Plionarctos
Template:Short description Template:Automatic taxobox
Plionarctos is an extinct genus of short-faced bear endemic to North America from the Late Miocene to the Pliocene.
Taxonomy
Described by Childs Frick in 1926,[1] Plionarctos is the oldest known genus within the subfamily of the short-faced bears (Tremarctinae),[2] and is believed to be ancestral to Arctodus, Arctotherium and Tremarctos.[3] Plionarctos probably evolved from Ursavus which emigrated into North America from Eurasia during the Miocene,[4] or possibly Protarctos.[5] A new species, Plionarctos harroldum, was described in 2001 from the White Bluffs Fauna in Washington from remains previously attributed to Protarctos abstrusus.[3] Middle Pleistocene remains from France were reported but have since been reassigned to Ursus.[6]
Evolution
| Tremarctinae within Ursidae |
|
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Script error: No such module "Check for unknown parameters".Plionarctos first appeared in North America during the late Miocene epoch, being recorded from the Rattlesnake Formation of Oregon circa 7Ma.[7] Plionarctos was the sole representative of the Tremarctinae subfamily of bears during its existence, with P. edensis being thought to be ancestral to P. harroldorum.[3] Both Plionarctos edensis and Plionarctos harroldorum coexisted in the Late Hemphillian faunal stage of the Late Miocene, although only P. harroldorum is confirmed from the Blancan faunal stage.[3]
Plionarctos is last recorded ca. 2.9Ma from Taunton, Washington, from a specimen which appears to be evolutionarily intermediate between Plionarctos harroldum and Tremarctos floridanus.[8][9] Plionarctos was followed by three new genera of short-faced bear around the Plio-Pleistocene boundary.[10] These were Arctodus (pristinus), Tremarctos (floridanus) and Arctotherium sp., which emerged in the Late Blancan age of North America circa 2.6Ma.[11][12][13]
An investigation into the mitochondrial DNA of bear species indicates that the short-faced bears diverged from the Ursinae subfamily approximately 5.7 million years ago.[14][15] Around the Miocene-Pliocene boundary (~5.3 Ma) short-faced bears, along with other ursids, experienced an explosive radiation in diversity, as C4 vegetation (grasses) and open habitats dominated, the world experienced a major temperature drop and increased seasonality, and a faunal turnover which extinguished 60–70% of all Eurasian faunal genera, and 70–80% of North American genera.[16][17] Correspondingly, the three succeeding genera appear to genetically diverge around this time, with Arctodus splitting from Arctotherium and Tremarctos at between 5.5Ma and 4.8Ma,[10][18] and Arctotherium and Tremarctos branching off at 4.1Ma.[10]
Description
Plionarctos is thought to have weighed around the size of a smaller spectacled bear (60-150kg), and a skull length of 20cm.[7] Postcranial skeletons of Plionarctos are unknown.[7]
Diagnostics
Unlike other tremarctine bears, Plionarctos did not posses a premasseteric fossa. Although tooth sizes are similar, they also be differentiated from Tremarctos by the slightly shorter M2 molar.[7]
Paleobiology
Plionarctos existed between the middle Hemphillian faunal stage to the early Blancan faunal stage (7Mya - 2.9Mya).[7] Present on the coasts but rare in the Great Plains, Plionarctos is thought to have preferred more humid forested habitats.[7]
Like other tremarctine bears, Plionarctos is believed to have been sexually dimorphic.[7] A Plionarctos harroldum specimen from Taunton (Washington, 2.9Ma)[19] appears evolutionarily intermediate between P. harroldum and T. floridanus, such as being the size of T. floridanus.[20]
Fossil distribution
P. edensis
- Rattlesnake Formation, Grant County, Oregon (Plionarctos sp., Hemphillian, ca. 7Mya)[7]
- Montbrook Site, Levy County, Florida (Plionarctos sp., 5.5 - 5Mya)[21]
- Eden Formation, Riverside County, California (type P. edensis, Hemphillian)[7]
- Gray Fossil Site, Washington County, Tennessee (Plionarctos sp., ca. 4.9-4.5 Mya, Hemphillian)[22]
- Pipe Creek Sinkhole, Grant County, Indiana (5-4Mya, latest Hemphillian or earliest Blancan)[23]
- Aguanga Horizon, Riverside County, California (Blancan)?[7]
P. harroldorum
- Palmetto Mine, Polk County, Florida (Plionarctos sp., Upper Bone Valley Formation, 5 to 4.5Mya, Hemphillian)[3][7][24][25]
- Fort Green Mine, Polk County, Florida paleontological sites (Upper Bone Valley Formation, Hemphillian)[3][7]
- Bear Springs, Arizona (Early Blancan Red Knolls Fauna, ca. 3.1Mya)[26][27]
- Ash Hollow Formation, Ogalla / Bear Tooth Slide, Brown County, Nebraska (Hemphillian)[3][7]
- White Bluffs fauna, Franklin County, Washington (Early Blancan Ringold Formation, type P. harroldorum)[3]
- Taunton site, Adams County, Washington (Blancan, ca. 2.9Mya)[3][28]
References
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