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Dahl MB, Priemé A, Brejnrod A, Brusvang P, Lund M, Nymand J, Kramshøj M, Ro-Poulsen H, Haugwitz MS. Warming, shading and a moth outbreak reduce tundra carbon sink strength dramatically by changing plant cover and soil microbial activity. Sci Rep 2017; 7:16035. [PMID: 29167456 PMCID: PMC5700064 DOI: 10.1038/s41598-017-16007-y] [Citation(s) in RCA: 18] [Impact Index Per Article: 2.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/05/2017] [Accepted: 11/01/2017] [Indexed: 01/09/2023] Open
Abstract
Future increases in temperature and cloud cover will alter plant growth and decomposition of the large carbon pools stored in Arctic soils. A better understanding of interactions between above- and belowground processes and communities of plants and microorganisms is essential for predicting Arctic ecosystem responses to climate change. We measured ecosystem CO2 fluxes during the growing season for seven years in a dwarf-shrub tundra in West Greenland manipulated with warming and shading and experiencing a natural larvae outbreak. Vegetation composition, soil fungal community composition, microbial activity, and nutrient availability were analyzed after six years of treatment. Warming and shading altered the plant community, reduced plant CO2 uptake, and changed fungal community composition. Ecosystem carbon accumulation decreased during the growing season by 61% in shaded plots and 51% in warmed plots. Also, plant recovery was reduced in both manipulations following the larvae outbreak during the fifth treatment year. The reduced plant recovery in manipulated plots following the larvae outbreak suggests that climate change may increase tundra ecosystem sensitivity to disturbances. Also, plant community changes mediated via reduced light and reduced water availability due to increased temperature can strongly lower the carbon sink strength of tundra ecosystems.
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Affiliation(s)
- Mathilde Borg Dahl
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark
- Department of Biology, University of Copenhagen, Universitetsparken 15, DK-2100, Copenhagen Ø, Denmark
| | - Anders Priemé
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark.
- Department of Biology, University of Copenhagen, Universitetsparken 15, DK-2100, Copenhagen Ø, Denmark.
| | - Asker Brejnrod
- Department of Biology, University of Copenhagen, Universitetsparken 15, DK-2100, Copenhagen Ø, Denmark
| | - Peter Brusvang
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark
- Department of Biology, University of Copenhagen, Universitetsparken 15, DK-2100, Copenhagen Ø, Denmark
| | - Magnus Lund
- Arctic Research Centre, Department of Bioscience, Aarhus University, Frederiksborgvej 399, DK-4000, Roskilde, Denmark
| | - Josephine Nymand
- Department of Environment and Mineral Resources, Greenland Institute of Natural Resources, Box 570, DK-3900, Nuuk, Greenland
| | - Magnus Kramshøj
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark
- Department of Biology, University of Copenhagen, Universitetsparken 15, DK-2100, Copenhagen Ø, Denmark
| | - Helge Ro-Poulsen
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark
- Department of Biology, University of Copenhagen, Universitetsparken 15, DK-2100, Copenhagen Ø, Denmark
| | - Merian Skouw Haugwitz
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark
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Dighton J. Nutrient cycling in different terrestrial ecosystems in relation to fungi. ACTA ACUST UNITED AC 1995. [DOI: 10.1139/b95-397] [Citation(s) in RCA: 27] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/22/2022]
Abstract
Comparisons are made between nutrient cycling systems of arctic tundra, temperate forest, tropical forest, grassland, arable, and desert ecosystems. Detailed nutrient budgets are not given, but general differences between ecosystems are discussed primarily in relation to the role of soil fungi. General discussion reviews the impact of anthropogenic factors, including land management, pollution, and climate change on the role of fungi in nutrient cycling. Areas where further research is needed to complete our understanding of the functional aspects of fungi and nutrient cycling are highlighted and some of the techniques that may be employed are discussed. Key words: nutrient cycling, ecosystems, fungi.
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Newsham KK, Boddy L, Frankland JC, Ineson P. Effects of dry-deposited sulphur dioxide on fungal decomposition of angiosperm tree leaf litter III. Decomposition rates and fungal respiration. THE NEW PHYTOLOGIST 1992; 122:127-140. [PMID: 33874040 DOI: 10.1111/j.1469-8137.1992.tb00059.x] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
Ash (Fraxinus excelsior L.), birch (Betula spp.), hazel (Corylus avellana L.), sessile oak [Quercus petraea (Mattuschka) Liebl.] and sycamore (Acer pseudoplatanus L.) leaf litters from a virtually non-polluted and a heavily sulphur dioxide (SO2 )-polluted woodland were fumigated with environmentally-realistic concentrations (0.010-0.030μl l-1 ) of SO2 for 16-68 wk in an open-air field-fumigation experiment. Fumigation inhibited the respiration (CO2 evolution) and decomposition rates of the leaf litters. However, there were few differences in the responses between leaf litters from the two woodlands. In addition, pure cultures of four saprotrophic fungi were grown individually on irradiated hazel litter and exposed to c. 0.030μl l-1 of gaseous SO2 , for 28 d in the laboratory. The gas inhibited the respiration of Phoma exigua Desm. and Phoma macrostoma Mont, but not the respiration of Cladosporium cladosporioides (Fres.) de Vries or Coniothyrium quercinum Sacc. var. glandicola Grove. These results in part substantiated findings of previous experiments examining the effects of SO2 on the structures of saprotrophic fungal communities. The effects of SO2 on fungal decomposition of angiosperm tree leaf litter as possible causes of forest decline are discussed.
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Affiliation(s)
- K K Newsham
- School of Pure and Applied Biology, University of Wales, College of Cardiff, Cardiff CF1 3TL, UK
| | - Lynne Boddy
- School of Pure and Applied Biology, University of Wales, College of Cardiff, Cardiff CF1 3TL, UK
| | - Juliet C Frankland
- Institute of Terrestrial Ecology, Merlewood Research Station, Grange-over-Sands, Cumbria, LA11 6JU, UK
| | - P Ineson
- Institute of Terrestrial Ecology, Merlewood Research Station, Grange-over-Sands, Cumbria, LA11 6JU, UK
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Newsham KK, Ineson P, Boddy L, Frankland JC. Effects of dry-deposited sulphur dioxide on fungal decomposition of angiosperm tree leaf litter II. Chemical content of leaf litters. THE NEW PHYTOLOGIST 1992; 122:111-125. [PMID: 33874039 DOI: 10.1111/j.1469-8137.1992.tb00058.x] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
Ash (Fraxinus excelsior L.), birch (Betula spp.), hazel (Corylus avellana L.), sessile oak [Quercus petraea (Mattuschka) Liebl.] and sycamore (Acer pseudoplatanus L.) leaf litters from a non-polluted and a heavily sulphur dioxide (SO2 )-polluted woodland were fumigated with environmentally-realistic concentrations (0.010-0.030 μl l-1 ) of SO2 for 16-68 wk in an open-air field-fumigation experiment. Fumigation markedly increased sulphate and protons in leachates from the litters and decreased calcium and magnesium contents of the leaves. However, there were few differences in the responses between leaf litters from the two woodlands. This was attributed to rapid sulphate wash-out from the litters from the heavily polluted woodland, so that the litters from the two sites quickly reached the same sulphate status.
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Affiliation(s)
- K K Newsham
- School of Pure and Applied Biology, University of Wales, College of Cardiff, Cardiff CF1 3TL, UK
| | - P Ineson
- Institute of Terrestrial Ecology, Merlewood Research Station, Grange-over-Sands, Cumbria, LA11 6JU, UK
| | - Lynne Boddy
- School of Pure and Applied Biology, University of Wales, College of Cardiff, Cardiff CF1 3TL, UK
| | - Juliet C Frankland
- Institute of Terrestrial Ecology, Merlewood Research Station, Grange-over-Sands, Cumbria, LA11 6JU, UK
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