1 Stable isotope study of a new chondrichthyan fauna 2 (Kimmeridgian, Porrentruy, Swiss Jura): an unusual 3 freshwater-influenced isotopic composition for the 4 hybodont shark Asteracanthus 5 6 L. Leuzinger1,2,*, L. Kocsis3,4, J.-P. Billon-Bruyat2, S. Spezzaferri1, T. 7 Vennemann3 8 [1]{Département des Géosciences, Université de Fribourg, Chemin du Musée 6, 1700 9 Fribourg, Switzerland} 10 [2]{Section d’archéologie et paléontologie, Office de la culture, République et Canton du 11 Jura, Hôtel des Halles, 2900 Porrentruy, Switzerland} 12 [3]{Institut des Dynamiques de la Surface Terrestre, Université de Lausanne, Quartier UNIL- 13 Mouline, Bâtiment Géopolis, 1015 Lausanne, Switzerland} 14 [4]{Universiti Brunei Darussalam, Faculty of Science, Geology Group, Jalan Tungku Link, 15 BE 1410, Brunei Darussalam} 16 [*]{now at: CRILAR, 5301 Anillaco, La Rioja, Argentina} 17 Correspondence to: L. Leuzinger (
[email protected]) 18 19 Abstract 20 Chondrichthyan teeth (sharks, rays and chimaeras) are mineralised in isotopic equilibrium 21 with the surrounding water, and parameters such as water temperature and salinity can be 18 22 inferred from the oxygen isotopic composition (δ Op) of their bioapatite. We analysed a new 23 chondrichthyan assemblage, as well as teeth from bony fish (Pycnodontiformes). All 24 specimens are from Kimmeridgian coastal marine deposits of the Swiss Jura (vicinity of 25 Porrentruy, Ajoie district, NW Switzerland). While the overall faunal composition and the 26 isotopic composition of bony fish are generally consistent with marine conditions, unusually 18 27 low δ Op values were measured for the hybodont shark Asteracanthus. These values are also 28 lower compared to previously published data from older European Jurassic localities.