Abstract

AbstractMesozoic marine ecosystems were dominated by several clades of reptiles, including sauropterygians, ichthyosaurs, crocodylomorphs, turtles, and mosasaurs, that repeatedly invaded ocean ecosystems. Previous research has shown that marine reptiles achieved great taxonomic diversity in the Middle Triassic, as they broadly diversified into many feeding modes in the aftermath of the Permo-Triassic mass extinction, but it is not known whether this initial phase of evolution was exceptional in the context of the entire Mesozoic. Here, we use a broad array of disparity, morphospace, and comparative phylogenetic analyses to test this. Metrics of ecomorphology, including functional disparity in the jaws and dentition and skull-size diversity, show that the Middle to early Late Triassic represented a time of pronounced phenotypic diversification in marine reptile evolution. Following the Late Triassic extinctions, diversity recovered, but disparity did not, and it took over 100 Myr for comparable variation to recover in the Campanian and Maastrichtian. Jurassic marine reptiles generally failed to radiate into vacated functional roles. The signatures of adaptive radiation are not seen in all marine reptile groups. Clades that diversified during the Triassic biotic recovery, the sauropterygians and ichthyosauromorphs, do show early diversifications, early high disparity, and early burst, while less support for these models is found in thalattosuchian crocodylomorphs and mosasaurs. Overall, the Triassic represented a special interval in marine reptile evolution, as a number of groups radiated into new adaptive zones.

Highlights

  • The Mesozoic Era witnessed the rise of tetrapods as dominant components in marine ecosystems (Kelley and Pyenson 2015)

  • We focus on three models that explicitly test for rate heterogeneity in a temporal context; Brownian motion (BM), early burst (EB), and Pagel’s δ

  • Patterns of functional disparity, morphospace occupation and skullsize evolution, show that the Middle to early Late Triassic was not just a time of marked proliferation in terms of species numbers (e.g., Benson et al 2010; Benson and Butler 2011), and a time of explosive phenotypic evolution— something that had only previously been noted speculatively based on qualitative observations (Fröbisch et al 2013; Liu et al 2014)

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Summary

Introduction

The Mesozoic Era witnessed the rise of tetrapods as dominant components in marine ecosystems (Kelley and Pyenson 2015). The emergence of a diverse assemblage of marine reptiles in the Triassic marked the establishment of ecosystem complexity on a par with modern oceans (Fröbisch et al 2013; Liu et al 2014). Qualitative observations from the fossil record reveal that marine reptiles broadly diversified into a variety of trophic strategies in their first 20 Myr of evolution (Motani et al 2015a). These included largeskulled macropredatory ichthyosaurs (Fröbisch et al 2013), small suction-feeding edentulous ichthyosauromorphs (Motani et al 2015b), shell-crushing placodonts (Neenan et al 2014), DownloadedCfroommmhtotpnss://Awwttrwi.bcuamtiobnridlgicee.onrcge/co(hrett. These included largeskulled macropredatory ichthyosaurs (Fröbisch et al 2013), small suction-feeding edentulous ichthyosauromorphs (Motani et al 2015b), shell-crushing placodonts (Neenan et al 2014), DownloadedCfroommmhtotpnss://Awwttrwi.bcuamtiobnridlgicee.onrcge/co(hrett. pIP:/a/ddcrreesast:iv18e.c2o0m6.5m5.o2n31s,.oorng0/2liNceonv s2e0s2/1bayt /124:.104/:1),3,wsuhbijcehctptoerthmeiCtsamubnrriedsgteriCcoteredtererm-sse,ofduissetr,iabvuatiliaobnle, at https://www.acnamdbrreidpgreo.dorugc/tcioorne/itnermansy. hmttpesd:/i/udmoi.,oprgr/o1v0.i1d0e1d7/tphaeb.o2r0i1g6i.n1a5l work is properly cited

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