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This study examines the composition and diagenesis of interstitial solutions in the North Atlantic and Southern Ocean, focusing on pore water modifications and fluxes at the water-sediment interface. Key findings include universal enrichment of Na+, Ca2+, and alkalinity, alongside depletion of Mg2+ and K+, with diagenetic modeling indicating aerobic oxidation of organic matter as a dominant reaction. The research highlights the importance of fluid advection in shaping interstitial water profiles and the pot

Author

Biswajit Panda

Language

EN