2003•Journal of PaleontologyRequires access

Non-trilobite arthropods from the Silver Peak Range, Nevada

Ben M. Waggoner

Open publisher page 7 citations

Abstract

Two non-trilobite arthropods are described from the Emigrant Formation (Lower Cambrian-Lower Ordovician) in the Silver Peak Range, Esmeralda County, Nevada. A Middle or Upper Cambrian “arachnomorph” arthropod with a phosphatic exoskeleton has been noted in previous faunal lists, but has not been previously described. This fossil is here namedQuasimodaspis brentsaegen. et sp. nov.Q. brentsaebelongs in the Aglaspidida, a close outgroup to the true chelicerates; this is the second report of an aglaspidid from the Great Basin.Esmeraldacaris richardsonaegen. et sp. nov. is a newly discovered arthropod from the lower Ordovician, from beds transitional between the Emigrant Formation and the overlying Palmetto Formation. It is a survivor of an early arthropod lineage that does not belong in any extant taxon, but which may also include the OrdovicianCorcoraniaand the CambrianMollisonia.

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What this paper is about

Two non-trilobite arthropods are described from the Emigrant Formation (Lower Cambrian-Lower Ordovician) in the Silver Peak Range, Esmeralda County, Nevada. A Middle or Upper Cambrian “arachnomorph” arthropod with a phosphatic exoskeleton has been noted in previous faunal lists, but has not been previously described. This fossil is here namedQuasimodaspis brentsaegen. et sp. nov.Q. brentsaebelongs in the Aglaspidida, a close outgroup to the true chelicerates; this is the second report of an aglaspidid from the Great Basin.Esmeraldacaris richardsonaegen. et sp. nov. is a newly discovered arthropod from the lower Ordovician, from beds transitional between the Emigrant Formation and the overlying Palmetto Formation. It is a survivor of an early arthropod lineage that does not belong in any extant taxon, but which may also include the OrdovicianCorcoraniaand the CambrianMollisonia.

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Available abstract

Two non-trilobite arthropods are described from the Emigrant Formation (Lower Cambrian-Lower Ordovician) in the Silver Peak Range, Esmeralda County, Nevada. A Middle or Upper Cambrian “arachnomorph” arthropod with a phosphatic exoskeleton has been noted in previous faunal lists, but has not been previously described. This fossil is here namedQuasimodaspis brentsaegen. et sp. nov.Q. brentsaebelongs in the Aglaspidida, a close outgroup to the true chelicerates; this is the second report of an aglaspidid from the Great Basin.Esmeraldacaris richardsonaegen. et sp. nov. is a newly discovered arthropod from the lower Ordovician, from beds transitional between the Emigrant Formation and the overlying Palmetto Formation. It is a survivor of an early arthropod lineage that does not belong in any extant taxon, but which may also include the OrdovicianCorcoraniaand the CambrianMollisonia.

Key concepts: Trilobite, Arthropod, Paleontology, Ordovician, Geology, Range (aeronautics), Extant taxon, Taxon

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