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PALEONTOLOGY
Paleontology (sometimes spelled palaeontology) is the study of the developing history of life on Earth, including ancient plants and animals, based on their fossil record (evidence of their prehistoric existence as typically preserved in sedimentary rocks). This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilized feces (coprolites) and chemical residues.
Overview
Modern paleontology sets ancient life in its contexts 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 changed 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 living creatures and how they interact.
The major subdivisions of paleontology include paleozoology (animals), paleobotany (plants) and micropaleontology (microfossils). Paleozoologists may specialize 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.
Paleontology utilizes the same classic binomial nomenclature scheme, devised for the biology of living things by the mid-18th century Swedish biologist Carolus Linnaeus and increasingly sets these species in a genealogical framework, showing their degrees of interrelatedness using the still somewhat controversial technique of 'cladistics'.
The primary economic importance of paleontology lies in the use of fossils to determine the age and nature of the rocks that contain them or the layers above or below. This information is vital to the mining industry and especially the petroleum industry. Simply looking at the fossils contained in a rock remains one of the fastest and most accurate means of telling how old that rock is.
Fossils were known by primitive humans and were sometimes identified correctly as the remains of ancient lifeforms. The organized study of paleontology dates from the late 18th century.
Notable paleontologists
History includes a number of prominent paleontologists. Charles Darwin collected fossils of South American mammals during his trip on the Beagle and examined petrified forests in Patagonia. Mary Anning was a notable early paleontologist. She found several landmark fossils, in her home town of Lyme Regis. Although self-taught, she collected and described them in a very systematic way. Thomas Jefferson took a keen interest in mammoth bones. Besides looking at mammal teeth and digging up penguins, George Gaylord Simpson played a crucial role in bringing together ideas from biology, paleontology and genetics, to help create the 'Modern Synthesis' of evolutionary biology. His book "Tempo and Mode" is a classic in the field. Prominent names in invertebrate paleontology include Steven Stanley, Stephen Jay Gould, David Raup and Jack Sepkoski, who have done much to expand our understanding of long-term patterns in the evolution of life on earth. Large names in the field of paleoanthropology include Louis, Mary and Richard Leakey and Donald Johanson.
Other important figures include the Englishman William Smith, who first noted that similar fossil sequences were found regionally and Georges Cuvier, who initiated the study of ancient animals based on living animals. Notable American figures include Edward Drinker Cope, Othniel Charles Marsh, Paul Sereno, Henry Fairfield Osborn, Louis Agassiz, Charles Walcott and Roy Chapman Andrews. Distinguished European paleontologists include the Englishmen Thomas Huxley, William Buckland and Richard Owen, Finn Björn Kurtén, Czech paleoentomologists Dragutin Gorjanovic-Kramberger and Jarmila Kukalova-Peck, Belgian Louis Dollo and French Pierre Teilhard de Chardin. Franz Nopcsa von Felsö-Szilvás is often credited for being the founder of palaeobiology, a field of inquiry dealing with the biological and ecological functions that can be deduced from fossils. Elsewhere, South African John T. Robinson discovered the nearly complete fossil skull of Australopithecus africanus. More modern figures in paleontology include John Ostrom, Bob Bakker, David B. Weishampel, Jack Horner and Alex Rasnitsyn.
See also
External links
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