Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
7452026 | Quaternary International | 2014 | 18 Pages |
Abstract
Radiocarbon-dated palaeoecological records from the upland zone of the northern Apennines spanning the Mid-Late Holocene (last 7000 years) have been evaluated using established criteria for detecting anthropogenic impact on the landscape and environment. The integrated palaeoecological records across the study area collectively indicate human interference with natural vegetation succession and landscape modification from at least the Middle Neolithic. These activities resulted in the progressive decline of Abies, Ulmus, Fraxinus and Tilia, and the spread of Fagus, from â¼7000Â cal BP, accompanied at various times by evidence for biomass burning, soil erosion, the expansion of shrubland and herbaceous taxa, and the possible cultivation of Olea, Juglans and Castanea. Comparison of these data with the archaeological scheme for the region, and the climate history of the central-western Mediterranean, has revealed that the palaeoecological records broadly support the archaeological evidence, but suggest that several key vegetation changes also coincide with important periods of climate change, especially at â¼7800-5000Â cal BP.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Nicholas P. Branch, Nathalie A.F. Marini,