Cirripedes (Crustacea) from the Neogene and Pleistocene of Lee Creek Mine, Beaufort County, North Carolina, USA

Authors

  • Andrew Scott Gale School of the Environment and Life Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth PO1 3QL, UK; Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK
  • Eric Sadorf 315 Hemlock Street, Cary, North Carolina 27513, USA

DOI:

https://doi.org/10.24425/agp.2026.158194

Abstract

Seven species of balanomorph cirripedes are recorded from the Miocene to Pleistocene succession exposed in a phosphate mine in North Carolina; although collected loose, most probably originated from the Pliocene Yorktown Formation. Four of the species belong to the balanid subfamily Concavinae, i.e., Chesaconcavus proteus (Conrad, 1834), Arossia aurae Zullo, 1992, Paraconcavus talquinensis (Wiesbord, 1966), P. cf. prebrevicalcar (Ross, 1964), and one to the subfamily Amphibalaninae, i.e., Fistulobalanus multiseptatus (Ross, 1964). A chelonibiid (turtle barnacle), Protochelonibia collaretai sp. nov. is new, and the living balanine Balanus
calidus (Pilsbry, 1916) is recorded from the Pleistocene (Calabrian) James River Formation.

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Published

2026-06-29

How to Cite

Gale, Andrew Scott, and Eric Sadorf. “Cirripedes (Crustacea) from the Neogene and Pleistocene of Lee Creek Mine, Beaufort County, North Carolina, USA”. Acta Geologica Polonica, vol. 76, no. 2, June 2026, p. e80, doi:10.24425/agp.2026.158194.

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