Comparative morphological evaluation reveals a new species, Glyptotherium deuterophractum, from Brazilian fossil specimens, clarifying longstanding taxonomic misidentifications.
This study reexamines a glyptodontine skull, NHMD 2045557, from Lagoa Santa, Brazil. Initially misidentified as the type of Hoplophorus euphractus by J. Reinhardt, it was later referred to Glyptodon clavipes. This identification remained unchallenged for decades. Recent comprehensive revisions of glyptodontines from northeastern and southeastern Brazil have prompted a reevaluation of the Lagoa Santa material. Currently, it is referred to as Glyptotherium sp., or tentatively, as Glyptotherium cf. cylindricum , a species originally described from Mexico that is also found in Central and North America. However, even if the generic assignment to Glyptotherium is accepted, the specific identity of the Brazilian material remains unresolved. To address this issue, we conducted an exhaustive review of the historical literature, beginning with the foundational works of Lund, Reinhardt, and Winge. We also reexamined the skull NHMD 2045557. Although Lund collected this specimen, Reinhardt first described and illustrated it in 1875 as “ Schistopleurum euphractum ” to replace Hoplophorus euphractus . We argue that Reinhardt misidentified the skull as the type of Hoplophorus euphractus , which invalidates the combination “ Schistopleurum euphractum ”. According to the ICZN, the name-bearing type of H . euphractus fixes the application of the name (Art. 70). Thus, Reinhardt’s classification constitutes a misidentification rather than a taxonomic revision of the original species. Therefore, we propose a new species of Glyptotherium for the aforementioned skull, described as Glyptotherium deuterophractum sp. nov. Comparative analyses with other glyptodont species reveal a distinctive combination of cranial, dental, tarsal, and osteodermal characteristics that distinguish the Brazilian and Venezuelan material from Glyptotherium texanum (from the Pliocene and Early Pleistocene of Central America, Mexico, and the southern United States) and from Glyptotherium cylindricum (Late Pleistocene of Panama, Guatemala, Mexico, and the southern United States).
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Oliveira et al. (2026) studied this question.
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