Where: Esmeralda County, Nevada (37.8° N, 117.3° W: paleocoordinates 1.3° S, 94.8° W)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: middle Member (Poleta Formation), Dyeran (515.3 - 511.2 Ma)
• depostied above storm wave base. The base of the Dyeran is 88m above the base of the middle member of the Poleta Formation
• 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 10497: authorized by Mark Patzkowsky, entered by Phil Borkow on 11.05.2001
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
| |
Obolellata | |
Obolella sp. Billings 1861 | |
Trilobita | |
|