10.1594/PANGAEA.938502Oakes, Rosie LRosie LOakes0000-0001-8380-2049Fortiz, VictoriaVictoriaFortizBoudinot, F GarrettF GarrettBoudinot0000-0003-4011-5120Jones, Matthew MMatthew MJones0000-0001-5996-1728Leckie, R MarkR MarkLeckie0000-0002-7311-2180Sageman, Bradley BBradley BSageman0000-0001-5397-6654Sepúlveda, JulioJulioSepúlveda0000-0002-8251-6937Bralower, Timothy JTimothy JBralower0000-0002-3503-859XPANGAEA2021Cenomanian-Turonian BoundaryOceanic Anoxic Event 2trace elementDEPTH, sediment/rockAluminium oxideSilicon dioxidePhosphorus pentoxideScandiumTitanium dioxideVanadiumChromiumManganese oxideCobaltNickelCopperZincArsenicRubidiumStrontiumZirconiumNiobiumMolybdenumCadmiumBariumLanthanumCeriumHafniumRheniumGoldLeadThoriumUraniumRotary core drillingLaser-ablation inductively coupled plasma mass spectrometer (LA-ICP-MS)Dataset10.1594/PANGAEA.93850710.47894/mpal.70.3.011618 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalTrace element data from the Smoky Hollow #1 core drilled across the Cenomanian-Turonian boundary near Big Water, south-central Utah in 2014. Ground bulk samples were analyzed via Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) in the Laboratory for Isotopes and Metals in the Environment (LIME) at The Pennsylvania State University. Results are given with both raw (bulk) and normalized to Zr to correct for detrital input.-111.53194737.158466Utah, United States of AmericaNational Science Foundationhttps://doi.org/10.13039/100000001EAR-1338316ELT Collaborative Research: Perturbation of the Marine Food Web and Extinction During the Oceanic Anoxic Event at the Cenomanian/Turonian Boundary