The role of Eriophorum vaginatum in CH₄ flux from an ombrotrophic peatland
Vegetation composition was found to be an important factor controlling CH₄ emission from an ombrotrophic peatland in the UK, with significantly greater (P < 0.01) CH₄ released from areas containing both Eriophorum vaginatum L. and Sphagnum, than from similar areas without E. vaginatum. Positive c...
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Published in | Plant and soil Vol. 227; no. 1/2; pp. 265 - 272 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Dordrecht
Kluwer Academic Publishers
01.01.2000
Springer Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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Summary: | Vegetation composition was found to be an important factor controlling CH₄ emission from an ombrotrophic peatland in the UK, with significantly greater (P < 0.01) CH₄ released from areas containing both Eriophorum vaginatum L. and Sphagnum, than from similar areas without E. vaginatum. Positive correlations were observed between the amount of E. vaginatum and CH₄ emission, with the best predictor of flux being the amount of below-ground biomass of this species (r² = 0.93). A cutting experiment revealed that there was no significant difference (P > 0.05) in CH₄ flux between plots with E. vaginatum stems cut above the water table and plots with intact vegetation, yet there was a 56% mean reduction in CH₄ efflux where stems were cut below the water table (P < 0.05). The effect of E. vaginatum on CH₄ release was mimicked by the presence of inert glass tubes. These findings suggest that the main short-term role of E. vaginatum in the ecosystem is simply as a conduit for CH₄ release. The longer-term importance of E. vaginatum in controlling CH₄ fluxes through C substrate input was suggested by the positive correlation between the night-time CO₂ and CH₄ fluxes (r² = 0.70), which only occurred when the vegetation was not senescent. |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 |
ISSN: | 0032-079X 1573-5036 |
DOI: | 10.1023/A:1026573727311 |