Foliar methane and nitrous oxide fluxes in tropical tree species

Methane (CH₄) and nitrous oxide (N₂O) are critical biogenic greenhouse gases (GHGs) with global warming potentials substantially greater than that of carbon dioxide (CO₂). The exchange of these gases in tropical forests, particularly via foliar processes, remains poorly understood. We quantified foliar CH₄ and N₂O fluxes among tropical tree species and examined their potential association with the leaf economics spectrum (LES) traits. Sampling within Lawachara National Park, Bangladesh, we used in-situ measurements of foliar CH₄ and N₂O fluxes employing off-axis integrated cavity output spectroscopy (CH₄, CO₂ and H₂O) and optical feedback-cavity enhanced absorption spectroscopy (N₂O) analyzers. Leaves were measured under dark, low, and high (0, 100, and 1000 μmol·m<sup>-2</sup>·s<sup>-1</sup>) light conditions. Surveyed tree species exhibited both net foliar uptake and efflux of CH₄, with a mean flux not different from zero, suggesting negligible net foliar emissions at the stand level. Plant families showed differences in CH₄, but not N₂O fluxes. Consistent efflux was observed for N₂O, with a mean of 0.562 ± 0.060 pmol·m<sup>-2</sup>·s<sup>-1</sup>. Pioneer species exhibited a higher mean N₂O flux (0.81 ± 0.17 pmol·m<sup>-2</sup>·s<sup>-1</sup>) compared to late-successional species (0.37 ± 0.05 pmol·m<sup>-2</sup>·s<sup>-1</sup>). Pioneer species also showed a trend toward a higher mean CH₄ flux (0.24 ± 0.21 nmol·m<sup>-2</sup>·s<sup>-1</sup>) compared to mid-successional (-0.01 ± 0.26 nmol·m<sup>-2</sup>·s<sup>-1</sup>) and late-successional species (-0.05 ± 0.28 nmol·m<sup>-2</sup>·s<sup>-1</sup>). Moreover, among all leaf traits within the leaf economic spectrum, a significant positive relationship was observed between leaf N₂O flux and total leaf nitrogen. Our results suggest that pioneer tree species significantly contribute to net CH₄ and N₂O emissions, potentially counteracting the carbon sequestration benefits in regenerating tropical forests. These findings indicate that accurate GHG budgeting should include direct measurements of foliar CH₄ and N₂O fluxes. Moreover, the results suggest that forest conservation and management strategies that prioritize late successional species will better mitigate GHG emissions.

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Publication Details

Journal
The Science of The Total Environment
Published
2024-09-27
DOI
https://doi.org/10.1016/j.scitotenv.2024.176503
Citations
5
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
Field-Weighted Citation Impact
1.41

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article

Foliar methane and nitrous oxide fluxes in tropical tree species

Sean C. Thomas, Md Abdul Halim, Md. Rezaul Karim
5 citations
The Science of The Total Environment
Plant Water Relations and Carbon Dynamics
1.41
article

Foliar methane and nitrous oxide fluxes in tropical tree species

Sean C. Thomas, Md Abdul Halim, Md. Rezaul Karim
article en
5 citations

Abstract

Methane (CH₄) and nitrous oxide (N₂O) are critical biogenic greenhouse gases (GHGs) with global warming potentials substantially greater than that of carbon dioxide (CO₂). The exchange of these gases in tropical forests, particularly via foliar processes, remains poorly understood. We quantified foliar CH₄ and N₂O fluxes among tropical tree species and examined their potential association with the leaf economics spectrum (LES) traits. Sampling within Lawachara National Park, Bangladesh, we used in-situ measurements of foliar CH₄ and N₂O fluxes employing off-axis integrated cavity output spectroscopy (CH₄, CO₂ and H₂O) and optical feedback-cavity enhanced absorption spectroscopy (N₂O) analyzers. Leaves were measured under dark, low, and high (0, 100, and 1000 μmol·m<sup>-2</sup>·s<sup>-1</sup>) light conditions. Surveyed tree species exhibited both net foliar uptake and efflux of CH₄, with a mean flux not different from zero, suggesting negligible net foliar emissions at the stand level. Plant families showed differences in CH₄, but not N₂O fluxes. Consistent efflux was observed for N₂O, with a mean of 0.562 ± 0.060 pmol·m<sup>-2</sup>·s<sup>-1</sup>. Pioneer species exhibited a higher mean N₂O flux (0.81 ± 0.17 pmol·m<sup>-2</sup>·s<sup>-1</sup>) compared to late-successional species (0.37 ± 0.05 pmol·m<sup>-2</sup>·s<sup>-1</sup>). Pioneer species also showed a trend toward a higher mean CH₄ flux (0.24 ± 0.21 nmol·m<sup>-2</sup>·s<sup>-1</sup>) compared to mid-successional (-0.01 ± 0.26 nmol·m<sup>-2</sup>·s<sup>-1</sup>) and late-successional species (-0.05 ± 0.28 nmol·m<sup>-2</sup>·s<sup>-1</sup>). Moreover, among all leaf traits within the leaf economic spectrum, a significant positive relationship was observed between leaf N₂O flux and total leaf nitrogen. Our results suggest that pioneer tree species significantly contribute to net CH₄ and N₂O emissions, potentially counteracting the carbon sequestration benefits in regenerating tropical forests. These findings indicate that accurate GHG budgeting should include direct measurements of foliar CH₄ and N₂O fluxes. Moreover, the results suggest that forest conservation and management strategies that prioritize late successional species will better mitigate GHG emissions.

The Science of The Total EnvironmentVol. 954
Landscape Institute (GB)
Natural Sciences and Engineering Research Council of Canada
Life in Land
Openalex Percentile: Top 19%
Plant Water Relations and Carbon Dynamics
1.41
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