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  1. Charles Doolittle Walcott (March 31, 1850 – February 9, 1927) was an American paleontologist, administrator of the Smithsonian Institution from 1907 to 1927, and director of the United States Geological Survey.

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  2. Charles Doolittle Walcott, 1850-1927. The fourth Secretary of the Smithsonian, Charles Doolittle Walcott, was a paleontologist noted for his discovery of the Burgess Shale fossils in Canada in the early twentieth century. Largely self-educated, Walcott worked for the New York State Museum and US Geological Survey (USGS), and advanced to become ...

  3. Charles Doolittle Walcott, was a paleontologist. He is often noted for his discovery of the Burgess Shale fossils in Canada in the early twentieth century. After his time as USGS Director, he then served as Secretary of the Smithsonian Institution until his death in 1927.

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  5. paleontologist Charles D. Walcott, who suggested that living forms rapidly evolved during the time between the deposition of the youngest Precambrian and the oldest Cambrian sediments and that no record of this interval, the Lipalian interval, exists because the rocks have been eroded or remain undiscovered.….

  6. Charles Doolittle Walcott. 1917-1923 NAS President. When the United States entered the war, the Academy's president, William H. Welch, decided to accept a high-ranking position in the Army Medical Corps and resigned from his Academy post.

  7. CHARLES DOOLITTLE WALCOTT 473 known in the early studies of natural history in New York State. He had a profound influence on the young Walcott, lending him books and giving him many suggestions. Several years later, as Walcott recalled in a sketch written in 1916, when he was driving a wagon the wheel hit a drift-block of sandstone and split ...

  8. Charles Doolittle Walcott was an American paleontologist, administrator of the Smithsonian Institution from 1907 to 1927, and director of the United States Geological Survey. He is famous for his discovery in 1909 of well-preserved fossils, including some of the oldest soft-part imprints, in the Burgess Shale of British Columbia, Canada.

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