Biogeosciences, 16, 3165–3181, 2019 https://doi.org/10.5194/bg-16-3165-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Evidence for microbial iron reduction in the methanic sediments of the oligotrophic southeastern Mediterranean continental shelf Hanni Vigderovich1, Lewen Liang2, Barak Herut3, Fengping Wang2, Eyal Wurgaft1,a, Maxim Rubin-Blum3, and Orit Sivan1 1The Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev, Beer-Sheva, 8410501, Israel 2State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai, 200240, P.R. China 3Israel Oceanographic and Limnological Research, Haifa, 3108000, Israel aThe Department of Marine Chemistry and Geochemistry, Woods-Hole Oceanographic Institution, Woods-Hole, MA, USA Correspondence: Orit Sivan (
[email protected]) Received: 21 January 2019 – Discussion started: 31 January 2019 Revised: 8 July 2019 – Accepted: 9 July 2019 – Published: 23 August 2019 Abstract. Dissimilatory iron reduction is probably one of that may be involved in the iron reduction via several po- the oldest types of metabolisms that still participates in im- tential pathways: H2 or organic matter oxidation, an active portant biogeochemical cycles, such as those of carbon and sulfur cycle, or iron-driven anaerobic oxidation of methane. sulfur. It is one of the more energetically favorable anaer- We suggest that significant upward migration of methane in obic microbial respiration processes and is usually coupled the sedimentary column and its oxidation by sulfate may fuel to the oxidation of organic matter. Traditionally this process the microbial activity in the sulfate methane transition zone is thought to be limited to the shallow part of the sedimen- (SMTZ).