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giving a lower limit for the age of the solar system.
It is hypothesised that the accretion of Earth began soon after the formation of the calcium-aluminium-rich inclusions and the meteorites.
material and is consistent with the radiometric ages of the oldest-known terrestrial and lunar samples.
Following the development of radiometric age-dating in the early 20th century, measurements of lead in uranium-rich minerals showed that some were in excess of a billion years old.
These had assumed that the original heat of the Earth and Sun had dissipated steadily into space, but radioactive decay meant that this heat had been continually replenished.
Their values were consistent with Thomson's calculations.
He did not realize that the Earth mantle was convecting, and this invalidated his estimate.
In 1895, John Perry produced an age-of-Earth estimate of 2 to 3 billion years using a model of a convective mantle and thin crust.
For biologists, even 100 million years seemed much too short to be plausible.
In Darwin's theory of evolution, the process of random heritable variation with cumulative selection requires great durations of time.His value of 56 million years added additional evidence that Thomson was on the right track.