“…Most studies involving Ra isotopes as tracers of SGD have shown that inputs of Ra from seafloor sediments are often small in relation to the SGD source term (Beck et al, 2007;Charette et al, 2003;Garcia-Solsona et al, 2008b;Rama and Moore, 1996;Rodellas et al, 2012). Conversely, recent studies in shallow embayments with fine-grained sediments and/or affected by processes that favor Ra exchange across the sediment-water interface (e.g., bioirrigation, resuspension, hypoxia) have demonstrated that the sedimentary source can supply a relevant flux of Ra isotopes, which may be comparable to SGD-derived Ra inputs (Breier et al, 2009(Breier et al, , 2010Colbert and Hammond, 2008;Garcia-Orellana et al, 2014;Gleeson et al, 2013).…”