Also known as LWQ
Where: Emery County, Utah (39.1° N, 110.9° W: paleocoordinates 39.5° N, 64.9° W)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Ruby Ranch Member (Cedar Mountain Formation), Aptian to Aptian (125.0 - 100.5 Ma)
• bonebed is 15 m above contact with Morrison Formation
•
•Overall, based on zircon ages and chemostratigraphic studies, the Ruby Ranch Member ranges in age from approximately middle Aptian to middle Albian (about 118 to 105 Ma) for the western Paradox Basin and northern San Rafael Swell. Other radiometric ages indicate the presence of upper Albian strata as well (Chure and others, 2010; Ludvigson and others, 2010a, 2015; Sprinkel and others, 2012)
• bed-level stratigraphic resolution
Environment/lithology: fluvial; lenticular, nodular limestone and calcareous mudstone
Size class: macrofossils
Collection methods: quarrying, mechanical,
Primary reference: F. L. DeCourten. 1991. The Long Walk Quarry and Tracksite: unveiling the mysterious Early Cretaceous of the Dinosaur Triangle region. In W. R. Averett (ed.), Guidebook for Dinosaur Quarries and Tracksites Tour, Western Colorado and Eastern Utah 19-25 [M. Carrano/M. Carrano]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 27047: authorized by Matthew Carrano, entered by Matthew Carrano on 14.11.2002
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
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Titanosauriformes indet.1 Salgado et al. 1997 sauropod dorsal centra, caudals, partial dentary, teeth, limb and pes elements
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