Main conclusion <p>Methane was rarely produced in the stems of living trees in the upland forests. However, it was largely produced in the swollen lower stems in the wetland forests.</p> Abstract <p>The methane (CH<sub>4</sub>) fluxes on aboveground living trees have been widely observed over the last decades. However, aboveground living tree-based CH<sub>4</sub> production has been rarely studied in terrestrial ecosystems. Thus, it is essential to study aboveground CH<sub>4</sub> production in multiple tree species. In this study, we aimed to understand the CH<sub>4</sub> production in the stems of living trees in the subtropical forests from 445 individual living tree stems (1335 upper, middle, and lower tree stem segments). We found that substantial CH<sub>4</sub> concentrations of ≥ 1000 μL L<sup>−1</sup> and detectable CH<sub>4</sub> production of ≥ 0.2&#xa0;ng&#xa0;g<sup>−1</sup> dry weight (DW) h<sup>−1</sup> occurred only in ~ 5% of all sampled living tree stems in the upland forests. Substantial CH<sub>4</sub> concentrations and detectable CH<sub>4</sub> production occurred frequently in the swollen lower stems (a kind of eco-physiologic adaptation) but rarely in the straight stems of living trees in the wetland forests. Particularly, CH<sub>4</sub> production was significantly higher in the swollen lower stems compared to in the straight stems, with a mean rate of 22.2&#xa0;ng&#xa0;g<sup>−1</sup> DW h<sup>−1</sup>, and the produced CH<sub>4</sub> was demonstrated to be microbial according to its highly depleted <sup>13</sup>C abundance and its exponential kinetics in response to time. In global wetland forests, the existing eco-physiologic adaptations of living trees are potentially a distinctive CH<sub>4</sub> source, and thereby more research is required for understanding their CH<sub>4</sub> processes and fluxes.</p>

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Methane production in the stems of living trees in subtropical forests

  • Zhi-Ping Wang,
  • Josep Barba,
  • Jian-Guo Xue,
  • Xiang-Cheng Mi,
  • Ang Li,
  • Zhen-Ying Huang,
  • Shi-Jie Han

摘要

Main conclusion

Methane was rarely produced in the stems of living trees in the upland forests. However, it was largely produced in the swollen lower stems in the wetland forests.

Abstract

The methane (CH4) fluxes on aboveground living trees have been widely observed over the last decades. However, aboveground living tree-based CH4 production has been rarely studied in terrestrial ecosystems. Thus, it is essential to study aboveground CH4 production in multiple tree species. In this study, we aimed to understand the CH4 production in the stems of living trees in the subtropical forests from 445 individual living tree stems (1335 upper, middle, and lower tree stem segments). We found that substantial CH4 concentrations of ≥ 1000 μL L−1 and detectable CH4 production of ≥ 0.2 ng g−1 dry weight (DW) h−1 occurred only in ~ 5% of all sampled living tree stems in the upland forests. Substantial CH4 concentrations and detectable CH4 production occurred frequently in the swollen lower stems (a kind of eco-physiologic adaptation) but rarely in the straight stems of living trees in the wetland forests. Particularly, CH4 production was significantly higher in the swollen lower stems compared to in the straight stems, with a mean rate of 22.2 ng g−1 DW h−1, and the produced CH4 was demonstrated to be microbial according to its highly depleted 13C abundance and its exponential kinetics in response to time. In global wetland forests, the existing eco-physiologic adaptations of living trees are potentially a distinctive CH4 source, and thereby more research is required for understanding their CH4 processes and fluxes.