scholarly journals Maybe So, Maybe Not: Canis lepophagus at Hagerman Fossil Beds National Monument, Idaho, USA

2022 ◽  
Author(s):  
Kari A. Prassack ◽  
Laura C. Walkup
Keyword(s):  
North American ◽  
National Park ◽  
National Park Service ◽  
Geological Survey ◽  
National Monument ◽  
South Central ◽  
Park Service ◽  
Land Mammal ◽  
The U.S ◽  
Central Idaho

AbstractA canid dentary is described from the Pliocene Glenns Ferry Formation at Hagerman Fossil Beds National Monument, south-central Idaho, USA. The specimen possesses traits in alliance with and measurements falling within or exceeding those of Canis lepophagus. The dentary, along with a tarsal IV (cuboid) and an exploded canine come from the base of the fossiliferous Sahara complex within the monument. Improved geochronologic control provided by new tephrochronologic mapping by the U.S. Geological Survey-National Park Service Hagerman Paleontology, Environments, and Tephrochronology Project supports an interpolated age of approximately 3.9 Ma, placing it in the early Blancan North American Land Mammal Age. It is conservatively referred to herein as Canis aff. C. lepophagus with the caveat that it is an early and robust example of that species. A smaller canid, initially assigned to Canis lepophagus and then to Canis ferox, is also known from Hagerman. Most specimens of Canis ferox, including the holotype, were recently reassigned to Eucyon ferox, but specimens from the Hagerman and Rexroad faunas were left as Canis sp. and possibly attributed to C. lepophagus. We agree that these smaller canids belong in Canis and not Eucyon but reject placing them within C. lepophagus; we refer to them here as Hagerman-Rexroad Canis. This study confirms the presence of two approximately coyote-sized canids at Hagerman and adds to the growing list of carnivorans now known from these fossil beds.

An unexpected early record of Mictomys Vetus (Arvicolinae, Rodentia) from the Blancan (Pliocene) Glenns Ferry Formation, Hagerman Fossil Beds National Monument, Idaho

2008 ◽  
Vol 82 (3) ◽  
pp. 638-642 ◽  
Author(s):  
Dennis R. Ruez ◽  
Philip A. Gensler
Keyword(s):  
National Park ◽  
National Park Service ◽  
The United States ◽  
National Museum ◽  
University Of Michigan ◽  
National Monument ◽  
Park Service ◽  
The University ◽  
Land Mammal ◽  
Continental Glaciation

The cooling during the Pliocene that preceded major continental glaciation in North America is recorded by thick fluvial and lacustrine sequences at Hagerman Fossil Beds National Monument (HAFO) in southcentral Idaho (McDonald et al., 1996). Fossiliferous beds at HAFO occur within the nearly 200 m of exposed Glenns Ferry Formation west of the Snake River. This formation extends from southwestern Idaho into easternmost Oregon (Malde and Powers, 1962). The Glenns Ferry Formation within HAFO contains hundreds of localities that are within the Blancan North American Land Mammal Age. Collection of specimens from these localities since the late 1920s has resulted in large repositories of fossils currently housed, in part, at the United States National Museum, the University of Michigan Museum of Paleontology (UMMP), and the Idaho Museum of Natural History (IMNH); additionally, smaller collections were accumulated by other museums (McDonald et al., 1996). Today the paleontological resources of HAFO are stewarded by the National Park Service. In spite of the extensive previous collections, significant new discoveries are still being made at HAFO.

The Lepidoptera of White Sands National Monument 5: Two new species of Cochylini (Lepidoptera, Tortricidae, Tortricinae)

Zootaxa ◽  
2012 ◽  
Vol 3444 (1) ◽  
pp. 51 ◽  
Author(s):  
ERIC H. METZLER ◽  
GREGORY S. FORBES
Keyword(s):  
New Species ◽  
New Mexico ◽  
National Park ◽  
National Park Service ◽  
National Monument ◽  
Two New Species ◽  
Park Service ◽  
White Sands National Monument ◽  
White Sands ◽  
The U.S

In 2006, 10-year studies of the moths in two park units of the U.S. National Park Service in southern New Mexico were initiated: White Sands National Monument in Otero County, New Mexico, USA; and Carlsbad Caverns National Park, in Eddy County, New Mexico, USA. Two new species of Cochylini, Eugnosta brownana Metzler & Forbes and Cochylis yinyangana Metzler, are described. Adults and male and female genitalia of both species are illustrated.

scholarly journals Describing the Mountainsnails (Oreohelix Sp.) of Grand Teton National Park, Wyoming

2013 ◽  
Vol 36 ◽  
pp. 94-97
Author(s):  
Lusha Tronstad ◽  
Gary Beauvais ◽  
Jeanne Serb ◽  
Kevin Roe
Keyword(s):  
National Park ◽  
National Park Service ◽  
Endangered Species Act ◽  
The State ◽  
Recent Past ◽  
Grand Teton National Park ◽  
Important Group ◽  
Park Service ◽  
Very High ◽  
The U.S

Invertebrates are receiving an increasing amount of conservation attention across North America. Currently, about 40% of the animals listed under the U.S. Endangered Species Act (ESA) are invertebrates (www.NatureServe.org). The National Park Service and other agencies require better information on invertebrate faunas in order to effectively conserve this important group of animals. One way to prioritize invertebrate groups for study is to assess the number of rare taxa within a given genus. In this context, Oreohelix (mountainsnails) are a top priority because the genus is assumed to support a very high percentage of rare and endemic taxa. Additionally, Oreohelix species in Wyoming and surrounding states have been petitioned for ESA listing in the recent past. The diversity of Oreohelix forms in Wyoming is not well-understood, and the current taxonomy may not reflect the true pattern of diversity within the state. Therefore, we are studying both the morphology and genetic structure of Oreohelix in Grand Teton National Park to begin to understand the diversity of mountainsnails in the state. We collected Oreohelix from 4 locations in Grand Teton National Park. Based on shell and internal characteristics, all individuals were identified as O. subrudis. We are currently preparing specimens for DNA sequencing.

scholarly journals Preservation and DNA Fingerprinting of the Historic Tidal Basin Cherries

1999 ◽  
Vol 17 (4) ◽  
pp. 189-192
Author(s):  
Margaret R. Pooler
Keyword(s):  
National Park ◽  
Rapd Markers ◽  
National Park Service ◽  
The United States ◽  
Genetic Distances ◽  
Tidal Basin ◽  
Washington Dc ◽  
Park Service ◽  
Flowering Cherry ◽  
The U.S

Abstract The historic Japanese flowering cherry trees planted around the Tidal Basin in Washington, DC, were given to the United States in 1912 as a gift from Japan, yet only a small portion of the original trees remain. In cooperation with the National Park Service, the U.S. National Arboretum clonally propagated a portion of these trees. DNA from these and other P. x yedoensis plants obtained from domestic commercial nurseries were compared using RAPD markers. Twenty-one 10-nucleotide primers yielded 80 repeatable bands that were used to assess genetic distances among the accessions. The genetic distances ranged from 0.65 to 1.0, with thirteen accessions identical at all loci tested. The most genetically dissimilar trees were P. x yedoensis accessions that were collected as seed in Japan. Accessions obtained from commercial nurseries including ‘Afterglow’, ‘Akebono’, and Yoshino were also dissimilar to the Tidal Basin trees. This study indicated that most of the older trees planted around the Tidal Basin are genetically very similar, but that variability in P. x yedoensis exists, especially in accessions collected as seed from Japan.

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