Abstract
Millimetre sized chitinophosphatic brachiopods ("microbrachiopods") largely, but by no means entirely, centred around the family Acrotretidae are commonly regarded as being in decline after the early Ordovician. Work on Irish Upper Ordovician limestones however shows that this is not the case, material recovered showing both numerical abundance and taxonomic diversity in beds of Ashgill age. Although forms are known from the Devonian, the published record of these neglected fossils from the Silurian is sparse, so that the effects, if any, of the end‐Ordovician event on this ecologically enigmatic group cannot as yet be determined.
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