Isotopic evidence for axial tree stem methane oxidation within subtropical lowland forests

© 2021 The Authors New Phytologist © 2021 New Phytologist Foundation.

Bibliographische Detailangaben
Veröffentlicht in:The New phytologist. - 1979. - 230(2021), 6 vom: 01. Juni, Seite 2200-2212
1. Verfasser: Jeffrey, Luke C (VerfasserIn)
Weitere Verfasser: Maher, Damien T, Tait, Douglas R, Reading, Michael J, Chiri, Eleonora, Greening, Chris, Johnston, Scott G
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2021
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article Research Support, Non-U.S. Gov't carbon cycle climate change greenhouse gases methane (CH4) methanogens methanotrophy wetland forest Soil mehr... Methane OP0UW79H66
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245 1 0 |a Isotopic evidence for axial tree stem methane oxidation within subtropical lowland forests 
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500 |a Date Completed 04.06.2021 
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500 |a Citation Status MEDLINE 
520 |a © 2021 The Authors New Phytologist © 2021 New Phytologist Foundation. 
520 |a Knowledge regarding mechanisms moderating methane (CH4 ) sink/source behaviour along the soil-tree stem-atmosphere continuum remains incomplete. Here, we applied stable isotope analysis (δ13 C-CH4 ) to gain insights into axial CH4 transport and oxidation in two globally distributed subtropical lowland species (Melaleuca quinquenervia and Casuarina glauca). We found consistent trends in CH4 flux (decreasing with height) and δ13 C-CH4 enrichment (increasing with height) in relation to stem height from ground. The average lower tree stem δ13 C-CH4 (0-40 cm) of Melaleuca and Casuarina (-53.96‰ and -65.89‰) were similar to adjacent flooded soil CH4 ebullition (-52.87‰ and -62.98‰), suggesting that stem CH4 is derived mainly by soil sources. Upper stems (81-200 cm) displayed distinct δ13 C-CH4 enrichment (Melaleuca -44.6‰ and Casuarina -46.5‰, respectively). Coupled 3D-photogrammetry with novel 3D-stem measurements revealed distinct hotspots of CH4 flux and isotopic fractionation on Melaleuca, which were likely due to bark anomalies in which preferential pathways of gas efflux were enhanced. Diel experiments revealed greater δ13 C-CH4 enrichment and higher oxidation rates in the afternoon, compared with the morning. Overall, we estimated that c. 33% of the methane was oxidised between lower and upper stems during axial transport, therefore potentially representing a globally significant, yet previously unaccounted for, methane sink 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a carbon cycle 
650 4 |a climate change 
650 4 |a greenhouse gases 
650 4 |a methane (CH4) 
650 4 |a methanogens 
650 4 |a methanotrophy 
650 4 |a wetland forest 
650 7 |a Soil  |2 NLM 
650 7 |a Methane  |2 NLM 
650 7 |a OP0UW79H66  |2 NLM 
700 1 |a Maher, Damien T  |e verfasserin  |4 aut 
700 1 |a Tait, Douglas R  |e verfasserin  |4 aut 
700 1 |a Reading, Michael J  |e verfasserin  |4 aut 
700 1 |a Chiri, Eleonora  |e verfasserin  |4 aut 
700 1 |a Greening, Chris  |e verfasserin  |4 aut 
700 1 |a Johnston, Scott G  |e verfasserin  |4 aut 
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773 1 8 |g volume:230  |g year:2021  |g number:6  |g day:01  |g month:06  |g pages:2200-2212 
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