Abstract
The continuous variation in a group of Late Devonian—Early Carboniferous camerate spores from southern Ireland, assigned to species of Auroraspora, Colatisporites and Endoculeospora can be denoted by recognizing the Auroraspora macra morphon. This non-typological unit is introduced by discussing: (1) the taxonomy of the constituent species [Auroraspora macra Sullivan 1968,
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