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Plant root carbon inputs drive methane production in tropical peatlands

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Plant root carbon inputs drive methane production in tropical peatlands. / Girkin, N. T.; Siegenthaler, A.; Lopez, O. et al.
In: Scientific Reports, Vol. 15, No. 1, 3244, 25.01.2025.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Girkin, NT, Siegenthaler, A, Lopez, O, Stott, A, Ostle, N, Gauci, V & Sjögersten, S 2025, 'Plant root carbon inputs drive methane production in tropical peatlands', Scientific Reports, vol. 15, no. 1, 3244. https://doi.org/10.1038/s41598-025-87467-w

APA

Girkin, N. T., Siegenthaler, A., Lopez, O., Stott, A., Ostle, N., Gauci, V., & Sjögersten, S. (2025). Plant root carbon inputs drive methane production in tropical peatlands. Scientific Reports, 15(1), Article 3244. https://doi.org/10.1038/s41598-025-87467-w

Vancouver

Girkin NT, Siegenthaler A, Lopez O, Stott A, Ostle N, Gauci V et al. Plant root carbon inputs drive methane production in tropical peatlands. Scientific Reports. 2025 Jan 25;15(1):3244. doi: 10.1038/s41598-025-87467-w

Author

Girkin, N. T. ; Siegenthaler, A. ; Lopez, O. et al. / Plant root carbon inputs drive methane production in tropical peatlands. In: Scientific Reports. 2025 ; Vol. 15, No. 1.

Bibtex

@article{b35fe5550d4144b9ac0ffb0b66f1f0ec,
title = "Plant root carbon inputs drive methane production in tropical peatlands",
abstract = "Tropical peatlands are carbon-dense ecosystems that are significant sources of atmospheric methane (CH4). Recent work has demonstrated the importance of trees as an emission pathway for CH4 from the peat to the atmosphere. However, there remain questions over the processes of CH4 production in these systems and how they relate to substrate supply. Principally, these questions relate to the relative contribution of recent photosynthetically fixed carbon, released as root exudates, versus carbon substrate supply from the slowly decomposing peat matrix to CH4 emissions within these ecosystems. Here, we examined the role of root inputs in regulating CH4 production inferred from soil emissions using a combination of in situ tree girdling, in situ13C natural abundance labelling via stem injections, and a 13CO2 labelling of transplanted plants of two contrasting plant functional types, a broadleaved evergreen tree, and a canopy palm. Girdling of broadleaved evergreen trees reduced CH4 fluxes by up to 67%. Stem injections of trees and palms with a natural abundance label resulted in significant isotopic enrichment of CH4 fluxes, reinforcing the link between root carbon inputs and peat CH4 fluxes. Ex situ13CO2 labelling of plants resulted in significant 13C enrichment of peat CH4 fluxes. Taken together, our results demonstrate for the first time that plant root exudates make a substantial contribution to CH4 production in tropical peatlands.",
keywords = "Methane, Stable isotope labelling, Girdling, PLFA, Tropical peat",
author = "Girkin, {N. T.} and A. Siegenthaler and O. Lopez and A. Stott and N. Ostle and V. Gauci and S. Sj{\"o}gersten",
year = "2025",
month = jan,
day = "25",
doi = "10.1038/s41598-025-87467-w",
language = "English",
volume = "15",
journal = "Scientific Reports",
issn = "2045-2322",
publisher = "Nature Publishing Group",
number = "1",

}

RIS

TY - JOUR

T1 - Plant root carbon inputs drive methane production in tropical peatlands

AU - Girkin, N. T.

AU - Siegenthaler, A.

AU - Lopez, O.

AU - Stott, A.

AU - Ostle, N.

AU - Gauci, V.

AU - Sjögersten, S.

PY - 2025/1/25

Y1 - 2025/1/25

N2 - Tropical peatlands are carbon-dense ecosystems that are significant sources of atmospheric methane (CH4). Recent work has demonstrated the importance of trees as an emission pathway for CH4 from the peat to the atmosphere. However, there remain questions over the processes of CH4 production in these systems and how they relate to substrate supply. Principally, these questions relate to the relative contribution of recent photosynthetically fixed carbon, released as root exudates, versus carbon substrate supply from the slowly decomposing peat matrix to CH4 emissions within these ecosystems. Here, we examined the role of root inputs in regulating CH4 production inferred from soil emissions using a combination of in situ tree girdling, in situ13C natural abundance labelling via stem injections, and a 13CO2 labelling of transplanted plants of two contrasting plant functional types, a broadleaved evergreen tree, and a canopy palm. Girdling of broadleaved evergreen trees reduced CH4 fluxes by up to 67%. Stem injections of trees and palms with a natural abundance label resulted in significant isotopic enrichment of CH4 fluxes, reinforcing the link between root carbon inputs and peat CH4 fluxes. Ex situ13CO2 labelling of plants resulted in significant 13C enrichment of peat CH4 fluxes. Taken together, our results demonstrate for the first time that plant root exudates make a substantial contribution to CH4 production in tropical peatlands.

AB - Tropical peatlands are carbon-dense ecosystems that are significant sources of atmospheric methane (CH4). Recent work has demonstrated the importance of trees as an emission pathway for CH4 from the peat to the atmosphere. However, there remain questions over the processes of CH4 production in these systems and how they relate to substrate supply. Principally, these questions relate to the relative contribution of recent photosynthetically fixed carbon, released as root exudates, versus carbon substrate supply from the slowly decomposing peat matrix to CH4 emissions within these ecosystems. Here, we examined the role of root inputs in regulating CH4 production inferred from soil emissions using a combination of in situ tree girdling, in situ13C natural abundance labelling via stem injections, and a 13CO2 labelling of transplanted plants of two contrasting plant functional types, a broadleaved evergreen tree, and a canopy palm. Girdling of broadleaved evergreen trees reduced CH4 fluxes by up to 67%. Stem injections of trees and palms with a natural abundance label resulted in significant isotopic enrichment of CH4 fluxes, reinforcing the link between root carbon inputs and peat CH4 fluxes. Ex situ13CO2 labelling of plants resulted in significant 13C enrichment of peat CH4 fluxes. Taken together, our results demonstrate for the first time that plant root exudates make a substantial contribution to CH4 production in tropical peatlands.

KW - Methane

KW - Stable isotope labelling

KW - Girdling

KW - PLFA

KW - Tropical peat

U2 - 10.1038/s41598-025-87467-w

DO - 10.1038/s41598-025-87467-w

M3 - Journal article

VL - 15

JO - Scientific Reports

JF - Scientific Reports

SN - 2045-2322

IS - 1

M1 - 3244

ER -