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.2023 Oct 16;13(1):17558.
doi: 10.1038/s41598-023-43015-y.

The rise of macropredatory pliosaurids near the Early-Middle Jurassic transition

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The rise of macropredatory pliosaurids near the Early-Middle Jurassic transition

Sven Sachs et al. Sci Rep..

Abstract

The emergence of gigantic pliosaurid plesiosaurs reshaped the trophic structure of Mesozoic marine ecosystems, and established an ~ 80 million-year (Ma) dynasty of macropredatory marine reptiles. However, the timescale of their 'defining' trait evolution is incompletely understood because the fossil record of gigantic pliosaurids is scarce prior to the late-Middle Jurassic (Callovian), ~ 165.3 Ma. Here, we pinpoint the appearance of large body size and robust dentitions to early-Middle Jurassic (Bajocian) pliosaurids from northeastern France and Switzerland. These specimens include a new genus that sheds light on the nascent diversification of macropredatory pliosaurids occurring shortly after the Early-Middle Jurassic transition, around ~ 171 Ma. Furthermore, our multivariate assessment of dental character states shows that the first gigantic pliosaurids occupied different morphospace from coeval large-bodied rhomaleosaurid plesiosaurs, which were dominant in the Early Jurassic but declined during the mid-Jurassic, possibly facilitating the radiation and subsequent ecomorph acme of pliosaurids. Finally, we posit that while the emergence of macropredatory pliosaurids was apparently coordinated with regional faunal turnover in the epeiric basins of Europe, it paralleled a globally protracted extinction of other higher trophic-level marine reptiles that was not completed until after the earliest-Late Jurassic, ~ 161.5 Ma.

© 2023. Springer Nature Limited.

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Conflict of interest statement

The authors declare no competing interests.

Figures

Figure 1
Figure 1
Skeletal remains of the holotype (MNHNL BU159) ofLorrainosaurus keileni. (a) Reconstruction in lateral view showing recovered elements. (b) Tooth crown with root. (c) Posterior section of mandible in lateral view. (d) Glenoid section of mandible in articular view. (e) Complete mandible in ventral view. (f) Enlargement of the mandibular symphysis. (g) Coracoid in dorsal view.
Figure 2
Figure 2
Maxilla fragment from the holotype (MNHNL BU159) ofLorrainosaurus keileni in (a) lateral, (b) dorsal, (c) ventral, and (d) medial views.
Figure 3
Figure 3
Mandible from the holotype (MNHNL BU159) ofLorrainosaurus keileni in dorsal view: (a) photograph; (b) graphic illustrating individual bones and important structures.
Figure 4
Figure 4
Mandible from the holotype (MNHNL BU159) ofLorrainosaurus keileni in ventral view: (a) photograph; (b) graphic illustrating individual bones and important structures.
Figure 5
Figure 5
Mandible from the holotype (MNHNL BU159) ofLorrainosaurus keileni in right (top) and left (bottom) lateral views: (a) photograph; (b) graphic illustrating individual bones and important structures.
Figure 6
Figure 6
Postcranial elements from the holotype (MNHNL BU159) ofLorrainosaurus keileni. Left cervical rib in (a) posterior, (b) lateral, (c) dorsal, (d) anterior, (e) medial, and (f) ventral views. (g) Dorsal rib section. (h) Gastral rib. (i) Probable mesopodial element in dorsoventral view. Phalanx in (j) dorsoventral, (k) anteroposterior, (l) proximal, and (m) ventral views.
Figure 7
Figure 7
Left coracoid from the holotype (MNHNL BU159) ofLorrainosaurus keileni in (a) dorsal, and (b) ventral views.
Figure 8
Figure 8
Phylogenetic relationships ofLorrainosaurus keileni. (a) Strict consensus and (b) majority-rule consensus trees from the unweighted parsimony analysis (UPWa); (c) strict consensus tree from the weighted parsimony analysis (IWa) withK = 6; (d) strict consensus tree from IWa withK = 28.641590; (e) life reconstruction ofLorrainosaurus keileni (artwork by Joschua Knüppe); blue shading indicatesL. keileni and PIMUZ A/III0521. Numbers at nodes indicate (a) Bremer support values in UPWa; (b) percentage of trees reconstructed in UPWa; (c,d) symmetric resampling.
Figure 9
Figure 9
Dental morphospace occupation ofLorrainosaurus keileni. (a) Plot of principle coordinates analysis (PCoA) results with the PCo1/PCo2 axes showingL. keileni (bold type) versus rhomaleosaurid (grey shading) and Jurassic (blue shading) to Cretaceous (green shading) thalassophonean pliosaurids. (b) Cluster dendrogram of conical (circles), sub-trihedral (semicircles) and trihedral (triangles) thalassophonean tooth crown morphologies from the Middle (dark blue) and Late Jurassic (light blue) to Early (dark green) and Late Cretaceous (light green).
See this image and copyright information in PMC

References

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