Pedostratigraphic and geoarchaeological surveys of Funtana Meiga (Sinis) sections have been carried out with the aim to reconstruct environmental and climatic changes in central western costal of Sardinia (Italy) during Late Pelistocene and Holocene. Stratigraphic evidences, micromorphology and 14C data, indicate that the relatively stable land surfaces associated with significant soil formation (e.g. bioturbation, weathering, leaching and clay translocation processes) occurred during the Bronze Age, as well as instability phases, erosion, aeolian and colluvial accumulation in the Punic and Roman period
Variazioni ambientali oloceniche nella costa occidentale della Sardegna: evidenze pedostratigrafiche e geoarcheologiche
MELIS, RITA TERESA;DEL VAIS, CARLA;
2008-01-01
Abstract
Pedostratigraphic and geoarchaeological surveys of Funtana Meiga (Sinis) sections have been carried out with the aim to reconstruct environmental and climatic changes in central western costal of Sardinia (Italy) during Late Pelistocene and Holocene. Stratigraphic evidences, micromorphology and 14C data, indicate that the relatively stable land surfaces associated with significant soil formation (e.g. bioturbation, weathering, leaching and clay translocation processes) occurred during the Bronze Age, as well as instability phases, erosion, aeolian and colluvial accumulation in the Punic and Roman period
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