Sthenurus ("strong tail") is an extinct genus of . With a length around 3 m (10 ft), some species were twice as large as modern extant species. Sthenurus was related to the better-known Procoptodon. The subfamily Sthenurinae is believed to have separated from its sister taxon, the Macropodinae (kangaroos and wallabies), halfway through the Miocene, and then its population grew during the Pliocene.
At the Baldina Creek fossil site 30 kya (C14 dating), the genus had transitioned to a diet of grass-grazing. During this time, the area was open grasslands with sparse tree cover as the continent was drier than today, but at Dempsey's Lake (36-25 kya) and Rockey River (19 kya C14 dating), their diet was of both grazing and browsing. This analysis may be because of a wetter climatic period. The overall anatomy of the genus did not alter in response to the change in diet and dentition did not adapt to the varying toughness of the vegetation between grasses, shrubs, and trees.Darren R. Gröcke (N/A) VIEPS Department of Earth Sciences, Monash University, Clayton, VIC 3168, Australia ST-grock@artemis.earth.monash.edu.au Carbon-Isotope Shifts Recorded in Megafaunal Dietary Niches of C3 and C4 Plants in the Late Pleistocene of South Australia: Correlation with Palaeofloral Reconstructions. Monash University, Clayton. Retrieved on 2007-06-26.
Other animals found in the Cuddie Springs habitat include the flightless bird Genyornis, the red kangaroo, Diprotodon, humans, and many others.
Examination of skeletal remains of Sthenurus from Lake Callabonna, northern South Australia, revealed that as the animals were trapped as they floundered in the clay mud while attempting to cross the floor of the lake during low-water or dry times. The data show that three closely allied sthenurine species sympatry at Lake Callabonna: a new giant taxon, S. stirlingi, an intermediate-sized S. tindalei, and the considerably smaller S. andersoni. Comparative osteology of these Sthenurus species with Macropus giganteus emphasizes how different sthenurine kangaroos were from extant kangaroos, especially with the sthenurines' short, deep skulls, long front feet with very reduced lateral digits, and the monodactyl hind feet.WELLS, RT; TEDFORD, RH BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY Issue: 225 Pages: 1-111 Published: 1995
Teapot Creek, a tributary of the MacLaughlin River in the Southern Monaro, southeastern New South Wales, contains a sequence of terraces. The highest and oldest of these terraces was reported to contain the remains of fossil mammals found in Plio-Pleistocene fossil deposits elsewhere in eastern Australia. Sthenurus atlas, S. occidentalis, and S. newtonae are some of the species identified from the fossils found in the terrace.Armand, L (Armand, L); Ride, WDL (Ride, WDL); Taylor, G (Taylor, G) PROCEEDINGS OF THE LINNEAN SOCIETY OF NEW SOUTH WALES Volume: 122 Pages: 101-121 Published: DEC 22 2000
Their skeletal structure was very robust with powerful hind limbs, a broad pelvis, a short neck, and longer arms and phalanges than modern species. Their phalanges may have been used to hold stems and twigs. These unique adaptations suited their feeding habits of browsing in the case of S. occidentalis, but other species were most likely grazers.
The body mass of the largest species is estimated to be , nearly three times that of the largest extant species. Due to their giant height and weight, the largest species possibly did not hop as a form of locomotion, but rather walked bipedally in a similar manner to Hominidae. This gait would have been used at slow speeds, since hopping at slow speeds would have been inefficient. Pentapedal movement and bipedal hopping no longer seem to have been options for these massive kangaroos.
A morphological difference exists between the scapulae (shoulder blades) of the Sthenurine and the extant and extinct macropodids.
They possessed a short, deep skull, which was suited for stereoscopic vision; this allowed for better depth perception.
In S. stirlingi, fossil evidence shows that the tooth row curves medially (anteriorly and posteriorly) from a line tangential to the labial side of the molars at the anterior ridge of the masseteric processes.
The fossils of teeth may also suggest that the sthenurines and macropodines shared a common ancestor. They share many synapomorphic character states. They each have well-developed lophs on molars and both lack a posthypocristid.
Skull
Teeth
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