File:Kayentatherium wellesi.jpg

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Summary

This tritylodont reptile is from the Early Jurassic Kayenta Formation of northeastern Arizona.

The St. George Dinosaur Discovery Site at Johnson Farm (St. George, Utah) is home to exceptionally well-preserved dinosaur tracks, some displaying skin impressions. These tracks, along with hundreds of fossil fish, plants, rare dinosaur remains, invertebrates traces and important sedimentary structures, show evidence that this site was produced along the western edge of a large, Early Jurassic (age between 195-198 million years ago) freshwater lake named Lake Dixie. Source: <a rel="nofollow" class="external text" href="http://www.sgcity.org/dinotrax/">www.sgcity.org/dinotrax/</a>

Licensing

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Date/TimeThumbnailDimensionsUserComment
current18:46, 8 January 2017Thumbnail for version as of 18:46, 8 January 20171,024 × 683 (544 KB)127.0.0.1 (talk)<p>This tritylodont reptile is from the Early Jurassic Kayenta Formation of northeastern Arizona. </p> <p>The St. George Dinosaur Discovery Site at Johnson Farm (St. George, Utah) is home to exceptionally well-preserved dinosaur tracks, some displaying skin impressions. These tracks, along with hundreds of fossil fish, plants, rare dinosaur remains, invertebrates traces and important sedimentary structures, show evidence that this site was produced along the western edge of a large, Early Jurassic (age between 195-198 million years ago) freshwater lake named Lake Dixie. Source: <a rel="nofollow" class="external text" href="http://www.sgcity.org/dinotrax/">www.sgcity.org/dinotrax/</a> </p>
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