Propalaehoplophorus
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''Propalaehoplophorus'', also written as ''Propalaeohoplophorus'', is an extinct genus of
glyptodont Glyptodonts are an extinct subfamily of large, heavily armoured armadillos. They arose in South America around 48 million years ago and spread to southern North America after the continents became connected several million years ago. The best-kn ...
, which lived in
South America South America is a continent entirely in the Western Hemisphere and mostly in the Southern Hemisphere, with a relatively small portion in the Northern Hemisphere at the northern tip of the continent. It can also be described as the southe ...
during the
Early Miocene The Early Miocene (also known as Lower Miocene) is a sub-epoch of the Miocene Epoch made up of two stages: the Aquitanian and Burdigalian stages. The sub-epoch lasted from 23.03 ± 0.05 Ma to 15.97 ± 0.05 Ma (million years ago). It was prece ...
epoch.


Description

This animal was to be very similar to the subsequent glyptodonts of the
Pliocene The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58Pleistocene The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fina ...
, such as ''
Glyptodon ''Glyptodon'' (from Greek for 'grooved or carved tooth': γλυπτός 'sculptured' and ὀδοντ-, ὀδούς 'tooth') is a genus of glyptodont (an extinct group of large, herbivorous armadillos) that lived from the Pleistocene, around 2.5 ...
'' and ''
Panochthus ''Panochthus'' is an extinct genus of glyptodont, which lived in the Gran Chaco- Pampean region of Argentina ( Lujan, Yupoí and Agua Blanca Formations), Brazil ( Jandaíra Formation), Bolivia (Tarija and Ñuapua Formations), Paraguay and Urug ...
'', but was much smaller in size. The total body length of the animal was just under a meter, and the highest point of the carapace was around 50 centimeters high.


Carapace

The dorsal armor was made up of transversal plaques files but were still present, along the lateral and front margins, two or three rows of osteoderms that indicate slight flexibility. The ornamentation of the plates consisted in a large central -oval figure, surrounded by a row of polygonal peripheral figures. The carapace was short and convex, with 19-20 transverse osteoderms on the midline, which became 27 on the side edges due to two bifurcations. The plates are equipped with clear but shallow furrows, and the central figures are generally flat, even if slightly swollen in the back. Small hair piles were present, located in the points of origin of the radial furrows. The tail was protected by five or six mobile rings, followed by a solid bone tube, probably corresponding to four rings welded together; the tube stopped abruptly, and was closed posteriorly by an irregular plate.


Skull

The skull was narrow, but already equipped with the characteristic bone processes descending below the orbit area, typical of the glyptodonts. There was a cephalic shield consisting of 28-29 irregular plates, all separated from each other, by the ornamentation that recalled that of the carapace but less marked. The teeth were not as hypsodont as those of subsequent glyptodonts, and their shape was less symmetrical: the lobes were more enlarged in the outside. The front teeth were still simple. It has been observed in some specimens that two or three dimples were present on the premaxilla and in the front of the jaw, perhaps corresponding to rudimentary incisors fall. The muzzle was still relatively elongated, and the sagittal and occipital ridge were clear. Cranium and carapace of ''Propalaehoplophorus'' minor the spine, on the other hand, had already acquired the arched shape and the degree of vertebral fusion typical of the most recent glyptodonts. The rear legs were much longer than the front ones, and the femur was similar to that of the wardrobe, long and relatively slender. The foot was pentadactyl and equipped with toes and large fingers, similar to those of ''
Neosclerocalyptus ''Neosclerocalyptus'' was 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 360 kilogra ...
''. The scapula was still relatively high and narrow, while the humerus was like that of armadillos, and had a well-developed deltoid ridge, as well as that for the humerus, and a large foramina. The hand was equipped with pointed claws.


Classification

The genus ''Propalaehoplophorus'' was described for the first time by
Florentino Ameghino Florentino Ameghino (born Giovanni Battista Fiorino Giuseppe Ameghino September 19, 1853 – August 6, 1911) was an Argentine naturalist, paleontologist, anthropologist and zoologist, whose fossil discoveries on the Argentine Pampas, especially ...
in 1887, on the basis of fossil remains found in
lower Miocene The Early Miocene (also known as Lower Miocene) is a sub-epoch of the Miocene Epoch made up of two stages: the Aquitanian and Burdigalian stages. The sub-epoch lasted from 23.03 ± 0.05 Ma to 15.97 ± 0.05 Ma (million years ago). It was prece ...
strata in Argentina; type species is ''P. australis'', which is known from several deposits in Argentina. Another well known species is ''P. minor'', which is also from Argentina. ''Propalaehoplophorus'' is the best known member of the Propalaehoplophorini, the group including the oldest definitively known glyptodonts, whose skeleton still preserve more armadillo-like characteristics. ''Propalaehoplophorus'' is the eponymous genus of this group and draws its name from the genus ''
Palaehoplophorus ''Palaehoplophorus'' (also spelled, historically, ''Palaeohoplophorus'') is an extinct genus of glyptodont. It lived from the Middle to the Late Miocene, and its fossilized remains were discovered in South America. Description This animal, lik ...
'', which in turn derives from ''
Hoplophorus ''Hoplophorus'' is an extinct genus of glyptodont, a subfamily of armadillos . The only confidently known species was ''H. euphractus'', found in Pleistocene deposits in Brazil, though fossils possibly from another species are known from Bolivia. ...
'', another genus of glyptodont, but it is known from the Pleistocene of Brazil.


Distribution

Fossils of ''Propalaehoplophorus'' have been found in the
Santa Cruz Santa Cruz (or Santacruz) is a Spanish language, Spanish or Portuguese language, Portuguese term meaning "holy cross" and referring to the Christian cross, cross on which Crucifixion of Jesus, Jesus was crucified. Santa Cruz may also refer to: P ...
and
Sarmiento Formation The Sarmiento Formation (Spanish: ''Formación Sarmiento''), in older literature described as the Casamayor Formation, is a geological formation in Chubut Province, Argentina, in central Patagonia, which spans around 30 million years from the mid- ...
s of
Argentina Argentina (), officially the Argentine Republic ( es, link=no, República Argentina), is a country in the southern half of South America. Argentina covers an area of , making it the second-largest country in South America after Brazil, th ...
, the Honda Group and Nazareno Formation of
Bolivia , image_flag = Bandera de Bolivia (Estado).svg , flag_alt = Horizontal tricolor (red, yellow, and green from top to bottom) with the coat of arms of Bolivia in the center , flag_alt2 = 7 × 7 square p ...
and the
Río Frías Formation Río Frías Formation ( es, Formación Río Frías) is a Middle Miocene geologic formation made up sedimentary rock located in Aysén Region, western Patagonia. The formation crops out along the upper couse of Cisnes River ( es, Río Cisnes).Mar ...
of
Chile Chile, officially the Republic of Chile, is a country in the western part of South America. It is the southernmost country in the world, and the closest to Antarctica, occupying a long and narrow strip of land between the Andes to the east a ...
.''Propalaehoplophorus''
at
Fossilworks Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals ...
.org


Bibliography

* F. Ameghino. 1891. Nuevos restos de mamíferos fósiles descubiertos por Carlos Ameghino en el Eoceno inferior de la Patagonia austral. – Especies nuevas, adiciones y correcciones ew remains of fossil mammals discovered by Carlos Ameghino in the lower Eocene of southern Patagonia. – New species, additions, and corrections Revista Argentina de Historia Natural 1:289-328 * F. Ameghino. 1894. Enumeration synoptique des especes de mammifères fossiles des formations éocènes de Patagonie. Boletin de la Academia Nacional de Ciencias en Cordoba (Republica Argentina) 13:259-452 * R. Lydekker. 1894. Contributions to a knowledge of the Fossil Vertebrates of Argentina. Part II. 2. The extinct edentates of Argentina. Anales del Museo de La Plata. Paleontología Argentina 3:1-118 * Vizcaíno, S. F.; Blanco, R. E.; Bender, J. B. N.; Milne, N. (2011). "Proportions and function of the limbs of glyptodonts". Lethaia. 44: 93. doi:10.1111/j.1502-3931.2010.00228.x


References

Prehistoric cingulates Prehistoric placental genera Miocene xenarthrans Miocene mammals of South America Friasian Santacrucian Neogene Bolivia Fossils of Bolivia Fossil taxa described in 1887 Taxa named by Florentino Ameghino Golfo San Jorge Basin Sarmiento Formation {{paleo-mammal-stub