PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Sedimentology and palaeoenvironmental reconstruction of the late Pleistocene deposits along the Bizerte Coast, N-E Tunisia

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The N–E Tunisian coast (Bizerte region) shows several Quaternary sedimentary archives of middle to late Pleistocene age. Sedimentological analyses carried out (grain size, morphoscopy, exoscopy, petrography, mineralogy, and fossil content) on 12 sections reveal a succession that begins with infratidal deposits attributed to the last Interglacial period, followed by intertidal, continental (palaeosol) and/or aeolian deposits (aeolianites). The arrangement of these deposits, their lithological characteristics and their faunal contents are the basis for a palaeoenvironment reconstruction and estimation of palaeoclimatic conditions. A warmer climate and a high sea level characterize the beginning of this interval, followed by a sea level fall accompanied by an alternation of humid and arid climate. This alternation is reflected by intercalations of the palaeosol levels between the aeolian deposits.
Rocznik
Strony
art. no. 16
Opis fizyczny
Bibliogr. 49 poz., fot., tab., wykr.
Twórcy
autor
  • University of Carthage, Faculty of Sciences in Bizerte, Department of Earth Science, Bizerte, Tunisia
autor
  • University of Carthage, Faculty of Sciences in Bizerte, Department of Earth Science, Bizerte, Tunisia
autor
  • University of Carthage, Faculty of Sciences in Bizerte, Department of Earth Science, Bizerte, Tunisia
autor
  • University of Carthage, Faculty of Sciences in Bizerte, Department of Earth Science, Bizerte, Tunisia
Bibliografia
  • 1. Abbott, R., 1960. Sea Shells of North America. Golden Press, New York.
  • 2. Balescu, S., Huot, S., Mejri, H., Barré, M., Brisson, L.F., Lamothe, M., Oueslati, A., 2015. Luminescence dating of Middle Pleistocene (MIS 7) marine shoreline deposits along the eastern coast of Tunisia: a compari son of K-feldspar and Na-feld-spar IRSL ages. Quaternary Geochronology:, 30: 1-6.
  • 3. Ben Ayed, N., Bobier, C., Paskoff, R., Oueslati, A., Viguier, C., 1979. Sur la tectonique récente de la plage de R'mel, a l'est de Bizerte (Tunisie nord-orientale). Géologie Méditerranée, 4: 423-425.
  • 4. Chakroun, A., 2006. Etude sédimentologique et paléontologique des affleurements du Quaternaire le long de la côte Nord Orientale de la Tunisie. Ph.D. Thesis, University of Tunis and University of Perpignan.
  • 5. Chakroun, A., Zaghbib-Turki, D., 2017. Facies and fauna proxies used to reconstruct the MIS 5 and MIS 7 coastal environments in eastern Tunisia. Geological Quarterly, 61 (2): 186-204; https:// doi.org 10.7306/gq.1312
  • 6. Chakroun, A., Zaghbib-Turki, D., Miskovsky, J.C., Davaud, E., 2009. Two Tyrrhenian transgressive cycles in coastal depos its of Cap Bon Peninsula, Tunisia. Quaternary, 20: 215-226.
  • 7. Chakroun, A., Zaghbib-Turki, D., Turki, M.M., 2016. The Upper Pleistocene deposits in Rafraf (Northeastern Tunisia): new data on the Persististrombus latus level. Arabian Journal of Geosciences, 9: 1-13. https://doi.org/10.1007/s12517-016-2360-7
  • 8. Costa, P.J.M., Andrade, C., Dawson, A.G., Mahaney, W.C., Freitas, M.C., Paris, R., Tabordo, R., 2012. Microtextural characteristics of quartz grains transported and deposited by tsumanis and storms. Sedimentology Geology, 275: 55-69. https:// doi.org/10.1016/j.sedgeo.2012.07.013
  • 9. Crampon, N., 1971. Etude géologique de la bordure des Mogods, du pays de Bizerte et du nord des Hedil (Tunisie septentrionale). Ph.D. Thesis, Université de Nancy.
  • 10. de Menocal, P.B., 2004. African climate change and faunal evolution during the Pliocene-Pleistocene. Earth and Planetary Science Letters, 220: 3-24. https://doi:10.1016/S0012-821X(04)00003-2
  • 11. Elmejdoub, N., Jedoui, Y., 2009. Pleistocene raised marine deposits of the Cap Bon Peninsula (N-E Tunisia): records of sea-level high stands, climatic changes and coastal uplift. Geomorphology, 112: 179-189. https://doi.org/10.1016/j.geomorph.2009.06.001
  • 12. Folk, R.L., Ward, M.C., 1957. Brazos River bars: a study in the significance of grain size parameters. Journal of Sedimentology Petrology, 27: 3-27.
  • 13. Frébourg, G., Hasler, C.A., Le Guern, P., Davaud, E., 2008. Facies characteristics and diversity in carbonate eolianites. Facies, 54: 175-191. https://doi.org/10.1007/s10347-008-0134-8
  • 14. Gianolla, D., Negri, M., Basso, D., Sciunnach, D., 2010. Malacological response to Pleistocene sea-level change in the northern Po Plain, NItaly: detailed palaeoenvironmental reconstructions from two Lombardian cores. Rivista Italiana di Paleontologia e Stratigrafia, 116: 79-102. https://doi.org/10.13130/2039-4942/5942
  • 15. Gzam, M., Elmajdoub, N., Jedoui, Y., 2016. Late Quaternary sea level changes of Gabes coastal plain and shelf: Identification of the MIS 5c and MIS 5a onshore highstands, southern Mediterranean. Journal of Earth System Science, 125: 13-28. https:// doi.org/10.1007/s12040-015-0649-7
  • 16. Issel, A., 1914. Lembi fossiliferi Quaternari e recenti osservati nella Sardegna meridionale. Rendi conti Z R Academia Nazionale dei Lincei e Series, 523:759-770.
  • 17. Jedoui, Y., 2000. Sédimentologie et géomorphologie des dépôts littoraux quaternaire: reconstitution des variations des paléoclimats et du niveau marin dans le Sud-Est tunisien. Ph.D. Thesis, University of Tunis.
  • 18. Jedoui, Y., Davaud, E., Ben Ismail, H., Reyss, J.L., 2002. Sedimentological analysis of marine Pleistocene deposits of southeastern Tunisia: evidence of two positive eustatic pulsations during the marine isotopic substage 5e (Eemian, Tyrrhenian). Bulletin de la Société Géologique de France, 173: 63-72.
  • 19. Jedoui, Y., Reyss, J.L., Kallel, N., Montacer, M., Ismail, H.B., Davaud, E., 2003. U-seris evidence for two high Last Interglacial sea levels in southeastern Tunisia. QuaternaryScience Re- views,22: 343-351. https://doi.org/10.1016/S0277-3791(02)00133-6
  • 20. Laborel, J., 1980. Les Gastéropodes Vermétidés : leur utilisation comme marqueurs biologiques de rivages fossiles. Oceanis, 5: 221-239.
  • 21. Laborel, J., 1987. Marine biogenic construction in the Mediterranean. Report Port-Cros National Park, Marseille.
  • 22. Le Guern, P., 2004. Caractérisation pétrographique et pétrotexturale des éolianites holocenes et pléistocenes. Ph.D. Thesis, Faculté des Sciences de l'Universitė de Geneve. https:// doi.org/ 10.13097/archive-ouverte/unige:708
  • 23. Le Guern, P., Davaud, E., 2005. Recognition of ancient carbonate wind deposits: lessons from a modern analogue, Chrissi Island, Crete. Sedimentology, 52: 915-926. https:// doi.org/10.1111/j.1365-3091.2005.00700.x
  • 24. Loope, D.B., Abegg, F.E., 2001. Recognition and geologic preservation of ancient carbonate eolianites. SEPM Special Publication, 71: 3-16. https:// doi.org/10.2110/pec.01.71.0003
  • 25. Lozac'hmeur, J.H., Mascarenhas, A., 1985. Pesca artesanal equipamentos e materiais de pesca. Refloxoes sobre a pesca em Cabo Verde Praia. Secretaria de Estado das pescas.
  • 26. Mahaney, W.C., 2002. Atlas Od Sand Grain Surface Textures and Applications. Oxford University Press, New York.
  • 27. Mahmoudi, M., 1986. Stratigraphie, sédimentologie et diagenese des dépôts Tyrrhéniens du Sahel Tunisien (Tunisie orientale). Ph.D. Thesis, Université de Paris sud.
  • 28. Martinez, C.L., Paskoff, R., 1984. Indices de distension pendant le Quaternaire recent en Tunisie: leur signification sans un régime de compression généralisée. Notebook O.R.S.T.O.M. Géologie, XIV, 2: 153-161.
  • 29. Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrice, J., Moore, T.C., Shackleton, N.J., 1987. Age dating orbital theory of the ice ages: development of a high-resolution 0 to 300.000 years chronostratigraphy. QuaternaryReserch, 27: 1-29.
  • 30. Mauz, B., Elmejdoub, N., Nathan, R., Jedoui, Y., 2009. Last interglacial coastal environments in the Mediterranean-Saharan transition zone. Palaeogeography, Palaeoclimatology, Palaeoecology, 279: 137-146. https:// doi.org/10.1016/j.palaeo.2009.05.006
  • 31. Mauz, B., Faneli, F., Elmejdoub, N., Barbieri, R., 2012. Coastal response to climate change: Mediterranean shorelines during the last interglacial (MIS5). Quaternary Science Reviews, 2: 1-10. https:// doi.org/10.1016/j.quascirev.2012.02.021
  • 32. Mauz, B., Sivan, D., Galili, E., 2020. MIS 5e sea-level proxies in the eastern Mediterrannean coastal region. Earth System Science Data. https:// doi.org/10.5194/essd-2020-357
  • 33. Meco, J., 1977. Los Strombus neogenos y cuaternarias del Atlantico eurafricano (taxinomia, biostratigraphia y paleoecologia). Paleontologia de Canaria, 1: 1-142.
  • 34. Mejri, H., 2012. Paleorivages marin pleistocene du littoral est tunisien: chronologie IRSL, paleoenvironnements et regime tectonique. Ph.D. Thesis, Universite de Sfax, Universite de Lille.
  • 35. Miossec, A., 1977. Traces de stationnement de la mer au Quaternaire récent sur le littoral des Mogods (Tunisie septentrionale). Ecole Normale Supérieure de Tunis.
  • 36. Muhs, D.R., Meco, J., Kathleen, R., Simmons, K.R., 2014. Uranium series ages of corals, sea level history, and palaeozoogeography, Canary Island, Spain: an exploratory study for two Quaternaryinterglacial periods. Palaeogeography, Palaeoclimatology, Palaeoecology, 394: 99-118. https:// doi.org/10.1016/j.palaeo.2013.11.015
  • 37. Oueslati, A., 1994. Les cötes de la Tunisie. Recherches sur leur évolution au Quaternaire. La Faculté des Sciences humaines et sociales de Tunis, 2: 1-402.
  • 38. Paskoff, R., 1999. Cheminées de dissolution et éolianites du Pléistocene supérieur en Tunisie septentrionale. Geoarqueoligia i Quaternari Litoral. Memorial M Pi-Lar Fumanal Valencia, Universitatt de Valencia: 375-380.
  • 39. Paskoff, R., Sanlaville, P., 1976. Sur le Quaternaire marin de la région de Mahdia, Sahel de Sousse (Tunisie). Comptes Rendus hebdomadaires des Séances de l'Académie des Sciences, D, Sciences Naturelles, 283: 1715-1718.
  • 40. Paskoff, R., Sanlaville, P., 1983. Les côtes de la Tunisie: variation du niveau marin depuis le Tyrrhénien. Maison de l'Orient et de la Méditerranée: 19-33.
  • 41. Paskoff, R., Sanlaville, P., 1986. Oscillations climatiques en Tunisie littorale depuis le dernier interglaciaire jusqu'au début de l'Holocene. Bulletin Association Franęaise des Etudes du Quaternaire, 1-2:78-83.
  • 42. Pettijohn, F.J., Potter, P.E., Siever, R., 1987. Sand and Sandstone (2nd ed). Spinger, New York.
  • 43. Perrier, R., 1954. La faune de la France illustrée. Fasc. 9. Bryozoaire, Brachiopodes, Mollusques, Protocordés (Amphioxus, Tuniciers). Librairie Delagrave, Paris.
  • 44. Rouvier, H., 1977. Géologie de l'extręme nord tunisien, tectonique et paléogéographies superposées ř l'extrémité orientale de la chaine nord maghrébine. Ph.D. Thesis, Université de Paris.
  • 45. Sahli, W., Saadi, J., Regaya, K., 2019. Sedimentology and high-frequency cycles of the late Pleistocene of the Bizerte area (N-E Tunisia). Arabian Journal of Earth Science, 12:1-14. https:// doi.org/10.1007/s12517-019-4719-z
  • 46. Sessa, J.A., Callapez, P.M., Dinis, P.A., Hendy A.J.W., 2013. Paleoenvironmental and paleobiogeographical implications of a Middle Pleistocene mollusk assemblage from the marine terraces of Baia das Pipas, Angola. Journal of Paleontology, 87: 1016-1040. https:// doi.org/10.1666/12-119
  • 47. Solignac, M., 1927. Etude géologique de la Tunisie Septentrionale. Ph.D. Thesis, University of Lyon.
  • 48. Temani, R., Gaaloul, N., Jedoui, Y., Razgailah, S., 2008. Les dépôts du Pléistocene supérieur du Cap Bon (Tunisie Nord Orientale) caractérisation biosédimentologique et évolution spatio-temporelle. Géo-Eco-Trop, 32: 83-90.
  • 49. Vos, K., Vandenberghe, N., Elsen, J., 2014. Surface texture analysis of quartz grains by scanning elec tron microscopy (SEM): from sample preparation to environmental interpretation. Earth- Science Reviews, 128: 93-100. https:// doi.org/10.1016/j.earscirev.2013.10.013
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-77161ea1-9adb-49ef-9f56-a9931d0eb649
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.