Bulletin of the Mizunami Fossil Museum, no. 45 (March 15, 2019), p. 7–13, 3 fi gs., 1 table. © 2019, Mizunami Fossil Museum Oligocene pagurized gastropods from the River Bend Formation, North Carolina, USA Rodney M. Feldmann1, Carrie E. Schweitzer2, and George E. Phillips3 1Department of Geology, Kent State University, Kent, Ohio 44242 USA <
[email protected]> 2Department of Geology, Kent State University at Stark, 6000 Frank Ave. NW, North Canton, Ohio 44720 USA <
[email protected]> 3Conservation and Biodiversity Section, Mississippi Museum of Natural Science, 2148 Riverside Drive, Jackson, Mississippi 39202 USA <
[email protected]> Abstract Fourteen specimens of pagurized gastropods are completely enveloped by anascan cheilostome bryozoan colonies, and most of them bear serpulid worm tubes referred to Hydroides sp. These specimens from the Oligocene River Bend Formation in North Carolina constitute the first such occurrence on the Atlantic coastal region of North America. Key words: Decapoda, Paguroidea, biotic associations, Cymatium, North Carolina Introduction immediately adjacent to the Onslow County quarry, this “very arenaceous bivalve biocalcirudite” (Ward, The River Bend Formation is an Oligocene, sandy, 2002) contains conspicuous numbers of the scallop carbonate unit exposed in quarries in east-central North Rebeccapecten trentensis (Harris, 1919), the jingle shell Carolina. The formation has yielded an abundance of Anomia ruffini Conrad, 1843, the cyclostome bryozoan fossil material, but to date no decapod crustaceans have Meandropora cf. M. cerebriformis (de Blainville, 1843), and been reported. Discovery of small gastropods invested by the small regular echinoid Psammechinus carolinensis bryozoans and serpulid worms provide evidence that the Kier, 1997. (based on MMNS samples collected by D.