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We can establish the fissure fill caves as coastal because they contain marine fossils together with terrestrial and freshwater species. It is on these limestones that I set this painting, a deliberate transfer to avoid one other cycad-stuffed 'semi-arid' Triassic scene. The island residence of M. watsoni was ruled by reptiles - however not essentially those you count on. Though dinosaurs have been widespread, represented by each sauropodomorphs and theropods, the most plentiful and various reptile group had been sphenodonts.
These guys deserve their very own posts and paintings sooner or later, their Mesozoic run being way more than simply spreading tuatara clones the world over. Anyway, the decaying physique of one of these - Planocephalosaurus - could be seen in the foreground of the painting above. As these indicate, the sphenodonts contemporary with M. watsoni weren't large, however they still seemingly gave the resident mammaliaforms a hard time in competing for comparable meals resources.
It is interesting to ponder how these animals carved up their respective ecologies to avoid direct competition with one another. Scientists predict that, if Morganucodon were alive immediately, the sight of them would make grown women leap on their chairs, clutching the skirt tails in fear. What of Morganucodon itself? The skeleton of M. watsoni is small (about 10 cm nose to tail base) and very mammal-like, with differences restricted to high quality anatomical details.
As a result of artwork of Mesozoic mammals scurrying about at night time is so rare, I needed to capture this in my painting. I'm out of time. So many other issues to say, but they will have to wait for one more time.
