Sulfate Profiles and Barium Fronts in Sediment on the Blake Ridge: Present and Past Depths of Anaerobic Methane Oxidation Above a Large Gas Hydrate Reservoir

Ocean Drilling Program (ODP) Sites 994, 995, and 997 were drilled into a large gas hydrate deposit on the crest of the Blake Ridge (southeast U.S. margin) where upward CH₄ fluxes (F_Out) quantitatively consume pore water SO₄^2- over a narrow interval of sediment through anaerobic methane oxidation. High-resolution pore water SO₄^2- and sediment Ba profiles have been constructed at these sites to assess present and past depths of the SMI and (F_Out). Pore water SO₄^2- profiles are linear with zero SO₄^2- concentration occurring at 21.4, 21.6, and 22.8 mbsf at holes 994A, 995A and 997A, respectively. Using steady state solutions to diffusion equations with appropriate parameters, the steep SO₄^2- gradients support upward CH₄ fluxes between 7.2 and 8.6 mol/m²”ky at present-day, with the range primarily reflecting different approaches for incorporating porosity. Taking into account the generally decreasing porosity with depth and the high clay content of the sediment, the best estimates for F_Out are 7.9, 7.6 and 7.2 mol CH₄/m²”ky at sites 994, 995 and 997, respectively. However, non-steady state solutions to diffusion equations show that the SO₄^2- gradients do not imply steady state conditions. Elevated Ba concentrations (530-1410 ppm) exist in sediment between 18.23 and 20.65, between 17.31 and 20.31, between 19.40 and 21.80, and between 19.58 and 21.91 mbsf at holes 994A, 994C, 995A, and 997A, respectively. These Ba fronts coincide with highs in bulk sediment Ba/Al (to 0.025) and are caused by Ba cycling just above time averaged depths of the SMI. Because the Ba fronts lie immediately above the present-day depths of pore water SO₄^2- depletion, because the Ba fronts contain substantial Ba, and because no other Ba fronts are found in the upper 25 m at the three sites, the depth of the SMI beneath the seafloor has been nearly constant for considerable time (>18,000 years). Thus, CH₄ fluxes can be determined through SO₄^2- gradients and steady state solutions to diffusion equations. More importantly, F_Out through the crest of the Blake Ridge has not varied significantly across major changes in sea level and hydrostatic pressure. >http://www.elsevier.nl:80/inca/publications/store/2/1/2/</a>