New Moroccan Dinosaur Discovery Challenges Ancient Continental Isolation Theory

The unearthing of a new species of duck-billed dinosaur in Morocco, named Taleta taleta, supports the hypothesis of intercontinental migrations at the end of the Cretaceous period.
About 66 million years ago, the breakup of the supercontinent Pangaea had created isolated land masses, supposedly home to distinct faunas. The presence of this type of dinosaur, usually associated with the northern hemisphere, on African soil, challenges the idea of total isolation of species.
This find in the phosphate deposits of the Oulad Abdoun basin is not an isolated case. It is the third dinosaur of the Arenysaurini tribe discovered in the region, after Ajnabia odysseus and Minqaria bata. The discovery of the first, Ajnabia, had already indicated that, "despite isolation by oceans, hadrosaurids managed to disperse to Africa at the end of the Cretaceous," as the researchers point out. The arrival of Taleta taleta confirms the existence of a dispersal pattern from Europe.
Moreover, these three African species show significant morphological differences, particularly in their jaws and teeth. This diversity indicates that, once they arrived in Africa, these dinosaurs adapted to exploit different ecological niches without competing. Scientists describe this phenomenon as "dispersal-induced adaptive radiation, with lambeosaurines rapidly diversifying to occupy new niches after their dispersal from Europe to North Africa."
This expansion and diversification on the African continent contrasts with the situation of their North American relatives. Indeed, paleontologists note that "this African radiation coincided with the decline of lambeosaurines in North America." This divergent dynamic shows that dinosaur evolution was not a uniform global phenomenon, but followed distinct regional trajectories.
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