Disentangling anthropogenic drivers of climate change impacts on alpine plant species: Alps vs. Mediterranean mountains final report

A. Lamprecht, M. Rutzinger, H. Pauli, Manfred Bardy-Durchhalter, Katrin Euller, R. Niederheiser, K. Steinbauer, K. Wilfing, B. Erschbamer, Rosa Fernández Calzado, V. Cecco, Andreas Gattringer, G. Kazakis, M. Mallaun, J. M. Mesa, Dietmar Moser, Hlektra Remoundou, A. Stanisci, J. Theurillat, P. Vittoz, J. Wessely, M. Winkler
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Climate factors and additionally nitrogen deposition and land-use changes have been identified as global change factors posing threats on high-mountain biodiversity, ecosystem stability and services. On the other hand, the characteristic micro-topographic variability of high mountain ecosystems may buffer them against global change impacts. Monitoring data from European mountain peaks show that changes in biodiversity patterns are closely related to rising temperatures. However, the effects of climate change on plant biodiversity differ significantly between temperate and Mediterranean biomes with species richness increases synchronously with warming in the former and richness decreases in the latter. The MediAlps project aimed at disentangling anthropogenic and natural factors underlying differential changes in plant species composition and richness observed on mountain summits in the European Alps and the Mediterranean biome at the local and regional spatial scale. Changes in plant species richness and composition and present land-use impact based on systematic field observations were recorded on long-term monitoring plots on 23 summits. Soil temperature, water potential and local dry nitrogen deposition were measured in situ. Topographic parameters were recorded with photogrammetric methods. At the regional level, climate data and regional nitrogen deposition data from online resources (CHELSA, EMEP) were used and past land-use impact was assessed via guideline-aided semi-structured interviews. (Generalized) linear mixed-effects models and structural equation models (SEM) were employed to assess the impact of these drivers on biodiversity changes. Furthermore, spatio-temporal analyses based on satellite images were conducted. Climate change is and will probably continue to be the main driver of plant biodiversity, species composition and their changes on mountain summits in both biomes. 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引用次数: 1

Abstract

Global warming has been strongly accelerating in the last decades. Climate models tell us that this trend will continue in the future, accompanied by a marked decline in precipitation in Southern Europe, whereas the Alps will likely receive more winter and less summer precipitation. Climate factors and additionally nitrogen deposition and land-use changes have been identified as global change factors posing threats on high-mountain biodiversity, ecosystem stability and services. On the other hand, the characteristic micro-topographic variability of high mountain ecosystems may buffer them against global change impacts. Monitoring data from European mountain peaks show that changes in biodiversity patterns are closely related to rising temperatures. However, the effects of climate change on plant biodiversity differ significantly between temperate and Mediterranean biomes with species richness increases synchronously with warming in the former and richness decreases in the latter. The MediAlps project aimed at disentangling anthropogenic and natural factors underlying differential changes in plant species composition and richness observed on mountain summits in the European Alps and the Mediterranean biome at the local and regional spatial scale. Changes in plant species richness and composition and present land-use impact based on systematic field observations were recorded on long-term monitoring plots on 23 summits. Soil temperature, water potential and local dry nitrogen deposition were measured in situ. Topographic parameters were recorded with photogrammetric methods. At the regional level, climate data and regional nitrogen deposition data from online resources (CHELSA, EMEP) were used and past land-use impact was assessed via guideline-aided semi-structured interviews. (Generalized) linear mixed-effects models and structural equation models (SEM) were employed to assess the impact of these drivers on biodiversity changes. Furthermore, spatio-temporal analyses based on satellite images were conducted. Climate change is and will probably continue to be the main driver of plant biodiversity, species composition and their changes on mountain summits in both biomes. However, there are biome-specific differences with precipitation playing an important role in the Mediterranean biome in addition to temperature, which clearly is the most important single factor in the temperate biome. These changes will likely lead to a further thermophilisation in both biomes. The upwards movement of species from lower elevations will likely also result in a biotic homogenization of the vegetation, exacerbated by the decline of high-elevation endemic species. Species richness will likely continue to increase in the temperate biome until the “pay-off” of extinction debts or threshold effects of population size on extinction risks set in. With decreasing precipitation species richness in the Mediterranean biome will probably decline in the long run, too. Nevertheless, other anthropogenic drivers have to be considered as well, although their influence is arguably much smaller than that of climate variables, namely nitrogen deposition with a negative influence on species richness change in the temperate biome and present land-use with a positive one in the Mediterranean biome. In addition to MediAlps’ main focus on comparing multiple anthropogenic ecological drivers in the Alps with the Mediterranean mountains, the project substantially contributed to a spatially larger scaled long-term observation effort in the frame of the GLORIA (Global Observation Research Initiative in Alpine Environments) program.
解开气候变化对高山植物物种影响的人为驱动因素:阿尔卑斯山与地中海山脉的最终报告
在过去的几十年里,全球变暖一直在加速。气候模型告诉我们,这一趋势将在未来继续下去,同时南欧的降水将显著减少,而阿尔卑斯山冬季降水可能会增加,夏季降水可能会减少。气候因子以及氮沉降和土地利用变化已被确定为对高山生物多样性、生态系统稳定性和服务构成威胁的全球变化因子。另一方面,高山生态系统特有的微地形变异性可以缓冲其对全球变化的影响。来自欧洲山峰的监测数据表明,生物多样性模式的变化与气温上升密切相关。气候变化对温带和地中海生物群落植物多样性的影响存在显著差异,温带和地中海生物群落物种丰富度随气候变暖同步增加,地中海生物群落物种丰富度随气候变暖同步增加,地中海生物群落物种丰富度随气候变暖同步减少。MediAlps项目旨在解开欧洲阿尔卑斯山脉和地中海生物群系在当地和区域空间尺度上观察到的植物物种组成和丰富度差异变化的人为因素和自然因素。通过系统的野外观测,记录了23个峰顶长期监测样地的植物物种丰富度和组成变化及其土地利用影响。就地测量了土壤温度、水势和局部干氮沉降。用摄影测量法记录地形参数。在区域层面,利用在线资源(CHELSA, EMEP)的气候数据和区域氮沉降数据,并通过指南辅助半结构化访谈评估过去的土地利用影响。采用(广义)线性混合效应模型和结构方程模型(SEM)评估了这些驱动因素对生物多样性变化的影响。并基于卫星影像进行了时空分析。气候变化现在是并可能继续是两个生物群系中植物生物多样性、物种组成及其山顶变化的主要驱动因素。然而,在地中海生物群系中,除了温度之外,降水也起着重要的作用,这显然是温带生物群系中最重要的单一因素。这些变化可能会导致两个生物群系进一步的嗜热化。低海拔物种的向上迁移也可能导致植被的生物同质化,并因高海拔特有物种的减少而加剧。温带生物群落的物种丰富度可能会继续增加,直到灭绝债务的“偿还”或种群规模对灭绝风险的阈值效应出现。随着降水的减少,地中海生物群落的物种丰富度也可能在长期内下降。然而,也必须考虑其他人为驱动因素,尽管它们的影响可以说比气候变量的影响小得多,即氮沉积对温带生物群落物种丰富度变化具有负面影响,而对地中海生物群落的土地利用具有积极影响。除了MediAlps的主要重点是比较阿尔卑斯山脉与地中海山脉的多种人为生态驱动因素外,该项目还在GLORIA(高山环境全球观测研究倡议)计划的框架下为空间上更大规模的长期观测工作做出了重大贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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