Roderick Impey Murchison, ../../ (1862)
“ In speaking of the structure of Russia, I thus wrote:—"The Carboniferous system is surmounted to the east of the Volga by a vast series of beds of marls, schists, limestones, sandstones, and conglomerates, to which I propose to give the name of 'Permian System,' because, although this series represents as a whole the Lower New Red Sandstone (Rothe-todte-liegende) and the Magnesian Limestone or Zechstein, yet it cannot be classed exactly, whether by the succession of the strata or their contents, with either of the German or British subdivisions of this age." ”
