Skip to main navigation menu Skip to main content Skip to site footer

Articles

Vol 54 (2018)

Microvertebrates from the Silurian–Devonian boundary beds of the Eastport Formation, Maine, eastern USA

DOI
https://doi.org/10.4138/atlgeol.2018.006
Submitted
November 13, 2017
Published
June 15, 2018

Abstract

Agnathan and gnathostome remains, associated with lingulid brachiopod fragments and distinctive ostracods, have been extracted from a small calcareous mudstone sample collected from the type section of the Eastport Formation on the northern shore of Moose Island, Maine. The vertebrate assemblage includes osteostracan, anaspid, and thelodont scales, and acanthodian scales, spines and teeth, which support a late Pridoli, or possibly earliest Lochkovian, age for the stratum. The thelodont Paralogania denisoni n. sp. is described, associated with a single thelodont scale referred tentatively to Talivalia? sp. indet., and acanthodians Nostolepis striata, Gomphonchus sandelensis, andPoracanthodes punctatus in a fauna that shows similarities to late Pridoli assemblages in Britain, parts of Europe, Russia, Greenland, and arctic Canada.