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George Gaylord Simpson
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). He was an expert on extinct mammals and their intercontinental migrations. Simpson was extraordinarily knowledgeable about Mesozoic fossil mammals and fossil mammals of North and South America. He anticipated such concepts as punctuated equilibrium (in Tempo and Mode) and dispelled the myth that the evolution of the horse was a linear process culminating in the modern Equus caballus. He coined the word hypodigm in 1940, and published extensively on the taxonomy of fossil and extant mammals. Simpson was influentially, and incorrectly, opposed to Alfred Wegener's theory of continental drift, but accepted the theory of plate tectonics (and continental drift) when the evidence became conclusive.
He was Professor of Zoology at Columbia University, and Curator of the Department of Geology and Paleontology at the American Museum of Natural History from 1945 to 1959. He was Curator of the Museum of Comparative Zoology at Harvard University from 1959 to 1970, and a Professor of Geosciences at the University of Arizona from 1968 until his retirement in 1982.
George Gaylord Simpson was born on June 16, 1902 in Chicago to Helen J. (nee Kinney) and attorney Joseph A. Simpson, with two older sisters, Margaret and Martha. His mother was the daughter of missionaries and had attended Oberlin College. As an infant, Simpson's family moved to Denver, Colorado so that his father could purse land speculation and mining. He grew up in the Capitol Heights neighborhood and spent much of his time outdoors exploring the Rocky Mountain region, but was often unhealthy and plagued by a eye condition that made it difficult to participate in activities like sports. He attended public schools in Denver, graduating in 1918, at the age of 16, and going on to attend the University of Colorado at Boulder. Simpson was interested in creative writing and worked for a literary magazine, but turned his sights to science after taking a geology course under Arthur Tieje. In 1922, Simpson transferred to Yale University in order to pursue geology and paleontology, and graduated in 1923 with a bachelor's in geology.
Simpson was elected to the American Philosophical Society in 1936 and the United States National Academy of Sciences in 1941. In 1943 Simpson was awarded the Mary Clark Thompson Medal from the National Academy of Sciences. For his work, Tempo and mode in evolution, he was awarded the academy's Daniel Giraud Elliot Medal in 1944. He was elected to the American Academy of Arts and Sciences in 1948. He was awarded the Linnean Society of London's prestigious Darwin-Wallace Medal in 1958. Simpson also received the Royal Society's Darwin Medal 'In recognition of his distinguished contributions to general evolutionary theory, based on a profound study of palaeontology, particularly of vertebrates,' in 1962. In 1966, Simpson received the Golden Plate Award of the American Academy of Achievement.
At the University of Arizona, Tucson, the Gould-Simpson Building was named in honor of Simpson and Minnesota geologist and polar explorer Lawrence M. Gould, who, like Simpson, also accepted an appointment as Professor of Geosciences at the University of Arizona after his formal retirement. Simpson was noted for his work in the fields of paleobiogeography and animal evolution.
In his 1944 magnum opus Tempo and Mode in Evolution, Simpson placed significant emphasis on quantum evolution as a major component explaining the morphological change seen in the fossil record, though by the time of writing his 1953 work The Major Features of Evolution, this emphasis had waned. The evolution of Simpson's view on quantum evolution was not due to influence from Theodosius Dobzhansky and Ernst Mayr, as argued by Stephen Jay Gould, but due to the evidence presented by palaeontologists such as Bryan Patterson and Thomas Westoll.
Due in part to his views on differing tempos of evolution, Simpson supported gradistic taxonomy, endorsing the view that humans should be classified as part of a separate family from all other great apes due to their highly derived features having come about from a rapid evolutionary tempo, while all other apes evolved more slowly.
Simpson strongly defended the autonomy of organismic biology and opposed the reductionist approaches to biology, which aimed to reduce biology to physico-chemical processes, that he saw as common among biochemists and molecular biologists.
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George Gaylord Simpson
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). He was an expert on extinct mammals and their intercontinental migrations. Simpson was extraordinarily knowledgeable about Mesozoic fossil mammals and fossil mammals of North and South America. He anticipated such concepts as punctuated equilibrium (in Tempo and Mode) and dispelled the myth that the evolution of the horse was a linear process culminating in the modern Equus caballus. He coined the word hypodigm in 1940, and published extensively on the taxonomy of fossil and extant mammals. Simpson was influentially, and incorrectly, opposed to Alfred Wegener's theory of continental drift, but accepted the theory of plate tectonics (and continental drift) when the evidence became conclusive.
He was Professor of Zoology at Columbia University, and Curator of the Department of Geology and Paleontology at the American Museum of Natural History from 1945 to 1959. He was Curator of the Museum of Comparative Zoology at Harvard University from 1959 to 1970, and a Professor of Geosciences at the University of Arizona from 1968 until his retirement in 1982.
George Gaylord Simpson was born on June 16, 1902 in Chicago to Helen J. (nee Kinney) and attorney Joseph A. Simpson, with two older sisters, Margaret and Martha. His mother was the daughter of missionaries and had attended Oberlin College. As an infant, Simpson's family moved to Denver, Colorado so that his father could purse land speculation and mining. He grew up in the Capitol Heights neighborhood and spent much of his time outdoors exploring the Rocky Mountain region, but was often unhealthy and plagued by a eye condition that made it difficult to participate in activities like sports. He attended public schools in Denver, graduating in 1918, at the age of 16, and going on to attend the University of Colorado at Boulder. Simpson was interested in creative writing and worked for a literary magazine, but turned his sights to science after taking a geology course under Arthur Tieje. In 1922, Simpson transferred to Yale University in order to pursue geology and paleontology, and graduated in 1923 with a bachelor's in geology.
Simpson was elected to the American Philosophical Society in 1936 and the United States National Academy of Sciences in 1941. In 1943 Simpson was awarded the Mary Clark Thompson Medal from the National Academy of Sciences. For his work, Tempo and mode in evolution, he was awarded the academy's Daniel Giraud Elliot Medal in 1944. He was elected to the American Academy of Arts and Sciences in 1948. He was awarded the Linnean Society of London's prestigious Darwin-Wallace Medal in 1958. Simpson also received the Royal Society's Darwin Medal 'In recognition of his distinguished contributions to general evolutionary theory, based on a profound study of palaeontology, particularly of vertebrates,' in 1962. In 1966, Simpson received the Golden Plate Award of the American Academy of Achievement.
At the University of Arizona, Tucson, the Gould-Simpson Building was named in honor of Simpson and Minnesota geologist and polar explorer Lawrence M. Gould, who, like Simpson, also accepted an appointment as Professor of Geosciences at the University of Arizona after his formal retirement. Simpson was noted for his work in the fields of paleobiogeography and animal evolution.
In his 1944 magnum opus Tempo and Mode in Evolution, Simpson placed significant emphasis on quantum evolution as a major component explaining the morphological change seen in the fossil record, though by the time of writing his 1953 work The Major Features of Evolution, this emphasis had waned. The evolution of Simpson's view on quantum evolution was not due to influence from Theodosius Dobzhansky and Ernst Mayr, as argued by Stephen Jay Gould, but due to the evidence presented by palaeontologists such as Bryan Patterson and Thomas Westoll.
Due in part to his views on differing tempos of evolution, Simpson supported gradistic taxonomy, endorsing the view that humans should be classified as part of a separate family from all other great apes due to their highly derived features having come about from a rapid evolutionary tempo, while all other apes evolved more slowly.
Simpson strongly defended the autonomy of organismic biology and opposed the reductionist approaches to biology, which aimed to reduce biology to physico-chemical processes, that he saw as common among biochemists and molecular biologists.