Paleontologists assign more than 80
genera of ground sloths to multiple
families.
Megalonychidae The
megalonychid ground sloths first appeared in the
Late Eocene, about 35 million years ago, in Patagonia. Megalonychids first reached North America by island-hopping, prior to the formation of the
Isthmus of Panama. Some lineages of megalonychids increased in size as time progressed. The first species of these were small and may have been partly tree-dwelling, whereas the
Pliocene (about 5 to 2 million years ago) species were already approximately half the size of the huge
Late Pleistocene Megalonyx jeffersonii from the
last ice age. Some West Indian island species were as small as a large cat; their dwarf condition typified both tropical adaptation and their restricted island environment. This small size also enabled them a degree of arboreality.
Megalonyx, which means "giant claw", was a widespread North American genus that lived past the close of the
last (Wisconsin) glaciation, when so many large mammals died out. Remains have been found as far north as Alaska and the
Yukon. Ongoing excavations at Tarkio Valley in southwestern
Iowa may reveal something of the familial life of
Megalonyx. An adult was found in direct association with two juveniles of different ages, suggesting that adults cared for young of different generations. The earliest known North American megalonychid,
Pliometanastes protistus, lived in the southern U.S. about 9 million years ago and is believed to have been the predecessor of
Megalonyx. Several species of
Megalonyx have been named; in fact it has been stated that "nearly every good specimen has been described as a different species". A broader perspective on the group, accounting for age, sex, individual and geographic differences, indicates that only three species are valid (
M. leptostomus,
M. wheatleyi, and
M. jeffersonii) in the late Pliocene and Pleistocene of North America, although work by McDonald lists five species. Jefferson's ground sloth has a special place in modern
paleontology, for
Thomas Jefferson's letter on
Megalonyx, read before the
American Philosophical Society of
Philadelphia in August 1796, marked the beginning of
vertebrate paleontology in North America.) and
Eremotherium, which are the largest known ground sloths, thought to have had body masses of 3.5-4 tons. The skeletal structure of these ground sloths indicates that the animals were massive. Their thick bones and even thicker joints (especially those on the hind legs) gave their appendages tremendous power that, combined with their size and fearsome claws, provided a formidable defense against predators. The earliest megatheriid in North America was
Eremotherium eomigrans which arrived 2.2 million years ago, after crossing the recently formed
Panamanian land bridge. With more than five tons in weight, 6 meters in length, and able to reach as high as , it was larger than an
African bush elephant bull. Unlike relatives, this species retained a
plesiomorphic extra claw. While other species of
Eremotherium had four fingers with only two or three claws,
E. eomigrans had five fingers, four of them with claws up to nearly a foot long.
Nothrotheriidae Recently recognized, ground sloths of
Nothrotheriidae are often associated with those of the
Megatheriidae, and together the two form the superfamily Megatherioidea. The most prominent members of the group are the South American genus
Thalassocnus, known for being aquatic, and
Nothrotheriops from North America. The last ground sloths in North America belonging to
Nothrotheriops died so recently that their
subfossil dung has remained undisturbed in some caves. One of the skeletons, found in a
lava tube (cave) at
Aden Crater, adjacent to
Kilbourne Hole,
New Mexico, still had skin and hair preserved, and is now at the Yale
Peabody Museum. The largest samples of
Nothrotheriops dung can be found in the collections of the Smithsonian Museum. Another
Nothrotheriops was excavated at
Shelter Cave, also in
Doña Ana County,
New Mexico.
Mylodontidae '',
Texas Memorial Museum,
University of Texas at Austin The
mylodontid ground sloths together with their relatives the scelidotheriids form the
Mylodontoidea, the second radiation of ground sloths. The discovery of their fossils in caverns associated with human occupation led some early researchers to theorize that the early humans built
corrals when they could procure a young ground sloth, to raise the animal to butchering size. However, radiocarbon dates do not support simultaneous occupation of the site by humans and sloths.
Subfossil remains like coproliths, fur and skin have been discovered in some quantities. The
American Museum of Natural History has exhibited a sample of
Mylodon dung from Argentina with a note that reads "deposited by
Theodore Roosevelt". Mylodontids are the only ground sloths confirmed to have had
osteoderms embedded within their skin, though osteoderms were only present in a handful of genera and absent in many others. The largest mylodontid is
Lestodon, with an estimated mass of .
Scelidotheriidae The ground sloth family
Scelidotheriidae was demoted in 1995 to the subfamily Scelidotheriinae within Mylodontidae. Based on collagen sequence data showing that its members are more distant from other mylodontids than
Choloepodidae, it was elevated back to full family status in 2019. }} == Extinction ==