Charles Doolittle Walcott | |
|---|---|
 | |
| 4th Secretary of the Smithsonian Institution | |
| In office 1907–1927 | |
| Preceded by | Samuel Pierpont Langley |
| Succeeded by | Charles Greeley Abbot |
| 3rd Director of the United States Geological Survey | |
| In office 1894 (1894) – 1907 (1907) | |
| Preceded by | John Wesley Powell |
| Succeeded by | George Otis Smith |
| 4th Director of the National Advisory Committee for Aeronautics | |
| In office 1920–1927 | |
| President | Calvin Coolidge |
| Preceded by | John R. Freeman |
| Succeeded by | Joseph Sweetman Ames |
| Personal details | |
| Born | (1850-03-31)March 31, 1850 New York Mills, New York, U.S. |
| Died | February 9, 1927(1927-02-09) (aged 76) Washington, D.C., U.S. |
| Resting place | Rock Creek Cemetery Washington, D.C. |
| Spouses | |
| Children | 4 |
| Signature | .png) |
| Scientific career | |
| Awards | Bigsby Medal(1895) Wollaston Medal(1918) Mary Clark Thompson Medal(1921) |
| Fields | Paleontology |
| Institutions | Smithsonian Institution US Geological Survey |
| Author abbrev. (zoology) | Walcott |
Charles Doolittle Walcott (March 31, 1850 – February 9, 1927) was an Americanpaleontologist, administrator of theSmithsonian Institution from 1907 to 1927, and the third director of theUnited States Geological Survey.[1][2] He is famous for his discovery in 1909 of well-preservedfossils, including some of the oldest soft-part imprints, in theBurgess Shale ofBritish Columbia, Canada.
Charles Doolittle Walcott was born on March 31, 1850, inNew York Mills, New York. His grandfather, Benjamin S. Walcott, moved from Rhode Island in 1822. His father, also Charles Doolittle Walcott, died when Charles Jr. was only two. Walcott was the youngest of four children.[3] He was interested in nature from an early age, collecting minerals andbird eggs and, eventually, fossils. He attended various schools in the Utica area but left at the age of eighteen without completing high school, the end of his formal education.[4] His interest in fossils solidified as he became a commercial fossil collector.[4]
On January 9, 1872, Walcott married Lura Ann Rust, daughter of the owner of a farm in New York where Walcott made one of his most importanttrilobite discoveries (Walcott-Rust quarry). She died on January 23, 1876. Walcott's interest in fossils led to his acquaintance withLouis Agassiz of Harvard University, who encouraged him to work in the field ofpaleontology; later that year, he began work as the assistant to the state paleontologist,James Hall. He lost this job after two years but was soon recruited to the newly formedUS Geological Survey as a geological assistant.[4]
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Walcott began his professional paleontology career by discovering new localities, such as theWalcott-Rust quarry in upstate New York and the Georgia Plane trilobite beds in Vermont, and by selling specimens to Yale University. In 1876, he became the assistant toJames Hall, State Geologist of New York. Walcott also became a member of theAmerican Association for the Advancement of Science.
In 1879, Walcott joined theUS Geological Survey and rose to become chief paleologist in 1893 and then director in 1894. His work focused onCambrian strata in locations throughout the United States and Canada; his numerous field trips andfossil discoveries made important contributions tostratigraphy.
He married Helena Breese Stevens in 1888. They had four children between 1889 and 1896: Charles Doolittle Walcott, Sydney Stevens Walcott, Helena Breese Walcott, and Benjamin Stuart Walcott.
Walcott was elected to theNational Academy of Sciences in 1896, theAmerican Philosophical Society in 1897, and theAmerican Academy of Art and Sciences in 1899.[5][6][7] In 1901, he served both as president of theGeological Society of America[8] and thePhilosophical Society of Washington.[9] In 1902, he met withAndrew Carnegie and became one of the founders and incorporators of theCarnegie Institution of Washington. He served in various administrative and research positions in that organization. In 1921 Walcott was awarded the inauguralMary Clark Thompson Medal from theNational Academy of Sciences.[10]
He served aspresident of the American Association for the Advancement of Science in 1923. He previously spearheaded the U.S. Geological Survey under PresidentTheodore Roosevelt.[4]
Walcott had an interest in the conservation movement and assisted its efforts.[4]
Walcott became Secretary of theSmithsonian Institution in 1907 after the death ofSamuel Pierpont Langley, holding the post until his own death. He was succeeded byCharles Greeley Abbot. Because of Walcott's responsibilities at the Smithsonian, he resigned as director of the United States Geological Survey.[4] As part of the centennial celebration of Darwin's birth, Walcott was awarded an honorary doctorate by the University of Cambridge in 1909.[11]
In 1910, the year after his discovery of508 million year old (middle Cambrian) fossils in theBurgess shale, Walcott returned to the area accompanied by his sons Stuart and Sidney. Together they examined all the layers on the ridge above the point where the fossil-laden rock had been found, eventually finding the fossiliferous band. Between 1910 and 1924, Walcott returned repeatedly to collect more than 65,000 specimens from what is now known as theWalcott Quarry, named after him. The find includes exceptional preservation of the soft parts of its fossils, one of the oldest fossil beds containing soft-part imprints.
Walcott's wife Helena died in a train crash in Connecticut in 1911. In 1914, Walcott married his third wife,Mary Morris Vaux, an amateur artist and avid naturalist. She accompanied him on his expeditions, enjoying the study of nature. She made watercolor illustrations of wildflowers as she traveled with him in Canada.
Although Walcott spent a considerable amount of time at the Burgess Shale quarry on what became known as Fossil Ridge, he also traveled widely in other areas of the CanadianRockies. Some of his numerous scientific publications feature spectacular panoramic photographs of the mountains taken from high passes or high on mountain slopes.
In 1914 Walcott convened a conference in Washington, D.C. for the purpose of stimulating interest in aeronautic science, and its relation to the U.S. government. The conference led to anact of congress organizing an Advisory Committee for Aeronautics (later named theNational Advisory Committee for Aeronautics) "to supervise and direct the scientific study of the problems of flight with a view to their practical solution."[12] This committee was composed of twelve members, two each from the Army and Navy, one each representing the Smithsonian Institution, theWeather Bureau, and theNational Bureau of Standards. Five additional members were chosen "who shall be acquainted with the needs of aeronautical science, either civil or military, or skilled in aeronautical engineering or its allied sciences". Brigadier GeneralGeorge P. Scriven,Chief Signal Officer of the Army, was chairman of the committee; Walcott was elected chairman of the Executive Committee.William F. Durand was one of the civilian members of the Committee.[12]
In light of theWright brothers patent war and to discredit the Wright brothers,Glenn Curtiss in 1914 helped Walcott secretly make major modifications to a failed aerodrome built in 1903 by ProfessorSamuel Langley to make it appear able to fly. After the flight demonstrations, Walcott ordered the Langley machine be restored to its 1903 condition to cover up the deception before it was put on display.[13][14] It took until 1928 for the Smithsonian Board of Regents to pass a resolution acknowledging that the Wright brothers deserved the credit for "the first successful flight with a power-propelled heavier-than-air machine carrying a man."[15][16]
After Walcott's death in Washington, D.C., his samples, photographs, and notes remained in storage until their rediscovery by a new generation of paleontologists in the late 1960s. Since then, many of his interpretations have been revised.
Walcott would be little known today if he had not been brought to attention byStephen Jay Gould's bookWonderful Life (1989). In this book, Gould put forth his opinion that Walcott failed to see the differences among the Burgess Shale species and "shoehorned" most of these fossils into existing phyla. Many paleontologists would now take a much less negative view of Walcott's descriptions and of the theoretical perspective that shaped them.[17]
Walcott's work on Ordovician trilobites of New York also tended to be overlooked until, in the early 1990s, Rochester-based amateur paleontologist Thomas Whiteley revived Walcott's research and re-opened theWalcott–Rust quarry near Russia, New York. This localized stratum has some of the best preservedLaurentian trilobites ever found, including enrolled specimens with soft body parts.
The Walcott Peak, near where he first discovered the Burgess Shale onMount Burgess inCanada, was named after him. The nearbyWalcott Quarry, with thePhyllopod bed of Burgess Shale fossils betweenWapta Mountain andMount Field, is also named for him. TheCharles Doolittle Walcott Medal is awarded by theNational Academy of Sciences every five years for outstanding work in the field ofPrecambrian andCambrian life and history.
TheWorld War IILiberty ShipSS Charles D. Walcott was named in his honor.
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| Preceded by | Director of theUnited States Geological Survey 1894–1907 | Succeeded by |
| Preceded by | Secretary of theSmithsonian Institution 1907–1927 | Succeeded by |
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