Arcuites

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Arcuites
Temporal range: Silurian
Trace fossil classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Subphylum: Chelicerata
Order: Eurypterida
Ichnogenus: Arcuites
Vrazo & Ciurca, 2017
Type ichnospecies
Arcuites bertiensis
Vrazo & Ciurca, 2017

Arcuites is an ichnofossil genus, interpreted as a eurypterid swimming trace. Traces produced by swimming eurypterids were described from the Silurian Williamsville Formation (Ontario, Canada) and Tonoloway Formation (Pennsylvania, United States) by Vrazo & Ciurca in 2017 as a new ichnogenus and ichnospecies, named Arcuites bertiensis. [1]

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<span class="mw-page-title-main">Hughmilleriidae</span> Extinct family of eurypterids

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Ciurcopterus is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Ciurcopterus have been discovered in deposits of Late Silurian age in North America. Classified as part of the family Pterygotidae, the genus contains two species, C. sarlei from Pittsford, New York and C. ventricosus from Kokomo, Indiana. The genus is named in honor of Samuel J. Ciurca, Jr., who has contributed significantly to eurypterid research by discovering a large amount of eurypterid specimens, including the four specimens used to describe Ciurcopterus itself.

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<span class="mw-page-title-main">Timeline of eurypterid research</span>

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The Bertie Group or Bertie Limestone, also referred to as the Bertie Dolomite and the Bertie Formation, is an upper Silurian geologic group and Lagerstätte in southern Ontario, Canada, and western New York State, United States. Details of the type locality and of stratigraphic nomenclature for this unit as used by the U.S. Geological Survey are available on-line at the National Geologic Map Database. The formation comprises dolomites, limestones and shales and reaches a thickness of 495 feet (151 m) in the subsurface, while in outcrop the group can be 60 feet (18 m) thick.

References

  1. Matthew B. Vrazo; Samuel J. Ciurca, Jr (2017). "New trace fossil evidence for eurypterid swimming behaviour". Palaeontology. 61 (2): 235–252. doi: 10.1111/pala.12336 .