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• W4313588802 abstract "Abstract The coast is very sensitive to variations in environmental conditions. The interaction of marine and continental processes causes a high dynamism, generating depositional formations with a high value for paleoenvironmental reconstruction. This work focused on the case of two edapho-sedimentary sequences located under the current beach, near of archaeological tumuli context at Areoso Island (Ría de Arousa, NW Iberia). With a geoarchaeological approach, sea level rise, environmental conditions and human occupation over 6000 years are interpreted. The results of granulometric and mineralogical data, elemental composition and stratigraphic features, help to identify three formation environments: granite weathering, continental (soil formation and erosion) and marine-aeolian. Geomorphological evolution from the last 6.0 kyr BP has been controlled by climate and sea level change and anthropogenic causes. The continental facies evidence low sea level up to 4.8 kyr BP. After 3.2 kyr BP, the formation of a beach-dune system was verified at an elevation similar to the present one. These results are coherent with others obtained in lagoons in the Galician coast. These edapho-sedimentary sequences located in an open coastal system will help to improve the Holocene sea level rise curve in the NW Iberia and to understand the context in which the most important archaeological structures on the island, the tumuli, began to be eroded." @default.
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• W4313588802 date "2023-01-04" @default.
• W4313588802 modified "2023-10-18" @default.
• W4313588802 title "Sea level change and human occupation over 6000 years at Areoso Island (Ria de Arousa, NW Iberia)" @default.
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• W4313588802 doi "https://doi.org/10.21203/rs.3.rs-2383025/v1" @default.
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