Item request has been placed! ×
Item request cannot be made. ×
loading  Processing Request

3000 ans de modification des environnements littoraux à Kition-Bamboula, Larnaca, Chypre, Méditerranée

Item request has been placed! ×
Item request cannot be made. ×
loading   Processing Request
  • معلومة اضافية
    • Contributors:
      Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE); Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE); Station Marine d'Endoume; Université de la Méditerranée - Aix-Marseille 2; Département de Géologie et d'Océanographie Talence (DGO); Université Sciences et Technologies - Bordeaux 1 (UB); Laboratoire Chimie de l'environnement (LCE); Aix Marseille Université (AMU)-Institut de Chimie - CNRS Chimie (INC-CNRS)-Centre National de la Recherche Scientifique (CNRS); Nottingham Trent University; Laboratoire de Géologie; Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS); Maison méditerranéenne des sciences de l'Homme (MMSH); Aix Marseille Université (AMU)-Centre National de la Recherche Scientifique (CNRS); Histoire et Sources des Mondes antiques (HiSoMA); École normale supérieure de Lyon (ENS de Lyon); Université de Lyon-Université de Lyon-Université Lumière - Lyon 2 (UL2)-Université Jean Moulin - Lyon 3 (UJML); Université de Lyon-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS)-Approches Littéraires, Linguistiques et Historiques des Sources (ALLHiS); Université Jean Monnet - Saint-Étienne (UJM)
    • بيانات النشر:
      HAL CCSD
      AFEQ-CNF INQUA
    • الموضوع:
      1999
    • Collection:
      Université de Lyon: HAL
    • نبذة مختصرة :
      International audience ; The Paleo-environmental reconstruction of the coastal sector of Kition Bamboula demonstrates that this area was an open bay that became separated from the Mediterranean sea. The evolution has been basically led by relative sea-level variations, tectonic mobility and variations in sediment supply. Coupled with archeological data, the cores stratigraphy emphasizes six distinct environments of deposition since 3000 years B.P. (A) Around 3000 BP, an open marine embayment is characterized by a calm sedimentation. The influences of external dynamics are mitigated by the presence of a Postdoma reef barrier. This first type of environment was used as a mycenian harbour between XIV-XIIIth centuries BC. (B) Between 2000 BP and 1600 BP, a lagoon is characterized by marine juvenile molluscs dying quickly in this environment that corresponds to a «leaky lagoon». The initial marine embayment was then partially closed by a spit and used as a Phoenician military harbour. (C) After 1600 BP, an hypersaline lagoon with sporadic dessication, formed as the consequence of the almost complete closure of the lagoon which could be due either to tectonic uplift or sedimentary processes. Gypsum was formed by either subaqueous or interstitial crystallisation. Restricted connections with the open sea were discontinuous. Pelagic foraminifera were introduced during occasional marine floodings probably related to storms. (D) A re-opening of the coastal pan converted the sabkha into a brackish lagoon. This lagoon was used by Romans as a port. This re-opening might be linked to relative sea-level rise. (E) Finally, the lagoon was partially closed, transformed in marshland and described by travellers as the ancient harbour. (F) Since British colonization, an artificial filling-up of the coastal plain has transformed the quite steady paludal wetland into an urban complex. ; Dans le cadre de la fouille archéologique du port de Kition Bamboula à Larnaca, nous avons pu mettre en évidence six phases de modifications littorales ...
    • الرقم المعرف:
      10.3406/quate.1999.1637
    • الدخول الالكتروني :
      https://shs.hal.science/halshs-00091964
      https://shs.hal.science/halshs-00091964v1/document
      https://shs.hal.science/halshs-00091964v1/file/quate_1142-2904_1999_num_10_2_1637.pdf
      https://doi.org/10.3406/quate.1999.1637
    • Rights:
      http://creativecommons.org/licenses/by-nc-sa/ ; info:eu-repo/semantics/OpenAccess
    • الرقم المعرف:
      edsbas.44916BE9