Notoungulata is an extinct order of that inhabited South America from the early Paleocene to the end of the Pleistocene, living from approximately 61 million to 11,000 years ago.
Taxonomy
Notoungulata is divided into two major suborders, Typotheria and
Toxodonta, alongside some basal groups (
Notostylopidae and Henricosborniidae) which are potentially
Paraphyly.
Notoungulates make up over half the described diversity of indigenous South American ungulates,
with over 150 genera in 14 different families.
This order is proposed to be united with other South American native ungulates in the super-order Meridiungulata. The notoungulate and litoptern native ungulates of South America have been shown by studies of collagen and mitochondrial DNA sequences to be a sister group to the , making them true ungulates.
Cifelli has argued that Notioprogonia is paraphyletic, as it would include the ancestors of the remaining suborders. Similarly, Cifelli indicated that Typotheria would be paraphyletic if it excluded Hegetotheria and he advocated inclusion of Archaeohyracidae and Hegetotheriidae in Typotheria.
Notoungulata were for many years taken to include the order Arctostylopida, whose fossils are found mainly in China. Recent studies, however, have concluded that Arctostylopida are more properly classified as glires, and that the notoungulates were therefore never found outside South and Central America.
Notoungulates are united by a number of morphological characters of the skull, particularly the inner ear and teeth.
Based on an analysis of 133 morphological characters in 50 notoungulate genera, Billet in 2011 concluded that Homalodotheriidae, Leontiniidae, Toxodontidae, Interatheriidae, Mesotheriidae, and Hegetotheriidae are the only monophyletic families of notoungulates. Some studies have suggested that Pyrotheria, often ranked as an independent order, should also be included within Notoungulata.
Phylogeny
Classification
Ecology
Notoungulates varied widely in body size, with early diverging notoungulates like
Simpsonotus, and some hegetotheriid and interatheriid typotherians having a body mass of approximately , while the toxodontid
Toxodon is suggested to have had a body mass exceeding . Typotheres generally occupied small-medium body size niches, while toxodontians were generally medium-large sized animals.
The families
Interatheriidae,
Hegetotheriidae,
Mesotheriidae and
Toxodontidae separately evolved high crowned (
hypsodont) ever-growing (hypeselodont) cheek teeth,
with high crowned species constituting the majority of notoungulates from the Late Oligocene onward.
This adaptation was historically suggested to be the result of a diet increasingly incorporating grass, but this has been questioned, and other authors suggesting that it may have been due to the increasing intake of abrasive particles from volcanic sources.
Many typotheres have bodyforms convergent on rodents, hyraxes and rabbits,
with some rabbit-like hegetotheriids suggested to have developed a rabbit-like bounding locomotion.
The basal notungulate
Notostylops and the mesotheriids are suggested to have engaged in digging, with mesotheriids suggested to have had an ecology similar to
.
Toxodontids have sometimes been compared to rhinoceroses and hippopotamuses in overall bodyform and tooth morphology.
The Miocene toxodontian
Homalodotherium had claws on its forelimbs and is thought to have had an ecology similar to the extinct
chalicotheres, rearing on its hindlegs to feed.
Like perissodactyls, notoungulates were likely primitively hindgut fermenters,
but it has also been proposed that some of them may have had fermentation more similar to
based on their skeletal anatomy, though this is uncertain.
Evolutionary history
The oldest notoungulates appeared during the
Paleocene,
probably originating from "
condylarth" ancestors that had migrated from North America. Notoungulates and other South American native ungulates reached their apex of diversity during the
Eocene and
Oligocene. Notoungulate species diversity was stable during the Miocene, though 45% of the family diversity of the group became extinct during the interval, including Homalodotheriidae, Leontiniidae, and Interatheriidae. The diversity of the group declined during the Pliocene and Pleistocene, which is coeval in time with the Great American Interchange, which allowed ungulates and other mammals from North America to enter South America. This decline has historically been attributed to competition with the new North American arrivals, though earlier views had probably overstated the importance of this,
with climatic change also likely being an important factor.
As part of the Great American interchange, the toxodontid
Mixotoxodon migrated into Central and North America, with its furthest northern record being in Texas.
The last hegetotheriids are known from the Early Pleistocene (with a supposed Middle Pleistocene record being considered questionable).
The youngest known member of Typotheria, the mesotheriid
Mesotherium, has its last records in the late Middle Pleistocene, around 220,000 years ago.
The last notoungulates, the toxodontids
Toxodon,
Mixotoxodon and
Piauhytherium became extinct at the end of the
Late Pleistocene around 12,000 years ago as part of the Late Pleistocene megafauna extinctions, along with most other large mammals in the Americas. The extinction coincides with the arrival of the first humans to the Americas and they are suggested to have been a causal factor in the extinction.
Bibliography
Further reading
