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Influence of land use and climate on recent forest expansion: a case study in the E urosiberian– M editerranean limit of north‐west S pain
Author(s) -
ÁlvarezMartínez Jose Manuel,
SuárezSeoane Susana,
Stoorvogel Jetse J.,
Luis Calabuig Estanislao
Publication year - 2014
Publication title -
journal of ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.452
H-Index - 181
eISSN - 1365-2745
pISSN - 0022-0477
DOI - 10.1111/1365-2745.12257
Subject(s) - microclimate , climate change , physical geography , mediterranean climate , land cover , environmental science , land use , abiotic component , elevation (ballistics) , habitat , geography , ecology , geometry , mathematics , archaeology , biology
Summary In Mediterranean mountainous areas, forests have expanded in recent decades because traditional management practices have been abandoned or reduced. However, understanding the ecological mechanisms behind landscape change is a complex undertaking because the influence of land use may be reinforced or constrained by abiotic factors such as climate. In this work, we evaluated their combined effects on recent forest expansion across climatic, topographic and management gradients. We used orthorectified aerial photographs from the second half of the twentieth century (1956, 1974, 1983, 1990 and 2004) to monitor changes in forest distribution in a set of 20 head‐water basins in the Cantabrian Mountains of north‐west Spain, at the Eurosiberian–Mediterranean limit. In particular, we evaluated the role of land‐use history (comparing natural vs. anthropic basins) and microclimate (comparing shaded vs. sunny aspects) of forest gain/loss rates and spatial distribution shifts. Finally, we applied Species Distribution Modelling techniques (MaxEnt and BIOMOD ) in the stated scenarios of land‐use history and microclimate, to assess habitat suitability for forest expansion on the basis of topography, soil properties and mesoclimatic variables. Forest cover increased from 10.72% in 1956 to 27.67% in 2004 in the area. The rate of expansion was significantly higher in natural basins and, particularly, on shaded slopes. In all cases, the mean elevation of new forest patches increased during the study period, which was particularly evident on natural sunny slopes. The performance of the models and the magnitude of the effects varied across land‐use histories and microclimatic conditions. Soil properties and temperature and precipitation in late spring and early summer were the main drivers of forest expansion in modelling exercises, although expansion rates and upward altitudinal shifts were primarily controlled by land‐use history and the biogeographic origin of the forests. Synthesis . The combination of monitoring and modelling techniques used in this work contributed to the understanding of forest expansion in cultural systems, indicating that ecological succession is not a homogeneous process, but varies spatially due to human and abiotic constraints since historical times.