Abstract
The latest Cretaceous saw the final diversification of dinosaurs before the K/Pg extinction. Discussions of end-Cretaceous dinosaur diversity have focused on well-sampled faunas from Laurasia; far less is known about dinosaurian faunas of the Southern Hemisphere, especially Africa. The late Maastrichtian Phosphates of Morocco provide a rare window into African dinosaur diversity. Abelisaurids, lambeosaurines, and titanosaurian sauropods are known. However, no diagnostic titanosaur remains have been recovered, leaving the affinities of these sauropods unclear. We describe Phosphatotitan khouribgaensis gen. et sp. nov., a new titanosaur from the Maastrichtian of Sidi Chennane, Khouribga Province. Phosphatotitan is represented by dorsal, sacral, and caudal vertebrae, and the pelvis. The new species differs from titanosaurs described from the Cretaceous of Africa and Europe but resembles South American Lognkosauria, and especially Patagotitan, in having short dorsal and caudal centra, expanded dorsal and caudal neural spines, and a broad pubis. Its small size relative to other Lognkosauria (3.5–4 tonnes) suggests a lineage selected for small size. The close relationships of Morocco’s titanosaurs and abelisaurids to South American species may reflect a wide distribution of these clades prior to the opening of the South Atlantic and the separation of Africa and South America ~100 Ma, while a complex pattern of oceanic dispersal may explain the presence of distinct saltasauroid lineages worldwide. The latest Cretaceous Gondwanan dinosaur faunas were highly endemic due to a combination of continental fragmentation, extinction, and dispersal, creating high endemism in southern continents and within Africa, suggesting that Maastrichtian dinosaur diversity is underestimated.
| Original language | English |
|---|---|
| Pages (from-to) | 241 |
| Journal | Diversity |
| Volume | 18 |
| Issue number | 5 |
| DOIs | |
| Publication status | Published - 22 Apr 2026 |
Data Availability Statement
All data are available in the paper or its online Supporting Materials.Acknowledgements
Thanks to Fernando Novas and Charlie Scherer for discussions. Thanks to the Universidad de la Patagonia San Juan Bosco for access to specimens. Thanks to Mustapha Meharich for assistance in Ouled Bou Ali. Thanks to Mick Green and Shaun Smith for help with preparation.Funding
This research received no external funding. Research work of XPS is supported by the Basque Government (IT 1485-22) and the Spanish Ministry of Science, Innovation and Universities, The State Research Agency and the European Regional Development Fund (Project PID2024-158833OB-I00 funded by MICIU/AEI/10.13039/501100011033/FEDER,UE).
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