Abstract
The continental margin off Uruguay and northern Argentina is characterized by high fluvial input by the de la Plata River and a complex oceanographic regime. Here we present first results from RV Meteor Cruise M78/3 of May–July 2009, which overall aimed at investigating sediment transport processes from the coast to the deep sea by means of hydroacoustic and seismic mapping, as well as coring using conventional tools and the new MARUM seafloor drill rig (MeBo). Various mechanisms of sediment instabilities were identified based on geophysical and core data, documenting particularly the continental slope offshore Uruguay to be locus of submarine landsliding. Individual landslides are relatively small with volumes <2km3. Gravitational downslope sediment transport also occurs through the prominent Mar del Plata Canyon and several smaller canyons. The canyons originate at a midslope position, and the absence of buried upslope continuations strongly suggests upslope erosion as main process for canyon evolution. Many other morphological features (e.g., slope-parallel scarps with scour geometries) and abundant contourites in a 35-m-long MeBo core reveal that sediment transport and erosion are controlled predominantly by strong contour currents. Despite numerous landslide events, their geohazard potential is considered to be relatively small, because of their small volumes and their occurrence at relatively deep water depths of more than 1,500 m.
Similar content being viewed by others
References
Antobreh AA, Krastel S (2006) Morphology, seismic characteristics and development of Cap Timiris Canyon, offshore Mauritania: a newly discovered canyon preserved off a major arid climatic region. Mar Petrol Geol 23:37–59
Antoine D, André JM, Morel A (1996) Oceanic primary production. 2. Estimation at global scale from satellite (coastal zone color scanner) chlorophyll. Glob Biogeochem Cycles 10:43–55
Babonneau N, Savoye B, Cremer M, Klein B (2002) Morphology and architecture of the present canyon and channel system of the Zaire deep-sea fan. Mar Petrol Geol 19:445–467
Canals M, De Mol B (2009) Results from the European deep ocean margins research training network. Int J Earth Sci 98:715–720
Damuth JE (1994) Neogene gravity tectonics and depositional processes on the deep Niger Delta continental margin. Mar Petrol Geol 11:320–346
Damuth JE, Kumar N (1975) Amazon cone: morphology, sediments, age and growth pattern. Geol Soc Am Bull 86:873–878
de Santa Ana H, Ucha N, Gutiérrez L, Veroslavsky G (2004) Gas hydrates estimation on the gas potential from reflection seismic data in the continental shelf of Uruguay. Revista SUG 11:46–52
Farre JA, McGregor BA, Ryan WBF, Robb JM (1983) Breaching the shelfbreak: passage from youthful to mature phase in submarine canyon evolution. In: Stanley DJ, Moore GT (eds) The shelfbreak. Critical interface on continental margins. SEPM Spec Publ 33:25–39
Faugères JC, Stow DAV, Imbert P, Viana A (1999) Seismic features diagnostic of contourite drifts. Mar Geol 162:1–38
Flood RD, Shor AN (1988) Mud waves in the Argentine Basin and their relationship to regional bottom circulation patterns. Deep-Sea Res 35:943–971
Franke D, Neben S, Schreckenberger B, Schulze A, Stiller M, Krawczyk CM (2006) Crustal structure across the Colorado Basin, offshore Argentina. Geophys J Int 165:850–864
Freudenthal T, Wefer G (2007) Scientific drilling with the sea floor drill rig MeBo. Sci Drill 5:63–66
Freudenthal T, Wefer G (2009) Shallow drilling in the deep sea: the sea floor drill rig MEBO. In: Proc IEEE OCEANS Conf, OCEANS 2009 EUROPE, 11–14 May 2009, Bremen, Germany, pp 180–183. doi:10.1109/OCEANSE.2009.5278133
Gilberto DA, Bermec CS, Acha EM, Mianzan H (2004) Large-scale spatial patterns of benthic assemblages in the SW Atlantic: the Rio de la Plata estuary and adjacent shelf waters. Estuar Coast Shelf Sci 61:1–13
Green AN, Goff JA, Uken R (2007) Geomorphological evidence for upslope canyon-forming processes on the northern KwaZulu-Natal shelf, SW Indian Ocean, South Africa. Geo-Mar Lett 27(6):399–409. doi:10.1007/s00367-007-0082-2
Greene HG, Ward SN (2003) Mass movement features along the central California margin and their modeled consequences for tsunami generation. In: Locat J, Mienert J (eds) Submarine mass movements and their consequences. Advances in natural and technological hazards Research, vol 9. Kluwer, Dordrecht, pp 343–356
Greene HG, Murai LY, Watts P, Maher NA, Fisher MA, Paull CE, Eichhubl P (2006) Submarine landslides in the Santa Barbara Channel as potential tsunami sources. Nat Hazards Earth Syst Sci 6:63–88
Harbitz CB, Løvholt F, Pedersen G, Masson D (2006) Mechanisms of tsunami generation by submarine landslides: a short review. Norw J Geol 86:255–264
Heezen BC, Hollister CD, Ruddiman WF (1966) Shaping of the continental rise by deep geostrophic bottom currents. Science 152:502–508
Hensen C, Zabel M, Pfeifer K, Schwenk T, Kasten S, Riedinger N, Schulz HD, Boetius A (2003) Control of sulphate pore-water profiles by sedimentary events and the significance of anaerobic oxidation of methane for burial of sulfur in marine sediments. Geochim Cosmochim Acta 67(14):2631–2647
Hernández-Molina FJ, Paterlini M, Violante R, Marshall P, de Isasi M, Somoza L, Rebesco M (2009) Contourite depositional system on the Argentine Slope: an exceptional record of the influence of Antarctic water masses. Geology 37:507–510
Hinz K, Neben S, Schreckenberger B, Roeser HA, Block M, Goncalves de Souza K, Meyer H (1999) The Argentine continental margin north of 48°S: sedimentary successions, volcanic activity during breakup. Mar Petrol Geol 16:1–25
Klaus A, Ledbetter MT (1988) Deep-sea sedimentary processes in the Argentine Basin revealed by high-resolution seismic records (3.5 kHz echograms). Deep-Sea Res 35:899–917
Krastel S, Schmincke H-U, Jacobs CL (2001) Formation of submarine canyons on the flanks of ocean islands: examples from the Canary Islands. Geo-Mar Lett 20:160–167. doi:10.1007/s003670000049
Laberg JS, Camerlenghi A (2008) The significance of contourites for submarine slope stability. In: Rebesco M, Camerlenghi A (eds) Contourites. Developments in sedimentology, vol 60. Elsevier, Amsterdam, pp 537–556
Lonardi AG, Ewing M (1971) Sediment transport and distribution in the Argentine Basin. 4. Bathymetry of the continental margin. Argentine Basin and other related provinces. Canyons and sources of sediments. In: Physics and chemistry of the earth, vol 8. Pergamon Press, Oxford, pp 79–121
Lykousis V, Sakellariou D, Locat J (eds) (2007) Submarine mass movements and their consequences. Advances in Natural and Technological Hazards Research, vol 27. Springer, Dordrecht
Maldonado A, Barnolas A, Bohoyo F, Escuita C, Galindo-Zaldívar J, Hernández-Molina J, Jabaloy A, Lobo FJ, Nelson CH, Rodríguez-Fernández J, Somoza L, Vázquez J-T (2005) Miocene to recent contourite drifts development in the northern Weddell Sea (Antarctica). Glob Planet Change 45:99–129
Max MD, Ghidella M, Kovacs L, Paterlini M, Valladares JA (1999) Geology of the Argentine continental shelf and margin from aeromagnetic survey. Mar Petrol Geol 16:41–64
McCave IN (2002) Sedimentary settings on continental margins – an overview. In: Wefer G, Billett D, Hebbeln D, Jørgensen BB, Schlüter M, van Weering TCE (eds) Ocean margin systems. Springer, Berlin Heidelberg, pp 1–14
McHugh CMG, Ryan WBF, Eittreim S, Reed D (1998) The influence of San Gregorio fault on the morphology of Monterey Canyon. Mar Geol 146:63–91
Mosher DC, Shipp RC, Moscardelli L, Chaytor JD, Baxter CDP, Lee HJ, Urgeles R (eds) (2010) Submarine mass movements and their consequences. Advances in Natural and Technological Hazards Research, vol 28. Springer, Dordrecht
Olson DB, Podesta GP, Evans RH, Brown OB (1988) Temporal variations in the separation of Brazil and Malvinas Currents. Deep-Sea Res 35:1971–1990
Peterson RG, Stramma L (1991) Upper-level circulation in the South Atlantic Ocean. Prog Oceanogr 26:1–73
Peterson RG, Johnson CS, Krauss W, Davis RE (1996) Lagrangian measurements in the Malvinas Current. In: Wefer G, Berger W, Siedler G, Webb DJ (eds) The South Atlantic: present and past circulation. Springer, Berlin Heidelberg, pp 239–247
Piola AR, Romero SI (2004) Analysis of space-time variability of the Plata River plume. Gayana (Concepción) 68(2):482–486
Piola AR, Matano RP, Palma ED, Möller OO, Campos EJD (2005) The influence of the Plata River discharge on the western South Atlantic shelf. Geophys Res Lett 32:L01603. doi:10.1029/2004GL021638
Pratson LF, Coakley BJ (1996) A model for the headward erosion of submarine canyons induced by downslope-eroding sediment flows. Geol Soc Am Bull 108:225–234
Pratson LF, Ryan WBF, Mountain GS, Twichell DC (1994) Submarine canyon initiation by downslope-eroding sediment flows: evidence in late Cenozoic strata on the New Jersey continental slope. Geol Soc Am Bull 106:395–412
Rahiman TIH, Pettinga JR, Watts P (2007) The source mechanism and numerical modeling of the 1953 Suva tsunami, Fiji. Mar Geol 237:55–70
Rebesco M, Camerlenghi A (eds) (2008) Contourites. Developments in sedimentology, vol 60. Elsevier, Amsterdam
Rebesco M, Stow DA (2001) Seismic expression of contourites and related deposits: a preface. Mar Geophys Res 22:303–308
Reid JL (1989) On the total geostrophic circulation of the South Atlantic Ocean: flow patterns, tracers and transports. Prog Oceanogr 23:149–244
Schnabel M, Franke D, Engels M, Hinz K, Neben S, Damm V, Grassmann S, Pelliza H, Dos Santos PR (2008) The structure of the lower crust at the Argentine continental margin, South Atlantic at 44°S. Tectonophysics 454:14–22
Schwenk T, Spieß V, Hübscher C, Breitzke M (2003) Frequent channel avulsions within the active channel-levee system of the middle Bengal Fan - an exceptional channel-levee development derived from Parasound and Hydrosweep data. Deep Sea Res II 50(5):1023–1045
Spieß V, cruise participants (2002) Report and preliminary results of Meteor Cruise M 49/2, Montevideo (Uruguay) - Montevideo, 13.02. - 07.03.2001. Berichte, Fachbereich Geowissenschaften, Universtät Bremen
Stow D, Faugères J-C (2008) Contourite facies and the facies model. In: Rebesco M, Camerlenghi A (eds) Contourites. Developments in sedimentology, vol 60. Elsevier, Amsterdam, pp 223–256
Stow D, Mayall M (2000) Deep-water sedimentary systems: new models for the 21st century. Mar Petrol Geol 17:125–136
Tappin DR, Watts P, McMurty M, Lafoy Y, Matsumoto T (2001) The Sissano, Papua New Guinea tsunami of July 1998—offshore evidence on the source mechanism. Mar Geol 175:1–23
Twichell DC, Roberts DG (1982) Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons. Geology 10:408–412
Uliana MA, Biddle KT, Cerdan J (1989) Mesozoic extension and formation of Argentine sedimentary basins. In: Tankard AJ, Balkwill HR (eds) Extensional tectonics and stratigraphy of the North Atlantic margins. AAPG Memoir 46:519–614
von Lom-Keil H, Spiess V, Hopfauf V (2002) Fine-grained sediment waves on the western flank of the Zapiola Drift, Argentine Basin: evidence for variations in Late Quaternary bottom flow activity. Mar Geol 192:239–258
Ward SN (2001) Landslide tsunami. J Geophys Res 106(B6):11201–11215
Watts P, Imamura F, Grilli ST (2000) Comparing model simulations of three benchmark tsunami generation cases. Sci Tsunami Hazards 18(2):107–124
Acknowledgements
We thank the scientists and crew of Meteor Cruise M78/3 for their help in collecting the data. The paper was greatly strengthened by reviews from Aggeliki Georgiopoulou, Frank Strozyk, and the journal editors. Our research was funded by grants of the Deutsche Forschungsgemeinschaft in the frame of the Excellence Cluster “The Future Ocean” and the DFG-Research Center/Excellence Cluster “The Ocean in the Earth System”.
Author information
Authors and Affiliations
Consortia
Corresponding author
Rights and permissions
About this article
Cite this article
Krastel, S., Wefer, G., Hanebuth, T.J.J. et al. Sediment dynamics and geohazards off Uruguay and the de la Plata River region (northern Argentina and Uruguay). Geo-Mar Lett 31, 271–283 (2011). https://doi.org/10.1007/s00367-011-0232-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00367-011-0232-4