<p>Wetlands are the largest natural source of methane (CH<sub>4</sub>), and trees as well as soils can be CH<sub>4</sub> sources. CH<sub>4</sub> emissions from dead trees are poorly understood. We examined stem CH<sub>4</sub> emissions targeting trees in different stages, namely, three living, four recently deceased and three old dead Japanese cypresses (<i>Chamaecyparis obtusa</i>) by the dynamic closed chamber method. We aimed to identify the differences in stem CH<sub>4</sub> emissions among trees in three categories and their impacts on the CH<sub>4</sub> budget of wetlands and to examine the factors controlling stem CH<sub>4</sub> fluxes. Stem CH<sub>4</sub> fluxes showed seasonal variation in all categories, and CH<sub>4</sub> emissions from recently deceased trees dropped rapidly since the measurement started. Recently deceased trees displaying the highest CH<sub>4</sub> emissions followed by old dead trees, while the lowest emissions were observed for living trees. In an incubation experiment, CH<sub>4</sub> production was confirmed from all dead trees but not significant production from living trees. Stem CH<sub>4</sub> emissions from old dead trees were greater at lower positions, and seasonal variations were significantly correlated with soil CH<sub>4</sub> emissions, which supported the degassing of belowground CH<sub>4</sub> through trees. On the other hand, stem CH<sub>4</sub> emissions from recently deceased trees did not show a consistent height dependency, suggesting the presence of additional sources. When compared per soil surface area, CH<sub>4</sub> emissions from dead cypress were smaller than those from wetland soils. However, CH<sub>4</sub> emissions from Japanese cypress can change when they die due to inundation and increased dead trees could be an additional CH<sub>4</sub> source.</p>

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Methane Emissions from the Stems of Living and Dead Chamaecyparis obtusa Sieb. Et Zucc

  • Ayaka Sakabe,
  • Zhining Liu,
  • Yoshiko Kosugi

摘要

Wetlands are the largest natural source of methane (CH4), and trees as well as soils can be CH4 sources. CH4 emissions from dead trees are poorly understood. We examined stem CH4 emissions targeting trees in different stages, namely, three living, four recently deceased and three old dead Japanese cypresses (Chamaecyparis obtusa) by the dynamic closed chamber method. We aimed to identify the differences in stem CH4 emissions among trees in three categories and their impacts on the CH4 budget of wetlands and to examine the factors controlling stem CH4 fluxes. Stem CH4 fluxes showed seasonal variation in all categories, and CH4 emissions from recently deceased trees dropped rapidly since the measurement started. Recently deceased trees displaying the highest CH4 emissions followed by old dead trees, while the lowest emissions were observed for living trees. In an incubation experiment, CH4 production was confirmed from all dead trees but not significant production from living trees. Stem CH4 emissions from old dead trees were greater at lower positions, and seasonal variations were significantly correlated with soil CH4 emissions, which supported the degassing of belowground CH4 through trees. On the other hand, stem CH4 emissions from recently deceased trees did not show a consistent height dependency, suggesting the presence of additional sources. When compared per soil surface area, CH4 emissions from dead cypress were smaller than those from wetland soils. However, CH4 emissions from Japanese cypress can change when they die due to inundation and increased dead trees could be an additional CH4 source.