Potentialités et contraintes d'occupation du littoral du Bas-Médoc : bilan du projet LITAQ et réflexion sur les paléo-risques
BERTRAND, Frédéric
Pôle de recherche pour l'organisation et la diffusion de l'information géographique [PRODIG]
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Pôle de recherche pour l'organisation et la diffusion de l'information géographique [PRODIG]
BERTRAND, Frédéric
Pôle de recherche pour l'organisation et la diffusion de l'information géographique [PRODIG]
Pôle de recherche pour l'organisation et la diffusion de l'information géographique [PRODIG]
ARNAUD-FASSETTA, Gilles
Pôle de recherche pour l'organisation et la diffusion de l'information géographique [PRODIG (UMR_8586 / UMR_D_215 / UM_115)]
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Pôle de recherche pour l'organisation et la diffusion de l'information géographique [PRODIG (UMR_8586 / UMR_D_215 / UM_115)]
Langue
EN
Article de revue
Ce document a été publié dans
Quaternaire. 2019-04-25, vol. 30, n° 1, p. 97-111
Résumé en anglais
The adaptation of territorial systems to the ongoing climate change is an issue which implies to test past populations abilities to cope, to “bounce back” or to adapt during similar past environmental changes. The ...Lire la suite >
The adaptation of territorial systems to the ongoing climate change is an issue which implies to test past populations abilities to cope, to “bounce back” or to adapt during similar past environmental changes. The chronostratigraphical and archaeological results, obtained in the frame of the LITAQ project, make it possible to better understand changes encountered by a coastal system (now on the shore front) whose intense occupation since the Neolithic period was linked to the exploitation of specific resources (salt, grazing), then inherent to a fluvial mouth and estuarine system, at present fossilized under the modern dune. One of the issues raised by these results is linked to the decline of salt-related activities during the whole Bronze period, whereas it is bracketed by a period of growing during the Neolithic (for which we were far from measuring the real amplitude) and by the first Iron Age during which salt production appears to be the main motivation for the settlement and the use of coastal marshes. However, the chronological gap, of about thirteen centuries, recorded between the Early Bronze Age (~2200 BC) and the Late Bronze Age (~900 BC), prevents us from using climate changes as a deterministic and unique factor of land-use changes of the Médoc Peninsula around the first millennium. The complex rhythms, that accompany those changes during this period and the subsequent Iron Age, invite us to consider the territorial vulnerability in a context of hydrogeomorphological modifications of the coast synchronously to those of natural components involved in the salt production process. Modalities of the spatial development of this activity (as deduced from the analysis of inventoried remains) in a context of restricted tidal exchanges (i.e. barred estuary), testify to the adaptability of protohistoric Médocan communities, which faced a slow and progressive disturbance of the coastal system; they attest also to the past resilience, in its systemic sense, of a territory nowadays far from major influences.< Réduire
Mots clés en anglais
coastal environment
palaeo-risks
estuary
salt marshes
vulnerability
land use
adaptation
Lien vers les données de la recherche
Project ANR
Using the world in ancient societies : processes and forms of appropriation of space in Long Time - ANR-10-LABX-0052
Initiative d'excellence de l'Université de Bordeaux - ANR-10-IDEX-0003
Initiative d'excellence de l'Université de Bordeaux - ANR-10-IDEX-0003