Abstract

Sediments of the Pekin Formation (Upper Triassic) of the Deep River Basin of North Carolina yield remains of ovulate cones assignable to the genus Voltzia. Ovuliferous scales have a narrow attachment and flare distally into an ascending five-lobed portion. Three seeds were borne on the upper surface of the scale. The cone is placed in a new species, V. andrewsii, that shares some similarities with V. coburgensis. Voltzia andrewsii n. sp. retained certain primitive features of the ovuliferous scale, yet coexisted with a conifer, Compsostrobus neotericus, that had ovulate cones with relatively advanced structure.

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