Post by grrraaahhh on Jan 25, 2012 5:05:56 GMT -9
With the recent short-faced bear fossil discovery in Tennessee (Gray Fossil Site), I thought some of the forum audience might be interested to know that there have been additional-similar fossil discoveries made in the western United States. We are still talking about the Tremarctine branch and Plionarctos lineage but earlier disovery. The following article reference is from 2001:
ABSTRACT—The Pliocene Ringold Formation of eastern Washington has yielded important new materials of tremarctine bears of the anagenetic Plionarctos lineage. The genus is reviewed in light of this new material and observations made on other described specimens. One of these was previously described from the medial Hemphillian Rattlesnake Formation of Oregon and is recognized as a tremarctine bear, thus extending the earliest record of the group into the early part of the late Miocene. The late Hemphillian P. edensis, the genotypic species, is rediagnosed, although no new material is added to its hypodym. A new species from the early Blancan White Bluffs sites, P. harroldorum, appears to have been derived from P. edensis. Referred Plionarctos sp. from the medial Blancan Taunton Locality has some dental features that are more derived and approach those of the Pleistocene Tremarctos floridanus. Plionarctos forms a paraphyletic stem-group for the Tremarctinae. Species of this genus can be traced successively into the Pliocene where they form the stock from which the Pleistocene and Recent species of Tremarctos, Arctodus, and Pararctotherium arose.
Tedford, R. H. & Martin, J. Plionarctos, a tremarctine bear (Ursidae; Carnivora) from western North America. J. Vert. Paleontol. 21, 311–321 (2001).
www.bioone.org/doi/abs/10.1671/0272-4634%282001%29021%5B0311:PATBUC%5D2.0.CO%3B2
P.S. For fossil photo viewing, scroll down to the end of the hyperlink.
ABSTRACT—The Pliocene Ringold Formation of eastern Washington has yielded important new materials of tremarctine bears of the anagenetic Plionarctos lineage. The genus is reviewed in light of this new material and observations made on other described specimens. One of these was previously described from the medial Hemphillian Rattlesnake Formation of Oregon and is recognized as a tremarctine bear, thus extending the earliest record of the group into the early part of the late Miocene. The late Hemphillian P. edensis, the genotypic species, is rediagnosed, although no new material is added to its hypodym. A new species from the early Blancan White Bluffs sites, P. harroldorum, appears to have been derived from P. edensis. Referred Plionarctos sp. from the medial Blancan Taunton Locality has some dental features that are more derived and approach those of the Pleistocene Tremarctos floridanus. Plionarctos forms a paraphyletic stem-group for the Tremarctinae. Species of this genus can be traced successively into the Pliocene where they form the stock from which the Pleistocene and Recent species of Tremarctos, Arctodus, and Pararctotherium arose.
Tedford, R. H. & Martin, J. Plionarctos, a tremarctine bear (Ursidae; Carnivora) from western North America. J. Vert. Paleontol. 21, 311–321 (2001).
www.bioone.org/doi/abs/10.1671/0272-4634%282001%29021%5B0311:PATBUC%5D2.0.CO%3B2
P.S. For fossil photo viewing, scroll down to the end of the hyperlink.