Adolf Carl Noé was an Austrian-born paleobotanist. He is credited for identifying the first coal ball in the United States in 1922, which renewed interest in them. He also developed a method of peeling coal balls using nitrocellulose. Many of the paleobotanical materials owned by the University of Chicago's Walker Museum were provided by Noé, where he was also a curator of fossil plants. He was also a research associate at the Field Museum of Natural History, where he assisted with their reconstruction of a Carboniferous forest.
A coal ball
A coal ball is a type of concretion, varying in shape from an imperfect sphere to a flat-lying, irregular slab. Coal balls were formed in Carboniferous Period swamps and mires, when peat was prevented from being turned into coal by the high amount of calcite surrounding the peat; the calcite caused it to be turned into stone instead. As such, despite not actually being made of coal, the coal ball owes its name to its similar origins as well as its similar shape with actual coal.
A coal ball
Sir Joseph Dalton Hooker, who along with Edward William Binney was the first to report on coal balls
Calcite (middle) and dolomite (top and bottom) are common materials found in coal balls.
A coal ball from southern Illinois