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Subglacial landforms as proxy for offshore freshened groundwater in formerly glaciated margins - Nature

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IntroductionOffshore freshened groundwater (OFG) is subsurface porewater with salinity below that of ambient seawater, occurring in sediments and rocks beneath or seaward of the shoreline. The definition refers to a salinity state rather than to a process and this distinction led to a recent proposal to rename the phenomenon Offshore Relatively Fresh Groundwater (ORFG), since "freshened" can be read as implying ongoing change1. OFG has emerged as a significant yet poorly constrained part of the global hydrological cycle, with reservoirs identified along continental margins worldwide2,3. Global water stress is growing, particularly in densely populated coastal regions. OFG is also of broader scientific importance for understanding geohazards, biogeochemical cycling, subseafloor microbiology, and the preservation of archaeological records. There is therefore an urgent need to better constrain the emplacement, stability, and distribution of OFG2,3,4,5,6,7,8,9,10.

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