Richard Owen,
Antiquity of Man as Deduced from the Discovery of a Human Skeleton
(1884)
“ The general movement of subsidence being resumed, no. 8 is overflowed by waters which leave upon it nearly two feet of pure mud, no. 7. Then a retreat of the overflowing waters with exposure of the surface allows of successive growths and decadence of the plants constituting peat, of which the stratum no. 6, nearly four feet thick, exclusively consists. I need hardly remark that the species of Sphagnum, a genus which contributes most to bog-formations, are mosses that grow in air; they send their roots most abundantly in swampy, clayey soils. ”
