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 The Palaeontology Portal
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Modern paleontology sets ancient life in its context by studying how long-term physical changes of global geography paleogeography and climate paleoclimate have affected the evolution of life, how ecosystems have responded to these changes and have adapted the planetary environment in turn and how these mutual responses have affected today's patterns of biodiversity. Hence, paleontology overlaps with geology (the study of rocks and rock formations) as well as with botany, biology, zoology and ecology – fields concerned with life forms and how they interact. The major subdivisions of paleontology include paleozoology (animals), paleobotany (plants) and micropaleontology (microfossils). Paleozoologists may specialise in invertebrate paleontology, which deals with animals without backbones or in vertebrate paleontology, dealing with fossils of animals with backbones, including fossil hominids (paleoanthropology). Micropaleontologists study microscopic fossils, including organic-walled microfossils whose study is called palynology. There are many developing specialties such as paleobiology, paleoecology, ichnology (the study of tracks and burrows) and taphonomy (the study of what happens to organisms after they expire). Major areas of study include the correlation of rock strata with their geologic ages and the study of evolution of lifeforms.  The Ediacaran biota were ancient lifeforms representing the earliest known complex multicellular organisms. They appeared soon after the Earth thawed from the Cryogenian period's extensive glaciers, and largely disappeared soon before the rapid appearance of biodiversity known as the Cambrian explosion, which saw the first appearance in the fossil record of the basic patterns and body-plans that would go on to form the basis of modern animals. Little of the diversity of the Ediacaran biota would be incorporated in this new scheme, with a distinct Cambrian biota arising and usurping the organisms that dominated the Ediacaran fossil record. Some Ediacaran organisms might have been closely related to groups that would rise to prominence later, but most non-microscopic fossils are morphologically distinct from later lifeforms, resembling discs, mud-filled bags, or quilted mattresses. Classification is difficult, and the assignment of some species even at the level of kingdom — animal, fungus, protist or otherwise — is uncertain: one paleontologist has even gained support for a separate kingdom Vendobionta. Their strange form and apparent disconnectedness from later organisms have led some to consider them a "failed experiment" in multicellular life, with later multicellular life independently re-evolving from unrelated single-celled organisms. (more...)
Artist credit: User:Apokryltaros Dinosaur-related topics - Dinosaur - Creationist perspectives on dinosaurs - Cretaceous-Tertiary extinction event - Cultural depictions of dinosaurs- Dinosaur-bird connection - Dinosaur classification - Feathered dinosaurs - List of dinosaurs - Living dinosaurs - Paleontology - Physiology of dinosaurs - Prehistoric life - Prehistoric reptiles Featured dinosaur articles - Acrocanthosaurus - Albertosaurus - Allosaurus - Archaeopteryx - Chicxulub Crater - Compsognathus - Cretaceous–Tertiary extinction event - Daspletosaurus - Deinonychus - Dinosaur - Diplodocus - Gorgosaurus - Iguanodon - Lambeosaurus - List of dinosaurs - Majungasaurus - Massospondylus - Parasaurolophus - Psittacosaurus - Stegosaurus - Styracosaurus - Tarbosaurus - Thescelosaurus - Triceratops - Tyrannosaurus - Velociraptor Current Dinosaur FACs - None yet...
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