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Variations de la ligne de rivage au cours du Post-glaciaire le long de la côte nord du Finistère. Analyses polliniques de tourbes et de dépôts organiques littoraux

1969; Volume: 6; Issue: 4 Linguagem: Inglês

10.3406/quate.1969.1140

2804-1836

Marie Thérèse Morzadec-Kerfourn,

Peat and organic deposits along the coastline of North-Finistere has been formed since the end of the Atlantic period to the Sub-atlantic. The history of the woodland is dominated by Alnus comportment. Evidence of three types of land occupation between 5700 and 3500 B.P. is given by pollen analysis. The study of these submerged peat give some informations about the shoreline displacement along the north coast of Brittany since the Neolithic.