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Born:
June 7, 1896, Hanover, Ger.
Died:
June 10, 1971, Tübingen, W.Ger. (aged 75)

Otto Heinrich Schindewolf (born June 7, 1896, Hanover, Ger.—died June 10, 1971, Tübingen, W.Ger.) was a German paleontologist, known for his research on corals and cephalopods. Schindewolf was a faculty member of the University of Marburg from 1919 until 1927, when he became director of the Geological Survey of Berlin; in 1948 he became a professor at the University of Tübingen, where he retired as professor emeritus in 1964.

Schindewolf’s research on invertebrate fossils led him to question whether the modern theory of evolution, which includes the study of how population genetics may account for change within a given species, could always be applied to the origin of types; he doubted in particular whether the theory could explain the origin of the higher taxonomic categories, such as families, orders, and classes. Studying different fossil species of coral and ammonites obtained from sequential geological strata, he concluded that the most recent taxonomic categories could not have arisen by slow, intermediate steps, generally thought to characterize evolution, but rather by large, single transformations. He drew attention, for example, to the ammonites, in which the anatomical chambers that were successively occupied by the animal preserve the details of both its development and its evolution. The genetic changes responsible for these structural characteristics would have occurred in a single generation and at an early stage of the embryo, he argued; in the following generations the structure would persist through successively later stages of the individual until it became firmly established even in the adult form. Though his views are not accepted by many biologists, particularly the population geneticists, who consider them too controversial, he has drawn attention to fundamental problems in evolution.

Schindewolf wrote Grundfragen der Paläontologie (1950; “Basic Questions of Paleontology”), Grundlagen und Methoden der paläontologischen Chronologie (3rd ed., 1950; “Foundations and Methods of Paleontological Chronology”), and Studien zur Stammesgeschichte der Ammoniten (1961–68; “Studies on the Phylogeny of Ammonites”).

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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.

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The Editors of Encyclopaedia BritannicaThis article was most recently revised and updated by Adam Augustyn.
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