ArticleProceedings of the National Academy of Sciences of the United States of America2026
Regional variability but global flux balance in the deep sulfur cycle.
Article in Proceedings of the National Academy of Sciences of the United States of America, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
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7 authors.
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Abstract
Sulfur is a key volatile that influences Earth's redox state, climate, and deep geochemical cycles. Subduction zones are the primary pathways carrying sulfur from the surface into the mantle, yet the global sulfur budget and recycling efficiency remain uncertain. Here, we compile a trench-by-trench inventory of subducting sulfur using sediment compositions from ocean drilling programs collected near major trenches, integrated with spatially resolved estimates of oceanic crustal and serpentinite thicknesses derived from seismic data. Our results reveal pronounced spatial heterogeneity in sulfur fluxes, driven by large variations in sedimentary sulfur contents and fundamental tectonic differences between erosive and accretionary margins. Slab-to-arc sulfur recycling efficiency averages 37% globally but varies markedly among individual subduction systems. Despite this heterogeneity, the global sulfur cycle appears balanced on the modern Earth: Sulfur input into the mantle via slab subduction (57 ± 3 Mt y
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