Clair Cameron Patterson (born Claire Cameron Patterson Jr.; June 2, 1922 – December 5, 1995) was an American geochemist. Born in Des Moines and raised in nearby Mitchellville, Iowa, he graduated from Grinnell College. He later received his Ph.D. from the University of Chicago and spent his entire professional career at the California Institute of Technology (Caltech).
In collaboration with George Tilton, Patterson developed the lead–lead dating method, adapting established procedures for uranium–lead dating. By using lead isotopic data from the Canyon Diablo meteorite, he calculated an age for the Earth of 4.55 billion years, a figure far more accurate than estimates existing at the time and one that has remained largely unchallenged since 1956.
Patterson first encountered ubiquitous lead contamination in the late 1940s as a graduate student at the University of Chicago. Later, his work on this subject led to a major reevaluation in the United States and worldwide of the unregulated growth of industrial lead concentrations in the atmosphere and human body. His activism on this issue proved seminal in the banning of leaded gasoline and leaded solder in food cans.
Patterson was born in Des Moines and raised in Mitchellville, Iowa. His father was a mail carrier, and his mother served on the local school board. He had a brother and a sister. From a young age, he displayed intellectual curiosity. He graduated from high school in 1939 at the age of 16 and enrolled at nearby Grinnell College, where he studied chemistry and met his future wife, Lorna "Laurie" McCleary. He received a bachelor's degree in chemistry in 1943.
Patterson and McCleary both attended graduate school at the University of Iowa, where he earned an M.A. in molecular spectroscopy and they married in 1944. They subsequently worked as civilian scientists on the Manhattan Project, first at the University of Chicago and later at Oak Ridge, Tennessee, where Patterson specialized in mass spectrometry.
After World War II, the Pattersons returned to Chicago, where Laurie worked as an infrared spectroscopist while Patterson pursued a Ph.D. under Harrison Brown at the University of Chicago. During his doctoral research, Patterson discovered that lead contamination was pervasive throughout his laboratory, even in his own hair. This finding sparked his long-term interest in environmental lead pollution and led to pioneering studies demonstrating the widespread presence of toxic lead in the atmosphere and the environment.
Following a postdoctoral year at the University of Chicago, Patterson and Brown moved to the California Institute of Technology (Caltech) in Pasadena, California, in 1952 as founding members of Caltech's new geochemistry program, now part of the Division of Geological and Planetary Sciences. Patterson remained at Caltech for the rest of his life. He and Laurie had four children.
Measurement of the Earth's age
Patterson's postdoc work at the University of Chicago was under Harrison Brown, who teamed him with George Tilton to study geological aging of zircon crystals. Zircon is extremely useful for geological dating: when forming, it collects tiny imperfections of uranium, but never lead. It follows that if lead is present in zircon, it must have come from decay of the uranium present. (The process is known as U-Pb dating.) The team measured the concentrations and isotopic compositions of foreign elements inside the zircon. Tilton measured the uranium and Patterson the types and amounts of lead. Patterson's goal was to calculate the composition of primordial lead in the Earth. Then it would be possible to calculate the age of the Earth—and, in turn, of the Solar System by using the same techniques on meteorites.
After beginning their work in 1948, Patterson soon noted that his lead samples were being contaminated. The age of the igneous rock from which the zircon came was known, and Tilton's uranium measurements aligned with what was expected in the zircon at that particular age; but Patterson's data typically was skewed with "too much" lead. After six years, the team published a paper on methods of determining the ages of zircon crystals and Patterson earned his Ph.D., but they were no closer in determining the age of the Earth.
Brown received a grant from the United States Atomic Energy Commission to continue work on dating the Earth, but more importantly, he was selected to commission a new mass spectrometer in Pasadena, California at Caltech. In 1953, Brown and Patterson arrived at Caltech, where Patterson was authorized to build his own lab from scratch. He proceeded to secure all points of entry from air and other contaminants. He acid-cleaned all apparatuses and even distilled all chemicals shipped to him. In essence, Patterson created one of the first laboratory clean rooms, here to prevent lead contamination of his work and his data. He finished his analysis of the Canyon Diablo meteorite in 1953, and used the mass spectrometer at the Argonne National Laboratory on isolated iron-meteorite lead to collect data on the abundance of lead isotopes. With the new data, he published "Age of Meteorites and the Earth" in 1956, the first paper explaining the "true" age of the solar system's accretion as 4.550Gy ± 70My; a figure that has remained largely unchallenged since.
Before his paper, it was largely believed the Earth was around 3.3 billion years old. Patterson generously shared credit for the work with his colleagues.
Tracing geochemical evolution of Earth
Patterson's ability to isolate quantities of lead at microgram levels from ordinary rocks and to determine their isotopic compositions enabled him to analyse for lead in sediment samples of the Atlantic and Pacific oceans. Deriving comparative bases from the different ages during which landmasses had drained into the oceans, he showed that the impact of anthropogenic lead being dispersed into the environment was more than 100 times the amount of lead leached naturally into the ocean by surface streams. To Patterson, the Earth's geochemical cycle for lead appeared to be badly out of balance.
To work around the limitations of then-available analytic procedures, Patterson developed new approaches. He found that in comparing similar metals, such as barium, surface ocean waters contained up to 20 times more lead than deep ocean waters. Such evidence caused him to doubt the commonly held view that anthropogenic activities had increased lead concentrations only by a factor of (about) two over naturally occurring levels.
Patterson returned to the problem of his initial experiments and the contamination he had found in the blanks used for sampling. He determined—by analysing ice-core samples from Camp Century in Greenland taken in 1964 and from Antarctica in 1965—that atmospheric lead levels had begun to increase steadily and dangerously soon after tetraethyl lead (TEL) was introduced after being developed to reduce engine knock in internal combustion engines. Patterson then identified 'leaded' engine fuels and the several other uses of lead in manufacturing as the cause of the contamination of his samples. Aware of the significant public-health implications of his findings, he devoted the rest of his life to eliminating lead from being introduced into the environment.
Campaign against lead poisoning
In 1965 Patterson published his paper Contaminated and Natural Lead Environments of Man, beginning his efforts to draw public attention to the problem of increasing lead levels in the environment including the food chain. He criticized the experimental methods of other scientists and thus encountered strong opposition from those then recognized as experts, including Robert A. Kehoe, a noted scientist and strong proponent of the lead producing manufacturers.