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- W1970103375 abstract "A review of lithofacies and fossil distributions in the Downton strata of the Welsh Borderland and Wales indicates that these beds form a suitable basis for definition of a chronostratigraphical division of Series rank within the Silurian System. The basal boundary stratotype for the Downton Series is defined at the base of the Ludlow Bone Bed Member of the Downton Castle Sandstone Formation in a section at Whitcliffe Road, Ludlow. Shallow water marine sediments span the boundary, with no evidence of a measurable time break. Correlation of the base of the Downton Series from eastern North America through Baltoscandia and Poland suggests that it lies at or very close to the base of the Monograptus ultimus Biozone and thus approximates to the base of the Přiacute;dolí beds of Bohemia. This paper formed a submission to the Subcommission on Silurian Stratigraphy in May. 1981. □Silurian, Downtown Series, standard subdivision, lithostratigraphy, biostratigraphy, chronostratigraphy, correlation." @default.
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- W1970103375 date "1982-04-01" @default.
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- W1970103375 title "The Downton Series as the fourth Series of the Silurian System" @default.
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- W1970103375 doi "https://doi.org/10.1111/j.1502-3931.1982.tb01968.x" @default.
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