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Reduced snow cover and altering vegetation patterns in the Alps, both caused by climate change, are having significant combined effects on biodiversity and ecosystem functioning in the high mountains, according to a new study.
Mountain ranges covering extensive portions of the planet are warming more faster than adjacent lowland regions, resulting in massive decreases in snow cover and rapid upward migration of dwarf plants like heather. Scientists at The University of Manchester have found that these changes are disrupting the timing of crucial alpine ecosystem functions performed by plants and soil microorganisms. The research, published today in the journal Global Change Biology and funded by the UK Natural Environment Research Council, shows that high mountain ecosystems may be less capable of retaining the important nutrients needed to sustain plant growth and maintain biodiversity in these harsh environments. Dr Arthur Broadbent, lead author of the study, said: "Our paper reveals how important the timing of many plant and soil processes are in seasonal ecosystems. People may be familiar with mismatches between plant flowering and the emergence of pollinators caused by climate change. In our study, we have demonstrated that plant and soil processes show fascinating seasonal dynamics, and that the timing of these processes can also be disrupted by climate change. The high mountains are like a canary in the coalmine because they are warming much faster than the global average. That makes our findings particularly alarming." Every year, seasonal changes in mountain ecosystems prompt large transfers of nutrients between plants and microbial communities in alpine soils. Following snowmelt in spring, plants start to grow and compete with soil microbes for nutrients, thereby triggering a shift in the storage of nutrients from soil to plants. This transfer is reversed in autumn, as plants die back, and nutrients are returned to the soil within dead leaves and roots. During alpine winters, snow acts like an insulting blanket that allows soil microbes to continue functioning and store nutrients in their biomass and enables plants to survive cold alpine winters. Climate change is predicted to cause an 80-90% loss of snow cover by the end of the century in parts of the European Alps and advance the timing of snowmelt by five to 10 weeks. Prof Michael Bahn, a collaborator on the project from the University of Innsbruck, said: "Declining winter snow cover is one of the most obvious and pronounced impacts of climate change in the Alps. Its effects on the functioning and biodiversity of alpine ecosystems are a major concern for people living in Alpine regions and beyond." The scientists from The University of Manchester, in collaboration with the University of Innsbruck, Helmholtz Zentrum Munchen, and the Centre for Ecology and Hydrology, carried out the work on a long-term field experiment in the European Alps. The findings highlight the detrimental effect of climate change on seasonal transfers and retention of nutrients between plants and soil microbes. Richard Bardgett, Principal Investigator and Professor of Ecology at The University of Manchester's Department of Earth and Environmental Sciences, said "Our work demonstrates how the combination of different facets of climate change can severely disrupt below-ground ecological processes that underpin plant growth in alpine ecosystems, with potential long-term consequences for their biodiversity and functioning." For scientists, understanding how ecosystems respond to multiple simultaneous climate change impacts remains a major challenge. Interactions between direct and indirect climate change factors, such as snow cover change or less obvious ones such as dwarf-shrub expansion, can lead to sudden and unexpected changes in ecosystem functioning. These effects are impossible to predict by studying climate change factors in isolation. (ANI)
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