Where: Esmeralda County, Nevada (37.8° N, 117.3° W: paleocoordinates 3.5° S, 96.8° W)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: middle Member (Poleta Formation), Montezuman to Montezuman (520.0 - 516.0 Ma)
• depostied above storm wave base.
• group of beds-level stratigraphic resolution
Environment/lithology: lithified, gray, calcareous siltstone and lithified, shelly/skeletal limestone
Preservation: trace
Collection methods: bulk,
• Most of the trilobites are found as broken sclerites in thin bioclastic limestone, but intact cephala are occasionally found in the shaly siltstone.
Primary reference: J. S. Hollingsworth. 1999. Proposed stratotype section and point for the base of the Dyeran Stage. Laurentai 99: V field conference of the Cambrian Stage and Subdivision 38-42 [M. Patzkowsky/P. Borkow]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 10496: authorized by Mark Patzkowsky, entered by Phil Borkow on 11.05.2001
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Trilobita | |
Holmiella sp. Fritz 1972 trilobite | |
Nevadia parvoconica trilobite | |
Geraldinella sp. trilobite | |
Nevadella sp. Raw 1936 trilobite
Nevadella eucharis Walcott 1913 trilobite |