Greater Levantine Formation: Difference between revisions

Greater Levantine Formation (view source)

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 * Dungville Basin: First excavated in 1924 with the purpose of finding sauropods from the Greater Levantine Formation for public display. Several specimens of ''[[Makrylaimis]]'' as well as partial specimens of ''[[Joanusaurus]]'' have been excavated in the Dungville Basin.
-* [[Great Lime Quarry]]: First excavated by geologists from the [[University of Stretton]] in the late 1920s. [[Jour & Leon]] led an expedition in 1931 which discovered that, during the Jurassic, the quarry was a mudhole where several enormous sauropods got stuck and apparently caused a feeding frenzy that lured and trapped many carnivorous dinosaurs. Most specimens of the ''[[Joanusaurus]]'' subspecies ''J. angleii'' are from this site, as well as the ''[[Ligmaceratops]]'' and''[[Strettonsaurus]]''.
+* [[Great Lime Quarry]]: First excavated by geologists from the [[University of Stretton]] in the late 1920s. [[Jour & Leon]] led an expedition in 1931 which discovered that, during the Jurassic, the quarry was a mudhole where several enormous sauropods got stuck and apparently caused a feeding frenzy that lured and trapped many carnivorous dinosaurs. Most specimens of the ''[[Joanusaurus]]'' subspecies ''J. angleii'' are from this site, as well as ''[[Ligmaceratops]]'' and ''[[Strettonsaurus]]''.
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