Multi-mode chemical exchange in seafloor alteration revealed by lithium and potassium isotopes

Elemental exchange during seafloor alteration exerts substantial control on the chemical compositions of seawater and oceanic crust, as well as the global elemental cycling. However, detailed processes and mechanisms for element transport and isotopic exchange remain unclear. Here, we report Li and K isotopic compositions across an altered MORB-like pillow basalt from Mariana Trench. We find large and systematic isotopic variations on a centimeter scale, with 87Li decreasing from +9.07%o to +6.21%o and 841K increasing from -0.12%o to +0.33%o from the rim to the core. The heavier-than-mantle Li and K isotopic compositions in the core likely inherit from an enriched mantle source rather than post-magmatic alteration processes. The low K and high Li isotopic compositions at the outmost rims result from adsorption during seawater-rock interactions. The basinshaped elemental and isotopic variations were subsequently formed by chemical diffusion and spontaneous seawater penetration from the weathered rind to the interior of pillow basalt sample. This study uses a smallscale sampling approach and provides the first evidence for multi-mode chemical exchange in oceanic basalts and improves our understanding of the seafloor alteration processes.

Automated summary

Elemental exchange during seafloor alteration has significant effects on the chemical compositions of seawater and oceanic crust, as well as global elemental cycling. This study investigates Li and K isotopic compositions in an altered pillow basalt from Mariana Trench, revealing large isotopic variations on a centimeter scale and providing evidence for multi-mode chemical exchange in oceanic basalts. This research enhances our understanding of seafloor alteration processes.