DEADLY WATERS: PALEOENVIRONMENTAL ANALYSIS OF THE LATE DEVONIAN HANGENBERG BIOEVENT IN THE APPALACHIAN BASIN
Data from two Cleveland Shale localities (Big Creek, near Cleveland, Ohio; Rocky Branch, near Gahanna, Ohio) exhibit complex signals. Trace fossil data, recorded as ichnofabric index (a semi-quantitative metric of relative bioturbation), show variation from laminated to sparsely burrowed strata interpreted to indicate depositional conditions ranging from dysoxic to anoxic in the bottom waters. Trace metal data (including Mo, V, Ni, and U) demonstrate variation, but also reveal extended episodes of euxinia (sulfidic waters) with possible evidence of transition metal drawdown. Lipid biomarkers reveal evidence for abundant isorenieratane, a tracer for photic zone euxinia, wide-spread throughout the Cleveland Shale strata. Hopane/sterane ratios are fairly low, typically below 0.5, which is less than the Phanarozoic average (0.5-2) for organic-rich source rocks; values increase into the overlaying shallower Carboniferous rocks. Consistently low hopane/sterane values indicate a stable microbial community structure and a relative abundance of eukaryotic phytoplankton versus bacteria throughout the extinction event. Sterane biomarker distributions encompass a great variety of structures but in terms of abundance are heavily dominated by C29 steranes derived from green algal clades—a general characteristic of Paleozoic marine settings. Together, these proxies reveal a history of prolonged anoxia/euxinia punctuated with brief oxygenation episodes across the duration of the Hangenberg Bioevent in the Appalachian Basin.