
Organism · Placental mammals
Sclerocalyptus ornatus
Source time context (not species duration) · ≈ 2.6–0.01 Ma
Inferred life reconstruction
Sclerocalyptus ornatus
Overview
Sclerocalyptus ornatus is a fossil glyptodont known from its skull and body armor plates. Records include vertebrae and shoulder bones as well as plate fragments. It reveals the hard body covering together with the internal skeleton.[2]
Loading illustration…
Key facts
AGM 006 records a partial skull, carapace fragments, vertebrae, and a shoulder blade. Different body regions appear together in one specimen inventory, broadening comparisons from the skull to the trunk.[2]
Time and place
It is a glyptodont known from Pleistocene layers. This interval spans approximately 2.6 million to 12,000 years ago. Research reexamining the Roth collection from the Argentine Pampas also considers comparative material of this species.[3][5]
The time range describes source context, not the complete duration of this species.
Size, form and skeleton
The skull and bony plates of the carapace provide direct clues to its form. Comparative studies also examine the ends of the nasal bones and ossified nasal cartilage. Hard external plates and internal skull structures reveal different features.[1][2]
A study treating Sclerocalyptus ornatus as “Neosclerocalyptus ornatus” reports a skull length of 320 mm for specimen MLP 16-28. This skull, about 32 cm long, provides a concrete indication of the armored mammal’s head size.[6]
Loading illustration…
Habitat and reproduction
How were bones connected inside an armor-covered body? Examining vertebrae and the shoulder blade together with carapace material reveals aspects of trunk organization. Research questions begin by viewing several regions side by side.[2]
Fossil discovery
Its naming history includes names such as Glyptodon ornatus and Sclerocalyptus. Later researchers proposed reassigning Roth collection specimen PIMUZ A/V 447 to ornatus. Renewed comparison of old collections refined the connection between name and form.[4][3]
References
- Comparative study of head structure in Neosclerocalyptus
- Glyptodont study — Composition of specimen AGM 006
- Study of xenarthrans in the Santiago Roth collection
- Study of the name and armour plates of Sclerocalyptus
- International Commission on Stratigraphy — Pleistocene boundaries
- Zurita, Carlini & Scillato-Yané (2008) — A new species of Neosclerocalyptus Paula Couto, 1957 (Xenarthra, Glyptodontidae, Hoplophorinae) from the middle Pleistocene of the Pampean region, Argentina
- Zurita, Carlini & Scillato-Yané (2008) — A new species of Neosclerocalyptus Paula Couto, 1957 (Xenarthra, Glyptodontidae, Hoplophorinae) from the middle Pleistocene of the Pampean region, Argentina
- Florida Museum of Natural History — Catalogue of Pachyarmatherium type specimens
- Downing·White (1995) — Armor and skeleton of Pachyarmatherium
- McDonald(2005) — Body size and evolution of North American edentates
Research questions
Which features can be used to reclassify a skull collected long ago? The front of the snout, region around the nostrils, and armor form can be compared together. Finding the same regions in several specimens makes classification criteria more concrete.[1][3]
Observation
Move your gaze from the large armor outline to individual small plates, then to the front of the head. Body-covering plates and skull organization provide different clues to glyptodonts.[1][2]
Related organisms
Armor plates and internal skeletons of ancient mammals
Examine the different records of bodies and time preserved in these two organisms. Sclerocalyptus ornatus: a fossil glyptodont known from its skull and body armor plates, with records of vertebrae and shoulder bones as well as plate fragments. It is known from Pleistocene layers; the Pleistocene spans approximately 2.6 million to 12,000 years ago. Pachyarmatherium leiseyi: a fossil mammal with thick armor of bony plates. A narrow overlapping region lies between the shoulder and pelvic armor. The institutional type-specimen inventory records this species as Early Pleistocene. The Pleistocene as a whole spans approximately 2.6 million to 12,000 years ago.