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.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
