THE KRAKEN'S BACK: NEW EVIDENCE REGARDING POSSIBLE CEPHALOPOD ARRANGEMENT OF ICHTHYOSAUR SKELETONS
Hydrodynamic considerations regarding the probability of displacement (PD) of ichthyosaur vertebral centra arrays (n=12) show that three different biserial arrangements have PDs of 17%, 89% and 100% respectively by currents strong enough to displace a single centra. The critical Specimen U array at Berlin‑Ichthyosaur State Park has PD=~100, indicating that it is highly unlikely that the biserial pattern was imparted by submarine currents. The unwinnowed wackestone matrix confirms that competent water velocities did not frequently occur in this deep-water depositional environment. The Luning Formation also hosts Protopaleodictyon ichnosp. and supergiant amphipods.
We recently obtained photographs of a retired exhibit formerly on display at the University of Nevada, Las Vegas, Museum of Natural History. The display reconstructed a well‑preserved Shonisaurus skeleton as it was found in the field. The exhibit is well documented by photographs from a variety of vantage points. The skeleton appears to have been partly disassembled during the Triassic, and a biserial array of centra very similar to the Specimen U array occurs adjacent to the nearly complete skeleton. The UNLV array has a PD=~100, again indicating that the biserial pattern was not the result of current assembly. Finally, at least three of these centra show what may be triangular bite marks removed from their margins.