The Palaeontology Portal
IntroductionPaleontology (/ˌpeɪliɒnˈtɒlədʒi, ˌpæli-, -ən-/ PAY-lee-on-TOL-ə-jee, PAL-ee-, -ən-), also spelled palaeontology or palæontology, 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 classify organisms and study their 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 has been used since 1822 formed 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 it 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, nearly 4 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. (Full article...) Selected article on the prehistoric world and its legaciesCoal balls, despite their name, are calcium-rich masses of permineralised life forms, generally having a round shape. Coal balls were formed roughly 300 million years ago, during the Carboniferous Period. They are exceptional at preserving organic matter, which makes them useful to scientists, who cut and peel the coal balls to research the geological past of the Earth. In 1855, two English scientists, Joseph Dalton Hooker and Edward William Binney, discovered coal balls in England, and the initial research on coal balls was carried out in Europe. It was not until 1922 that coal balls were discovered and identified in North America. Since then, coal balls have been discovered in other countries and they have led to the discovery of over 300 species and 130 genera. Coal balls can be found in coal seams across North America and Eurasia. North American coal balls are relatively widespread, both stratigraphically and geologically, as compared to coal balls from Europe. The oldest known coal balls were found in Germany and the former Czechoslovakia. Did you know?
General images -The following are images from various paleontology-related articles on Wikipedia.
Selected article on paleontology in human science, culture and economicsIn 1858, Charles Darwin and Alfred Russel Wallace published a new evolutionary theory that was explained in detail in Darwin's On the Origin of Species (1859). Unlike Lamarck, Darwin proposedcommon descent and a branching tree of life. The theory was based on the idea of natural selection, and it synthesized a broad range of evidence from animal husbandry, biogeography, geology, morphology, and embryology. The debate over Darwin's work led to the rapid acceptance of the general concept of evolution, but the specific mechanism he proposed, natural selection, was not widely accepted until it was revived by developments in biology that occurred during the 1920s through the 1940s. Before that time most biologists argued that other factors were responsible for evolution. The synthesis of natural selection with Mendelian genetics during the 1920s and 1930s founded the new discipline of population genetics. Throughout the 1930s and 1940s, population genetics became integrated with other biological fields, resulting in a widely applicable theory of evolution that encompassed much of biology—the modern evolutionary synthesis. (see more...) On this day...April 26:
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TopicsGeneral - 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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