Also known as Bryce Canyon National Park

Where: Garfield County, Utah (37.6° N, 112.2° W: paleocoordinates 43.5° N, 79.5° W)

• coordinate estimated from map

• small collection-level geographic resolution

When: John Henry Member (Straight Cliffs Formation), Late/Upper Santonian (85.8 - 83.5 Ma)

• "uppermost John Henry Member", Paunsaugunt Plateau

Environment/lithology: terrestrial; lithology not reported

Size classes: macrofossils, mesofossils

Primary reference: R. L. Nydam. 2013. Lizards and snakes from the Cenomanian through Campanian of southern Utah: filling the gap in the fossil record of Squamata from the Late Cretaceous of the Western Interior of North America. In A. L. Titus & M. A. Loewen (ed.), At the Top of the Grand Staircase: The Late Cretaceous of Southern Utah 370-423 [P. Barrett/T. Cleary/M. Carrano]more details

Purpose of describing collection: general faunal/floral analysis

PaleoDB collection 181388: authorized by Paul Barrett, entered by Terri Cleary on 09.09.2016, edited by Patricia Holroyd and Matthew Carrano

Creative Commons license: CC BY (attribution)