No one has noticed this abstract talking about the potential size of the giant
T. rex phalanx (and the Broome sauropod track) ?
FOOT STRESS SCALING CONSTRAINS ESTIMATES OF MASS FOR
ISOLATED, LARGE SAURISCHIAN DINOSAUR SPECIMENS
SNIVELY, Eric, University of Wisconsin - La Crosse, La Crosse, WI, United States of
America
Tracks and autopodial specimens of sauropod and theropod dinosaurs are
occasionally cited as representing exceptionally large individuals. These specimens
include sauropod tracks of the Broome Sandstone of Western Australia and Plagne in
Southern France, the biggest measuring 1.5 m or more in their largest linear dimension.
Among particularly large fossils of theropods, a Tyrannosaurus rex phalanx (UCMP
137538) is substantially larger than the homologous bone in the next largest specimen. A
common method of first approximating mass of large fossil animals is to cube ratios of
linear size between isolated elements and their homologs from more complete specimens,
and multiply the ratio by a mass estimate for the smaller individual. However, in humans
and elephants body mass scales linearly with surface area of the feet, which maintains
foot stress overall and/or stress from mass distribution between fore and hind limbs.
Squaring ratios of linear dimensions of foot fossils may be a better method of mass
extrapolation than cubing these dimensions.
The large Broome sauropod tracks have been precisely measurable, as clear surface
imprints with discrete anatomical features. Squaring ratios of their digital span to those of
other titanosauriform sauropods yields much lower estimate of body volume than cubing
the ratios, approaching but not exceeding current volumetric estimates of very large
sauropods based on body fossils. Squared-ratio and surface area estimates for the T. rex
phalanx suggest a mass between 11.5 and 14 tonnes, depending on conservative mass
estimates for other specimens.
Although foot areas correlate linearly and precisely with mass in humans, the
squared-ratio/stress-based methods must be part of a larger range of mass estimates
methods for morphologically diverse fossil taxa, especially based on isolated elements.