Abstract

Mesozoic marine reptiles and modern marine mammals are often considered ecological analogs, but the extent of their similarity is largely unknown. Particularly important is the presence/absence of deep-diving suction feeders among Mesozoic marine reptiles because this would indicate the establishment of mesopelagic cephalopod and fish communities in the Mesozoic. A recent study suggested that diverse suction feeders, resembling the extant beaked whales, evolved among ichthyosaurs in the Triassic. However, this hypothesis has not been tested quantitatively. We examined four osteological features of jawed vertebrates that are closely linked to the mechanism of suction feeding, namely hyoid corpus ossification/calcification, hyobranchial apparatus robustness, mandibular bluntness, and mandibular pressure concentration index. Measurements were taken from 18 species of Triassic and Early Jurassic ichthyosaurs, including the presumed suction feeders. Statistical comparisons with extant sharks and marine mammals of known diets suggest that ichthyosaurian hyobranchial bones are significantly more slender than in suction-feeding sharks or cetaceans but similar to those of ram-feeding sharks. Most importantly, an ossified hyoid corpus to which hyoid retractor muscles attach is unknown in all but one ichthyosaur, whereas a strong integration of the ossified corpus and cornua of the hyobranchial apparatus has been identified in the literature as an important feature of suction feeders. Also, ichthyosaurian mandibles do not narrow rapidly to allow high suction pressure concentration within the oral cavity, unlike in beaked whales or sperm whales. In conclusion, it is most likely that Triassic and Early Jurassic ichthyosaurs were ‘ram-feeders’, without any beaked-whale-like suction feeder among them. When combined with the inferred inability for dim-light vision in relevant Triassic ichthyosaurs, the fossil record of ichthyosaurs does not suggest the establishment of modern-style mesopelagic animal communities in the Triassic. This new interpretation matches the fossil record of coleoids, which indicates the absence of soft-bodied deepwater species in the Triassic.

Highlights

  • Many large predators in the modern marine ecosystem are mammals

  • If an abrupt change in their feeding ecology is inferred from the fossil record, it probably reflects the changes in their prey community and its environment

  • Hyoid Corpus Ossification/Calcification The fossilized hyobranchial apparatus of ichthyosaurs comprises a pair of CB1, whose posterior ends are located near that of the mandible in virtually all specimens examined, the bones were preserved more anteriorly or posteriorly in some specimens than in others (Fig. 4)

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Summary

Introduction

A similar role was probably played by marine reptiles in the Mesozoic, until their last members became extinct 65.5 million years ago during the end-Cretaceous mass extinction [1,2], leaving the niches open for marine mammals. It is not known how similar their feeding ecology was to that of modern marine mammals. Being derived from fourlegged reptiles, they evolved a fish-shaped body profile about 200 million years before cetaceans Their fossil record is more complete than that of other marine reptile groups [6]. It is important to reconstruct the evolution of ichthyosaurian feeding ecology through geologic time

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