“…More recently, Pachut and Anstey (2002) applied cladistic techniques to a data set consisting of 202 specimens, recognizing eight species of the Middle and Upper Ordovician bryozoan genus Peronopora. A subsequent paper (Anstey and Pachut, 2004) extended the earlier analysis by comparing cladisticallydefined species to those recognized using phenetic methods. Eight Boardman and Utgaard (1966), plate 133, figures 1a and 1b, respectively: 1, tangential section of massive topotype with abundant mesozooecia in central macula and common cystiphragms (USNM 146486); 2, longitudinal section of same zoarium (USNM topotype suite 43829) illustrating a monticule at the top of the image; vertical, attenuated, mesozooecia bend out of the plane of the section; 3, 4, Peronopora decipiens (lectotype, UMMP 6676-3), from Boardman and Utgaard (1966), plate 135, figures 1c, 1f, respectively: 3, tangential section illustrating a monticule and mesozooecia; 4, longitudinal section showing a break in median lamina (broken vertical line), making it discontinuous, and autozooecia budding from its left and right sides; overlapping series of cystiphragms are common within autozooecia;.…”