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.[2] The fauna is representative of four North American Land Mammal Ages (NALMAs):
Only the uppermost layers of the White River Group extend into the Arikareean (specifically, the informal "brown siltstone member" of the Brule Formation).[2] All NALMA and Epoch information in this list refers solely to each species' distribution through the White River Group, as some species survive into later time intervals outside of the White River area.
Birds
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Archaealectrornis |
†A. sibleyi |
|
"early Oligocene"[3] |
A potential pheasant or guan-like bird |
|
| †Badistornis |
†B. aramus |
Orellan |
early Oligocene |
An aramid (limpkin relative) known from both leg fossils and possible egg fossils. |
|
| †Bathornis |
†B. celeripes |
Chadronian - Orellan |
late Eocene - early Oligocene |
The type genus of Bathornithidae, an extinct family of large predatory birds related to seriemas.[4][5] |
 |
| †B. cursor |
Chadronian |
late Eocene |
| †B. geographicus |
Whitneyan |
"mid" Oligocene |
| †B. veredus (type) |
Chadronian - Orellan |
late Eocene - early Oligocene |
| Buteo |
†B. grangeri |
Orellan |
early Oligocene |
A hawk in the living genus Buteo |
|
| "Gavia" |
†"G." pusilla |
Orellan |
early Oligocene |
A potential loon |
|
| †Gnotornis |
†G. aramielus |
Whitneyan |
"mid" Oligocene |
A heron |
|
| †Palaeogyps |
†P. prodromus |
Chadronian |
late Eocene |
A potential cathartid (New World vulture) |
|
| †Palaeonossax |
†P. senectus |
Whitneyan |
"mid" Oligocene |
A potential cracid (guan or curassow relative) |
|
| †Palaeoplancus |
†P. sternbergi |
Whitneyan |
"mid" Oligocene |
An osprey-like accipitriform,[5] initially regarded as an eagle |
|
| †Paracrax |
†P. antiqua |
Orellan |
early Oligocene |
A bathornithid initially mistaken for a cormorant (Phalacrocorax mediterraneus) |
|
| †P. gigantea |
Whitneyan |
"mid" Oligocene |
A large bathornithid, closely related and similar to the conspecific Bathornis; however, it seems to have occupied more arid environments.[6] |
|
| †P. wetmorei |
Whitneyan |
"mid" Oligocene |
|
| †Phasmagyps |
†P. patritus |
Chadronian |
late Eocene |
A potential cathartid (New World vulture) |
|
| †Procrax |
†P. brevipes |
Chadronian |
late Eocene |
A potential cracid (guan or curassow relative) with short legs similar to piping guans (Pipile)[3] |
|
Mammals
†Apatemyids
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Apatemys |
†A. sp. |
Chadronian[7] |
late Eocene |
An apatemyid (part of an extinct group of aye-aye-like insectivores) |
|
| †Sinclairella |
†S. dakotensis |
Chadronian[7] - Whitneyan |
late Eocene - "mid" Oligocene |
An apatemyid |
|
Chiropterans
| Genus / Taxon |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Chadronycteris |
†C. rabenae |
Chadronian 3 |
late Eocene |
A vespertilionoid bat |
|
| †Oligomyotis |
†O. casementi |
Orellan |
early Oligocene |
A vespertilionid (vesper bat) |
|
| Vespertilionidae |
|
Chadronian 3 |
late Eocene |
An indeterminate vespertilionid, larger than Chadronycteris[27] |
|
Eulipotyphlans
Modern ants often use tiny tooth fossils as grains when building their anthills, and teeth from eulipotyphlans (relatives of shrews, moles, and hedgehogs) are common at anthill sites close to the Chadronian-Orellan transition.[7][28] Both erinaceomorph (hedgehog-like) and "soricomorph" (shrew and mole-like) eulipotyphlans occur in the White River fauna, though erinaceomorphs would go extinct in North America later on in the Cenozoic, near the end of the Miocene.[29]
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Amphechinus |
†A. sp. |
Chadronian[7] |
late Eocene |
An erinaceid (early hedgehog) |
|
| †Ankylodon |
†A. annectens |
Orellan |
early Oligocene |
A late-surviving sespedectid (hedgehog relative) |
|
| †A. progressus |
Chadronian?[7] - Orellan |
late Eocene? - early Oligocene |
|
| †Apternodus |
†A. brevirostris |
Chadronian? |
late Eocene? |
An apternodontid (early mole-like mammal)[30] |
|
| †A. dasophylakas |
Chadronian |
late Eocene |
|
| †A. gregoryi |
Chadronian - Orellan |
late Eocene - early Oligocene |
|
| †A. iliffensis |
Chadronian |
late Eocene |
|
| †A. major |
Chadronian |
late Eocene |
|
| †A. mediaevus |
Chadronian |
late Eocene |
|
| †Centetodon |
†C. chadronensis |
Chadronian - Orellan[28] |
late Eocene - early Oligocene |
A geolabidid (shrew relative) |
|
| †C. magnus |
Chadronian - Orellan |
late Eocene - early Oligocene |
|
| †C. marginalis |
Chadronian - Orellan |
late Eocene - early Oligocene |
|
| †C. wolffi |
Chadronian - Whitneyan |
late Eocene - "mid" Oligocene |
|
| †Clinopternodus |
†C. gracilis |
Chadronian |
late Eocene |
A micropternodontid (early mole-like mammal) |
|
| †Domnina |
†D. gradata |
Chadronian - Whitneyan |
late Eocene - "mid" Oligocene |
A heterosoricine shrew |
|
| †D. thompsoni |
Chadronian |
late Eocene |
|
| †Micropternodus |
†M. borealis |
Chadronian - Orellan |
late Eocene - early Oligocene |
A micropternodontid |
|
| †M. montrosensis |
Chadronian - Orellan |
late Eocene - early Oligocene |
|
| †Noritrimylus |
†N. compressus[7] |
Chadronian - Orellan |
late Eocene - early Oligocene |
A heterosoricine shrew |
|
| †N. metaxy |
Whitneyan |
"mid" Oligocene |
|
| †Oligoryctes |
†O. altitalonidus |
Chadronian - Orellan |
late Eocene - early Oligocene |
An oligoryctid (shrew relative) |
|
| †O. cameronensis |
Chadronian |
late Eocene |
|
| cf. †O. cameronensis |
Chadronian |
late Eocene |
|
| †O. tenutalonidus[7] |
Chadronian |
late Eocene |
|
| †Oligoscalops |
†O. galbreathi |
Chadronian - Orellan |
late Eocene - early Oligocene |
A proscalopid (early mole-like mammal) |
|
| †Proscalops |
†P. sp. |
Chadronian[7] - Whitneyan |
late Eocene - "mid" Oligocene |
A proscalopid |
|
| †P. tertius |
Orellan - Whitneyan |
early - "mid" Oligocene |
|
| †Proterix |
†P. bicuspis |
Whitneyan |
"mid" Oligocene |
An galericine (gymnure-like) erinaceid |
|
| †P. loomisi |
Whitneyan |
"mid" Oligocene |
|
| †P. minimus |
Chadronian[7] - Orellan |
late Eocene - early Oligocene |
|
†Leptictids
Leptictids are an extinct group of mammals with an insectivorous diet, a flexible snout, and hopping adaptations.
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Blacktops |
†B. sp. |
Chadronian[7] - Orellan |
late Eocene - early Oligocene |
A leptictid |
|
| †Leptictis |
†L. dakotensis |
Chadronian[7] - Whitneyan |
late Eocene - "mid" Oligocene |
A leptictid |
|
| †Megaleptictis |
†M. altidens |
Chadronian?[31] - Orellan[32] |
late Eocene? - early Oligocene |
A large leptictid known from a complete skull with possible adaptations for herbivory.[31] |
|
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Copedelphys |
†C. stevensoni |
Chadronian[7] - Whitneyan |
late Eocene - "mid" Oligocene |
A herpetotheriid metatherian (opossum-like marsupial relative) |
|
| †Herpetotherium |
†H. fugax |
Chadronian - Whitneyan |
late Eocene - "mid" Oligocene |
A herpetotheriid. The most abundant non-rodent species found in ant mounds.[7][28] |
|
| †H. valens |
Chadronian - Orellan |
late Eocene - early Oligocene |
A herpetotheriid.[7] |
|
| †Nanodelphys |
†N. hunti |
Chadronian[7] - Whitneyan |
late Eocene - "mid" Oligocene |
A peradectid. |
|
†Palaeanodonta
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Epoicotherium |
†E. unicum |
Chadronian |
late Eocene |
An epoicotheriid (mole-like mammals potentially related to pangolins). |
|
| †Xenocranium |
†X. pileorivale |
Chadronian |
late Eocene |
An epoicotheriid |
 |
†Pantolestans
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Chadronia |
†C. margaretae |
Chadronian |
late Eocene |
A pantolestid (part of an extinct group of otter-like mammals) |
|
| †Cymaprimadon |
†C. kenni |
Chadronian |
late Eocene |
A pantolestid |
|
Perissodactyls
Equids
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Mesohippus |
|
|
|
A rather small three-toed equid (horse) with browsing habits |
 |
| †Miohippus |
|
|
|
A three-toed equid (horse), around the size of a sheep |
 |
Primates
| Taxon |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Chumashius |
†C. sp. |
Chadronian |
late Eocene |
An omomyid (tarsier relative) |
|
| †Omomyidae |
indet. |
Chadronian |
late Eocene |
An indeterminate omomyid, similar to Chumashius but larger.[7] |
|
Rodents
Modern ants often use tiny tooth fossils as grains when building their anthills, and rodent teeth are common at anthill sites close to the Chadronian-Orellan transition.[7][28]
Reptiles
Crocodilians
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| Alligator |
†A. prenasalis |
Chadronian |
late Eocene |
The earliest known species of alligator. |
 |
Snakes
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| †Boavus |
†B. cf. occidentalis |
Chadronian - Orellan |
late Eocene - early Oligocene |
A boine boid (true boa).[34] |
|
| †Calamagras |
†C. angulatus |
Orellan - Arikareean |
Oligocene |
An erycine boid (sand boa).[34][37] |
|
| †C. murivorus |
Orellan |
early Oligocene |
|
| †Coprophis |
†C. dakotaensis |
Orellan |
early Oligocene |
A rare booid based on eroded fossils found within a mammal coprolite.[34] |
|
| †Geringophis |
†G. vetus |
Orellan |
early Oligocene |
An erycine boid (sand boa).[34][37] |
|
| †Helagras |
†H. orellanensis |
Orellan |
early Oligocene |
An erycine boid (sand boa).[34] |
|
| †Hibernophis[38] |
†H. breithaupti |
Orellan |
early Oligocene |
A booid based on complete skeletons.[38] |
|
| †Texasophis |
†T. galbreathi |
Orellan |
early Oligocene |
A colubrid.[34] |
|
Turtles
Indeterminate fossils of an anosteirine carettochelyid and a ptychogastrin geoemydid are also known from the White River Group.[39]
| Genus |
Species |
NALMA |
Epoch |
Notes |
Image |
| Apalone |
†A. leucopotamica |
Chadronian - Orellan |
late Eocene - early Oligocene |
A trionychid (softshell turtle).[39] |
|
| Chrysemys |
†C. antiqua |
Chadronian - Whitneyan |
late Eocene - "mid" Oligocene |
An emydid (pond turtle), sometimes known as "Trachemys" antiqua. A potential relative of modern painted turtles (Chrysemys).[39] |
|
| cf. †Echmatemys |
cf. †E. sp. |
Chadronian |
late Eocene |
A "batagurid" (geoemydid) similar to Echmatemys.[39] |
|
| Gopherus |
†G. laticuneus |
Chadronian - Whitneyan |
late Eocene - "mid" Oligocene |
A gopher tortoise in the subgenus Oligopherus. Gopherus fossils are also known from the Whitneyan.[39] |
|
| †Hesperotestudo |
†H. brontops |
Chadronian |
late Eocene |
A testudinid (tortoise). Hesperotestudo-like fossils are also known from the Whitneyan.[39] |
|
| †Pseudograptemys[39] |
†P. inornata |
Chadronian |
late Eocene |
An emydid (pond turtle) closely related to Graptemys (map turtles).[39] |
|
| †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.[39] |
 |
| †S. nebrascensis |
Chadronian - Orellan |
late Eocene - early Oligocene |
|
| †Xenochelys |
†X. formosa |
Chadronian |
late Eocene |
A kinosternid (mud turtle).[39] |
|
Further reading
- Rachel Benton, Dennis O. Terry Jr., Emmett Evanoff, & H. Gregory McDonald, The White River Badlands: Geology and Paleontology, Indiana University Press 2015
- Donald R. Prothero & Robert J. Emry (ed.), The Terrestrial Eocene-Oligocene Transition in North America, Cambridge University Press, 1996
- William Berryman Scott, A history of land mammals in the western hemisphere, MacMillan Publishing Company, 1913
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- Prothero, Donald R.; Emry, Robert J. (2004). "5. The Chadronian, Orellan, and Whitneyan North American Land Mammal Ages". In Woodburne, Michael O. (ed.). Late Cretaceous and Cenozoic Mammals of North America: Biostratigraphy and Geochronology. Columbia University Press. pp. 156–168. doi:10.7312/wood13040-007. ISBN 978-0-231-13040-0. JSTOR 10.7312/wood13040.11.
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