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• W4385617511 endingPage "111760" @default.
• W4385617511 startingPage "111760" @default.
• W4385617511 abstract "The palaeoecology of the Xenacanthiformes (Chondrichthyes) is still a matter of discussion. Historically considered as freshwater organisms, hypotheses of euryhaline ecology including migratory behaviour were recently proposed based on the histology of their dorsal spines. However, recent studies still argued for a full freshwater ecology based on the geochemical compositions of their teeth. Their ecology is particularly interesting to investigate for those coming from the environmentally ambiguous Early Permian intra-mountainous localities of Buxières-les-Mines (Bourbon-l'Archambault Basin, Allier) and the Muse oil-shale bed (OSB) (Autun Basin, Saône-et-Loire) from the French Massif central. These two localities were interpreted as freshwater settings but doubts on marine influences exist. To assess their palaeoenvironment and the palaeoecology settings based on xenacanthiforms occurrences, we have analysed the stable isotope compositions (δ18O, δ13C and δ34S) of the bioapatite of their vertebrate faunas. From these stable isotope compositions, we interpret that Buxières-les-Mines was a large and deep freshwater lake, equivalent to the modern Indonesian Lake Matano, whereas the Muse OSB is interpreted as a shallow tropical lake with drying events, equivalent to the Lake Punta Laguna in Amazonia or the Lake Tanganyika in Africa. The oxygen isotope compositions of the xenacanth dorsal spines of Buxières-les-Mines are relatively constant from the apex to the base. Such uniform isotopic compositions recorded during the life of xenacanths support either their sedentary lifestyle or stenohalinity. The apparent ability of small xenacanthiforms to endure drying up, as shown by the variations in isotope composition of the Muse OSB specimens, could explain their resilience during the Early Permian whereas Carboniferous xenacanthiforms occurring in large lake and river systems almost disappeared." @default.
• W4385617511 created "2023-08-07" @default.
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• W4385617511 date "2023-10-01" @default.
• W4385617511 modified "2023-10-18" @default.
• W4385617511 title "Palaeoenvironmental and palaeoecological reconstructions based on oxygen, carbon and sulfur isotopes of Early Permian shark spines from the French Massif central" @default.
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• W4385617511 cites W1977055850 @default.
• W4385617511 cites W1977352653 @default.
• W4385617511 cites W1977808305 @default.
• W4385617511 cites W1978485565 @default.
• W4385617511 cites W1983529668 @default.
• W4385617511 cites W1985315619 @default.
• W4385617511 cites W1988378253 @default.
• W4385617511 cites W1989092684 @default.
• W4385617511 cites W1993994348 @default.
• W4385617511 cites W1994027801 @default.
• W4385617511 cites W1995386982 @default.
• W4385617511 cites W1995546577 @default.
• W4385617511 cites W1996293428 @default.
• W4385617511 cites W1997170235 @default.
• W4385617511 cites W1998115262 @default.
• W4385617511 cites W2006657131 @default.
• W4385617511 cites W2011434968 @default.
• W4385617511 cites W2012622110 @default.
• W4385617511 cites W2016431310 @default.
• W4385617511 cites W2018439141 @default.
• W4385617511 cites W2023532676 @default.
• W4385617511 cites W2023662274 @default.
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• W4385617511 cites W2036342458 @default.
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• W4385617511 cites W2071402402 @default.
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• W4385617511 cites W2148413459 @default.
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• W4385617511 doi "https://doi.org/10.1016/j.palaeo.2023.111760" @default.
• W4385617511 hasPublicationYear "2023" @default.
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