Depositional and anthropic processes in the Holocene record of the Can Sadurní cave (Begues, Barcelona, Spain): microstratigraphic contributions
DOI:
https://doi.org/10.21701/bolgeomin.129.1.010Keywords:
coluvión, Holoceno, karst, micromorfología, redilesAbstract
The geoarchaeological and microstratigraphic study of the Can Sadurní cave sequence (Begues, Barcelona) reveals the presence of detrital and anthropogenic depositional processes, alternating at certain stages. These influenced the location of the diagenetic processes. The cultural sequence of the site ranges from Epipaleolithic to Late Roman Empire, with some chronocultural interruptions. During the Epipaleolithic and Mesolithic, solifluction processes were responsible for sedimentation. From the Neolithic, mass wasting and colluvial processes were dominant. Dense flows are distinguished mainly during the Cardial Early Neolithic and Early Postcardial. This type of contribution is also present to a lesser extent during the Postcardial Middle Neolithic, Late Neolithic/Chalcolithic and Early Bronze Age. Non-laminated colluvial inputs appear in the rest of the sequence. These episodes alternate with periods of stability, in which the rate of detrital sedimentation is lower or almost non-existent. This is replaced by the presence of in situ stabling areas during the Epicardial and Early Postcardial Neolithic, although evidence is detected from the Cardial Early Neolithic. Associated with these contexts, hydromorphic processes are accentuated leading to the formation of vivianite -an iron phosphate mineral- typical of a reducing medium with high organic matter.
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Ministerio de Educación y Ciencias
Grant numbers HAR2014-55131
Generalitat de Catalunya
Grant numbers 2014/100780
