The Glenns Ferry Formation is a Pliocene stratigraphic unit in the western United States. Outcrops of the formation in Hagerman Fossil Beds National Monument preserve the remains of seven fish species, five of which are extinct. These include the teleosteans Mylopharodon hagermanensis , Sigmopharyngodon idahoensis , and Ptychocheilus oregonensis , Ameirurus vespertinus , and the sunfish Archoplites taylori . [1] A nearly complete skull of the catfish Ameirurus vespertinus was recovered in 2001 from the wall of the Smithsonian Horse Quarry. [1]
The Pliocene Epoch is the epoch in the geologic timescale that extends from 5.333 million to 2.58 million years BP. It is the second and youngest epoch of the Neogene Period in the Cenozoic Era. The Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch. Prior to the 2009 revision of the geologic time scale, which placed the four most recent major glaciations entirely within the Pleistocene, the Pliocene also included the Gelasian stage, which lasted from 2.588 to 1.806 million years ago, and is now included in the Pleistocene.
Hagerman Fossil Beds National Monument near Hagerman, Idaho, contains the largest concentration of Hagerman horse fossils in North America. The fossil horses for which the monument is famous have been found in only one locale in the northern portion of the monument called the Hagerman Horse Quarry. The 4,351-acre (17.61 km2) monument is internationally significant because it protects the world's richest known fossil deposits from the late Pliocene epoch, 3.5 million years ago. These plants and animals represent the last glimpse of that time that existed before the Ice Age, and the earliest appearances of modern flora and fauna. This is also significant because the fossils present during this period of the Pliocene represent species which were alive during the early stages in the evolution of man, albeit on a different continent. The fossil beds were designated a National Natural Landmark in 1975.
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 2001.
The Ogallala Formation is a Miocene to Pliocene geologic unit in the High Plains of the western United States and the location of the Ogallala Aquifer.. Notably, it records the North American Land Mammal Ages (NALMAs) Hemphillian, Clarendonian, and Barstovian. The Ogallala Formation outcrops of Lake Meredith National Recreation Area preserve fish fossils. Similar specimens from the same formation are found at Alibates Flint Quarries National Monument in Texas.
The Cherry Canyon Formation is a Permian geologic unit in Guadalupe Mountains National Park. The formation contains fan sandstones that were deposited under ancient seawater during the Middle Permian. These rocks contain abundant fish fossils like sharks' teeth preserved within small phosphatic nodules.
The Gardener's Clay Formation is a Pleistocene geologic unit straddling the New York-New Jersey border. Fossil fish vertebrae and teeth are preserved in its sediments.
The Hannold Hill Formation is an Eocene geologic unit in the western United States. It preserves the fossilized remains of the ray Myliobatis and gar.
The Culpeper Basin is one of the Newark Supergroup's Triassic rift basins. It frames the eastern front of the Appalachian Mountains From Culpeper County, Virginia into Maryland. The Groveton Member of the Bull Run Formation is exposed there. The formations has produced disarticulated fish remains including isolated bones and scales.
The Pen Formation is a Campanian-age geologic unit in the western United States.
The Bell Canyon Formation is a Permian geologic unit in the western United States. The formation's Lamar Limestone Member of Guadalupe Mountains National Park has produced fossil holocephalan teeth.
The Doughnut Formation is an Upper Mississippian geologic unit in the western United States. Fish fossils have been discovered shale outcrops of this formation in Dinosaur National Monument.
The Brushy Canyon Formation is a Permian geologic unit in Guadalupe Mountains National Park. The formation contains fan sandstones that were deposited under ancient seawater during the Middle Permian. These rocks contain abundant fish fossils like sharks' teeth preserved within small phosphatic nodules.
The Cabrillo Formation is a Maastrichtian stage geologic formation in coastal San Diego County, southern California. It is part of the Rosario Group.
The Kishenehn Formation is a Paleogene stratigraphic unit in Montana. Fossil amiiforme and teleost fish have been found in outcrops of the formation's Coal Creek Member in Glacier National Park. Mosquitos have also been found in the Coal Creek Member, and have been found to be hematophagous. It is considered a Middle Eocene Lagerstätte.
The Bull Run Formation is a Triassic stratigraphic unit in the eastern United States. Fossil fish bones and scales have been found in outcrops of the formation's Groveton Member in Manassas National Battlefield Park.
The Cliff House Sandstone is a late Campanian stratigraphic unit comprising sandstones in the western United States. Outcrops of the formation in Mesa Verde National Park have produced fossil shark teeth along with the jaws, teeth and fins of Enchodus.
The Hidden Valley Dolomite is a Silurian−Devonian geologic formation in the northern Mojave Desert of California, in the western United States.
The Fernando Formation is a Pliocene stratigraphic unit in California. Outcrops of the formation in Santa Monica Mountains National Recreation Area have produced fossil shark teeth.
The Drake Bay Formation is a Pliocene stratigraphic unit in California. In 1993, paleontologists excavated a whale skeleton associated with fossil shark teeth and fish vertebrae that may have belonged to a giant salmon from Drake Bay sediments at Point Reyes National Seashore.
The Mountain Springs Formation is Devonian stratigraphic unit in Arizona. The remains of both antiarch and arthrodire placoderms are known from the formation.
The Temple Butte Formation is a Middle-to-Upper Devonian stratigraphic unit in Arizona. The formation's eastern facies in Lake Mead National Recreation Area and Parashant National Monument preserve the remains of prehistoric freshwater fishes like Bothriolepis and placoganoids. In Grand Canyon National Park marine fish left behind the fossilized remains of their bony plates.
Ochopristis is a genus of Late Cretaceous cartilaginous fish whose fossils have been found in the Aguja and Pen Formations of Big Bend National Park, Texas, USA.
Squatirhina is a genus of Late Cretaceous cartilaginous fish whose fossils have been found in the Aguja and Pen Formations of Big Bend National Park, Texas, USA.
The New Mexico Museum of Natural History and Science is a natural history and science museum in Albuquerque, New Mexico near Old Town Albuquerque. The Museum was founded in 1986. It operates as a public revenue facility of the New Mexico Department of Cultural Affairs.
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