River gravels in the Pecos Valley just north of Roswell, Chaves Cor.rnty, New Mexico, produced fossil vertebrates identified as Gopherus cf. G. agassizii, Equus occidentalis, Equus sp., Camelops hesternus, Bison sp., and Mnmmuthus columbi. These fossils indicate a Rancholabrean (late Pleistocene) age and represent the first Pleistocene megafauna described from river gravels in southeast New Mexico. The presence of the tortoise Gopherus suggests a local frost-free climate
Biological communities in Mexico experienced profound changes in species composition and structure a...
What did the San Pedro River valley look like 11,000 years ago? It wasn't the same then as it is tod...
Sedimentary deposits in the Salton Trough of California record the infilling of the northern part of...
River gravels in the Pecos Valley just north of Roswell, Chaves Cor.rnty, New Mexico, produced fossi...
Southeastern New Mexico (SENM) has a wealth of Pleistocene vertebrate faunas. There are 40 named sit...
New Mexico has a diverse record of Pliocene and Pleistocene vertebrates, including faunas from all t...
Significant mammalian faunas of Pliocene (Blancan) and early Pleistocene (early and medial Irvington...
In 1935, vertebrate fossils were first found in Arroyo de la Parida, about 6 km northeast of Socorro...
A fossiliferous remnant of a small lacustrine unit was discovered in an arroyo midway between the Sa...
A mandible of a tapir (Tapirus sp.) from the late Pliocene (early Blancan North American land mammal...
Late Pleistocene groundwater discharge deposits (paleowetlands) in the upper Las Vegas Wash north of...
Sandia Cave is an important latest Pleistocene(late Rancholabrean) vertebrate fauna, with more than ...
Despite high taxonomic diversity elsewhere in North America during the Pleistocene, vertebrate fauna...
mammals. Some 22 taxa are from the vicinity of the Blancan/Irvingtonian transition, 12 most likely a...
Mammalian fossils collected from the second terrace above Clear Creek in Denton County, Texas, are h...
Biological communities in Mexico experienced profound changes in species composition and structure a...
What did the San Pedro River valley look like 11,000 years ago? It wasn't the same then as it is tod...
Sedimentary deposits in the Salton Trough of California record the infilling of the northern part of...
River gravels in the Pecos Valley just north of Roswell, Chaves Cor.rnty, New Mexico, produced fossi...
Southeastern New Mexico (SENM) has a wealth of Pleistocene vertebrate faunas. There are 40 named sit...
New Mexico has a diverse record of Pliocene and Pleistocene vertebrates, including faunas from all t...
Significant mammalian faunas of Pliocene (Blancan) and early Pleistocene (early and medial Irvington...
In 1935, vertebrate fossils were first found in Arroyo de la Parida, about 6 km northeast of Socorro...
A fossiliferous remnant of a small lacustrine unit was discovered in an arroyo midway between the Sa...
A mandible of a tapir (Tapirus sp.) from the late Pliocene (early Blancan North American land mammal...
Late Pleistocene groundwater discharge deposits (paleowetlands) in the upper Las Vegas Wash north of...
Sandia Cave is an important latest Pleistocene(late Rancholabrean) vertebrate fauna, with more than ...
Despite high taxonomic diversity elsewhere in North America during the Pleistocene, vertebrate fauna...
mammals. Some 22 taxa are from the vicinity of the Blancan/Irvingtonian transition, 12 most likely a...
Mammalian fossils collected from the second terrace above Clear Creek in Denton County, Texas, are h...
Biological communities in Mexico experienced profound changes in species composition and structure a...
What did the San Pedro River valley look like 11,000 years ago? It wasn't the same then as it is tod...
Sedimentary deposits in the Salton Trough of California record the infilling of the northern part of...