Not Entirely Ichthyosaur: A Mysterious Lamniform and Ichthyopterygian-Fall Association From the Abyssal Upper Cretaceous of the Northern Apennines (Italy)

Abstract

Axial remains of a large ichthyosaur and a medium-sized anacoracid shark from the deep-water sediments of the Cenomanian of the Northern Apennines (Northern Italy) are described in detail. The specimens were found closely associated (less than 0.3 m apart), and offer an invaluable window into the taphonomy and dead-fall stages of pelagic vertebrates in a Mesozoic abyssal plain. The anacoracid shark remains, initially misinterpreted as an ichthyosaur, consist of eight articulated vertebrae embedded in a block of dark arenaceous matrix, and represent the first occurrence of an articulated shark from the Northern Apennines. The ichthyosaur remains consist of seven discoidal vertebrae and several unidentified fragments. Due to the absence of diagnostic skeletal elements, both specimens are assigned only at higher taxonomic levels. The two fossils, which come from the same outcrop and possibly from the same stratigraphic horizon, share a common taphonomic history, in terms of both their preservation and diagenesis. Mineralogy of the matrices of both is dominated by manganese micro-nodules, consistent with the deposition of polymetallic nodules in bathyal-abyssal settings. Biostratinomic processes that impacted the two specimens also provide insight on the development of Mesozoic marine vertebrate-falls in the deep-sea. Localized pyrite framboids inside the bone spongiosa are possible evidence of the sulfophilic stage (microbially mediated sulfur mobilization during lipid decay) in the ichthyosaur fall. Burrows assigned to Taenidium on the surface of the shark block, interpreted as worm-like feeding burrows or arthropod locomotion and feeding trails, might represent evidence of the enrichment opportunistic stage. Although intriguing, we have no evidence to support the hypothesis that this peculiar association of two pelagic predators is due to ecological interaction between the two animals.

Of His Bones Are Crinoid Made: Taphonomy and Deadfall Ecology of Marine Reptiles From a Pelagic Setting (Middle-Upper Jurassic of Northeastern Italy)

“…Similarly, pyrite framboids, a proxy for sulfur microbial mobilization during lipid decay, were not found inside the bone spongiosa of MPPPL 18797, V7101 and MCLSC T1. We believe that the lack of evidence for this stage could be environmental, as pyrite framboids, which were found in bones of both shallower ) and deeper (Serafini et al 2023c) settings might not had formed (or preserved) due to the constant oxic conditions at the RAV seafloor.…”