Exploring seven hundred years of transhumance, climate dynamic, fire and human activity through a historical mountain pass in central Spain
Exploring seven hundred years of transhumance, climate dynamic, fire and human activity through a historical mountain pass in central Spain作者机构:Research Group Archaeobiology Institute of History CSIC Dept.Botany Faculty of Sciences University of Granada Dept.of Plant Biology Faculty of Biology Complutense University LETG CAEN GEOPHEN-UMR 6554 CNRS University of Caen-Normandie
出 版 物:《Journal of Mountain Science》 (山地科学学报(英文))
年 卷 期:2016年第13卷第7期
页 面:1139-1153页
核心收录:
学科分类:060201[历史学-历史地理学] 12[管理学] 120203[管理学-旅游管理] 1202[管理学-工商管理] 06[历史学] 07[理学] 070502[理学-人文地理学] 0705[理学-地理学] 0602[历史学-中国史]
基 金:funded by the project HAR2013-43701-P (Spanish Economy and Competitiveness Ministry) Excellence Research Projects Program from the Andalusian Government P11-RNM-7033
主 题:Climate and human impacts Fire Late Holocene Gredos range Vegetation history
摘 要:A high-altitude peat sequence from the heart of the Spanish Central System(Gredos range) was analysed through a multi-proxy approach to determine the sensitivity of high-mountain habitats to climate, fire and land use changes during the last seven hundred years, providing valuable insight into our understanding of the vegetation history and environmental changes in a mountain pass close to a traditional route of transhumance. The pollen data indicate that the vegetation was dominated by shrublands and grasslands with scattered pines in high-mountain areas, while in the valleys cereals, chestnut and olive trees were cultivated. Strong declines of high-mountain pines percentages are recorded at 1540, 1675, 1765, 1835 and 1925 cal AD, which may be related to increasing grazing activities and/or the occurrence of anthropogenic fires. The practice of mountain summer farming and transhumance deeply changed and redesigned the landscape of the high altitudes in central Spain(Gredos range) since the Middle Ages, although its dynamics was influenced in some way by climate variability of the past seven centuries.