PALAIOS, 2019, v. 34, 515–541 Research Article DOI: http://dx.doi.org/10.2110/palo.2019.050 TAPHONOMY OF THE LOWER JURASSIC KONSERVAT-LAGERSTATTE¨ AT YA HA TINDA (ALBERTA, CANADA) AND ITS SIGNIFICANCE FOR EXCEPTIONAL FOSSIL PRESERVATION DURING OCEANIC ANOXIC EVENTS 1,2 2 3,4 2 2 A.D. MUSCENTE, ROWAN C. MARTINDALE, JAMES D. SCHIFFBAUER, ABBY L. CREIGHTON, AND BROOKE A. BOGAN 1Department of Geology, Cornell College, 600 First Street SW, Mount Vernon, Iowa, 52314, USA 2Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, 2275 Speedway, Austin, Texas, 78712, USA 3Department of Geological Sciences, University of Missouri, 101 Geological Sciences Building, Columbia, Missouri, 65211, USA 4X-ray Microanalysis Core Facility, University of Missouri, 1 Geological Sciences Building, Columbia, Missouri, 65211, USA email:
[email protected] ABSTRACT: Konservat-Lagerstatten¨ provide the most complete snapshots of ancient organisms and communities in the fossil record. In the Mesozoic, these deposits are rarely found in marine facies outside Oceanic Anoxic Event (OAE) intervals, suggesting that OAEs set the stage for exceptional fossil preservation. Although anoxia does not guarantee survival of non-biomineralized tissues or articulated skeletons, other OAE phenomena may promote their conservation. Here, we test this hypothesis with a taphonomic analysis of the Konservat-Lagerstatte¨ in the black shales and siltstones of the Jurassic Fernie Formation at Ya Ha Tinda (Alberta, Canada). This deposit contains crustacean cuticles, coleoid gladii with ink sacs and mantle tissues, and articulated skeletons of fish, crinoids, and ichthyosaurs. The fossils were preserved in the Pliensbachian and Toarcian (Early Jurassic) when euxinic conditions were common in the area, in part, due to the ~183 Ma Toarcian OAE.