Abstract
Abstract The Albemarle Group is one of the major defining stratigraphic units of the Carolina terrane, the best‐known division of the southern Appalachian peri‐Gondwanan block of Carolinia. As such, the group is a significant factor in the correlation of Carolinia with other peri‐Gondwanan blocks both in the Appalachians and globally. The traditionally held Ediacaran age of the group has been in question for more than a decade because of a report of Late Cambrian and younger fossils from two quarries in the group. The fossil report led to a major revision of the stratigraphy and structural reinterpretation of the Carolina terrane. Our recent studies have focused on the stratigraphy, paleontology, and geochronology of the Cid Formation in the vicinity of one of the reported Paleozoic fossil locales. Contrary to the structural reinterpretation of the Albemarle Group, Cid mudstone is shown to be in conformable and gradational contact with Flat Swamp felsic volcanics of the Cid Formation; we have obtained a p...
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