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Joseph Leidy (born Sept. 9, 1823, Philadelphia—died April 30, 1891, Philadelphia) was a zoologist, one of the most distinguished and versatile scientists in the United States, who made important contributions to the fields of comparative anatomy, parasitology, and paleontology.

Soon after his appointment as librarian and curator at the Philadelphia Academy of Natural Sciences (1846), he became chairman of the Board of Curators (1847–91). The founder of paleontology in the United States, he made extensive studies of fossil deposits in the western states. The first of his many works on the subject, “On the Fossil Horse of America” (1847), showed that the horse had lived and become extinct on the North American continent long before the arrival of Columbus. He subsequently proved the prehistoric presence in the western United States of the lion, tiger, camel, and rhinoceros.

In 1848 he published Researches into the Comparative Anatomy of the Liver, the first thorough study made of that organ. Upon his appointment as professor of anatomy at the University of Pennsylvania (1853–91), he established himself as a leader in parasitology with the publication of A Flora and Fauna Within Living Animals (1853), the first important study of the parasites of the alimentary canal. His discovery of Trichina spiralis in pork led to Rudolf Leuckart’s discovery of the cause of trichinosis in man.

Mushrooms growing in forest. (vegetable; fungus; mushroom; macrofungi; epigeous)
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The chief U.S. authority of his time on protozoa, Leidy published several works on the lower animal orders. One, Fresh Water Rhizopods of North America (1879), became a standard work. In all, he published more than 600 works, among which are the Elementary Treatise on Human Anatomy (1861), recognized as a classic American text on the subject, and “On the Extinct Mammalia of Dakota and Nebraska” (1869), described by the prominent U.S. paleontologist Henry Osborn as possibly the most important paleontological work produced in the United States.

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paleontology, scientific study of life of the geologic past that involves the analysis of plant and animal fossils, including those of microscopic size, preserved in rocks. It is concerned with all aspects of the biology of ancient life forms: their shape and structure, evolutionary patterns, taxonomic relationships with each other and with modern living species, geographic distribution, and interrelationships with the environment. Paleontology is mutually interdependent with stratigraphy and historical geology because fossils constitute a major means by which sedimentary strata are identified and correlated with one another. Its methods of investigation include that of biometry (statistical analysis applied to biology), which is designed to provide a description of the forms of organisms statistically and the expression of taxonomic relationships quantitatively.

Paleontology has played a key role in reconstructing Earth’s history and has provided much evidence to support the theory of evolution. Data from paleontological studies, moreover, have aided petroleum geologists in locating deposits of oil and natural gas. The occurrence of such fossil fuels is frequently associated with the presence of the remains of certain ancient life-forms.

Paleontological research dates back to the early 1800s. In 1815 the English geologist William Smith demonstrated the value of using fossils for the study of strata. About the same time, the French zoologist Georges Cuvier initiated comparative studies of the structure of living animals with fossil remains.

Cross section of Earth showing the core, mantle, and crust
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The Editors of Encyclopaedia BritannicaThis article was most recently revised and updated by Adam Augustyn.
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