Phasmagyps

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Phasmagyps
Temporal range: Chadronian
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Scientific classification Red Pencil Icon.png
Kingdom: Animalia
Phylum: Chordata
Class: Aves
Order: Accipitriformes
Family: Cathartidae
Genus: Phasmagyps
Wetmore, 1927
Species:
P. patritus
Binomial name
Phasmagyps patritus
Wetmore, 1927

Phasmagyps, is an extinct genus of New World vulture in the family Cathartidae, known from one Oligocene fossil found in Colorado. [1] The genus contains a single described species, Phasmagyps patritus which is possibly the oldest New World vulture known, [2] though its placement in the family Cathartidae has been questioned. [3]

A genus is a taxonomic rank used in the biological classification of living and fossil organisms, as well as viruses, in biology. In the hierarchy of biological classification, genus comes above species and below family. In binomial nomenclature, the genus name forms the first part of the binomial species name for each species within the genus.

New World vulture family of birds

The New World vulture or condor family Cathartidae contains seven species in five genera, all but one of which are monotypic. It includes five vultures and two condors found in warm and temperate areas of the Americas. The "New World" vultures were widespread in both the Old World and North America during the Neogene.

The Oligocene is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present. As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich; the name comes from the Ancient Greek ὀλίγος and καινός, and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period.

Contents

History and classification

Phasmagyps is known from a single fragmentary fossil bone, the holotype housed in the paleontology collections of the Colorado Museum of Natural History in Boulder, Colorado and given the number 1078. [1] In 1923 Philip Reinheinter collected the specimen from the Weld County Trigonias quarry, possibly a fossilized watering hole. The quarry worked sedimentary rocks that are positioned approximately 25 feet (7.6 m) above the contact between the Pierre Shale and the Chadron Formation, thus dating the fossils to the Lower Chadronian. The fossil was first studied by the American paleontologist and ornithologist Alexander Wetmore; his 1927 type description of the new genus and species was published in the journal Proceedings of the Colorado Museum of Natural History. In the description, Wetmore did not give any etymological explanations for the genus and species names, though phasma is Latin and Greek for a phantom or apparition and Gyps identifies the genus as a vulture. The fossil was reexamined in the early 1980s by avian paleontologist Storrs L. Olson. In a 1985 paper he gives a brief comment on the genus. He stated without going into specific details, that while the fossil is superficially similar to those of Cathartidae members, however it possesses notable features which are different and as such he regarded the position of the genus as problematic. [3] In their 2005 description of a Peruvian fossil, Marcelo Stucchi and Steven Emslie noted the disputed nature of Phasmagyps, but maintained the placement in Cathartidae and noted the genus as the oldest member of the family in the Americas. [2]

Holotype single physical example (or illustration) of an organism, known to have been used when the species (or lower-ranked taxon) was formally described

A holotype is a single physical example of an organism, known to have been used when the species was formally described. It is either the single such physical example or one of several such, but explicitly designated as the holotype. Under the International Code of Zoological Nomenclature (ICZN), a holotype is one of several kinds of name-bearing types. In the International Code of Nomenclature for algae, fungi, and plants (ICN) and ICZN the definitions of types are similar in intent but not identical in terminology or underlying concept.

University of Colorado Museum of Natural History Natural history museum in Boulder, Colorado

The University of Colorado Museum of Natural History is a museum of natural history in Boulder, Colorado. With more than four million artifacts and specimens in the areas of anthropology, botany, entomology, paleontology and zoology, the museum houses one of the most extensive and respected natural history collections in the Rocky Mountain and Plains regions, making it one of the top university natural science museums in the country. In 2003, the University of Colorado Museum received accreditation by the American Alliance of Museums, an honor achieved by only 18 of 500 university natural history museums and only 5% of all 17,500 US museums.

Boulder, Colorado Home rule municipality in Colorado, United States

Boulder is the home rule municipality that is the county seat and the most populous municipality of Boulder County, Colorado, United States. It is the state's 11th-most-populous municipality; Boulder is located at the base of the foothills of the Rocky Mountains at an elevation of 5,430 feet (1,655 m) above sea level. The city is 25 miles (40 km) northwest of Denver.

Description

When first described by Wetmore, Phasmagyps was described as being one third larger than the modern Black vulture, Coragyps atratus. This is contradicted by James Ducey's 1992 paper which lists Phasmagyps as being "not much larger than the Black Vulture". [4] The single known fossil is a partial upper leg bone, specifically the lower section of the right tibiotarsus. As preserved, the largest diameter of the bone is 17.9 millimetres (0.70 in) around the outer condyle, and the width across the condyles is 14.9 millimetres (0.59 in). The diameter at the smallest area of the preserved bone shaft is 9.2 millimetres (0.36 in). [1]

Black vulture A New World vulture found from the southeastern United States to Central Chile and Uruguay

The black vulture, also known as the American black vulture, is a bird in the New World vulture family whose range extends from the southeastern United States to Central Chile and Uruguay in South America. Although a common and widespread species, it has a somewhat more restricted distribution than its compatriot, the turkey vulture, which breeds well into Canada and south to Tierra del Fuego. It is the only extant member of the genus Coragyps, which is in the family Cathartidae. Despite the similar name and appearance, this species is unrelated to the Eurasian black vulture, an Old World vulture in the family Accipitridae. It inhabits relatively open areas which provide scattered forests or shrublands. With a wingspan of 1.5 m (4.9 ft), the black vulture is a large bird though relatively small for a vulture. It has black plumage, a featherless, grayish-black head and neck, and a short, hooked beak.

Tibiotarsus

The tibiotarsus is the large bone between the femur and the tarsometatarsus in the leg of a bird. It is the fusion of the proximal part of the tarsus with the tibia.

Condyle (anatomy) Wikimedia disambiguation page

A condyle is the round prominence at the end of a bone, most often part of a joint - an articulation with another bone. It is one of the markings or features of bones, and can refer to:

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References

  1. 1 2 3 Wetmore, A. (1927). "Fossil Birds from the Oligocene of Colorado" (PDF). Proceedings of the Colorado Museum of Natural History. 7 (2): 1–14.
  2. 1 2 Stucchi, M.; Emslie, S.D. (2005). "A new condor (Ciconiiformes, Vulturidae) from the Late Miocene/Early Pliocene Pisco Formation, Peru" (PDF). The Condor. 107: 107–113. doi:10.1650/7475.
  3. 1 2 Olson, S.L. (1985). The Fossil Record of Birds (PDF). Avian Biology. p. 191. Retrieved 3 December 2012.
  4. Ducey, J. (1992). "Fossil Birds of the Nebraska Region" (PDF). Transactions of the Nebraska Academy of Sciences and Affiliated Societies. XIX: 83–96.