To establish the conventional BP age of the sedimentary features, 11 organogenic samples were taken for 14C analysis

using fragments of shells of lagoonal mollusks, vegetal and peat remains (Table 1). The CEDAD laboratories at the University of Lecce, Italy, measured radiocarbon ages. The samples were analyzed using the accelerator mass spectrometry (AMS) technique to determine the 14C content. The conventional 14C ages BP include the 13C/12C corrections and were calibrated using the Calib 7.0 program (Stuiver and Reimer, 1993), and the calibration data sets Intcal13 and Marine13 for terrestrial and marine samples, respectively (Reimer this website et al., 2013). The regional correction (delta R) for marine reservoir effect was 316 ± 35 (Siani et al., 2000). This study used the following archive documents and historical cartography:

(a) the map of the central lagoon by Domenico Margutti of 1691, (b) the hydrographical map of the lagoon by Augusto Dénaix of ca 1810 and (c) the map of the Genio Civile di Venezia of 1901. The original historical maps are the property of the Archivio di Stato di Venezia where they can be found, but a recent collection of historical map reproductions is available in Baso et al. (2003) and D’Alpaos (2010). The map of Margutti was digitized within the Image Map Archive Gis Oriented (IMAGO) Project ( Furlanetto et al., 2009), covering an area in the central lagoon of about 160 km2. MK-1775 in vitro The map of Augusto Dénaix of ca 1810 is a military topographical hydrographical map of the Venice Lagoon and its littoral between the Adige and Piave rivers. It comprises 36 tables, out of which only the ones covering the study area were used. The scale is 1:15,000. The map of the Genio Civile di Venezia M.A.V. of 1901 is a topographic and hydrographic map of the Venice Lagoon and its littoral between the Adige and Sile

rivers. It comprises 18 tables, out of which only the ones covering the Acesulfame Potassium study area were used. The scale is 1:15,000. The description of the georeferencing procedure can be found in Furlanetto and Primon (2004). For the study area we extracted information about the hydrography by digitizing the spatial distribution of palaeochannels. The interpretation of the acoustic profiles is based on a classical seismic stratigraphic method (in terms of reflector termination and configuration) (Mitchum and Vail, 1977). Detailed analysis of acoustic profiles produced a 2D map of the sedimentary features. The initial and final coordinates of each acoustic reflector, with its description, were saved in a Geographical Information System (GIS) through the software GeoMedia®, for further mapping and interpretation (Madricardo et al., 2007, Madricardo et al., 2012 and de Souza et al., 2013). In the GIS it was possible to correlate the acoustic reflectors and to draw the areal extent of each sedimentary feature.