“…In other environments, availability of oxygen is often transient and forms steep chemical gradients in sediments due to high biological demand (Glud, ; Jørgensen & Revsbech, ). Such variation is a hallmark of both shallow marine environments, impacted by regular diel photosynthetic and/or tidal forcing (Dillon et al., ; Fike et al., ; Nicholson, Stolz, & Pierson, ) and marine hydrothermal systems, where advection can abruptly change on unpredictable temporal and spatial scales (Gilhooly et al., ; Houghton et al., ; Yücel et al., ). The plethora of micro‐organisms capable of oxidizing intermediate valence sulfur species (e.g., thiosulfate, sulfite, elemental sulfur) in pure culture (Giovannelli, d'Errico, Manini, Yakimov, & Vetriani, ; Habicht, Canfield, & Rethmeier, ; Sievert, Hügler, Taylor, & Wirsen, ) suggests high turnover rates for these compounds, despite the lack of field‐based evidence for a sustained, long‐term pool of intermediates within the sediments (Brune, Frenzel, & Cypionka, ; D'Hondt et al., ; Jørgensen, ; Luther et al., ).…”