FP7Индивидуална стипендия2008–2010

ECTOARC · Ectomycorrhizal fungi and the stability of soil organic matter in a changing Arctic

7РП — „Хора“ (Действия „Мария Кюри“)

Период
2008-03-01 → 2010-02-28
Финансиране от ЕС
177 321 €
Участници
1
Схема
MC-IEF

Линиите свързват координатора с партньорите.

Накратко на български

Ектомикоризните гъби в Арктика и тяхното влияние върху разграждането на органичната материя в почвата се анализират чрез промени в растителността. Това помага да се разбере дали освобождаването на въглерод от почвите ще ускори глобалното затопляне.

Този кратък обзор е генериран от изкуствен интелект

Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.

Резултати накратко

Ectomycorrhizal fungi and the stability of soil organic matter in a changing Arctic

The Arctic region is currently facing large changes in climatic conditions, with expected consequences for the vulnerable terrestrial ecosystems. Northern ecosystems contain a large proportion of the global soil carbon (C) stock, and there is a risk that environmental changes will lead to a release of carbon dioxide from this pool, substantially amplifying atmospheric warming potential. However, populations of plants and microorganisms will likely change with changed environmental conditions. An increased abundance of shrubs and trees forming ectomycorrhizal symbiosis with soil fungi has already been observed across the Arctic tundra biome as a response to recent warming, and this trend is expected to continue. Ectomycorrhizal mycelia may contribute significantly to organic matter formation but also contribute to the degradation of organic matter by producing extracellular enzymes. This two-year Marie Curie project has explored the possible role of ectomycorrhizal fungi as main drivers of soil C dynamics when tree growth increase in northern biomes. The project explored two natural gradient systems in northern Sweden, a subarctic-alpine forest-heath ecotone and a long-term boreal forest chronosequence, in order to characterise shifts in fungal communities in relation to important ecosystem functions. The project combined novel molecular tools, high-throughput pyrosequencing, to characterise fungal communities, with ecosystem level measurements, such as C, nutrient and stable isotope pools and biomass estimates. Results from the forest-heath ecotone point to a strong, positive coupling between tree abundance, mycorrhizal fungal growth and decomposition rate of humus. Ectomycorrhizal mycelial production was ten-fold higher in forest than in the heath. In contrast, the total soil C pool in the forest was one-third of the pool in the health systems, although litter production was larger here. This points to a much higher turnover rate of soil organic matter in the forest, possibly related to higher ectomycorrhizal activity. The dataset of 80 000 fungal sequences also clearly showed that fungal communities shifted - both along the ecotone and down soil profiles. However, an overwhelming number of unknown taxa (over 90 % of the 1604 taxa) were found, highlighting a need for further research in the area. In conclusion, this study strongly suggests that trees, through their interaction with ectomycorrhizal fungi, play a more direct role in soil C turnover than previously thought. Two manuscripts are in preparation from this work; one concerning the bioinformatics pipeline that we developed to process the sequence data (see http://www.scata.mykopat.slu.se online) and one on results from the field study. This Marie Curie fellowship has led to a continuation contract between the fellow and Department of Forest Mycology and Pathology, and results from two other projects will be available within the coming year. If the direct coupling between tree production and humus decomposition via ectomycorrhizal fungal activities suggested by this project is confirmed by further studies, it will be extremely important to include this in models predicting future C balance of northern regions. Better predictions of climate effects will be of great value to people dependent in whole or in part on tundra resources to maintain their livelihoods, managers of wildlife and natural resources in far northern regions, and to public policymakers and others with interests in tundra regions. Arctic and Boreal ecosystems represent an important pool in both national and global C budgets. Increased certainty in predictions of northern ecosystem responses to global change, thus, is pivotal for the planning of sustainable management of northern natural resources and for sustainable development of the surrounding society that depend on them. Contact details: K. E. Clemmensen, Uppsala Biocenter, SLU, Department of Forest Mycology and Pathology, Karina.Clemmensen@mykopat.slu.se

Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз

Цел на проекта

The Arctic is currently facing large changes in climatic conditions, with expected consequences for the vulnerable terrestrial ecosystems. Arctic ecosystems contain a large proportion of the global soil carbon stock, and there is a risk that environmental changes will lead to a release of carbon dioxide from this pool substantially amplifying the atmospheric warming potential. However, populations of plants and microorganisms will likely change with changed environmental conditions. An increased abundance of plants associating with ectomycorrhizal (EM) fungi has already been observed across the arctic tundra biome as a response to recent warming, and this trend is expected to continue. Recent research suggests that EM mycelia contribute disproportionately relative to plant inputs to soil organic matter formation. Hence, increased abundance of EM plants and fungi could partly counterbalance the expected respiratory loss of carbon from tundra soils in the future. However, EM fungi also contribute to the degradation of organic matter by producing extracellular enzymes thereby decreasing carbon storage. It is crucial to sort out which of these mechanisms dominate in different ecosystems and under different environmental conditions in order to build reliable conceptual and predictive models describing the future carbon balance of the Arctic. This project is the first to explore the role of EM fungi as drivers of soil carbon dynamics in the Arctic in relation to global change. The project explores responses of EM fungi at three interlinked levels, that is, their abundance, species composition and functioning, to long-term field experiments simulating climate change in the sub- and high arctic. The project combines methods to measure ecological pools and processes (soil C and N pools, 13C and 15N natural abundance) with novel methods for studying EM community composition and functioning (fungal ingrowth bags, molecular community analyses, exoenzyme production).

Оригинален текст от CORDIS (на английски).

Участници

  • SVERIGES LANTBRUKSUNIVERSITET · UppsalaКоординаторШвеция

Връзки

Данни: CORDIS, © Европейски съюз