Sometime in the late 70s or early 80s, geology student Thomas Schröter was hiking through the red rocks of Algarve, Portugal when he spotted some fossil bone. They didn’t relate to the thesis he was working on, but he picked them up anyway. While not especially remarkable, the scraps nevertheless made the customary transition from field to museum collection and were later appraised as those of a metoposaur – salamander-like amphibians that could get up to 10 feet long and lived a lifestyle one of my professors once called “crocodiling before there were crocodiles.”
These enormous amphibians were, and are, anything but rare. They’re among the most common fossils found in the 237-201 million year old rock representing Late Triassic time, sometimes clustered together in dense bonebed where they died en masse. And as paleontologists Stephen Brusatte, Richard Butler, Octávio Mateus, and Sébastien Steyer found when they relocated the Algarve site in 2009 after reading a short description of the fragments plucked from the site, Schröter had discovered another such graveyard.
What brought so many Metoposaurus together to die isn’t clear. At this point, the researchers write, it’s unknown whether they died in the place they were entombed or their remains were washed in from elsewhere. But seasonal droughts could have played a role.
Regardless of the reason for their death, though, the fossils are part of a metoposaur band that ran across the middle of Pangaea, the only outliers being a cluster in prehistoric India and Madagascar. Future finds will alter this picture to greater or lesser degrees, but it may be that metoposaurs thrived in hot, highly-seasonal environments where early dinosaurs stayed small and croc cousins ruled while different predators waited along the shores of higher-latitude habitats. The only way to find out more is to keep digging.
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