Neosclerocalyptus is an extinct genus of glyptodont that lived during the Pliocene, Pleistocene, and Holocene of Southern South America, mostly Argentina. It was small compared to many glyptodonts at only around 2 meters long and either 320 kilograms, or between 383 kg - 598 kg.
Etymology The genus name Neosclerocalyptus is a modification of the name of its synonym, Sclerocalyptus, and derived from the Greek roots neo- meaning "young" or "new", scleros meaning "hard", and -calyptos meaning "covering", referring to the armored carapace of the animal.Palmer, T. S. (1904). Index generum mammalium: a list of the genera and families of mammals (No. 23). US Government Printing Office. The type species, N. ornatus, specific name meaning is "adorned" after the patterns on the holotype osteoderms.
History and taxonomy
Fossils of Neosclerocalyptus were first collected by a "Sir Woodbine Parish, KH" from the Pleistocene strata near the Matanzas River in Buenos Aires Province, Argentina, but where later sent to the Royal College of Surgeons in the UK, where they were later described by paleontologist Sir Richard Owen in 1845 as a species of the earlier named Glyptodon, naming it Glyptodon ornatus.Owen, R. (1845). Descriptive and illustrated catalogue of the fossil organic remains of mammalia and aves contained in the museum of the Royal College of Surgeons of England. The fossils were fragmentary, consisting only of 4 dorsal carapace osteoderms, but were destroyed during German bombing raids during World War II. The strata where the fossils were collected may be from the Ensenadan of the Pleistocene based on later analysis of the strata around the Matanzas River. Due to the fossils being lost, a neotype was designated by Richard Lydekker in 1887 that consisted of a complete dorsal carapace, caudal rings, and a caudal tube that were also collected from Buenos Aires and deposited in the collections of the Museo Argentino de Ciencias Naturales Bernardino Rivadavia, but it couldn't be found in the museum's collections. Lydekker illustrated a complete skeleton with a complete carapace in 1894 that had been collected from the Ensenadan deposits of the Mar del Plata in Buenos Aires that is extremely similar to that of the neotype and has been used as the "model" specimen of the species since.Lydekker, R. (1894). Contributions to a knowledge of the fossil vertebrates of Argentina. Taller de publicaciones del Museo. This is shown by Argentine paleontologist Florentino Ameghino when he stated, "It is a superb sample of a fully grown adult (.) and it should be preferably consulted by paleontologists because it represents approximately the actual shape of the animal".Ameghino, F. (1920). Sur les édentés fossiles de l’Argentine. Examen critique, révision et correction de l’ouvrage de la MR Lydekker. Obras Completas y Correspondencia Científica, 11, 447-909.
One of the best known species, N. pseudornatus, was first described by Florentino Ameghino in 1889 based on 13 dorsal carapace osteoderms that were collected from the Pleistocene strata in the "Toscas del Rio de La Plata" in Buenos Aires, though Ameghino named it as a species of the Brazilian glyptodont Hoplophorus. Since its naming, dozens more specimens have been assigned to N. pseudornatus, including skulls. In 1891, Ameghino erected the genus name Sclerocalyptus for the Brazilian glyptodont Hoplophorus euphractus, erroneously believing that the genus name was preoccupied, and placed Glyptodon ornatus and Hoplophorus pseudornatus among other species in the genus.Ameghino, F. (1891). Mamíferos y aves fósiles argentinas. Revista Argentina de Historia Natural, 1. Subsequently it was clear that these two species differ considerably with each other and, due to the rules of zoological nomenclature, the name Sclerocalyptus was considered synonymous with Hoplophorus (described first), and it was necessary to establish a new genus for Sclerocalyptus ornatus: Paula Couto, in 1957, then established the Neosclerocalyptus genus.Paula Couto, C. D. (1957). Sôbre um gliptodonte do Brasil. Boletim Divisão de Geologia e Mineralogia, 165, 1-37. The taxonomic confusion concerning the names of this species continued throughout the twentieth century and for the first part of the 2000s, but N. ornatus has consistently been seen as valid and the type species. Other species named include N. castellanosi (late Pliocene), N. pseudornatus (lower Pleistocene - Medium), N. gouldi (middle Pleistocene) and N. paskoensis (late Pleistocene-early Holocene). However, many other species that have been named have been synonymous with previously named species or synonymous with other genera, most of them named based on fragmentary fossils.
Species The following list is after Quiñones et al (2020), Zurita et al (2009), and Zurita (2007). Zurita et al (2009) argued that only 2 species of Neosclerocalyptus are valid (N. ornatus & N. pseudornatus), but subsequent analyses have kept 5 species as valid.
Type: N. (Glyptodon) ornatus (Owen, 1845; type species); Holotype (RCS 3606) was destroyed, but contained 4 dorsal carapace osteoderms. Other valid species: N. castellanosi Zurita et al., 2013; Holotype (MPH 0114) is a skull and dorsal carapace fragment. N. gouldi Zurita et al., 2008; Holotype (MCA 2010) is a skull, cephalic shield, right humerus, and fragmentary dorsal carapace. N. (Chacus) paskoensis (Zurita, 2002); Holotype (Ctes-PZ 5879) is a partial skull, dorsal carapace, and associated skeleton.Zurita, A. E. (2007). Sistemática y evolución de los Hoplophorini (Xenarthra: glyptodontidae: hoplophorinae. Mioceno tardío-Holoceno temprano) (Doctoral dissertation, Universidad Nacional de La Plata). N. (Hoplophorus) pseudornatus (Ameghino, 1889); Holotype (MACN 1233) is a fragment of the dorsal caparace including 13 osteoderms. Genus synonyms:
Lomaphorus chapalmalensis Ameghino, 1908; Holotype is dubious, with similarities to Neosclerocalyptus and Eosclerocalyptus. Hoplophorus clarazianus Ameghino, 1889; Holotype is several osteoderms and a skull, all fossils have been lost and the species is dubious, though the skull has been referred to Neosclerocalyptus. Hoplophorus compressus Ameghino, 1882; Holotype osteoderms' supposed diagnostic traits are the same as those in Neosclerocalyptus species, making it a nomen dubium. Hoplophorus cordubensis Ameghino, 1888; Dubious and possibly synonymous with Neosclerocalyptus or Isolina. Glyptodon elevatus Nodot, 1857; Holotype osteoderms' supposed diagnostic traits are the same as those in juveniles of Neosclerocalyptus species, making it a nomen dubium. Hoplophorus evidens Ameghino, 1889; Holotype is dubious but referred material represents a large, unique form of Neosclerocalyptus. Hoplophorus heusseri Ameghino, 1889; Dubious at the species level. Hoplophorus paranensis Ameghino, 1883; Synonymous with Neosclerocalyptus, but dubious at the species level.Toriño, P. (2015). Nuevos aportes de la sistemática de los" Plohophorini" de Uruguay (Mammalia, cingulata, glyptodontidae).
Dubious: N. (Hoplophorus) bergi (Ameghino, 1889); Holotype is dubious and similar to that of Hoplophorus and Panochthus. N. (Sclerocalyptus) matthewi (Castellanos, 1925); Holotype is dubious and is identical to that of "Hoplophorus cordubensis". N. (Hoplophorus) migoyanus (Ameghino, 1889); Dubious at family level. N. (Hoplophorus) perfectus (Gervais & Ameghino, 1880); Holotype is dubious and more similar to that of Hoplophorus and Panochthus. N. (Hoplophorus) scrobiculatus (Ameghino, 1889); Holotype may be a chimera and has been declared a species inquirenda.
Description Like all glyptodonts, this genus also possessed an armored carapace with osteoderms melted with each other, rigid, which covered a large part of the body and head. Neosclerocalyptus was a medium-sized glyptodont, and rarely exceeded 2 meters in length, with N. pseudornatus as the smallest species. One of the largest specimens, CCA-16A, that has been referred to an unnamed species of Neosclerocalyptus was estimated to weigh 471 kilograms (or 1038 lbs), making it the largest definitively known species of Neosclerocalyptus. It was characterized by an elongated and low carapace with two lateral "wings" projected forward in the area of the cervical append.
Neosclerocalyptus''' carapace contains 50-55 transverse rows along the sides of the shell. The dorsal carapace osteoderms of Neosclerocalyptus preserve a "rossette" pattern, though the antero-ventrally placed ones lack the pattern, with a flat and sub-circular central figure, surrounded by a single row of 7 to 10 polygonal peripheral figures, similar to Propalaehoplophorus. The external morphology of the osteoderms varies in location, with rectangular osteoderms along the dorsal midline in single rows and circular osteoderms covering the middle, side, and proximal carapace portions. From the median part of the dorsal side of the carapace towards the lateral sides of the carapace, osteoderms are progressively smaller, while the central figures of them become more circular. At the anterior regions, the dorsal osteoderms become pentagonal or hexagonal and the central figures become more circular. In the most ventral-lateral region, osteoderms are rectangular with antero-posterior main axis for a wider coverage. On the anterior-dorsal parts of the carapace, osteoderms become more hexagonal, smaller, and flatter in contrast to those of the ventral-lateral region. Central figures tend to be more rounded, increasing in size, and slightly towards the posterior margin of the osteoderm. The osteoderms were thin, strongly sutured, and not depressed in their internal surface, contrary to the tall and robust osteoderms of Glyptodon and Panochthus.Asakura, Y., & Oliveira, E. V. (2021). Paleobiology of Hoplophorus euphractus Lund, 1839, a large cingulate from Brazil Intertropical Region. PalZ, 95(2), 359-372. In the dorsal region, a slightly depressed smooth central figure was surrounded by a series of large polygonal figures often common to two contiguous plates; the furrows were sharp but narrow and shallow. A large hair holes were present around the cervical inlet. By moving away from the axis, the central figures became more prominent, and they came to occupy practically the entire surface of the small plaques on the side wings. Along the edges of the carapace, the central figure was enlarged and occupied a marginal position, due to the disappearance of the peripheral area along the free margin.González, L. R. (2010). Los Cingulata (Mammalia, Xenarthra) del Mioceno temprano y medio de Patagonia (edades santacrucense y “friasense”) (Doctoral dissertation, Universidad Nacional de La Plata (UNLP)).
The tail was protected by four or five mobile rings, each consisting of two series of plates. The terminal part of the tail was protected by a bone tube, almost cylindrical, a little depressed and slightly curved upwards, which corresponded to ten vertebrae. This tube was equipped with two large convex terminal plaques, preceded by side plates that were reduced to the front of the tail, and which were separated from each other via two rows of peripheral figures. The rest of the surface of the caudal tube was made up of oval elements separated by a single series of small polygonal figures.Alfredo E. Zurita, Matias Taglioretti, Martin Zamorano, Gustavo J. Scillato-Yané, Carlos Luna, Daniel Boh & Mariano Magnussen Saffer. 2013. A new species of Neosclerocalyptus Paula Couto (Mammalia: Xenarthra: Cingulata): the oldest record of the genus and morphological and phylogenetic aspects. Zootaxa 3721 (4): 387–398.Ameghino, F. (1889). Contribucion al conocimiento de los mamiferos fosiles de la República Argentina: Obra escrita bajo los auspicios de la Academia nacional de ciencias de la República Argentina para ser presentada á la Exposicion universal de Paris de 1889 (Vol. 6). PE Coni é hijos.