Having made a general study of the Devonian-Carboniferous junction in North-West Europe and a more detailed one of special areas, the author discusses here the correlation of the Pilton Beds of North Devonshire and the “K beds” of the Bristol and Forest of Dean areas with the Etroeungtian and other horizons near the Devonian-Carboniferous boundary on the Continent.
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H Paul (1937) studied this question.
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