Cherry Peak debris block, Bear River Range (Ordovician of the United States)

Where: Cache County, Utah (41.8° N, 111.6° W: paleocoordinates 8.1° S, 79.4° W)

• coordinate estimated from map

• hand sample-level geographic resolution

When: G2 or H trilobite zone, Garden City Formation, Floian (477.7 - 470.0 Ma)

• "Garden City Formation; trilobite zone uncertain, either G2 or H, early to middle Floian, late Early Ordovician"

• formation-level stratigraphic resolution

Environment/lithology: shallow subtidal; lithified, fine-grained grainstone

• "likely similar to the Fillmore [Formation], where a warm, shallow, storm-dominated, clear water environment is indicated(Hintze, 1973; Church, 1974)."
• "Debris block below a cliff face." "Specimen occurs on a fine well-sorted carbonate grainstone from a part of the section containing no other identified macrofossils." "Fine, well-sorted grainstone"

Size class: macrofossils

Reposited in the FMNH

Primary reference: D. B. Blake, T. E. Guensberg, and B. Lefebvre. 2016. New Early Paleozoic Asterozoa (Echinodermata) from the Armorican Massif, France, and the Western United States. Annales de Paléontologie 102:161-181 [P. Novack-Gottshall/P. Novack-Gottshall]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 216838: authorized by Phil Novack-Gottshall, entered by Phil Novack-Gottshall on 28.12.2020

Creative Commons license: CC BY (attribution)

Taxonomic list

• No other fossils, but some burrows present
Stenuroidea
  -
Lopidiaster jamisoni n. gen. n. sp.
Lopidiaster jamisoni n. gen. n. sp. Blake et al. 2016