene - Oligocene |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Subhyracodon | Rhinocerotidae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Protapirus | Tapiridae |
Genus | Species | Clade | Epoch | Image | Notes |
---|---|---|---|---|---|
† Agnotocastor |
| Castoridae | Eocene-Miocene | ||
† Ischyromys | †Ischyromyidae |
Genus | Species | NALMA | Age | Notes | Image |
---|---|---|---|---|---|
Alligator | † A. prenasalis | Chadronian | late Eocene | The earliest known species of alligator. |
Indeterminate iguanid, skink, and diploglossine (galliwasp) fossils are also known from the White River Group. [5]
Genus | Species | NALMA | Epoch | Notes | Image |
---|---|---|---|---|---|
† Aciprion | †A. formosum | Orellan | early Oligocene | An iguanian related to crotaphytids (collared lizards). [6] [7] | |
† Cremastosaurus | †C. carinicollis | Chadronian | late Eocene | A rare and enigmatic squamate based on vertebrae. [6] | |
†"C". rhambastes | |||||
† Cypressaurus | †C. sp. | Chadronian | late Eocene | A rare iguanid based on jaw fragments. [5] | |
† Exostinus | †E. serratus | Orellan | early Oligocene | A rare xenosaurid known from skull fragments. [6] [8] | |
† Helodermoides | †H. tuberculatus | Chadronian to Orellan | late Eocene to early Oligocene | A glyptosaurine anguid (an armored lizard related to glass lizards and alligator lizards). Previously considered a species of Glyptosaurus. [6] [9] [5] | |
† Hyporhina | †H. antiqua | Orellan to Whitneyan | early-mid Oligocene | An amphisbaenian (worm lizard). [6] | |
†H. tertia | Chadronian | late Eocene | |||
† Lowesaurus | †L. matthewi | Orellan to Arikareean | Oligocene | A rare helodermatid (beaded lizard). [6] | |
† Palaeoxantusia | †P. cf. P. borealis | Chadronian | late Eocene | A xantusiid (night lizard). [6] [5] | |
† Paraphrynosoma | †P. greeni | Orellan | early Oligocene | A rare iguanian known from a single jaw. [6] | |
† Parophisaurus | †P. pawneensis | Orellan | early Oligocene | An anguid related to Ophisaurus (eastern glass lizards). [6] | |
† Peltosaurus | †P. granulosus | Chadronian to Arikareean | late Eocene to late Oligocene | A common glyptosaurine anguid (an armored lizard related to glass lizards and alligator lizards). [6] [9] [5] | |
Polychrus | †P. charisticus [5] | Chadronian | late Eocene | A rare polychrotine (bush anole) based on jaw fragments. [5] | |
Rhineura | †R. coloradoensis | Chadronian | late Eocene | A rhineurid amphisbaenian closely related to the Florida worm lizard ( Rhineura floridana ). [6] [9] [5] | |
†R. hatcherii | Orellan to Whitneyan | early-mid Oligocene | |||
† Saniwa | †S. edura [5] | Chadronian | late Eocene | A rare varanid based on jaw fragments. [5] | |
† Spathorhynchus | †S. natronicus | Chadronian | late Eocene | A rare rhineurid based on a single skull. [6] [5] | |
† Tinosaurus | †T. sp. | Chadronian | late Eocene | A rare acrodontan based on jaw fragments. [5] | |
† Tuberculacerta [5] | †T. pearsoni | Chadronian | late Eocene | A rare phrynosomatine (relative of fence lizards) based on jaw fragments. [5] |
Genus | Species | NALMA | Epoch | Notes | Image |
---|---|---|---|---|---|
† Boavus | †B. cf. occidentalis | Chadronian to Orellan | late Eocene to early Oligocene | A boine boid (true boa). [6] | |
† Calamagras | †C. angulatus | Orellan to Arikareean | Oligocene | An erycine boid (sand boa). [6] [9] | |
†C. murivorus | Orellan | early Oligocene | |||
† Coprophis | †C. dakotaensis | Orellan | early Oligocene | A rare booid based on eroded fossils found within a mammal coprolite. [6] | |
† Geringophis | †G. vetus | Orellan | early Oligocene | An erycine boid (sand boa). [6] [9] | |
† Helagras | †H. orellanensis | Orellan | early Oligocene | An erycine boid (sand boa). [6] | |
† Hibernophis [10] | †H. breithaupti | Orellan | early Oligocene | A booid based on complete skeletons. [10] | |
† Texasophis | †T. galbreathi | Orellan | early Oligocene | A colubrid. [6] |
Indeterminate fossils of an anosteirine carettochelyid and a ptychogastrin geoemydid are also known from the White River Group. [11]
Genus | Species | NALMA | Epoch | Notes | Image |
---|---|---|---|---|---|
Apalone | †A. leucopotamica | Chadronian to Orellan | late Eocene to early Oligocene | A trionychid (softshell turtle). [11] | |
Chrysemys | †C. antiqua | Chadronian to Whitneyan | late Eocene to mid-Oligocene | An emydid (pond turtle), sometimes known as "Trachemys" antiqua. A potential relative of modern painted turtles (Chrysemys). [11] | |
cf. † Echmatemys | cf. †E. sp. | Chadronian | late Eocene | A "batagurid" (geoemydid) similar to Echmatemys. [11] | |
Gopherus | †G. laticuneus | Chadronian to Whitneyan | late Eocene to mid-Oligocene | A gopher tortoise in the subgenus Oligopherus. Gopherus fossils are also known from the Whitneyan. [11] | |
† Hesperotestudo | †H. brontops | Chadronian | late Eocene | A testudinid (tortoise). Hesperotestudo-like fossils are also known from the Whitneyan. [11] | |
† Pseudograptemys [11] | †P. inornata | Chadronian | late Eocene | An emydid (pond turtle) closely related to Graptemys (map turtles). [11] | |
† Stylemys | †S. amphithorax | Chadronian | late Eocene | A common testudinid (tortoise) related to gopher tortoises (Gopherus). Probably survived into the Whitneyan in the White River area. [11] | |
†S. nebrascensis | Chadronian to Orellan | late Eocene to early Oligocene | |||
† Xenochelys | †X. formosa | Chadronian | late Eocene | A kinosternid (mud turtle). [11] |
Genus | Species | NALMA | Epoch | Notes | Image |
---|---|---|---|---|---|
†Eopelobates | †E. grandis | Chadronian | late Eocene | A pelobatid frog related to Pelobates (the European spadefoot toads). [12] |
Merycoidodontoidea, previously known as "oreodonts" or "ruminating hogs," are an extinct superfamily of prehistoric cud-chewing artiodactyls with short faces and fang-like canine teeth. As their name implies, some of the better known forms were generally hog-like, and the group has traditionally been placed within the Suina, though some recent work suggests they may have been more closely related to camels. "Oreodont" means "mountain teeth," referring to the appearance of the molars. Most oreodonts were sheep-sized, though some genera grew to the size of cattle. They were heavy-bodied, with short four-toed hooves and comparatively long tails.
Merycoidodon is an extinct genus of herbivorous artiodactyl of the family Merycoidodontidae, more popularly known by the name Oreodon. It was endemic to North America during the Middle Eocene to Middle Miocene existing for approximately 30 million years.
Metamynodon is an extinct genus of amynodont that lived in North America and Asia from the late Eocene until early Oligocene, although the questionable inclusion of M. mckinneyi could extend their range to the Middle Eocene. The various species were large, displaying a suit of semiaquatic adaptations more similar to those of the modern hippopotamus, despite their closer affinities with rhinoceroses.
Poebrotherium is an extinct genus of camelid, endemic to North America. They lived from the Eocene to Miocene epochs, 46.3—13.6 mya, existing for approximately 32 million years.
The John Day Formation is a series of rock strata exposed in the Picture Gorge district of the John Day River basin and elsewhere in north-central Oregon in the United States. The Picture Gorge exposure lies east of the Blue Mountain uplift, which cuts southwest–northeast through the Horse Heaven mining district northeast of Madras. Aside from the Picture Gorge district, which defines the type, the formation is visible on the surface in two other areas: another exposure is in the Warm Springs district west of the uplift, between it and the Cascade Range, and the third is along the south side of the Ochoco Mountains. All three exposures, consisting mainly of tuffaceous sediments and pyroclastic rock rich in silica, lie unconformably between the older rocks of the Clarno Formation below and Columbia River basalts above.
Parictis is an extinct arctoid belonging to the family Subparictidae.
Miniochoerus is an extinct genus of small oreodont endemic to North America. They lived during the Late Eocene to Early Oligocene 38–30.8 mya, existing for approximately 7 million years. Fossils have been found only in North Dakota, South Dakota, Nebraska, Montana, and Wyoming.
Cormocyon is an extinct genus of borophagine canid native to North America. It lived from the Oligocene to the Early Miocene, 30.8—20.6 Mya, existing for about 10.2 million years. It is regarded as a primitive, transitional member of the Borophagini tribe.
The Orellan is a North American Land Mammal Age typically set from around 33,700,000 to 32,000,000 years BP, a period of 1.7 million years. The Orellan is preceded by the Chadronian and followed by the Whitneyan NALMA stages. Relative to global geological chronology, it is usually considered to fall within the earliest part of the Oligocene epoch, beginning around the same time as the Eocene-Oligocene boundary.
The Chadronian is a North American Land Mammal Age typically set from around 37,000,000 to 33,700,000 years BP, a period of 3.3 million years. The Chadronian is preceded by the Duchesnean and followed by the Orellan NALMA stages. Relative to global geological chronology, it is usually considered to fall within the later part of the Eocene epoch, ending around the same time as the Eocene-Oligocene boundary.
Brachyhyops is an extinct genus of entelodont artiodactyl mammal that lived during the Eocene Epoch of western North America and southeastern Asia. The first fossil remains of Brachyhyops are recorded from the late Eocene deposits of Beaver Divide in central Wyoming and discovered by paleontology crews from the Carnegie Museum of Natural History during the early 20th century. The type species, Brachyhyops wyomingensis, is based on a single skull and was named by E.H. Colbert in 1937, but was not officially described until 1938. During the latter half of the 20th century, additional specimens from North America have been recorded from Saskatchewan and as far south as Texas, indicating that Brachyhyops had a broad distribution and was well-dispersed throughout western North America.
Socognathus is a genus of prehistoric chamopsiid polyglyphanodontian lizards containing species that lived from the Middle Campanian stage to the late Maastrichtian. Several specimens of the type species, Socognathus unicuspis, have been found in Alberta, Canada. A second species, Socognathus brachyodon is known from the late Maastrichtian Lance Formation; its fossils have been found in Wyoming, United States.
Saniwa is an extinct genus of varanid lizard that lived during the Eocene epoch. It is known from well-preserved fossils found in the Bridger and Green River Formations of Wyoming, United States. The type species S. ensidens was described in 1870 as the first fossil lizard known from North America. A second species, S.orsmaelensis, is recognised from remains found in Europe. It is a close relative of Varanus, the genus that includes monitor lizards.
The Brule Formation was deposited between 33 and 30 million years ago, roughly the Rupelian age (Oligocene). It occurs as a subunit of the White River Group in South Dakota, Nebraska, Colorado, North Dakota, and Wyoming.
The Willwood Formation is a sedimentary sequence deposited during the late Paleocene to early Eocene, or Clarkforkian, Wasatchian and Bridgerian in the NALMA classification.
The White River Formation is a geologic formation of the Paleogene Period, in the northern Great Plains and central Rocky Mountains, within the United States.
The Washakie Formation is a geologic formation in northern Colorado and southern Wyoming. It preserves many mammal, bird, reptile and other fossils dating back to the Lutetian stage of the Eocene within the Paleogene period. The sediments fall in the Bridgerian and Uintan stages of the NALMA classification.
Bathornis is an extinct lineage of birds related to modern day seriemas, that lived in North America about 37–20 million years ago. Like the closely related and also extinct phorusrhacids, it was a flightless predator, occupying predatory niches in environments classically considered to be dominated by mammals. It was a highly diverse and successful genus, spanning a large number of species that occurred from the Priabonian Eocene to the Burdigalian Miocene epochs.
Coniophis is an extinct genus of snakes from the late Cretaceous period. The type species, Coniophis precedes, was about 7 cm long and had snake-like teeth and body form, with a skull and a largely lizard-like bone structure. It probably ate small vertebrates. The fossil remains of Coniophis were first discovered at the end of the 19th century in the Lance Formation of the US state of Wyoming, and were described in 1892 by Othniel Charles Marsh. For the genus Coniophis, a number of other species have been described. Their affiliation is, however, poorly secured, mostly based on vertebrae descriptions from only a few fossils.
Subparictis is an extinct genus of carnivoran mammals in the family Subparictidae that inhabited North America.