Evaluation of the Re-Os Geochronometer in Organic-rich Mudrocks as a Method for Constraining the Absolute Ages of Neoproterozoic Glaciogenic Deposits

Absolute-age constraints on the Neoproterozoic glaciations are generally poor due to a paucity of suitable plutonic and volcanic igneous rocks that are temporally and spatially related to Neoproterozoic glaciogenic deposits and are amenable to radiometric dating methods. In this study, the Re-Os isotope systematics of dark gray, sulfidic slates from the Old Fort Point Formation (OFP) of the Windermere Supergroup (near Jasper, Alberta) were examined to test the ability of the Re-Os geochronometer to provide an absolute age constraint for a Neoproterozoic glaciogenic deposit. The OFP has been interpreted as the deep water expression of post-glacial sea level rise and therefore is comparable stratigraphically to cap carbonates that immediately overlie glaciogenic deposits worldwide. Despite the relatively low Re (6-16 ppb) and Os (0.07-0.14 ppb) concentrations and total organic contents (~ 0.5% TOC) of the slates compared to other organic-rich mudrocks used in previous Re-Os isotope studies, precise well-fitted Re-Os isochrons have been obtained with two different dissolution methods. An age of 620.8 +/- 8.1 Ma (MSWD = 0.9; initial ¹⁸⁷Os/¹⁸⁸Os = 0.68 +/- 0.06) is obtained using conventional aqua regia dissolution. Using a method designed to selectively dissolve organic matter alone, an age of 609.0 +/- 8.3 Ma (MSWD = 1.5; initial ¹⁸⁷Os/¹⁸⁸Os = 0.62 +/- 0.05) is obtained. These absolute age results are in accord with existing age constraints (e.g., stratigraphically younger Hamill Group with a U-Pb zircon age of 569 Ma). The well-defined Re-Os systematics of the OFP slates demonstrates for the first time that the Re-Os system is not disturbed in organic-rich sediments during lower greenschist (-chlorite) grade metamorphic conditions. The whole-rock analysis of each individual sample yields consistently higher initial ¹⁸⁷Os/¹⁸⁸Os isotope ratios than the corresponding organic matter analysis and suggests that a significant radiogenic detrital Os component is present within the OFP slates. Because organic matter is likely dominated by the hydrogenous (seawater) Os budget, the initial ¹⁸⁷Os/¹⁸⁸Os ratio of 0.62 +/- 0.05 calculated from the organic matter regression represents the best estimate of the Os isotopic composition of the contemporaneous seawater at the time of sediment deposition. The corresponding age of 609.0 +/- 8.3 Ma is then considered to be the best depositional age determination for the OFP and provides a minimum absolute age constraint on the stratigraphically underlying glaciogenic Mount Vreeland Formation (northeastern British Columbia) and the correlative Ice Brook diamictites (Mackenzie Mountains, northwestern Canada). Thus, we conclude that the Mount Vreeland and Ice Brook diamictites are older than the ~ 580-570 Ma glaciogenic deposits of Eastern North America and may thus be considered as lower Marinoan in age. Further application of the Re-Os geochronometer to other organic-rich mudrock horizons spatially and temporally related to Neoproterozoic glaciogenic deposits will allow further opportunities for their correlation and provide better age constraints on the timing, number, and duration of the Neoproterozoic glaciations. This will allow a further assessment of the Snowball Earth Theory and its prediction of global, synchronous glaciations.