Lee and Zachary Richards in 2018 based on bending resistance measurements of several dinosaur humeri, found the humeri of carnosaur, therizinosaur, and tyrannosaur dinosaurs to be relatively resilient to stress. This increased ability to withstand stress supports the idea that Therizinosaurus and other therizinosaurians used their arms in a robust fashion that generated significant forces. They also suggested that the prominent claws of some members could have been used as a defense against predators and other various functions. Unlike the generally light and agile ornithomimosaurs who avoided predation with speed, Therizinosaurus and relatives relied on arms and claws to face threats (and were generally slow-runners to begin with). Paleoenvironment The remains of Therizinosaurus have been found in the well-known Nemegt Formation of the Gobi Desert. Although this formation has never been dated radiometrically because of the discontinuity of exposures and absence of datable volcanic rock facies, the vertebrate fossil assemblage suggests an early Maastrichtian stage possibly between 70 million and 68 million years ago. The Nemegt Formation is separated into three informal members. The lower member is mainly composed by fluvial sediments, while middle and upper members consist of alluvial plain, paludal, lacustrine, and fluvial sedimentation. The environments that Therizinosaurus inhabited have been determined by the sedimentation across the formation, the δ13C level preserved on the tooth enamel of many herbivorous dinosaurs and the numerous petrified wood across the formation. They consisted of large meandering and braided rivers with extensive woodlands composed of large, enclosed, canopy-like forests of Araucarias that supported diverse herbivorous dinosaurs like Therizinosaurus. The climate of the formation was relatively temperate (mean annual temperatures between 7.6 and 8.7 °C), characterized by monsoons with cold, dry winters and hot, rainy summers with the addition of mean annual precipitations between 775 mmm and 835 mmm, a precipitation that was subject to prominent seasonal fluctuations. The wet environments of the Nemegt Formation may have acted as an oasis-like area that attracted oviraptorids from arid neighbour localities such as the Barun Goyot Formation, as evidenced on the presence of Nemegtomaia in both regions. It has been previously suggested that the Nemegt Formation may have been similar to the modern-day Okavango Delta, which is also composed of mesic (well-watered) surroundings. The paleofauna of the Nemegt Formation was diverse and rich, composed of other dinosaurs such as the alvarezsaurs Mononykus and Nemegtonykus; deinonychosaurs Adasaurus and Zanabazar; ornithomimosaurs Anserimimus and Gallimimus; oviraptorosaurs Avimimus, Rinchenia