“…Beck's (1957) study of Tetraxylopteris provided the first clear example of the wealth of information which can be extracted from pyrite permineralizations when analyzed carefully in three planes of section. Since then, there has been a progressive increase in the utilization of pyritic specimens in analysis of the systematics and morphology of fossil plants (Beck, 1960;Carluccio et al, 1966;Marten, 1968;Stockmans, 1968;Scheckler and Banks, 1971a, b;Mustafa, 1975;Grierson, 1976;Bonamo, 1977;Serlin and Banks, 1978;Gensel, 1979;Stein, 1981; to name only a few of many possible examples). This has resulted from a developing knowledge of the chemical and structural properties of pyrite by paleobotanists, and from a growing confidence that such specimens can, indeed, produce useful, detailed data on histological features, modes of trace departure, branching patterns, and the like.…”