Portal:Paleontology
The Palaeontology Portal
Introduction![]() Paleontology, also spelled as palaeontology or palæontology, is the scientific study of the life of the past, mainly but not exclusively through the study of fossils. Paleontologists use fossils as a means to classify organisms, measure geologic time, and assess the interactions between prehistoric organisms and their natural environment. While paleontological observations are known from at least the 6th century BC, the foundation of paleontology as a science dates back to the work of Georges Cuvier in 1796. Cuvier demonstrated evidence for the concept of extinction and how life of the past was not necessarily the same as that of the present. The field developed rapidly over the course of the following decades, and the French word paléontologie was introduced for the study in 1822, which was derived from the Ancient Greek word for "ancient" and words describing relatedness and a field of study. Further advances in the field accompanied the work of Charles Darwin who popularized the concept of evolution. Together, evolution and extinction can be understood as complementary processes which shaped the history of life. Paleontology overlaps the most with the fields of geology and biology. It draws on technology and analysis of a wide range of sciences to apply them to the study of life and environments of the past, particularly for the subdisciplines of paleobiology and paleoecology that are analogous to biology and ecology. Paleontology also contributes to other sciences, being utilized for biostratigraphy to reconstruct the geologic time scale of Earth, or in studies on extinction to establish both external and internal factors that can lead to the disappearance of a species. Much of the history of life is now better understood because of advances in paleontology and the increase of interdisciplinary studies. Several improvements in understanding have occurred from the introduction of theoretical analysis to paleontology in the 1950s and 1960s that led to the rise of more focused fields of paleontology that assess the changing geography and climate of Earth, the phylogenetic relationships between different species, and the analysis of how fossilization occurs and what biases can impact the quality of the fossil record. (Full article...) Selected article on the prehistoric world and its legacies
Othnielosaurus is a genus of ornithischian dinosaur that lived about 155 to 148 million years ago, during the Late Jurassic-age Morrison Formation of the western United States. It is named in honor of famed paleontologist Othniel Charles Marsh, and was formerly assigned to the genus Laosaurus. This genus was coined to hold fossils formerly included in Othnielia, which is based on remains that may be too sparse to hold a name; as such, it is part of decades of research to untangle the taxonomy left behind by Marsh and his rival Edward Drinker Cope from the Bone Wars. Othnielosaurus has usually been classified as a hypsilophodont, a type of generalized small bipedal herbivore or omnivore, although recent research has called this and the existence of a distinct group of hypsilophodonts into question. (see more...)
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General images -The following are images from various paleontology-related articles on Wikipedia.
Selected article on paleontology in human science, culture and economics
The history of paleontology traces the history of the effort to study the fossil record left behind by ancient life forms. Although fossils had been studied by scholars since ancient times, the nature of fossils and their relationship to life in the past became better understood during the 17th and 18th centuries. At the end of the 18th century the work of Georges Cuvier ended a long running debate about the reality of extinction and led to the emergence of paleontology as a scientific discipline.
The first half of the 19th century saw paleontological activity become increasingly well organized. This contributed to a rapid increase in knowledge about the history of life on Earth, and progress towards definition of the geologic time scale. As knowledge of life's history continued to improve, it became increasingly obvious that there had been some kind of successive order to the development of life. After Charles Darwin published Origin of Species in 1859, much of the focus of paleontology shifted to understanding evolutionary paths. The last half of the 19th century saw a tremendous expansion in paleontological activity, especially in North America. The trend continued in the 20th century with additional regions of the Earth being opened to systematic fossil collection, as demonstrated by a series of important discoveries in China near the end of the 20th century. There was also a renewed interest in the Cambrian explosion that saw the development of the body plans of most animal phyla. (see more...) On this day...
Probable Ankylosaur Ossicles from the Middle Cenomanian Dunvegan Formation of Northwestern Alberta, Canada Michael E. Burns, Matthew J. Vavrek published 09 May 2014 Air Space Proportion in Pterosaur Limb Bones Using Computed Tomography and Its Implications for Previous Estimates of Pneumaticity Elizabeth G. Martin, Colin Palmer published 09 May 2014 Selected image
CategoriesTopicsGeneral - Paleontology - Fossil - Evolution - Extinction Quality ContentFeatured 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
- Spinosaurus
- Stegosaurus
- Stegoceras
- Styracosaurus
- Tarbosaurus
- Thescelosaurus
- Triceratops
- Tyrannosaurus
- Velociraptor
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