Abstract. Diverse assemblages of well preserved miospores and microplankton have been obtained from a series of samples collected across the boundary between the Bedford Shale and Berea Sandstone Formations in central Ohio. The miospores indicate a Late Devonian (pre-Carboniferous Tournaisian)* age for each of the samples. The microplankton support this age determination. A number of microplankton species not previously recorded from North America are present.
CITATION STYLE
Molyneux, S. G., Manger, W. L., & Owens, B. (1984). Preliminary account of Late Devonian palynomorph assemblages from the Bedford Shale and Berea Sandstone Formations of central Ohio, U.S.A. Journal of Micropalaeontology, 3(2), 41–51. https://doi.org/10.1144/jm.3.2.41
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