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law of faunal succession
law of faunal succession The principle, first recognized at the beginning of the 19th century by William Smith, that different strata each contain particular assemblages of fossils by which the rocks may be identified and correlated over long distances; and that these fossil forms succeed one another in a definite and habitual order. This law, together with the law of superposition of strata, enables the relative age of a rock to be deduced from its content of fossil faunas and floras.
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Cite this article
AILSA ALLABY and MICHAEL ALLABY. "law of faunal succession." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. 31 May. 2012 <http://www.encyclopedia.com>. AILSA ALLABY and MICHAEL ALLABY. "law of faunal succession." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. (May 31, 2012). http://www.encyclopedia.com/doc/1O13-lawoffaunalsuccession.html AILSA ALLABY and MICHAEL ALLABY. "law of faunal succession." A Dictionary of Earth Sciences. 1999. Retrieved May 31, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O13-lawoffaunalsuccession.html |
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law of faunal succession
law of faunal succession See faunal succession.
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Cite this article
MICHAEL ALLABY. "law of faunal succession." A Dictionary of Ecology. 2004. Encyclopedia.com. 31 May. 2012 <http://www.encyclopedia.com>. MICHAEL ALLABY. "law of faunal succession." A Dictionary of Ecology. 2004. Encyclopedia.com. (May 31, 2012). http://www.encyclopedia.com/doc/1O14-lawoffaunalsuccession.html MICHAEL ALLABY. "law of faunal succession." A Dictionary of Ecology. 2004. Retrieved May 31, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O14-lawoffaunalsuccession.html |
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