It was as heavy as four African elephants.
The remains of a 26.5-million-year-old giant, hornless rhino — one of the largest mammals ever to walk Earth — have been discovered in northwestern China, a new study finds.
The newly identified species, Paraceratherium linxiaense — named after its discovery spot in the Linxia Basin in Gansu province — towered over other animals during its lifetime. The 26-foot-long (8 meters) beast had a shoulder height of 16.4 feet (5 m), and it weighed as much as 24 tons (21.7 metric tons), the same as four African elephants, the researchers said.
The new species is larger than other giant rhinos in the extinct genus Paraceratherium, said study lead researcher Deng Tao, director and professor at the Institute of Vertebrate Paleontology and Paleoanthropology at the Chinese Academy of Sciences in Beijing. A new family tree analysis of Paraceratherium species, including P. linxiaense, reveals how these ancient beasts evolved as they migrated across Central and South Asia at a time when the Tibetan Plateau was lower than it is today, Tao told.
Researchers have known about the fossil trove at Linxia Basin, located at the northeastern border of the Tibetan Plateau, since the 1950s, when farmers there began discovering “dragon bones,” Tao said. Digs in the 1980s revealed rare, but fragmentary giant rhino fossils. That changed in 2015, with the discovery of a complete skull and jaw of one giant rhino individual, and three vertebrae from another individual, both dating to the late Oligocene epoch (33.9 million to 23 million years ago).
When the researchers saw the fossils, the bones’ completeness and “huge size … [were] a great surprise for us,” Tao said. An anatomical analysis, in addition to the fact that the fossils were larger than those from other known species in the Paraceratherium genus, revealed that they belonged to a previously unknown Paraceratherium species.
The skull and jaw bones showed that P. linxiaense had a giant, 3.7-foot-long (1.1 m) head; a long neck; two tusk-like incisors that pointed downward; and a deep nasal notch, indicating that the animal had a trunk like that of a tapir. The giant rhino likely wrapped its trunk around branches so it could easily strip off leaves with its front teeth, Tao said.
P. linxiaense stood on four long legs that were good for running, and its head could reach heights of 23 feet (7 m) “to browse leaves of treetops,” Tao said.
Most species within Paraceratherium lived in Central Asia (what is now Mongolia and Kazakhstan), but one far-flung species, P. bugtiense, lived farther south, in what is now western Pakistan. This distant location puzzled scientists, so Tao and his colleagues set out to see if they could discern this species’ relationship with other Paraceratherium species, including the newfound P. linxiaense.
The team created the rhino ancestor’s family tree by analyzing the anatomy of 11 giant rhino species and 16 other animal species in the superfamily Rhinocerotoidea, including two living rhinos. The analysis revealed that the Mongolian giant rhino (P. asiaticum) dispersed westward to what is now Kazakhstan, and its descendant lineage expanded to South Asia and evolved into P. bugtiense during the early Oligocene, Tao said.
At that time, Central Asia was arid, while South Asia was relatively humid, with a mosaic of forested and open landscapes, where giant rhinos likely browsed for food, Tao said.
During the late Oligocene, tropical conditions allowed giant rhinos to trek northward, back to Central Asia. It appears that the far-flung P. bugtiense crossed the Tibetan region, and evolved into two closely-related species: the newly found P. linxiaense, known from China, and P. lepidum, known from China and Kazakhstan.
Given that some of the world’s largest mammals took this impressive journey, it’s likely that the Tibetan region “was still not uplifted as a high-elevation plateau” at that time, Tao said. It may have been under 6,600 feet (2,000 m) during the Oligocene, and “giant rhinos could have dispersed freely through this region,” he said.