Cees W. Passchier, Gül Sürmelihindi, Pierre-Louis Viollet, Philippe Leveau, Christoph Spötl
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引用次数: 0
Abstract
The Roman mill complex of Barbegal in France is the largest preindustrial structure in Europe. Carbonate incrustations that formed from water flowing through basins, over flumes and waterwheels of the mill complex are partly preserved. The largest carbonate fragments are derived from three wooden flumes that once served the wheels of three mills in a train of eight. The deposits formed from the same water as it moved down from mill to mill. The shape, microstratigraphy and stable isotope patterns of the deposits of each flume reveal a unique history of use for each mill during the last 8 years of operation until their final abandonment. The sidewall carbonate deposits of the flumes vary in shape due to differences in the slope of the flumes during operation, associated with different-size millwheels in different basins. At least one of the flumes must have been mobile and was uplifted to fit a millwheel of a different size. During 8 years, two millwheels were exchanged and one flume was taken out of action. Carbonate deposits from two flumes were subsequently reused for some unknown industrial purpose in a water basin, and one was later embedded as spolia in a building during late antiquity.
期刊介绍:
Geoarchaeology is an interdisciplinary journal published six times per year (in January, March, May, July, September and November). It presents the results of original research at the methodological and theoretical interface between archaeology and the geosciences and includes within its scope: interdisciplinary work focusing on understanding archaeological sites, their environmental context, and particularly site formation processes and how the analysis of sedimentary records can enhance our understanding of human activity in Quaternary environments. Manuscripts should examine the interrelationship between archaeology and the various disciplines within Quaternary science and the Earth Sciences more generally, including, for example: geology, geography, geomorphology, pedology, climatology, oceanography, geochemistry, geochronology, and geophysics. We also welcome papers that deal with the biological record of past human activity through the analysis of faunal and botanical remains and palaeoecological reconstructions that shed light on past human-environment interactions. The journal also welcomes manuscripts concerning the examination and geological context of human fossil remains as well as papers that employ analytical techniques to advance understanding of the composition and origin or material culture such as, for example, ceramics, metals, lithics, building stones, plasters, and cements. Such composition and provenance studies should be strongly grounded in their geological context through, for example, the systematic analysis of potential source materials.