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Journal Article

Dimethyl sulfide emissions from a peatland result more from organic matter degradation than sulfate reduction

MPS-Authors
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Lehnert,  Ann-Sophie
IMPRS International Max Planck Research School for Global Biogeochemical Cycles, Max Planck Institute for Biogeochemistry, Max Planck Society;
Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Ruecker,  Alexander
Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Gomes-Alves,  Eliane
Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Trumbore,  Susan E.       
Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;

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BGC4463.pdf
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BGC4463s1.docx
(Supplementary material), 4MB

Citation

Lehnert, A.-S., Cooper, R. E., Ignatz, R., Ruecker, A., Gomes-Alves, E., Küsel, K., et al. (2024). Dimethyl sulfide emissions from a peatland result more from organic matter degradation than sulfate reduction. Journal of Geophysical Research: Biogeosciences, 129(1): e2023JG007449. doi:10.1029/2023JG007449.


Cite as: https://hdl.handle.net/21.11116/0000-000E-2659-4
Abstract
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