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Small shelly fossils from the argillaceous facies of
the Lower Cambrian Forteau Formation of western
Newfoundland
CHRISTIAN B. SKOVSTED and JOHN S. PEEL
Skovsted, C.B. and Peel, J.S. 2007. Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau For−
mation of western Newfoundland. Acta Palaeontologica Polonica 52 (4): 729–748.
A diverse fauna of helcionelloid molluscs, hyoliths, and other small shelly fossils is described from limestone layers
within the Forteau Formation of the Bonne Bay region in western Newfoundland. The fauna is dominated by internal
moulds of various molluscs and tubular problematica, but also includes hyolith opercula, echinoderm ossicles, and other
calcareous small shelly fossils preserved by phosphatisation. Originally organophosphatic shells are comparatively rare,
but are represented by brachiopods, hyolithelminths, and tommotiids. The fauna is similar to other late Early Cambrian
faunas from slope and outer shelf settings along the eastern margin of Laurentia and may be of middle Dyeran age. The
similarity of these faunas indicates that at least by the late Early Cambrian, a distinctive and laterally continuous outer
shelf fauna had evolved. The Forteau Formation also shares elements with faunas from other Early Cambrian provinces,
strengthening ties between Laurentia and Australia, China, and Europe during the late Early Cambrian. Two new taxa of
problematic fossil organisms are described, the conical Clavitella curvata gen. et sp. nov. and the wedge−shaped
Sphenopteron boomerang gen. et sp. nov.
Key words: Helcionellidae, Hyolitha, Brachiopoda, small shelly fossils, Cambrian, Laurentia, Newfoundland.
Christian B. Skovsted [Christian.Skovsted@geo.uu.se], Centre for Ecostratigraphy a
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