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Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/28027
Title: Vegetation changes in the southern Pyrenean flank during the last millennium in relation to climate and human activities: the Montcortés lacustrine record
Authors: Rull, Valentí; González-Sampériz, Penélope; Corella, Juan Pablo ; Morellón, Mario; Giralt, Santiago
Keywords: Palynology
Climatic change
Human forcing
Historical records
Last millennium
Issue Date: 2010
Publisher: Springer
Citation: Journal of Paleolimnology 46(3): 387-404 (2011)
Abstract: [EN] We report vegetation changes of the last millennium inferred from palynological analysis of a sediment core from Lake Montcorte`s, situated at *1,000 m elevation in the southern pre-Pyrenean flank. The record begins in the Middle Ages (*AD 800) and ends around AD1920, with an average resolution of *30 years. The reconstructed vegetation sequence is complex and shows the influence of both climate and humans in shaping the landscape. Prefeudal times were characterized by the presence of welldeveloped conifer forests, which were intensely burned at the beginning of feudal times (AD 1000) and were replaced by cereal (rye) and hemp cultivation, as well as meadows and pastures. In the thirteenth century, a relatively short period of warming, likely corresponding to the Medieval Warm Period, was inferred from the presence of a low Mediterranean scrub community that is today restricted to\800 melevation.This community disappeared during Little IceAge cooling in the fifteenth century, coinciding with a decline in human activities around the lake. Forest recovery began aroundAD1500, at the beginning of the Modern period, coinciding with wetter climate. Forests, however, declined again during the seventeenth century, coinciding with maximum olive and hemp cultivation. This situation was reversed in post-Modern times (nineteenth century), characterized by an intense agricultural crisis and a significant decline in population that favored forest re-expansion. Correlations with nearby Estanya Lake, situated about 350 m below, provide a regional picture of environmental change. Besides some climate forcing evident in both sequences, human activities seem to have been the main drivers of landscape and vegetation change in the southern Pyrenean flank, in agreement with conclusions from other studies in high-mountain environments.
Description: 18 p. (Sin paginación)
Publisher version (URL): http://dx.doi.org/10.1007/s10933-010-9444-2
URI: http://hdl.handle.net/10261/28027
DOI: 10.1007/s10933-010-9444-2
ISSN: 0921-2728
E-ISSN: 1573-0417
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