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Spatial variability of organic matter properties determines methane fluxes in a tropical forested peatland

Girkin, N. T.; Vane, C. H.; Cooper, H. V.; Moss-Hayes, V.; Craigon, J.; Turner, B. L.; Ostle, N.; Sjögersten, S.

Spatial variability of organic matter properties determines methane fluxes in a tropical forested peatland Thumbnail


Authors

NICHOLAS GIRKIN Nicholas.Girkin3@nottingham.ac.uk
Assistant Professor in Environmental Sci

C. H. Vane

H. V. Cooper

V. Moss-Hayes

J. Craigon

B. L. Turner

N. Ostle

SOFIE SJOGERSTEN Sofie.Sjogersten@nottingham.ac.uk
Professor of Environmental Science



Abstract

Tropical peatland ecosystems are a significant component of the global carbon cycle and feature a range of distinct vegetation types, but the extent of links between contrasting plant species, peat biogeochemistry and greenhouse gas fluxes remains unclear. Here we assessed how vegetation affects small scale variation of tropical peatland carbon dynamics by quantifying in situ greenhouse gas emissions over 1 month using the closed chamber technique, and peat organic matter properties using Rock-Eval 6 pyrolysis within the rooting zones of canopy palms and broadleaved evergreen trees. Mean methane fluxes ranged from 0.56 to 1.2 mg m−2 h−1 and were significantly greater closer to plant stems. In addition, pH, ranging from 3.95 to 4.16, was significantly greater closer to stems. A three pool model of organic matter thermal stability (labile, intermediate and passive pools) indicated a large labile pool in surface peat (35–42%), with equivalent carbon stocks of 2236–3065 g m−2. Methane fluxes were driven by overall substrate availability rather than any specific carbon pool. No peat properties correlated with carbon dioxide fluxes, suggesting a significant role for root respiration, aerobic decomposition and/or methane oxidation. These results demonstrate how vegetation type and inputs, and peat organic matter properties are important determinants of small scale spatial variation of methane fluxes in tropical peatlands that are affected by climate and land use change.

Citation

Girkin, N. T., Vane, C. H., Cooper, H. V., Moss-Hayes, V., Craigon, J., Turner, B. L., …Sjögersten, S. (2019). Spatial variability of organic matter properties determines methane fluxes in a tropical forested peatland. Biogeochemistry, 142(2), 231-245. https://doi.org/10.1007/s10533-018-0531-1

Journal Article Type Article
Acceptance Date Nov 21, 2018
Online Publication Date Nov 26, 2018
Publication Date Jan 31, 2019
Deposit Date Feb 15, 2019
Publicly Available Date Feb 15, 2019
Journal Biogeochemistry
Print ISSN 0168-2563
Electronic ISSN 1573-515X
Publisher Springer Verlag
Peer Reviewed Peer Reviewed
Volume 142
Issue 2
Pages 231-245
DOI https://doi.org/10.1007/s10533-018-0531-1
Keywords Tropical peat; Carbon dioxide; Methane; Organic matter; Rock-Eval pyrolysis; Geochemistry
Public URL https://nottingham-repository.worktribe.com/output/1552458
Publisher URL https://link.springer.com/article/10.1007%2Fs10533-018-0531-1
Contract Date Feb 15, 2019

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