“…In a 10-15 km wide coastal strip, the thickness, texture and depositional environment of the Holocene deposits (Tosi et al 2007b(Tosi et al , c, 2009bZecchin et al 2008Zecchin et al , 2009Rizzetto et al 2009) play a significant role in controlling shallow causes of land subsidence. Other factors that contribute to increasing land subsidence at a smaller areal extent are the salinization of clay deposits due to saltwater intrusion and the biochemical oxidation of outcropping peat soils (Gambolati et al 2005;Carbognin et al 2006).…”