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Deltaic plain development and environmental changes in the Petite Camargue, Rhone Delta, France, in the past 2000 years

Published online by Cambridge University Press:  20 January 2017

Tony Rey ,
David Lefevre  and
Claude Vella
Tony Rey*
Affiliation:
UMR 5140 CNRS, Université Paul Valéry - Montpellier III, Route de Mende, BP 5043, 34032 Montpellier cedex, France
David Lefevre
Affiliation:
UMR 5140 CNRS, Université Paul Valéry - Montpellier III, Route de Mende, BP 5043, 34032 Montpellier cedex, France
Claude Vella
Affiliation:
UMR 6635 CEREGE, Université Aix-Marseille I et III, Europôle de l'Arbois - BP 80, 13545 Aix-en-Provence cedex 04, France
*
*Corresponding author. Email Address:[email protected]
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Abstract

The deltaic plain of the Petite Camargue which constitutes the western part of the Rhone Delta, began its main progradation around 2000 yr ago. Several delta lobes follow each other and have participated in the deltaic evolution. The deltaic lobes have distinct morphologies which reflect the dynamic fluvial and marine processes under the influence of climatic and human controls. Two delta lobe systems were built by the Daladel and Peccaïs channels, after which a deflected wave-influenced delta lobe was formed by the La Ville and Saint-Roman channels. The latest channel, the Rhone Vif channel, is skewed because this channel was completely canalized and engineered up to its mouth in the beginning of the 16th century. Since the avulsion of this channel about 1550 A.D., the coastline of the Petite Camargue has been especially affected by the influence of waves and currents. The spits replaced the beach ridges which juxtaposed themselves and have migrated westward since the 16th century. The formation of the western part of the delta in the last 2000 yr is affected by not only the fluvial sedimentary fluxes and the coastal dynamics to the mouth but also climatic change and human influence.

Type
Review
Information
Quaternary Research , Volume 71 , Issue 3 , May 2009 , pp. 284 - 294
Copyright
University of Washington

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References

Aloisi, J.C. Sea-level variations on the French Mediterranean margin during the Holocene. Palaeoclimate Research 21, (2001). 99–121.Google Scholar
Aloisi, J.C., Monaco, A., Thommeret, J., and Thommeret, Y. The Holocene transgression in the Golfe of Lion (southwestern France): paleogeographic and paleobotanic evolution. Géographie Physique et Quaternaire 2, 32 (1978). 145–162.Google Scholar
Arnaud-Fassetta, G., (1998). Dynamiques fluviales holocènes dans le delta du Rhône. Thèse nouveau régime de Géographie Physique, Aix-Marseille I., p. 329 Google Scholar
Arnaud-Fassetta, G. Geomorphological records of a « flood-dominated regime » in the Rhône Delta (France) between the 1st century BC and the 2nd century AD. What correlations with the cathment palaeohydrology?. Geodinamica Acta 15, (2002). 79–92.Google Scholar
Ausseil-Badie, J., Barusseau, J.P., Descamps, C., Diop, E.H.S., Giresse, P., and Pazdur, M.F. Holocene deltaic sequence in the Saloum Estuary, Senegal. Quaternary Research 36, (1991). 178–194.Google Scholar
Bard, E., Arnaold, M., Fairbanks, R.G., and Harmelin, B. 236TH 234U 14C ages obtained from mass spectrometry on corals. Radiocarbon 35, (1993). 191–199.Google Scholar
Barusseau, J.P., Ba, M., Descamps, C., Diop, E.H.S., Giresse, P., and Saos, J.-L. Coastal evolution in Senegal and Mauritania at 103, 102 and 10-year scales; natural and human records. Quaternary International 29–30, (1995). 61–75.Google Scholar
Belotti, P., Caputo, C., Davoli, L., Evangelista, S., Garzanti, E., Pugliese, F., and Valeri, P. Morpho-sedimentary characteristics and Holocene evolution of the emergent part of the Ombrone River delta (southern Tuscany). Geomorphology 61, (2004). 71–90.CrossRefGoogle Scholar
Berger, J.-F., and Jung, C. Fonction, évolution et « taphonomie » des parcellaires en moyenne vallée du Rhône. Un exemple d'approche intégrée en archéomorphologie et en géoarchéologie dans Archéologie des parcellaires. Colloque organisé par AGER et Archea, Orléans, mars 1996. Actes Des Journées Du Programme Populus (1996). 95–112.Google Scholar
Berger, J.-F., Fiches, J.L., and Gazenbeek, M. Origin of fluvial fluctuations of the river Vidourle and their effect on the organization and evolution of the site of Ambrussum (Hérault, France) between the Iron Age and Late Antiquity. Fouache, E. International Conference, The Mediterranean World Environment and History, Université Paris-1, Panthéon-Sorbonne, 24–26 avril 2002, Working Group on Geoarchaeology. (2002). Elsevier, 77–108.Google Scholar
Berger, J.-F., Favory, F., Muxart, T., Tourneux, F.-P., and Van der Leeuw, S. Identifier, analyser et évaluer les dynamiques d'interactions entre les sociétés et leurs environnements. Lévèque, C., and Van der Leeuw, S.E. Quelles Natures Voulons-Nous? Pour Une Approche Socio-écologique Du Champ De L'environnement. (2003). Elsevier, Paris. 146–184.Google Scholar
Bhattacharya, J.-P., and Giosan, L. Wave-influenced deltas: geomorphological implications for facies reconstruction. Sedimentolgy 50, (2003). 187–210.Google Scholar
Bravard, J.-P. Géoarchéologie des vallées du Rhône–Alpes depuis le Tardiglaciaire. Bravard, J.-P., Prestreau, M. Dynamique du Paysage - Entretiens de Géoarchéologie. Documents d'Archéologie en Rhône-Alpes 15, (1995). Lyon, 129–150.Google Scholar
Bruneton, H., Arnaud-Fassetta, G., Provansal, M., and Sistach, D. Geomorphological evidences for fluvial change during the Roman period in the lower Rhône valley (southern France). Catena 45, (2001). 287–312.Google Scholar
Camuffo, D., and Enzi, S. Cambiamenti climatici negli ultimi 2000 anni. II Quaternario 7, (1994). 257–286.Google Scholar
Collectif Camargue., (1970). Étude hydrogéologique, pédologique et de salinité. D.D.A. et C.N.A. du Bas-Rhône et du Languedoc-Arles. Rapport en quatre volumes.Google Scholar
Descroix, L., and Gautier, E. Water erosion in the southern French Alps: climatic and human mechanisms. Catena 50, (2002). 53–80.CrossRefGoogle Scholar
Fitzgerald, D.M., (1982). Sediment by-passing at mixed. energy tidal inlets. Proceedings 18th Coastal. Engineering Conference, American Society of Civil Engineers, 1094–1118.Google Scholar
Florençon, P., (1996). Aigues-Mortes et la Méditerranée, recherches sur le port et choix de documents. Caisse nationale des monuments historiques, 2 volumes, .Google Scholar
Galloway, W.E., and Hobday, D.K. Terrigenous Clastic Depositional System. (1996). Springer-Verlag, Heidelberg.Google Scholar
Institut Rhône Saône, (2000). Etude globale pour une stratégie de réduction des risques dus aux crues du Rhône. Etude du transport solide. 1ère étape, rapport de synthèse. Institution interdépartementale des bassins Rhône-Saône, Valence, France., 5 volumes, .Google Scholar
Jorda, M., and Provansal, M. Impacts du climat et de l'anthropisation sur le détritisme en France du Sud-est (Provence et Alpes du Sud). Bulletin de la Société Géologique de France 197, (1996). 159–168.Google Scholar
Kondolf, G.M., Piégay, H., and Landon, N. Channel response to increased and decreased bedload supply from land use change: contrasts between two catchments. Geomorphology 45, (2002). 35–51.Google Scholar
Labeyrie, J., Lalou, C., Monaco, A., and Thommeret, J. Chronologie des niveaux eustatiques sur la côte du Roussillon de -33000 ans BP à nos jours. Comptes Rendus de l'Académie des Sciences 282, 4 (1976). 349–352.Google Scholar
Liébault, F., and Piégay, H. Causes of 20th century channel narrowing in mountain and piedmont rivers of southeastern France. Earth Surface Processes and Landforms 27, (2002). 425–444.Google Scholar
L'Homer, A., (1993). Notice explicative, Carte géologique. France (1/50000), feuille Grau du Roi (1017). Orléans.Google Scholar
L'Homer, A., Bazile, A., Thommeret, J., and Thommeret, Y. Principales étapes de l'édification du delta du Rhône de 7000 BP à nos jours; variations du niveau marin. Oceanis 7, (1981). 327–487.Google Scholar
Long, L. Carte archéologique au large de la Camargue. Bilan Scientifique Du DRASSM (2002). 53–57.Google Scholar
Ménard, M. 1532: devis d'un canal de dérivation du Petit Rhône pour le rétablissement du port d'Aigues-Mortes (original, Chambre des Comptes de Paris) publié dans Histoire civile, ecclésiastique et littéraire de la ville de Nîsmes, Paris, Chaubert-Hérissan, T.4. Preuves De l'Histoire (1753). 120–125. LXVI Google Scholar
Mohanti, M. Coastal processes and management of the Mahanadi River deltaic complex, east coast of India. Kay, R. Deltas of the World. (1993). 122–136.Google Scholar
Montaggioni, L.F., and Faure, G. Response of reef coral communities to sea-level rise; a Holocene model from Mauritius (western India Ocean). Sedimentology 44, (1997). 1053–1070.CrossRefGoogle Scholar
Panin, N. On the geomorphologic and geologic evolution on the River Danube-Black Sea interaction zone. Geo-Eco-Marina 2, (1997). 31–40.Google Scholar
Panin, N. The Danube Delta geomorphology and Holocene evolution: a synthesis. Géomorphologie: relief, processus. Environnement 4, (2003). 247–262.Google Scholar
Pichard, G. Les crues sur le Bas-Rhône de 1500 à nos jours. Pour une histoire hydro-climatique. Méditerranée 3–4, (1995). 105–116.Google Scholar
Pranzini, E. Updrift river mouth migration on cuspate deltas: two examples from the coast of Tuscany (Italy). Geomorphology 38, (2001). 125–132.CrossRefGoogle Scholar
Provansal, M., Berger, J.F., Bravard, J.P., Salvador, P.G., Arnaud-Fassetta, G., Bruneton, H., and Verot-Bourrely, A. Le régime du Rhône dans l'Antiquité et au Haut Moyen âge. Gallia (1999). 56 Google Scholar
Provansal, M., Bruneton, H., Vella, C., Arnaud-Fassetta, G., Ballais, J.L., and Leveau, P. Paléohydrologie holocène dans la basse vallée du Rhône, d'Orange à la mer. Bravard, J.-P., and Magny Dir, M. Histoire Des Rivières et Des Lacs de Lascaux à Nos Jours. (2002). Errance, Paris. 251–258.Google Scholar
Provansal, M., Vella, C., Arnaud-Fassetta, G., Sabatier, F., and Maillet, G. Role of fluvial sediment inputs in the mobility of the Rhône delta coast (France). Géomorphologie: Relief, Processus, Environnement 4, (2003). 271–282.CrossRefGoogle Scholar
Raynaud, Cl., (2005). Communes d'Aigues-Mortes, Saint-Laurent-d'Aigouze et Vauvert, Rapport de prospection–inventaire, Service Régional de l'Archéologie.Google Scholar
Rey, T., (2006). Dynamiques hydro-sédimentaires en Petite Camargue à l'Holocène. Thèse nouveau régime de Géographie Physique, Université Paul Valery-Montpellier III, 309 p.Google Scholar
Rey, T., Lefevre, D., and Vella, C. Données nouvelles sur les lobes deltaïques du paléogolfe d'Aigues-Mortes à l'Holocène (Petite Camargue, France). Quaternaire 4, 16 (2005). 329–338.Google Scholar
Roberts, H.H. Dynamics changes of Holocene Mississippi river delta plain: the delta cycle. J. Coast. Res. 13, 3 (1997). 605–627.Google Scholar
Roy, P.S., Cowell, P.J., Ferland, M.A., and Thom, B.G. Wave-dominated coasts. Carter, R.W.G., and Woodroffe, C.D. Coastal Evolution. (1994). Cambridge University Press, 121–186.Google Scholar
Sabatier, F., and Suanez, S. Evolution of the Rhône delta coast since the end of the 19th century. Géomorphologie: Relief; Processus, Environnement 4, (2003). 283–300.Google Scholar
Salvador, P.-G., (1991). Le thème de la métamorphose fluviale dans les plaines alluviale du Rhône et de l'Isère – Bassin de Malville et ombilic de Moirans–Bas Dauphiné. Thèse Université Jean Moulin-Lyon III, 498 p.Google Scholar
Salvador, P.-G., Bravard, J.-P., Vital, J., and Voruz, J.-L. Archaeological evidence for Holocene floodplain development in the Rhone Valley, France, geomorphology and geoecology. Zeitschrift für Geomorphologie Supplementband 88, (1993). 81–95.Google Scholar
Stanley, D.J., and Warne, A.G. Worldwide initiation of Holocene marine deltas by deceleration of sea level rise. Science 265, (1994). 228–231.Google Scholar
Stuiver, M., and Braziunas, T.F. Modeling atmospheric 14C influences and 14C ages of marine samples back to 10,000 BC. Radiocarbon 35, (1993). 137–189.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.K., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., Van der Plicht, J., and Spurk, M. INTCAL98 radiocarbon age calibration 24,000–0 cal yr BP. Radiocarbon 40, (1998). 1041–1083.CrossRefGoogle Scholar
Van der Leeuw, S.E. The ARCHAEOMEDES Research Team Climate, hydrology, land use, and environmental degradation in the lower Rhône Valley during the Roman period. Comptes Rendus Geoscience 337, (2005). 9–27.CrossRefGoogle Scholar
Vella, C. (1999). Perception et évaluation de la mobilité du littoral holocène sur la marge orientale du delta du Rhoˆne. The`se dedoctorat en géographie physique, Université de Provence., 225 p.Google Scholar
Vella, C., and Provansal, M. Relative sea-level rise and neotectonic events during the last 6500 yr on the southern Rhône delta, France. Marine Geology 170, (2000). 27–39.CrossRefGoogle Scholar
Vella, C., Fleury, T.-J., Raccasi, G., Provansal, M., Sabatier, F., and Bourcier, M. Evolution of the Rhône delta plain in the Holocene. Marine Geology 222–223, (2005). 235–265.Google Scholar
Warner, R.F. Gross channel change along the Durance River, southern France, over the last 100 years using cartographic data. Regulated Rivers: Research & Management 16, (2000). 141–157.Google Scholar