Long-term ecological changes in Mediterranean mountain lakes linked to recent climate change and Saharan dust deposition revealed by diatom analyses

被引:15
作者
Perez-Martinez, Carmen [1 ,2 ]
Ruhland, Kathleen M. [3 ]
Smol, John P. [3 ]
Jones, Vivienne J. [4 ]
Conde-Porcuna, Jose M. [1 ,2 ]
机构
[1] Univ Granada, Inst Water Res, Granada 18071, Spain
[2] Univ Granada, Fac Sci, Dept Ecol, Granada 18071, Spain
[3] Queens Univ, Dept Biol, Paleoecol Environm Assessment & Res Lab PEARL, Kingston, ON K7L 3N6, Canada
[4] UCL, Environm Change Res Ctr, Dept Geog, Pearson Bldg, London WC1E 6BT, England
关键词
Alkalinization; Aridity; Drought; Ca atmospheric input; Paleolimnology; Sierra Nevada; SIERRA-NEVADA; ENVIRONMENTAL VARIABLES; ALPINE LAKE; ASSEMBLAGES; COMMUNITY; WATER; ALPS; TRENDS; SPAIN; CHLOROPHYLL;
D O I
10.1016/j.scitotenv.2020.138519
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Anthropogenic climate change and the recent increase of Saharan dust deposition has had substantial effects on Mediterranean alpine regions. We examined changes in diatom assemblage composition over the past similar to 180 years from high-resolution, dated sediment cores retrieved from six remote lakes in the Sierra Nevada Mountains of Southern Spain. In all lakes, changes in diatom composition began over a century ago, but were more pronounced after similar to 1970 CE, concurrent with trends in rising regional air temperature, declining precipitation, and increased Saharan dust deposition. Temperaturewas identified as themain predictor of diatom assemblage changes, whereas both Saharan dust deposition drivers, the Sahel precipitation index and thewinter North Atlantic Oscillation, were secondary explanatory variables. Diatom compositional shifts are indicative of lake alkalinization (linked to heightened evapoconcentration and an increase in calcium-rich Saharan dust input) and reduced lake water turbulence (linked to lower water levels and reduced inflows to the lakes). Moreover, decreases in epiphytic diatom species were indicative of increasing aridity and the drying of catchment meadows. Our results support the conclusions of previous chlorophyll-a and cladoceran-based paleolimnological analyses of these same dated sedimentary records which show a regional-scale response to climate change and Saharan dust deposition in Sierra Nevada lakes and their catchments during the 20th century. However, diatom assemblages seem to respond to different atmospheric and climate-related effects than cladoceran assemblages and chlorophyll-a concentrations. The recent impact of climate change and atmospheric Saharan deposition on lake biota assemblages and water chemistry, aswell as catchment water availability, will have important implications for the valuable ecosystem services that th e Sierra Nevada provides. (C) 2020 Elsevier B.V. All rights reserved.
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页数:14
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