Abstract
IN his article, “Denudation of the Continents”, Gregor1 estimated the pre-human global denudation rate at about 90–100×1014 g/yr, and obtained an average rate of about 110×1014 g/yr for the time interval from Carboniferous to Recent. His method, however, produced a value of 400×1014 g/yr for pre-Carboniferous Phanerozoic time—a value he questioned seriously himself. We replotted Gregor's data on semilogarithmic paper, converting them from volumes/yr to g/yr using his density factor of 2.6, and fitted them as simple exponential functions by drawing two straight lines; one for Carboniferous to the present, the other for late Pre-Cambrian to Devonian (Fig. 1). The dashed line, which extrapolates to a value of about 300×1014 g/yr, shows the reason for Gregor's 400×1014 g/yr as the depositional rate for these Palaeozoic and late Pre-Cambrian rocks. Such a rate would have to prevail if the rocks of Devonian and older ages have been decaying with a 120–150 m.y. half-life since their time of deposition. It seems much more likely that the Devonian and older sequence represents an interrupted cycle of deposition and destruction, for which the half-life increased markedly after the beginning of a new cycle initiated during the Carboniferous.
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References
Gregor, B., Nature, 228, 273 (1970).
Garrels, R. M., and Mackenzie, F. T., Evolution of Sedimentary Rocks: A Geochemical Approach (Norton, New York, 1971).
Judson, S., Amer. Sci., 56, 356 (1968).
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GARRELS, R., MACKENZIE, F. Gregor's Denudation of the Continents. Nature 231, 382–383 (1971). https://doi.org/10.1038/231382a0
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DOI: https://doi.org/10.1038/231382a0
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