Abstract
The ranges of a number of distinctive miospores, determined from cored borehole sections in the Lower “Keuper” Marl of west Lancashire and from an outcrop of the Upper “Keuper” Marl and Rhaetic in north Somerset, provide a potential basis for the biostratigraphic subdivision of these deposits and a means of correlating between different British sequences which does not involve reference to the European stage sequence.
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