EARLY JURASSIC PALEOENVIRONMENTAL RECONSTRUCTION IN THE WESTERN CANADA SEDIMENTARY BASIN AND INFERENCE OF EXPANDED OCEAN ANOXIA/EUXINIA ACROSS THE TOARCIAN OAE FROM GLOBAL RE AND MO MASS BALANCE MODELS
The T-OAE was identified over 1.5 m around the Gordondale–PCS boundary from a N-CIE up to -7‰ from baseline δ13C values. A Mo/U covariation diagram suggests the depositional locality was open to global ocean water mass exchange, so RSTM enrichments are used to infer global paleo-ocean redox conditions. RSTMs are enriched in the Gordondale and T-OAE interval, suggesting deposition from anoxic/non-sulfidic and euxinic waters, whereas generally lower enrichments and elevated Re/Mo ratios for the PCS suggest deposition from suboxic to anoxic/non-sulfidic waters. There is no stratigraphic shift in the Re concentration of anoxic shales across the Gordondale/T-OAE, and an average area of sea floor anoxia up to a few percent is implied. Local euxinia is indicated in the lower Gordondale and uppermost Gordondale + T-OAE intervals by high Mo concentrations, high Mo/U and low Re/Mo. The lower Gordondale Mo data suggests a euxinic seafloor area of <0.2%; the upper Gordondale + T-OAE contain lower [Mo] and suggest a euxinic sea floor area up to a few percent. An expansion of euxinic conditions during the T-OAE in response to LIP activity is also indicated by previous Mo and Tl isotope studies and likely contributed to the Pliensbachian–Toarcian extinction event.