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Spicomellus is an extinct genus of early dinosaur from the El Mers III Formation (-) of Morocco. The genus contains a , S. afer, known from a single rib with fused . Spicomellus represents the oldest named ankylosaur.


Discovery and naming
The Spicomellus specimen, PV R 37412, was discovered in layers of the El Mers III Formation near in , Fès-Meknès region, Morocco. It was later acquired by London's Natural History Museum from a commercial fossil dealer. The specimen consists of a single with four co- spines. The holotype was and histologically sectioned to confirm that it was an ankylosaurian.

In 2021, Maidment et al. described Spicomellus afer as a new genus and species of ankylosaurian thyreophoran based on these fossil remains. The , Spicomellus, combines the words spica, meaning "spike" and mellum, which refers to a collar of spikes. The specific name, afer, is a Latin word referring to something inhabiting Africa.

Abundant diverse dinosaurs have been found in Jurassic sediments, but their remains are rarer in deposits. Spicomellus is the second described eurypodan taxon from , after .


Description
The preserved dermal spikes of the holotype were fused directly to the bone, a trait unique to Spicomellus and not known from any other . Some prehistoric animals, including (a ) and (a ), have superficially similar modified ribs. In all other known ankylosaurs, the are embedded into the muscle tissue, rather than fused to underlying bone.


Classification
Preliminary assessments of the holotype led researchers to consider stegosaurian relationships for the species. In their 2021 description of Spicomellus, Maidment et al. discussed several lines of evidence supporting the placement of Spicomellus a basal . They had considered the possibility that the rib was actually part of the jaw of an fish, since some members have teeth fused to their jaws. However, since there is no evidence of ortho—an important component of fish teeth—they considered this classification unsupported. Based on the T-shaped cross section of the rib, Spicomellus can reasonably be assigned to the . Furthermore, the structural fibers of the osteoderms are interwoven, with a -like arrangement, which is seen in ankylosaurs but not other thyreophorans.

Spicomellus is the oldest known ankylosaur that has currently been named from anywhere in the world. Few other ankylosaurs are known from a similar time. , known from a partial lower jaw, was found in England's Oxford Clay Formation, which dates to the age. An unnamed from the -aged Bearreraig Sandstone Formation of the Isle of Skye, Scotland, could be older than Spicomellus, but it is unclear if these fragmentary remains belonged to a or an .


Paleoecology
Spicomellus is known from the El Mers III Formation (El Mers Group) of Morocco. This would have been part of the supercontinent during the . It coexisted with the " Cetiosaurus" mogrebiensis and the and . Predators of the ecosystem consisted of indeterminate theropods (possible ).J. Jenny, A. Le Marrec, and M. Monbaron. (1981). Les empreintes de pas de dinosauriens dans le Jurassique moyen du Haut Atlas central (Maroc): nouveaux gisements et precisions stratigraphiques. Geobos. 14(3):427-431 The sauropod is also known from the contemporaneous terrestrial Guettioua Formation.M. Monbaron, D. A. Russell, and P. Taquet. (1999). Atlasaurus imelakei n.g., n.sp., a brachiosaurid-like sauropod from the Middle Jurassic of Morocco. Comptes Rendus de l'Académie des Sciences à Paris, Sciences de la Terre et des Planètes 329:519-526.

The discovery of Spicomellus also shows that the two major thyreophoran groups ( and ) coexisted for over 20 million years, and implies that the putative extinction of the stegosaurs in the may have happened for reasons other than an increased diversity of anyklosaurs at that time.

Studies by the describing authors of the and of the locality suggested a shallow marine depositional environment with continental mixed , evaporitic and .

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