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Morganucodon watsoni forage for insects and spiders at evening among Carboniferous limestones in early Mesozoic Wales. Empty, torn webs suggest they're having a good evening, while forest fires burn in the background. Vertebrate palaeontology textbooks all the time devote a great chunk of space to morganucodonts, a clade of Triassic-Jurassic Mammaliaformes representing some of the primary wholly 'mammal-like' synapsids. Not too long ago, I was requested to provide a reconstruction of Morganucodon watsoni for some mates (above).
Being better versed in reptiles than mammals, I had to undertake a good bit of research to bring myself up to hurry on morganucodont anatomy and evolution. Seems that fame for being dull is completely unwarranted: Morganucodon, its kinfolk, and the world they inhabited are actually fascinating. We'll begin with the setting. Fossils of M. watsoni occur in British Triassic/lower Jurassic 'fissure fills' cropping out round Bristol and south Wales.
These deposits signify historic infills of caves carved into much older Carboniferous limestones, which are perhaps best recognized for yielding the sauropodomorph Thecodontosaurus. Fissure fill outcrops happen in multiple quarries across the southern UK and are ceaselessly wealthy in fossil material, however the mammaliaforms are rare elements of the fauna constrained to only a few localities.
