Diprotodon optatum was the largest marsupial known to have lived, a plant-eater often compared to a rhinoceros, whose closest living relatives are wombats and koalas. It ranged over most of mainland Australia and disappeared about 40 000 years ago, after people had reached the continent. Its oldest fossils may reach 1.77 million years, though most are younger than 110 000. It was also the first Australian fossil mammal to be named, by Owen in 1838, from bones dug out of Wellington Caves in New South Wales.
One tonne or nearly three
Its weight depends heavily on method. In 1991 Murray used skull and tooth measurements and got about 1 150 kg, a figure he did not consider precise. Wroe and colleagues instead measured the girth of 17 thigh and upper arm bones against 18 marsupials and 32 placental mammals. Their 2004 answer was 2 272 to 3 417 kg, mean 2 786 kg, which most sources now repeat, though they warned that projecting so far beyond living marsupials is problematic.
Length is unsettled too. Mounted skeletons measure 2.75 to 3.4 m from head to tail, but with the discs of the spine restored the animal may have been 20 per cent longer, over 4 m. Adults fall into two clear size groups, once named as separate species. Price reviewed them in 2008, kept one species and read the larger form as probably male.
Walking on its wrists
The feet were small for the body and turned inwards, the hind toes at about 130 degrees from the ankle. A 2023 study of a smaller Pliocene relative, Ambulator, explains the odd arrangement. In these animals a wrist bone worked as a second heel, weight passed through the wrist and ankle, and the weak digits probably never touched the ground. That fits the fossil trackways, which show no finger or toe marks.
Two trackways are known. At Lake Callabonna in South Australia one animal left strides of about 1 500 mm, an estimated 6.3 km/h. On the Victorian Volcanic Plain the stride was 1 310 mm, the speed about 5.5 km/h and the stance more sprawled, perhaps a female carrying a large joey in her pouch.
A lakebed full of skeletons
Lake Callabonna also holds the largest known fossil assemblage. Hurst dug there in 1893 and reported up to 360 individuals, trapped in the mud as the lakebed dried. Some researchers read such clusters as herds, often mostly female. The Australian Museum thinks large herds unlikely, because marsupials are not known to form them, and takes these for smaller family groups drawn to a shrinking waterhole.
The bones also record last meals. One Callabonna skeleton had saltbush in its abdomen, and the gut contents of another, about 53 000 years old, held young leaves, stalks and twigs.
A 200 km round trip, from one tooth
The first incisors grew throughout life, so a single tooth keeps a record of where its owner fed. In 2017 Price and colleagues measured strontium along an upper incisor from the Darling Downs in Queensland, from an animal that lived around 300 000 years ago. The values cycled over nearly three years, as if it made a round trip of up to about 200 km each year. No living marsupial migrates this way. In 2023 Koutamanis and colleagues found that teeth from Wellington Caves and Bingara in New South Wales matched bedrock within 10 to 25 km, with no sign of long journeys. The results come from different regions, so both could be right, but neither settles it for the species.
Twenty-five thousand years ago, or forty
The Australian Museum still says Diprotodon died out about 25 000 years ago. Recent dating does not support a date that young. In 2001 Roberts and colleagues dated 28 fossil sites and placed the last megafauna between about 50 000 and 41 000 years ago, and a 2021 study rejected later survival at Cloggs Cave in south-eastern Australia. The youngest reliable fossils, from South Walker Creek in Queensland, are 40 100 ± 1 700 years old.
Direct evidence of contact with people is almost nil. No butchered megafauna bones are known. A rib from Tambar Springs has a small square hole, tentatively identified as spear damage. An incisor from Spring Creek with 28 fine marks was long cited as human work, until a 2020 reanalysis by Langley attributed them to a tiger quoll. Drought, hunting and burning of the landscape have all been proposed, and the cause remains open.


