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Table S1. Name and location of measured sections. Section numbers refer to those on the location map (Fig. 1). The section numeration used by Ricci Lucchi & Valmori (1980) is also shown (RV No.) for reference. Grid references are given using the Gauss-Boaga coordinate system. Exposure quality of each section is categorised in 'complete' sections. Table S2. Lithofacies description scheme (after Amy & Talling, 2006). Figure S1. Map showing the location of each numbered section (Web Table 1). Figure S2. Palaeocurrents measurements from basal flutes and grooves for major thick beds (revised with additional data from Amy & Talling, 2006). A key in the lower right part of the figure shows the position of the Ridracoli, Isola-Pianetto, Civorno, Pietralunga, and Borgo Pace structural elements (Fig. 1), together with the location of the Verghereto High and the Savio and Marecchia deep-seated tectonic lineaments. Note the lack of significant deflection of palaeocurrents in the vicinity of the Verghereto, Cavalmagra or Lamoli Highs. Figure S3. Transects orientated approximately parallel to palaeoflow through Bed 0 on the (A) Pianetto, Civorno, and Borgo Pace, (B) Isola, and (C) Ridracoli and Pietralunga structural elements. The location of the cross-sections is shown on Figure 1. Inset shows gridded sandstone and mudstone interval thickness from logged sections spanning the entire outcrop area. (D) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S4. Transect orientated approximately parallel to palaeoflow through (A) Bed 1.5 and (B) Bed 7.1 for the Ridracoli and Pietralunga structural elements. The position of the cross-section is shown on Figure 1. Inset shows gridded sandstone and mudstone interval thickness from logged sections spanning the entire outcrop area for Bed 1.5. (C) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S5. Transects orientated approximately parallel to palaeoflow through Bed 2.5 on the (A) Pianetto, Civorno, and Borgo Pace, (B) Isola, and (C) Ridracoli and Pietralunga structural elements. The location of the cross-sections is shown on Figure 1. Inset shows gridded sandstone and mudstone interval thickness, and palaeocurrent data, from logged sections spanning the entire outcrop area. (D) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S6. Transect orientated approximately parallel to palaeoflow through (A) Colombine 1 and (B) Bed 8 for the Ridracoli and Pietralunga structural elements. The position of the cross-section is shown on Figure 1. Inset shows gridded sandstone and mudstone interval thickness from logged sections spanning the entire outcrop area for Bed 8. (C) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S7. Transects orientated approximately parallel to palaeoflow through Bed 2 on the (A) Pianetto, Civorno, and Borgo Pace, (B) Isola, and (C) Ridracoli and Pietralunga structural elements. The location of the cross-sections is shown on Figure 1. Inset shows gridded sandstone and mudstone interval thickness from logged sections spanning the entire outcrop area. (D) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S8. Transects orientated approximately parallel to palaeoflow through Bed 5.1 on the (A) Pianetto, Civorno, and Borgo Pace, (B) Isola, and (C) Ridracoli and Pietralunga structural elements. The location of the cross-sections is shown on Figure 1. Inset shows gridded sandstone thickness from logged sections spanning the entire outcrop area. (D) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S9. Transects orientated approximately parallel to palaeoflow through Bed 1 on the (A) Pianetto, Civorno, and Borgo Pace, (B) Isola, and (C) Ridracoli and Pietralunga structural elements. The location of the cross-sections is shown on Figure 1. Inset shows gridded sandstone and mudstone interval thickness, and palaeocurrent data from logged sections spanning the entire outcrop area. (D) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S10. Transects orientated approximately parallel to palaeoflow through Bed 7 on the (A) Pianetto, Civorno, and Borgo Pace, (B) Isola, and (C) Ridracoli and Pietralunga structural elements. The location of the cross-sections is shown on Figure 1. Inset shows gridded sandstone and mudstone interval thickness, and palaeoflow data from logged sections spanning the entire outcrop area. (D) Inferred vertically-exaggerated qualitative basin profile (Fig. 3). Figure S11. Plots of turbidite sandstone thickness verses distance along a trend of 135û, for sections on the Ridracoli and Pietralunga structural elements. The Figure allows exponential trends in sandstone thickness to be assessed for the beds. Turbidite Shape and Depositional Process 4

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