Barium cycling in shallow sediment above active mud volcanoes in the Gulf of Mexico

Abstract

Methane and other hydrocarbons fluxing upward through deep-marine sediment may strongly impact the cycling of Ba near the seafloor. Piston cores across two mud volcanoes in the northern Gulf of Mexico (GOM) were therefore examined to understand Ba cycling at regions of intense hydrocarbon gas expulsion. Pore waters were analyzed for dissolved Cl −, SO 4 2− and Ba 2+, and sediment samples were analyzed for their extractable Ba contents. These data clearly show that saline fluids charged with hydrocarbons and dissolved Ba 2+ (but lacking SO 4 2−) advect from depth and profoundly influence the Ba cycle in shallow sediment. Close to the seafloor, several processes occur over time. Usually, anaerobic oxidation of methane (AOM) and other hydrocarbons in the sediment consumes dissolved SO 4 2− diffusing from bottom water. As a consequence, focused CH 4 fluxing produces a sulfate–hydrocarbon transition (SHT) that shoals across the mud volcanoes. Dissolved Ba 2+ crossing this horizon reacts with SO 4 2−, precipitating Ba fronts composed of barite immediately above the SHT. Smooth barite-rich carbonate nodules might form when this process remains at the same sediment horizon from extended time. Sometimes, however, venting releases dissolved Ba 2+ into the water column, which induces barite precipitation onto the seafloor around the mud volcanoes. Episodic venting may also form and break carbonate crusts on the seafloor, producing rocky carbonate nodules cemented with barite. For both fronts and nodules, burial past the SHT leads to barite dissolution, release of dissolved Ba 2+, and amplification of the shallow Ba cycle.