Year: 2026
Type: article
Abstract: Offshore relatively fresh groundwater (ORFG; <10 grams per liter) represents an underexplored frontier in addressing global freshwater scarcity, yet its origin, persistence, and vulnerability remain poorly constrained. Here, we reveal a vast climate-driven freshwater reservoir beneath the Pearl River estuary and adjacent shelf. Integrating hydrochemical profiling, isotopic tracing, and groundwater dating, we demonstrate that this ORFG is a relic of ancient meteoric recharge, emplaced during Late Pleistocene sea-level lowstands and preserved beneath the seafloor for tens of millennia. Secular equilibrium in offshore 226 Ra/ 230 Th activity ratios, consistent 14 C ages of 6 to 10 thousand years in onshore groundwater, and pronounced onshore-offshore contrasts in salinity and δ 18 O collectively confirm its fossil nature rather than slowly circulating modern groundwater. Numerical modeling further constrains the timescale of natural degradation, underscoring the system’s resilience. These findings establish ORFG as not only as a long-lived archive of paleohydrological cycles but also as a potential strategic freshwater reserve, with substantial implications for coastal water security in a changing climate.
Source: Science Advances
Language: English
Subfield: Geochemistry and Petrology
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: gold
Estimated APC paid: $4,500
Awards: G4743129019, G4919041120, G7898446851
OpenAlex ID: W7147025392
