Portal:Paleontology

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Introduction

A paleontologist at work at John Day Fossil Beds National Monument

Paleontology, sometimes spelled palaeontology, (/ˌpliɒnˈtɒləi, ˌpæli-, -ən-/) is the scientific study of life that existed prior to, and sometimes including, the start of the Holocene Epoch (roughly 11,700 years before present). It includes the study of fossils to determine organisms' evolution and interactions with each other and their environments (their paleoecology). Paleontological observations have been documented as far back as the 5th century BC. The science became established in the 18th century as a result of Georges Cuvier's work on comparative anatomy, and developed rapidly in the 19th century. The term itself originates from Greek παλαιός, palaios, "old, ancient", ὄν, on (gen. ontos), "being, creature" and λόγος, logos, "speech, thought, study".

Paleontology lies on the border between biology and geology, but differs from archaeology in that it excludes the study of anatomically modern humans. It now uses techniques drawn from a wide range of sciences, including biochemistry, mathematics, and engineering. Use of all these techniques has enabled paleontologists to discover much of the evolutionary history of life, almost all the way back to when Earth became capable of supporting life, about 3.8 billion years ago. As knowledge has increased, paleontology has developed specialised sub-divisions, some of which focus on different types of fossil organisms while others study ecology and environmental history, such as ancient climates.

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Artist's impression of Massospondylus depicting the animal as bipedal.
Massospondylus (meaning 'elongated vertebra') is a genus of prosauropod dinosaur from the early Jurassic Period (Hettangian to Pliensbachian ages, ca. 200–183 million years ago). It was described by Sir Richard Owen in 1854 from remains found in South Africa, and is thus one of the first dinosaurs to have been named. Fossils have since been found in Lesotho, Zimbabwe, and other parts of South Africa. Further material from Arizona's Kayenta Formation, India, and Argentina has been assigned to this genus, but may not belong to Massospondylus.

The type, and only universally recognized species, is M. carinatus, although six other species have been named during the past 150 years. Prosauropod systematics have undergone numerous revisions during the last several years, and many scientists disagree where exactly Massospondylus lies on the dinosaur evolutionary tree. The family name Massospondylidae was once coined for the genus, but because knowledge of prosauropod relationships is in a state of flux, it is unclear which other dinosaurs—if any—belong in a natural grouping of massospondylids; several 2007 papers support the family's validity.

Although Massospondylus was long depicted as quadrupedal, a 2007 study found it to be bipedal. It was probably a herbivore, although it is speculated that the prosauropods may have been omnivorous. This animal, 4–6 meters (13–20 ft) long, had a long neck and tail, with a small head and slender body. On each of its forefeet, it bore a sharp thumb claw that was used in defense or feeding. Recent studies indicate Massospondylus grew steadily throughout its lifespan, possessed air sacs similar to those of birds, and may have cared for its young. (see more...)

Selected article on paleontology in human science, culture and economics

The eponymous petrified wood at Petrified Forest National Park
Petrified Forest National Park is a United States national park in Navajo and Apache counties in northeastern Arizona. Named for its large deposits of petrified wood, the park covers about 146 square miles (380 km2), encompassing semi-desert shrub steppe as well as highly eroded and colorful badlands. The site, the northern part of which extends into the Painted Desert, was declared a national monument in 1906 and a national park in 1962.

The Petrified Forest is known for its fossils, especially fallen trees that lived in the Late Triassic, about 225 million years ago. The sediments containing the fossil logs are part of the widespread and colorful Chinle Formation, from which the Painted Desert gets its name. Beginning about 60 million years ago, the Colorado Plateau, of which the park is part, was pushed upward by tectonic forces and exposed to increased erosion. All of the park's rock layers above the Chinle, except geologically recent ones found in parts of the park, have been removed by wind and water. In addition to petrified logs, fossils found in the park have included Late Triassic ferns, cycads, ginkgoes, and many other plants as well as fauna including giant reptiles called phytosaurs, large amphibians, and early dinosaurs. Paleontologists have been unearthing and studying the park's fossils since the early 20th century. (see more...)

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A fossil life restoration of
A fossil of Mongolarachne

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A mounted replica skeleton of Tetragonias njalilus

A mounted replica skeleton of the Middle Triassic dicynodontid Tetragonias njalilus from Tanzania. The mount is on display at the Staatliches Museum für Naturkunde in Karlsruhe, Germany.
Photo credit: H. Zell

Topics

General - Paleontology - Fossil - Evolution - Extinction
History - History of paleontology - Bone Wars - List of years in paleontology
Locations - List of dinosaur-bearing rock formations - List of fossil sites - Como Bluff - Coon Creek Formation - Dinosaur Cove - Dinosaur National Monument - Dinosaur Park Formation - Dinosaur State Park and Arboretum - Glen Rose Formation - Hell Creek Formation - Lance Formation - Morrison Formation - Red Gulch Dinosaur Tracksite - Two Medicine Formation
Paleontologists - Mary Anning - Robert T. Bakker - Barnum Brown - William Buckland - Edward Drinker Cope - Jack Horner - Gideon Mantell - Othniel Charles Marsh - John Ostrom - Dong Zhiming
Geologic Time - Paleozoic Era - Cambrian (Early Cambrian - Middle Cambrian - Furongian) - Ordovician (Early Ordovician - Middle Ordovician - Late Ordovician) - Silurian (Llandovery - Wenlock - Ludlow - Pridoli) - Devonian (Early Devonian - Middle Devonian - Late Devonian) - Carboniferous (Mississippian - Pennsylvanian) - Permian (Cisuralian - Guadalupian - Lopingian) - Mesozoic Era - Triassic (Early Triassic - Middle Triassic - Late Triassic) - Jurassic (Early Jurassic - Middle Jurassic - Late Jurassic) - Cretaceous (Early Cretaceous - Late Cretaceous) - Cenozoic Era - Paleogene (Paleocene - Eocene - Oligocene) - Neogene (Miocene - Pliocene) - Quaternary (Pleistocene - Holocene)
Fringe and Pseudoscience - Creationist perspectives on dinosaurs - Living dinosaurs
Popular Culture - Cultural depictions of dinosaurs - Jurassic Park (novel) - Jurassic Park (film) - Stegosaurus in popular culture -Tyrannosaurus in popular culture - Walking with...

Quality Content

Featured paleontology articles - Achelousaurus - Acrocanthosaurus - Albertosaurus - Allosaurus - Amargasaurus - Ankylosaurus - Apatosaurus - Archaeopteryx - Baryonyx - Carnotaurus - Catopsbaatar - Ceratosaurus - Chicxulub Crater - Compsognathus - Cretaceous–Tertiary extinction event - Daspletosaurus - Deinocheirus - Deinonychus - Deinosuchus - Dilophosaurus - Dinosaur - Diplodocus - Dromaeosauroides - Edmontosaurus - Elasmosaurus - Giganotosaurus - Gorgosaurus - Herrerasaurus - Iguanodon - Istiodactylus - Lambeosaurus - List of dinosaur genera - Majungasaurus - Massospondylus - Megalodon - Nemegtomaia - Nigersaurus - Opisthocoelicaudia - Paranthodon - Parasaurolophus - Plateosaurus - Psittacosaurus - Seorsumuscardinus - Stegosaurus - Stegoceras - Styracosaurus - Tarbosaurus - Thescelosaurus - Triceratops - Tyrannosaurus - Velociraptor
Good paleontology articles - Abelisauridae - Alioramus - Amphicoelias - Archaeoraptor - Batrachotomus - Ceratopsia - Coelurus - Dromaeosauridae - Giganotosaurus - Gryposaurus - Heterodontosauridae - Herrerasaurus - Hypacrosaurus - Kritosaurus - Othnielosaurus - Pachycephalosaurus - Saurolophus - Sauropelta - Scelidosaurus - Species of Allosaurus - Species of Psittacosaurus - Spinosaurus - Tyrannosauroidea

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