Thomas C. Chamberlin,
Geology
(1906)
“ But, as a matter of fact, a large amount of organic matter has not gone back completely to the inorganic state, and this residue constitutes a factor of no small importance in the geological record.The organic residue.—There is a certain portion of vegetation that is not consumed by animals or by other plants, and that escapes combustion641 and all kinds of ordinary decay, and this constitutes a part of the organic residue. Animals never completely oxidize all the organic matter they take into their systems; their bodies never entirely consume themselves. ”
