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George Gaylord Simpson (June 16, 1902 – October 6, 1984) was an American paleontologist. Simpson was perhaps the most influential paleontologist of the twentieth century, and a major participant in the modern synthesis, contributing Tempo and Mode in Evolution (1944), The Meaning of Evolution (1949) and The Major Features of Evolution (1953).
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- Paleontology
Apr 8, 2024 · George Gaylord Simpson (born June 16, 1902, Chicago, Ill., U.S.—died Oct. 6, 1984, Tucson, Ariz.) was an American paleontologist known for his contributions to evolutionary theory and to the understanding of intercontinental migrations of animal species in past geological times.
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George Gaylord Simpson was one of the greatest and most influential paleontologists of all time. He made crucial contributions to evolutionary theory and played a vital role in developing the understanding of intercontinental migrations of extinct mammals.
May 9, 2018 · George Gaylord Simpson (1902-1984), an American paleontologist, moved frequently from New York's American Museum of Natural History, where he was curator, to lecture halls and remote fossil fields. His mastery of the fossil record led to significant advances in theoretical evolution and taxonomy.
George Gaylord Simpson (June 16, 1902 – October 6, 1984) was one the most influential paleontologist of the twentieth century and a major figure in the modern evolutionary synthesis, helping to integrate paleontology into this newly emerging synthetic theory.
BIOGRAPHY. George Gaylord Simpson was born in Chicago, on 16 June 1902. He was the third and last child of Helen J. (Kinney) and Joseph A. Simpson, having been preceded in the world by his sisters, Margaret (1895-1991) and Martha (1898-1984). His father was an attorney who handled railroad claims, but he soon became involved in land speculation ...
Biographical Memoir. Copyright 1991. national aCademy of sCienCes washington d.C. GEORGE GAYLORD SIMPSON. June 16, 1902-October 6, 1984. BY EVERETT C. OLSON1. GEORGE. GAYLORD SIMPSON'S passing in 1984 brought an era in vertebrate paleontology to an end.
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