Arthropoda Siebold, 1845
publication ID |
https://doi.org/ 10.5281/zenodo.13741171 |
persistent identifier |
https://treatment.plazi.org/id/03BD87E1-0668-FFDF-FF6D-4FC4FC6D7710 |
treatment provided by |
Felipe |
scientific name |
Arthropoda Siebold, 1845 |
status |
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Phylum Arthropoda Siebold, 1845 View in CoL View at ENA Class Trilobita Walch, 1771
Discussion.—Trilobites are represented in the acid resistant residues from Newfoundland by a phosphatic mould of the cephalon of an unidentified Dorypygidae ( Fig. 3A View Fig ), silicified cephala of the eodiscid Calodiscus lobatus (Hall, 1847) ( Fig. 3B View Fig ), corynexochids ( Fig. 3C View Fig ), and protaspid olenellids ( Fig. 3D View Fig ). With the exception of C. lobatus , no specimen can be identified to species, although a number of polymeroid trilobites have been reported from the Forteau Formation of western Newfoundland (e.g., Wanneria logani [Walcott, 1910], Olenellus thompsoni [Hall, 1859], Bonnia parvulus Billings, 1861 , B. columbensis Resser, 1938 , “ Conocephalites ” miser Billings, 1861, Antagmus sp. , and other unidentified ptychoparioids; Schuchert and Dunbar [1934]; James and Kobluk [1978]; Knight and Boyce [2000]).
Morphologically diverse, flattened fossils with distinct tubercles and small spines ( Fig. 7J–N) clearly represent fragmented shells of a larger animal, presumably a trilobite. Most specimens appear to be internal moulds formed between the carapace and the doublure. In particular, large curved fragments with small marginal spines may represent the cephalic margins, occasionally with the genal spine preserved ( Fig. 7K). The trilobite(s) would have been covered externally with a multitude of small tubercles, preferentially along the margins of the sclerites. However, no trilobite with comparable tubercles is known from the Lower Cambrian of western Newfoundland, but the current remains are likely derived from meraspids.
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