“…This represents 1.56×10 6 m 3 •yr −1 •km −1 suggesting a still low "natural" SGD value. A recharge ratio of between 23 and 52% (average 35%) for karstified carbonates [Allocca et al, 2014, Arfib and Charlier, 2016, Baudement et al, 2017, Martos-Rosillo et al, 2015, Polemio, 2016, Zagana et al, 2007, and between 10 and 21% (average 16%) for detritic aquifer formations [Séraphin et al, 2016, Yagbasan, 2016, Zagana et al, 2007 were reported in the north Mediterranean area (Spain to Turkey). Given that karstic aquifers represent almost 20% of the coastal areas in Mediterranean Europe [Goldscheider et al, 2020], an average value of about 20% for the recharge ratio, therefore tenfold higher than in the southern part of the Mediterranean domain (2 to 3%), can be considered.…”