19 Council on Undergraduate Research (Posters) II
Friday, 19 May 2006
8:00 AM - 11:40 AM
QUADRUPED TRACKS FROM THE LOWER JURASSIC MOENAVE FORMATION (HETTANGIAN), ST. GEORGE DINOSAUR DISCOVERY SITE AT JOHNSON FARM, WASHINGTON COUNTY, UTAH
Paper number: 19-19
Program: THEME SESSIONS
Time: 8:00 AM – 11:40 AM
Authors
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Andrew R.C. MilnerSt. George Dinosaur Discovery Site at Johnson Farm, St. George, UT
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C. Frederick LohrengelSouthern Utah University, Cedar City, UT
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Martin G. LockleyUniversity of Colorado at Denver, Denver, CO
Abstract
Measurements of the quadruped tracks and partial trackways, as well as acetate tracings and photographs, confirm the majority of footprints are indeed Batrachopus. Three other forms are recognized from SGDS: (1) possible sphenodontian tracks with elongate manual and pedal digits, potentially pertaining to the poorly known ichnotaxon Exocampe; (2) small (size ranges:2.7-2.8cm lengths; 1.3-1.7cm widths), four-toed, highly digitigrade pes prints resembling synapsid tracks from the Early Jurassic of Argentina, though these tracks may be extramorphological variants of Batrachopus; and (3) larger (size ranges:4.2-6cm lengths; 3.4-5cm widths), possible synapsid pes prints with four, and sometimes five, digits, nearly all showing partial metatarsal impressions. One of these five-toed specimens exhibits clear claw marks and is covered with skin impressions.