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- W2800531900 abstract "Abstract Pliosaurid marine reptiles played important roles in marine food chains from the Middle Jurassic to the middle Cretaceous, frequently as apex predators. The evolution of pliosaurids during the later parts of the Early Cretaceous has recently been illuminated by discoveries from Russia (Hauterivian) and Colombia (Barremian). However, knowledge of pliosaurids representing the Jurassic–Cretaceous transition (late Tithonian – Valanginian), is still largely incomplete, especially during the earliest Cretaceous. As such, the effect on pliosaurids of hypothesized faunal turnover during the Jurassic–Cretaceous boundary interval is poorly understood. We report pliosaurid teeth from the upper Volgian (Tithonian, Upper Jurassic) of the Kheta river basin (Eastern Siberia, Russia), to the Berriasian and Valanginian (Lower Cretaceous) of the Volga region (European Russia). These assemblages have yielded a series of distinct tooth morphotypes, including the first reports of conical‐toothed pliosaurids from the latest Jurassic and earliest Cretaceous. This challenges the hypothesis that only one lineage of pliosaurids crossed the Jurassic–Cretaceous boundary. It appears that conical‐toothed pliosaurids co‐existed with their trihedral‐toothed relatives for at least 25 million years during the latest Jurassic and earliest Cretaceous. In fact, our quantitative analyses indicate that pliosaurids reached their maximal dental disparity during this interval, showing little evidence of turnover associated with the Jurassic–Cretaceous transition. Instead, disparity decreased later in the Early Cretaceous, with the disappearance of trihedral‐toothed forms in the Barremian." @default.
- W2800531900 created "2018-05-17" @default.
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- W2800531900 date "2018-04-30" @default.
- W2800531900 modified "2023-10-18" @default.
- W2800531900 title "Increased pliosaurid dental disparity across the Jurassic–Cretaceous transition" @default.
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- W2800531900 cites W1963873526 @default.
- W2800531900 cites W1966035099 @default.
- W2800531900 cites W1966459976 @default.
- W2800531900 cites W1975897702 @default.
- W2800531900 cites W1977863231 @default.
- W2800531900 cites W1978650542 @default.
- W2800531900 cites W1984350559 @default.
- W2800531900 cites W1995980393 @default.
- W2800531900 cites W1997060752 @default.
- W2800531900 cites W1999335363 @default.
- W2800531900 cites W2011659665 @default.
- W2800531900 cites W2013765369 @default.
- W2800531900 cites W2018075346 @default.
- W2800531900 cites W2021584384 @default.
- W2800531900 cites W2023137063 @default.
- W2800531900 cites W2025071256 @default.
- W2800531900 cites W2029826273 @default.
- W2800531900 cites W2039088214 @default.
- W2800531900 cites W2048855769 @default.
- W2800531900 cites W2052823810 @default.
- W2800531900 cites W2056884786 @default.
- W2800531900 cites W2058803547 @default.
- W2800531900 cites W2059150184 @default.
- W2800531900 cites W2067073047 @default.
- W2800531900 cites W2079553112 @default.
- W2800531900 cites W2079667602 @default.
- W2800531900 cites W2082601709 @default.
- W2800531900 cites W2095724223 @default.
- W2800531900 cites W2110009186 @default.
- W2800531900 cites W2111382746 @default.
- W2800531900 cites W2115627158 @default.
- W2800531900 cites W2116500543 @default.
- W2800531900 cites W2126074260 @default.
- W2800531900 cites W2129301953 @default.
- W2800531900 cites W2132485647 @default.
- W2800531900 cites W2138815118 @default.
- W2800531900 cites W2142436460 @default.
- W2800531900 cites W2148117235 @default.
- W2800531900 cites W2148672095 @default.
- W2800531900 cites W2151409320 @default.
- W2800531900 cites W2159474455 @default.
- W2800531900 cites W2169373554 @default.
- W2800531900 cites W2170940557 @default.
- W2800531900 cites W2172444546 @default.
- W2800531900 cites W2172815884 @default.
- W2800531900 cites W2175644469 @default.
- W2800531900 cites W2177468829 @default.
- W2800531900 cites W2177858454 @default.
- W2800531900 cites W2177918895 @default.
- W2800531900 cites W2213051732 @default.
- W2800531900 cites W2229626094 @default.
- W2800531900 cites W2230526322 @default.
- W2800531900 cites W2266021199 @default.
- W2800531900 cites W2281208737 @default.
- W2800531900 cites W2283352195 @default.
- W2800531900 cites W2294329848 @default.
- W2800531900 cites W2295669701 @default.
- W2800531900 cites W2334117591 @default.
- W2800531900 cites W2334843863 @default.
- W2800531900 cites W2402712933 @default.
- W2800531900 cites W2412789765 @default.
- W2800531900 cites W2419408947 @default.
- W2800531900 cites W2498803552 @default.
- W2800531900 cites W2537029383 @default.
- W2800531900 cites W2564191667 @default.
- W2800531900 cites W2620051006 @default.
- W2800531900 cites W2622495419 @default.
- W2800531900 cites W2754031179 @default.
- W2800531900 cites W2758836683 @default.
- W2800531900 cites W2761811564 @default.
- W2800531900 cites W2780055815 @default.
- W2800531900 cites W2793456347 @default.
- W2800531900 cites W2915386033 @default.
- W2800531900 cites W3007449157 @default.
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- W2800531900 doi "https://doi.org/10.1111/pala.12367" @default.
- W2800531900 hasPublicationYear "2018" @default.
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