Glyptodont

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Glyptodonts
Temporal range:
Ma
Glyptodon fossil, Natural History Museum, Vienna
Illustration of the skeleton of Doedicurus
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Cingulata
Family: Chlamyphoridae
Subfamily: Glyptodontinae
Burmeister 1879
Genera

Glyptodonts are an extinct clade of large, heavily armoured armadillos, reaching up to 1.5 metres (4.9 ft) in height, and maximum body masses of around 2 tonnes. They had short, deep skulls, a fused vertebral column, and a large bony carapace made up of hundreds of individual scutes. Some glyptodonts had clubbed tails, similar to ankylosaurid dinosaurs.[1]

The earliest widely recognised fossils of glyptodonts in South America are known from the late Eocene, around 38 million years ago, and they spread to southern North America after the continents became connected around 2.7 million years ago.[2] The best-known genus within the group is Glyptodon.

Glyptodonts were historically considered to constitute the distinct family Glyptodontidae, with their relationships to modern armadillos being contested. In 2016, an analysis of the

pampatheres has also been proposed.[4]

Glyptodonts abruptly became extinct approximately 12,000 years ago at the end of the Late Pleistocene, as part of the Late Pleistocene extinctions, along with most other large animals in the Americas. Evidence has been found suggesting that they were hunted by recently arrived Paleoindians, which may have played a role in their extinction.[3]

Evolution

Glyptodonts first evolved during the

pampatheres, armadillos and a number of other types of xenarthrans (e.g., ground sloths
).

Cladogram of Cingulata[2][6][7]
 Cingulata 

Dasypodidae

 Chlamyphoridae 
 Euphractinae 

Euphractus

Zaedyus

Chaetophractus villosus

Chaetophractus nationi

C. vellerosus

Glyptodontinae (Doedicurus)

 Chlamyphorinae 

Chlamyphorus

Calyptophractus

Tolypeutinae

Priodontes







Analysis of inner ear morphology corroborates this position, while also finding that

pampatheres are the closest relatives of glyptodonts:[4]

Glyptodonts are divided into two major groups, which split during or prior to the Early Miocene. The first is the traditional Glyptodontinae, which is includes the well known genera of Glyptodon and Glyptotherium, which probably originated in Northern South America, while the second is the unnamed "Austral clade", containing the majority of glyptodont diversity, which as the name suggests probably originated in Southern South America.[8]

Cladogram after Barasoain et al. 2022:[8]

Description

ankylosaurid dinosaurs.[9]

Ecology

Glyptodonts are thought to have been herbivores that fed on low lying vegetation, with mixed feeding or grazing based diets.[10] Some glyptodonts were likely selective feeders, while others were likely bulk feeders.[10][11]

scutes, early Miocene, in the permanent collection of The Children's Museum of Indianapolis

Extinction

At the end of the Late Pleistocene, all then-living glyptodont species, which belonged to the genera Glyptodon, Hoplophorus, Glyptotherium, Panochthus, Doedicurus and Neosclerocalyptus, abruptly became extinct around 12,000 years ago as part of the Late Pleistocene extinctions, simultaneously with the vast majority of other large mammals in the Americas. The importance of human vs climatic factors in these extinctions has been the subject of contention. Several sites across South America are suggested to document hunting of glyptodonts by the recently arrived Paleoindians, which may have played a role in their extinction.[12][3] At the Muaco and Taima-Taima sites in Falcón State in northwestern Venezuela, several skulls of Glyptotherium display distinctive fracture marks on the skull roof that occurred around the time of death, suggested to have been caused by a deliberate percussive blow to a relatively thin part of the skull by a club or stone tool.[3]

References

External links