The trace fossil Neonereites multiserialis Pickerill and Harland, 1988 from the Devonian Wapske Formation, northwest New Brunswick

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Abstract

Preserved typically in positive hyporelief on sandstone soles, the ichnospecies can potentially be confused with morphologically similar ichnotaxa, particularly Granularia Pomel, Ophiomorpha Lundgren, Ardelia Chamberlain and Baer and Edaphichnium Bown and Kraus, and is best differentiated by undertaking, whenever possible, vertical transverse and longitudinal sectioning of the structures. The records and included proposed synonymy suggest that Neonereites multiserialis is Silurian (Wenlock) to Tertiary (Eocene) in age and is indicative of deep-water flysch environments. -Author

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APA

Pickerill, R. K. (1991). The trace fossil Neonereites multiserialis Pickerill and Harland, 1988 from the Devonian Wapske Formation, northwest New Brunswick. Atlantic Geology, 27(2), 119–126. https://doi.org/10.4138/1727

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