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A review of undulated sediment features on Mediterranean prodeltas: distinguishing sediment transport structures from sediment deformation

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Abstract

Most Mediterranean prodeltas show undulated sediment features on the foresets of their Holocene wedges. These features have been described all along the Mediterranean for the last 30 years and interpreted as either soft sediment deformation and incipient landsliding, and more recently, as sediment transport structures. We perform a review and detailed analysis of these undulated sediment features using ultrahigh-resolution seismic and bathymetric data as well as geotechnical information and hydrodynamic time series and hydrographic transects. In this study we show that the characteristics of the sediment undulations (configuration of the reflections down section and between adjacent undulations and overall morphologic characteristics) are incompatible with a genesis by sediment deformation alone and do not show evidence of sediment deformation in most cases. Various processes in the benthic boundary layer can be invoked to explain the variety of features observed in the numerous areas displaying sediment undulations.

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References

  • Agate M, Lucido M (1995) Caratteri morfologici e sismostratigrafici della piattaforma continentale della Sicillia Nord-Occidentale: naturalista siciliana 29: 3–25

  • Agate M, Di Grigoli G, Lo Iacono C, Lo Presti V, Mancuso M, Sulli A, Vaccaro F (2009) Decoding the instabilities features along the continental margin of sicily (central mediterranean Sea. Rend Online Soc Geol It 7:99–101

    Google Scholar 

  • Aksu AE, Piper DJW (1983) Progradation of the late Quatrnary Gediz delta. Mar Geol 54:1–25

    Google Scholar 

  • Albérola C, Rousseau S, Millot C, Astraldi M, Garcia-Lafuente JJ, Gasparini GP, Send U, Vangriesheim A (1995) Tidal currents in the Western Mediterranean Sea. Oceanol Acta 18:273–284

    Google Scholar 

  • Balanya JC, Garcia-Dueñas V, Azañon JM (1997) Alternating contractional and extensional events in the Alpujarride nappes of the Alborán Domain (Betics, Gibraltar Arc). Tectonics 16:226–238

    Google Scholar 

  • Bárcenas P, Fernández-Salas LM, Macías J, Lobo FJ, Díaz del Río V (2009) Estudio morfométrico comparativo entre las ondulaciones de los prodeltas de los rios de Andalucía Oriental. Revista de la Sociedad Geológica de España 22:43–56

    Google Scholar 

  • Bassetti MA, Jouët G, Dufois F, Berné S, Rabineau M, Taviani M (2006) Sand bodies at the shelf edge in the Gulf of Lions (Western Mediterranean): deglacial history and modern processes. Mar Geol 234:93–109

    Google Scholar 

  • Bellotti P, Chiocci FL, Milli S, Tortora P, Valeri P (1994) Sequence stratigraphy and depositional setting of the Tiber delta: integration of high-resolution seismics, well logs, and archeological data. J Sediment Res 64(3):416–432

    Google Scholar 

  • Benito G, Thorndycraft VR, Rico M, Sánchez-Moya Y, Sopeña A (2008) Palaeoflood and floodplain records from Spain: evidence for long-term climate variability and environmental changes. Geomorphology 101:68–77

    Google Scholar 

  • Berné S, Jouet G, Bassetti MA, Dennielou B, Taviani M (2007) Late glacial to preboreal sea-level rise recorded by the Rhône deltaic system (NW Mediterranean). Mar Geol 245:65–88

    Google Scholar 

  • Bhattacharya JP, Davies RK (2001) Growth faults at the prodelta to delta-front transition, Cretaceous Ferron sandstone, Utah, Mar. Petrol Geol 18:525–534

    Google Scholar 

  • Bøe R, Bugge T, Rise L, Eidnes G, Eide A, Mauring E (2004) Erosional channel incision and the origin of large sediment waves in Trondheimsfjorden, central Norway. Geo-Mar Lett 24:225–240

    Google Scholar 

  • Bolaños R, Jorda G, Cateura J, Lopez J, Puigdefabregas J, Gomeza J, Espino M (2009) The XIOM: 20 years of a regional coastal observatory in the Spanish Catalan coast. J Mar Syst 77:237–260

    Google Scholar 

  • Bornhold BD, Prior DB (1990) Morphology and sedimentary processes on the subacqueous Noeick river delta, British Columbia, Canada. In: Colella A, Prior DB (eds) Coarse-grained Deltas, Spec. Publ. 10. Int. Assoc. of Sedimentol, UK., pp 169–184

    Google Scholar 

  • Bossuet G, Ruffaldi P, Magny M, Richard H, Mouthon J (1996) Dynamique et approche quantitative des remplissages fini-et postwürmiens du bassin lacustre de Cerin (Jura, France). Bull Soc Géol Fr 167:483–494

    Google Scholar 

  • Cacchione DA, Drake DE, Losada MA, Medina R (1990) Bottom-boundary layer measurements on the continental shelf off the Ebro river, Spain. Mar Geol 95:179–192

    Google Scholar 

  • Calvert A, Sandvol E, Seber D, Baranzangi M, Roecker S, Mourabit T, Vidal F, Alguacil G, Jabour N (2000) Geodynamic evolution of the lithosphere and upper mantle beneath the Alborán region of the western Mediterranean: constraints from travel time tomography. J Geophys Res 105:10871–10898

    Google Scholar 

  • Cattaneo A, Correggiari A, Penitenti D, Trincardi F, Marsset B (2003) Morphobathymetry of small-scale mud reliefs on the Adriatic shelf. In: Locat J, Mienert J (eds) Submarine Mass Movements and their Consequences. Kluwer, Amsterdam, pp 401–408

    Google Scholar 

  • Cattaneo A, Correggiari A, Marsset T, Thomas Y, Marsset B, Trincardi F (2004) Seafloor undulation pattern on the adriatic shelf and comparison to deep-water sediment waves. Mar Geol 213(1–4):121–148

    Google Scholar 

  • Cattaneo A, Trincardi F, Asioli A, Correggiari A (2007) The western Adriatic shelf clinoform: energy-limited bottomset. Cont Shelf Res 27:506–525

    Google Scholar 

  • Cavaleri L (2005) The wind and wave atlas of the Mediterranean sea—the calibration phase. Adv Geosci 2:255–257

    Google Scholar 

  • Checa A, Díaz JI, Farrán M, Maldonado A (1988) Sistemas deltaicos holocenos de los ríos Llobregat, Besós y Foix: modelos evolutivos transgresivos. Acta Geològica Hispànica. 23:241–255

    Google Scholar 

  • Chiocci FL, Esu F, Tommasi P, Chiappa V (1996) Stability of the submarine slope of the Tiber River delta. In: Senneset K (ed) Landslides. Balkema, The Netherlands., pp 521–526

    Google Scholar 

  • Collettini C, Barchi MR (2004) A comparison of structural data and seismic images for low-angle normal faults in the northern Apennines (Central Italy): constraints on activity. In: Alsop GI, Holdworth RE (eds). Flow processes in faults and shear zones. J Geol Soc Lond Spec Publ 224, pp 95–112

  • Collettini C, Chiaraluce L, Pucci S, Barchi MR, Cocco M (2005) Looking at fault reactivation matching structural geology and seismology. J Struct Geol 27:937–942

    Google Scholar 

  • Correggiari A, Trincardi F, Langone L, Roveri M (2001) Styles of failure in late Holocene highstand prodelta wedges on the Adriatic shelf. J Sediment Res 71:218–236

    Google Scholar 

  • Demestre M, Guillén J, Maynou F, Palanques A, Puig P, Recasens L, Sánchez P, Belzunces M, Bucci A, Cruz A, de Juan S, Visauta E (2004) Estimación del impacto de las obras del Plan Director sobre los recursos pesqueros que explota la flota pesquera de la cofradía de Barcelona. Technical report pp 302

  • Díaz JI, Ercilla G (1993) Holocene depositional history of the Fluviá-Muga prodelta, northwestern Mediterranean Sea. Mar Geol 111:83–92

    Google Scholar 

  • Docherty C, Banda E (1995) Evidence of the eastward migration of the Alborán Sea: a case for basin formation by delamination of the subcrustal lithosphere? Tectonics 14:804–818

    Google Scholar 

  • Durrieu de Madron X, Zervakis V, Theocharis A, Georgopoulos D (2005) Comments to “Cascades of dense water around the world ocean”. Prog Oceanogr 64:83–90

    Google Scholar 

  • EEA (European Environment Agency) (2006) Waterbase: transitional, coastal and marine waters (v.4). Available on-line: http://dataservice.eea.europa.eu/dataservice/metadetails.asp?id=990

  • Elgamal A, Yang Z, Parra E (2002) Computationalcmodeling of cyclic mobility and post-liquefaction site response. Soil Dyn Earthq Eng 22:259–271. doi:10.1016/S0267-7261(02)00022-2

  • England P, Jackson J (1989) Active deformation of the continents. Ann Rev Earth Planet Sci 17:197–226

    Google Scholar 

  • Ercilla G, Díaz JI, Alonso B, Farrán M (1995) Late Pleistocene-Holocene sedimentary evolution of the northern Catalonia continental shelf (northwestern Mediterranean Sea). Cont Shelf Res 15:1435–1451

    Google Scholar 

  • Faccenna C, Piromallo C, Crespo-Blanc A, Jolivert L, Rossett F (2004) Lateral slab deformation and the origin of the Mediterranean arcs. Tectonics 23: doi:10.1029/2002TC001488

  • Fain AMV, Ogston AS, Sternberg RW (2007) Sediment transport event analysis on the western Adriatic continental shelf. Cont Shelf Res 27:431–451

    Google Scholar 

  • FAO (Food and Agriculture Organization of the United Nations) (2007) AQUASTAT: global river sediment yields database. Land Water Development Division. http://www.fao.org/ag/aGL/aglw/aquastat/sediment/index.asp

  • Fernández-Salas LM, Lobo FJ, Sanz JL, Diaz-del-Rio V, Garcia MC, Moreno I (2007) Morphometric analysis and genetic implications of pro-deltaic sea-floor undulations in the northern Alboran Sea margin, western Mediterranean Basin. Mar Geol 243:31–56

    Google Scholar 

  • Field ME, Barber Jr JH (1993) A submarine landslide associated with shallow sea-floor gas and gas-hydrates off northern California. In: Schwab WC et al. (eds) Submarine landslides: selected studies in the US exclusive economic zone, Surv. Bull. US Geol. Soc. 2002, USA. pp 151–157

  • Fildani A, Normark WR, Kostic S, Parker G (2006) Channel formation by flow stripping: large-scale scour features along the Monterey east channel and their relation to sediment waves. Sedimentology 53:1265–1287

    Google Scholar 

  • Font J, Salat J, Julià A (1990) Marine circulation along the Ebro continental margin. Mar Geol 95:165–177

    Google Scholar 

  • Gallignani P (1982) Recent sedimentation processes on the Calabrian continental shelf and slope (Tyrrenian Sea, Italy). Oceanol Acta 5:493–500

    Google Scholar 

  • Gardner JV, Prior DB, Field ME (1999) Humboldt slide–a large shear-dominated retrogressive slope failure. Mar Geol 154:323–338

    Google Scholar 

  • Heinio P, Davies RJ (2009) Trails of depressions and sediment waves along submarine channels on the continental margin of Espirito Santo Basin, Brazil. GSA Bull 121:698–711

    Google Scholar 

  • Hernández-Molina FJ, Somoza L, Rey J, Pomar L (1994) Late Pleistocene-Holocene sediments on the Spanish continental shelves: model for very high resolution sequence stratigraphy. Mar Geol 120:129–174

    Google Scholar 

  • Hill PR, Conway K, Lintern DG, Meulé S, Picard K, Barrie JV (2008) Sedimentary processes and sediment dispersal in the southern strait of Georgia, BC, Canada. Mar Environ Res 66:S39–S48

    Google Scholar 

  • Hughes Clarke JE, Brucker S, Hill P, Conway K (2009) Monitoring morphological evolution of fjord deltas in temperate and Arctic regions: international conference on seafloor mapping for Geohazard assessment, Editors: Chiocci FL, Ridente D, Casalbore D, Bosman A, Rendiconti online della Societá Geologica Italiana 7(4):147–150

  • Imran J, Syvitski JPM (2000) Impact of extreme river events on the coastal ocean. Oceanography 13:85–92

    Google Scholar 

  • Jiménez JA, Guillén J, Gracia V, Palanques A, García MA, Sánchez-Arcilla A, Puig P, Puigdefábregas J, Rodriguez G (1999) Water and sediment fluxes on the Ebro delta shoreface. On the role of low frequency currents. Mar Geol 157:219–239

    Google Scholar 

  • Jiménez-Munt I, Sabadini R, Gardi A, Bianco G (2006) Active deformation in the Mediterranean from Gibraltar to Anatolia inferred from numerical modeling and geodetic and seismological data. J Geophys Res 108 doi:10.1029/2001JB001544

  • Johnson C, Harbury N, Hurford A (1997) The role of extension in the Miocene denudation of the Nevado-Filabride complex, Betic Cordillera (SE Spain). Tectonics 16:189–204

    Google Scholar 

  • Jouet G, Berné S, Rabineau M, Bassetti MA, Bernier P, Dennielou B (2006) Shoreface migrations at the shelf edge and sea-level changes around the last glacial maximum (Gulf of Lions, NW Mediterranean Sea). Mar Geol 234:21–42

    Google Scholar 

  • Kostic S, Parker G (2006) The response to a canyon-fan transition: internal hydraulic jumps and depositional signatures. J Hydraul Res 44:631–653

    Google Scholar 

  • Kostic S, Parker G (2007) Conditions under which a supercritical turbidity current traverses an abrupt transition to vanishing bed slope without a hydraulic jump. J Fluid Mech 586:119–145

    Google Scholar 

  • Lambeck K, Bard E (2000) Sea-level changes along the French Mediterranean coast for the past 30,000 years. Earth Planet Sci Lett 175:203–222

    Google Scholar 

  • Lambeck K, Antonioli F, Purcell A, Silenzi S (2004) Sea level change along the Italian coast from the past 10,000 yr. Quat Sci Rev 23:1567–1598

    Google Scholar 

  • Le Vourch J, Millot C, Castagné N, Le Borgne P, Olry JP (1992) Atlas of thermal fronts of the Mediterranean Sea derived from satellite imagery, vol 16. Mémoires de l’Institut Océanographique, Monaco, p 146

    Google Scholar 

  • Leder N (2002) Wind-induced internal wave dynamics near the Adriatic shelf break. Cont Shelf Res 22:445–463

    Google Scholar 

  • Lee HJ, Syvitsky JPM, Parker G, Orange D, Locat J, Hutton JHW, Imran J (2002) Distinguishing sediment waves from slope failure deposits: field examples, including the “Humboldt Slide” and modelling results. Mar Geol 192:79–104

    Google Scholar 

  • Lionello P, Sanna A (2005) Mediterranean wave climate variability and its links with NAO and Indian monsoon. Clim Dyn 25:611–623

    Google Scholar 

  • Lionello P, Malanotte-Rizzoli P, Boscolo R, Alpert P, Artale V, Li L, Luterbacher J, May W, Trigo R, Tsimplis M, Ulbrich U, Xoplaki E (2006) The Mediterranean climate: an overview of the main characteristics and issues. In: Lionello P, Malanotte-Rizzoli P, Boscolo R (eds) Mediterranean climate variability. Elsevier, Amsterdam, p 421

    Google Scholar 

  • Liquete C, Arnau P, Canals M, Colas S (2005) Mediterranean river systems of Andalusia, southern Spain, and associated deltas: a source to sink approach. Mar Geol 222–223:471–495

    Google Scholar 

  • Liquete C, Canals M, Lastras G, Amblas D, Urgeles R, De Mol B, De Batist M, Hughes-Clarke JE (2007) Long-term development and current status of the Barcelona continental shelf: a source-to-sink approach, continental shelf research doi:10.1016/j.csr.2007.02.007

  • Liquete C, Canals M, Ludwig W, Arnau P (2009) Sediment discharge of the rivers of Catalonia, NE Spain, and the influence of human impacts. J Hydrol 366(1–4):76–88 doi:10.1016/j.jhydrol.2008.12.013

    Google Scholar 

  • Lonergan L, White N (1997) Origin of the Betic-Rif mountain belt. Tectonics 16:504–522

    Google Scholar 

  • Ludwig W, Dumont E, Meybeck M, Heussner S (2009) River discharges of water and nutrients to the Mediterranean and Black Sea: major drivers for ecosystem changes during past and future decades? Prog Oceanogr 80:199–217

    Google Scholar 

  • Lykousis V (1991) Submarine slope instabilities in the Hellenic arc region, northeastern Mediterranean Sea. Mar Georesour Geotechnol 10:83–96

    Google Scholar 

  • Lykousis V, Sakellariou D, Rousakis G (2003) Prodelta slope stability and associated coastal hazards in tectonically active margins: Gulf of Corinth (NE Mediterranean). In: Locat J, Meinert J (eds) Submarine mass movements and their consequences, pp 433–440

  • Lykousis V, Roussakis G, Sakellariou D (2009) Slope failures and stability analysis of shallow water prodeltas in the active margins of Western Greece, northeastern Mediterranean Sea. Int J Earth Sci (Geol Rundsch) 98:807–822

    Google Scholar 

  • Marsset T, Marsset B, Thomas Y, Cochonat P, Cattaneo A, Tricardi F (2004) Analysis of Holocene sedimentary features on the Adriatic shelf from 3D very high resolution seismic data (Triad survey). Mar Geol 213(1–4):73–89

    Google Scholar 

  • Martinez-Martinez JM, Azañon JM (1997) Mode of extensional tectonics in the southeastern Betics (SE Spain): implications for the tectonic evolution of the peri-Alborán orogenic system. Tectonics 16:205–225

    Google Scholar 

  • Mazumder R (2003) Sediment transport, aqueous bedform stability and morphodynamics under unidirectional current: a brief overview. J Afr Earth Sci 36:1–14

    Google Scholar 

  • McKenzie DP (1972) Active tectonics of the Mediterranean region. Geophys J R Astron Soc 30:109–185

    Google Scholar 

  • Milliman JD, Syvitski JPM (1992) Geomorphic/tectonic control of sediment discharge to the ocean: the importance of small mountainous rivers. J Geol 100:525–544

    Google Scholar 

  • Millot C (1990) The Gulf of Lions’ hydrodynamics. Cont Shelf Res 10:885–894

    Google Scholar 

  • Millot C, Crépon M (1981) Inertial fluctuations on the continental shelf of the Gulf of Lions-observations and theory. J Phys Oceanogr 11:639–657

    Google Scholar 

  • Millot C, Taupier-Letage I (2005a) Additional evidence of LIW entrainment across the Algerian Basin by mesoscale eddies and not by a permanent westward-flowing vein. Prog Oceanogr 66:231–250

    Google Scholar 

  • Millot C, Taupier-Letage I (2005b) Circulation in the Mediterranean Sea. Env Chem 5:29–66

    Google Scholar 

  • Millot C, Wald L (1980) The effect of Mistral wind on the Ligurian Current near provence. Oceanol Acta 3:399–402

    Google Scholar 

  • Monaco A, Courp T, Heussner S, Carbonne J, Fowler SW, Deniaux B (1990) Seasonality and composition of particulate fluxes during ECOMARGE-I, western Gulf of Lions. Cont Shelf Res 9–11:959–987

    Google Scholar 

  • Mosher DC, Thomson RE (2002) The foreslope hills: large-scale, fine-grained sediment waves in the Strait of Georgia, British Columbia. Mar Geol 192:275–295

    Google Scholar 

  • Mougenot D, Buillot G, Rehault JP (1983) Prograding shelf break types on passive margins: some European examples. In: Stanley DJ, Moore GT (eds) The shelfbrak: critical interface on continental margins, vol 3. SEPM Special publication, Tulsa, pp 61–77

    Google Scholar 

  • Nakajima T, Satoh M (2001) The formation of large mudwaves by turbidity currents on the levees of the Toyama deep-sea channel, Japan Sea. Sedimentology 48:435–463

    Google Scholar 

  • Normark WR, Piper DJW, Hess GR (1979) Distributary channels, sand lobes, and mesotopography of navy submarine fan, California Borderland, with applications to ancient fan sediments. Sedimentology 26:749–774

    Google Scholar 

  • Normark WR, Hess GR, Stow DAV, Bow AJ (1980) Sediment waves on the Monterrey fan levee: a preliminary physical interpretation. Mar Geol 42:201–232

    Google Scholar 

  • Normark WR, Piper DJW, Posamentier H, Pirmez C, Migeon S (2002) Variability in form and growth of sediment waves on turbidite channel levees. Mar Geol 192:23–58

    Google Scholar 

  • Palanques A, Puig P, Guillén J, Jiménez J, Gracia V, Sánchez-Arcilla A, Madsen O (2002) Near-bottom suspended sediment fluxes on the microtidal low-energy Ebro continental shelf (NW Mediterranean). Cont Shelf Res 22:285–303

    Google Scholar 

  • Parker G, Toniolo H (2007) Note on the analysis of plunging of density flows. J Hydraul Eng 133:690–694

    Google Scholar 

  • Platt JP, Vissers RLM (1989) Extensional collapse of thickened continental lithosphere: a working hypothesis for the Alborán Sea and Gibraltar arc. Geology 17:540–543

    Google Scholar 

  • Platt JP, Soto JI, Whitehouse MJ, Hurford AJ, Kelley SP (1998) Thermal evolution, rate of exhumation, and tectonic significance of metamorphic rocks from the floor of the Alborán extensional basin, western Mediterranean. Tectonics 17:671–689

    Google Scholar 

  • Probst JL, Amiotte-Suchet P (1992) Fluvial suspended sediment transport and mechanical erosion in the Maghreb (North Africa). J Hydrol Sci 37:621–637

    Google Scholar 

  • Puig P, Palanques A, Guillén J (2001) Near-bottom suspended sediment variability caused by storms and near-inertial waves on the Ebro mid continental shelf (NW Mediterranean). Mar Geol 178:81–93

    Google Scholar 

  • Puig P, Ogston AS, Guillén J, Fain AMV, Palanques A (2007) Sediment transport processes from the topset to the foreset of a crenulated clinoform (Adriatic Sea). Cont Shelf Res 27:452–474

    Google Scholar 

  • Rebesco M, Neagu RC, Cuppari A, Muto A, Accettella D, Dominici R, Cova A, Romano C, Caburlotto A (2009) Morphobathymetric analysis and evidence of submarine mass movements in the western Gulf of Taranto (Calabria margin, Ionian Sea). Int J Earth Sci 98:791–805

    Google Scholar 

  • RIKZ, IGN, EADS, BRGM, UAB, IFEN, EUCC (2004) Living with coastal erosion in Europe: sediment and space for sustainability. EUROSION Atlas Part II: Maps and statistics. Available on-line: http://www.eurosion.org/reports-online/part2.pdf

  • Romagnoli C, Gabbianelli G (1990) Late Quaternary sedimentation and soft sediment deformation features in the Coriglliano Basin. North Ionian sea (Mediterranean). Giornale di Geologia 52:33–53

    Google Scholar 

  • Sacchi M, Insinga D, Milia A, Molisso F, Raspini A, Torrente MM, Conforti A (2005) Stratigraphic signature of the Vesuvius 79 AD event off the Sarno prodelta system, Naples Bay. Mar Geol 222–223:443–469

    Google Scholar 

  • Seber D, Baranzagi M, Ibenbrahim A, Demnati A (1996) Geophysical evidence for lithospheric delamination beneath the Alborán Sea and the Rif-Betic mountains. Nature 379:785–790

    Google Scholar 

  • Shackleton NJ (1987) Oxygen isotopes, ice volume and sea level. Quat Sci Rev 6:183–190

    Google Scholar 

  • Shackleton NJ (2000) The 100,000-year Ice-Age cycle found to lag temperature, carbon dioxide, and orbital eccentricity. Science 289:1897–1902

    Google Scholar 

  • Sivan D, Wdowinski S, Lambeck K, Galili E, Raban A (2001) Holocene sea-level changes along the Mediterranean coast of Israel, based on archaeological observations and numerical model. Palaeogeogr Palaeoclimatol Palaeoecol 167:101–117

    Google Scholar 

  • Skempton AW (1954) Discussion of the structure of inorganic soils. J. Soil Mech Found Div 80:263–264

    Google Scholar 

  • Sultan N, Cochonat P, Canals M, Cattaneo A, Dennielou B, Haflidason H, Laberg JS, Long D, Mienert J, Trincardi F, Urgeles R, Vorren TO, Wilson C (2004) Triggering mechanisms of slope instability processes and sediment failures on continental margins: a geotechnical approach. Mar Geol 213(1–4):291–321

    Google Scholar 

  • Sultan N, Cattaneo A, Urgeles R, Lee H, Locat J, Trincardi F, Berne S, Canals M, Lafuerza S (2008) A geomechanical approach for the genesis of sediment undulations on the Adriatic shelf Geochem Geophys Geosyst 9 Q04R03 doi:10.1029/2007GC001822

  • Syvistski JP, Morehead MD, Bahr DB, Mulder T (2000) Estimating fluvial sediment transport: the rating parameters. Water Resour Res 36:2747–2760

    Google Scholar 

  • Syvitski JPM, Milliman JD (2007) Geology, geography, and humans battle for dominance over the delivery of fluvial sediment to the coastal ocean. J Geol 115:1–19

    Google Scholar 

  • Syvitsky JPM, Kettner AJ (2007) On the flux of water and sediment into the Northern Adriatic Sea. Cont Shelf Res 27:296–308

    Google Scholar 

  • Thorndycraft VR, Benito G, Rico M, Sopeña A, Sánchez-Moya Y, Casas A (2005) A long-term flood discharge record derived from slack-water flood deposits of the Llobregat River, NE Spain. J Hydrol 313:16–31

    Google Scholar 

  • Tommasi P, Chiocci F, Esu F (1998) Geotechnical properties of soft clayey sediments from the submerged tiber river delta, Italy. Mar Georesour Geotechnol 16:221–242

    Google Scholar 

  • Trincardi F, Normark WR (1988) Sediment waves on the Tiber pro-delta slope. Geo-Mar Lett 8:149–157

    Google Scholar 

  • Trincardi F, Cattaneo A, Correggiari A (2004) Mediterranean prodelta systems: natural evolution and human impact investigated by EURODELTA. Oceanography 17:34–45

    Google Scholar 

  • Tsimplis MN, Proctor R, Flather RA (1995) A two-dimensional tidal model for the Mediterranean Sea. J Geophys Res Oceans 100:16223–16239

    Google Scholar 

  • Ulses C, Estournel C, Durrieu de Madron X, Palanques A (2008) Suspended sediment transport in the Gulf of Lions (NW Mediterranean): Impact of extreme storms and floods. Cont Shelf Res 28:2048–2070

    Google Scholar 

  • UNEP (United Nations Environment Programme) (2003) Riverine transport of water, sediments and pollutants to the Mediterranean Sea. MAP Technical Reports Series 141, Athens, 111 pp

  • Urgeles R, De Mol B, Liquete C, Canals M, De Batist M, Hughes-Clarke JE, Amblàs D, Arnau PA, Calafat AM, Casamor JL, Centella V, De Rycker K, Fabrés J, Frigola J, Lafuerza S, Lastras G, Sànchez A, Zuñiga D, Versteeg W, Willmott V (2007) Sediment undulations on the Llobregat prodelta: Signs of early slope instability or bottom current activity?. J Geophys Res 112 Art. No. B05102

  • Vannucci G, Pondrelli S, Argnani A, Morelli A, Gasperini P, Boschi E (2004) An atlas of Mediterranean seismicity. Ann Geophys 47

  • Vanoudheusden E, Sultan N, Cochonat P (2004) Mechanical behaviour of unsaturated marine sediments: experimental and theoretical approaches. Mar Geol 213:323–342

    Google Scholar 

  • Verdicchio G, Trincardi F (2006) Short-distance variability in slope bed-forms along the southwestern Adriatic Margin (Central Mediterranean). Mar Geol 234:271–292

    Google Scholar 

  • Vissers RLM, Platt JP, van der Wal D (1995) Late orogenic extension of the Betic Cordillera and the Alborán domain: a lithospheric view. Tectonics 14:786–803

    Google Scholar 

  • Waelbroeck C, Labeyrie LD, Michel E, Duplessy J-C, McManus J, Lambeck K, Balbon E, Labracherie M (2002) Sea level and deep water changes derived from benthic foraminifera isotopic record. Quat Sci Rev 21:295–305

    Google Scholar 

  • Wheatcroft RA, Borgeld JC (2000) Oceanic flood layers on the northern California margin: large-scale distribution and small-scale physical properties. Cont Shelf Res 20:2163–2190

    Google Scholar 

  • Wheatcroft RA, Stevens AW, Hunt LM, Milligan TG (2006) The large-scale distribution and internal geometry of the fall 2000 Po river flood deposit: evidence from digital X-radiography. Cont Shelf Res 26:499–516

    Google Scholar 

  • Wynn RB, Stow DAV (2002) Classification and characterization of deep-water sediment waves. Mar Geol 192:7–22

    Google Scholar 

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Acknowledgments

This manuscript is a contribution to project E-MARSHAL (IGCP-585) funded by IUGS and UNESCO. The data on the Iberian prodeltas was acquired in the frame of the Spanish project PRODELTA (REN2002-02323). Data for some areas of the continental shelf (Fluvià-Muga and Ter prodeltas) were acquired by “Secretaría General del Mar” of the Ministerio de Medio Ambiente, y Medio Rural y Marino” and provided free of charge. For the Algerian data we thank captain and crew of R/V L’Atalante (campagne PRISME 2007) and funding from French ANR projects ISIS and DANACOR. Borehole geotechnical data was acquired in the frame EC funded project PROMESS-1 (EVR1-CT-2002-40024). Hydrodynamic transects and instrumented moorings were funded by the Office of Naval Research, NICOP Grant N00014-02-1-0252. The “Generalitat de Catalunya” is acknowledged for support through an excellence research group grant (2009-SGR-146). Seismic Microtechnology is acknowledged for Kingdom Suite educational license grant. We thank F. Foglini for Figs. 3 and 5. J. Déverchère (UBO-IUEM, Brest) and K. Yelles (CRAAG, Algiers) are thanked for discussions about the Algerian shelf. Constructive reviews by A. Fildani and P. Tommasi and editor F.L. Chiocci greatly improved the submitted version of the manuscript.

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Correspondence to Roger Urgeles.

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Urgeles, R., Cattaneo, A., Puig, P. et al. A review of undulated sediment features on Mediterranean prodeltas: distinguishing sediment transport structures from sediment deformation. Mar Geophys Res 32, 49–69 (2011). https://doi.org/10.1007/s11001-011-9125-1

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  • DOI: https://doi.org/10.1007/s11001-011-9125-1

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