Researchers at the University of Birmingham, the Natural History Museum and Virginia Tech University have named the animal Mambawakale ruhuhu. It is among the last to be studied of a collection of fossils dug up nearly 60 years ago from the Manda Beds, a geological formation in southern Tanzania.
The remains, which are the only known example of Mambawakale ruhuhu, include a partial skull, lower jaw, several vertebrae and a hand. From these, the research team were able to identify several distinctive features that set it apart from other archosaurs found in the Manda Beds.
These included a large skull, more than 75 cm in length, and a particularly large nostril, as well as a notably narrow lower jaw and strong variation in the sizes of the teeth at the front of the upper jaws.
Mambawakale ruhuhu would have been a large and terrifying predator, which roamed across Tanzania some 240 million years ago.
Richard Butler, Professor of Palaeobiology at the University of Birmingham
“Our analysis identifies Mambawakale as one of the oldest known archosaurs and an early member of the lineage that eventually evolved into modern crocodilians. It’s an exciting discovery, because identifying this animal helps us to understand the rapid early diversification of archosaurs and enables us to add a further link to the evolutionary story of modern-day crocodiles.”
The study, published in Royal Society Open Science, also ties up the final loose end of an ambitious fossil expedition, undertaken by scientists including the palaeontologist Alan Charig in 1963. Although most of the finds brought back from that expedition have now been formally described and catalogued, Mambawakale ruhuhu has remained unpublished until now.
In naming the specimen, the research team sought to recognise the previously little acknowledged contributions of Tanzanians to the success of the 1963 expedition. The name chosen derives from Kiswahili, one of the native languages of Tanzania. Mambawakale means ancient crocodile, and ruhuhu refers to the Ruhuhu Basin, the region within which the fossil was excavated.
