Phasmagyps | |
---|---|
Scientific classification | |
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.
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.
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]
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.
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 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.
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]
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.
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.
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:
The Accipitridae, one of the four families within the order Accipitriformes, are a family of small to large birds with strongly hooked bills and variable morphology based on diet. They feed on a range of prey items from insects to medium-sized mammals, with a number feeding on carrion and a few feeding on fruit. The Accipitridae have a cosmopolitan distribution, being found on all the world's continents and a number of oceanic island groups. Some species are migratory.
The Gruiformes are an order containing a considerable number of living and extinct bird families, with a widespread geographical diversity. Gruiform means "crane-like".
Anas is a genus of dabbling ducks. It includes the pintails, most teals, and the mallard and its close relatives. It formerly included additional species but following the publication of a molecular phylogenetic study in 2009 the genus was spit into four separate genera. The genus now contains 31 living species. The name Anas is the Latin for "duck".
Teratornithidae is an extinct family of very large birds of prey that lived in North and South America from the Late Oligocene to Late Pleistocene. They include some of the largest known flying birds.
Osteodontornis is an extinct seabird genus. It contains a single named species, Osteodontornis orri, which was described quite exactly one century after the first species of the Pelagornithidae was. O. orri was named after then-recently deceased naturalist Ellison Orr.
Neocathartes is an extinct genus of cariamid bird. It contains a single named species, Neocathartes grallator, known from some fossil bones found in Late Eocene Washakie Formation deposits of Wyoming. Similar bones have been recovered from the Early Eocene Willwood Formation. The genus originally set up by Wetmore, Eocathartes, was already in use for an unrelated fossil bird from Germany, so a new genus had to be established for the Wyoming fossil.
The Pelagornithidae, commonly called pelagornithids, pseudodontorns, bony-toothed birds, false-toothed birds or pseudotooth birds, are a prehistoric family of large seabirds. Their fossil remains have been found all over the world in rocks dating between the Late Paleocene and the Pliocene-Pleistocene boundary.
The genus Cathartes includes medium-sized to large carrion-feeding birds in the New World vulture (Cathartidae) family. The three species currently classified in this genus occur widely in the Americas.
Storrs Lovejoy Olson is an American biologist and ornithologist who spent his career at the Smithsonian Institution, retiring in 2008. One of the world's foremost avian paleontologists, he is best known for his studies of fossil and subfossil birds on islands such as Ascension, St. Helena and Hawaii. His early higher education took place at Florida State University in 1966, where he obtained a B.A. in Biology, and the University of Florida, where he received an M.S. in Biology. Olson's doctoral studies took place at Johns Hopkins University, in what was then the School of Hygiene and Public Health. He has been married to fellow paleornithologist Helen F. James.
Paleontology or palaeontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilised feces (coprolites), palynomorphs and chemical residues. Because humans have encountered fossils for millennia, paleontology has a long history both before and after becoming formalized as a science. This article records significant discoveries and events related to paleontology that occurred or were published in the year 1976.
Palaeochenoides is a genus of the prehistoric pseudotooth birds of somewhat doubtful validity. These were probably rather close relatives of either pelicans and storks, or of waterfowl, and are here placed in the order Odontopterygiformes to account for this uncertainty.
Eonessa is an enigmatic genus of bird possibly belonging to bird order Gruiformes and which consists of the single species Eonessa anaticula.
Cruschedula is an enigmatic bird genus considered to be nomen dubium which consists of the single species Cruschedula revola.
Branta rhuax is an extinct goose endemic to the island of Hawai'i. It was initially described into the monotypic genus Geochen but assigned to Branta by Storrs L. Olson in 2013 after reexamination of the subfossil material.
Gymnogyps varonai, sometimes called the Cuban condor, is an extinct species of large New World vultures in the family Cathartidae. G. varonai is related to the living California condor, G. californianus and the extinct G. kofordi either of which it may have evolved from. The species is solely known from fossils found in the late Pleistocene to early Holocene tar seep deposits in Cuba. G. varonai may have preyed upon carcasses from large mammals such as ground sloths.
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Oscar Paulino Arredondo de la Mata was a Cuban paleontologist. He described a number of birds and mammals of the Quaternary Period from fossils obtained from Cuban caves. He has been called the "father of Cuban vertebrate paleontology".
Gymnogyps howardae is an extinct large species of New World vultures in the family Cathartidae. Gymnogyps howardae is known only from the Late Pleistocene (Lujanian) asphalt deposits known as the Talara Tar Seeps, near to Talara, northwestern Peru. It lived about 126-12 thousand years ago.