4.5 Article

Non-flooded riparian Amazon trees are a regionally significant methane source

出版社

ROYAL SOC
DOI: 10.1098/rsta.2020.0446

关键词

methane; Amazon; floodplain; riparian; trees; soils

资金

  1. UK NERC [NE/N015606/1, NEC05779]
  2. Global Methane Budget MOYA consortium
  3. Newton Fund through the Met Office Climate Science for Service Partnership Brazil (CSSP Brazil)
  4. Royal Society Dorothy Hodgkin Research fellowship [DH160111]
  5. CNPq
  6. CAPES
  7. FAPERJ

向作者/读者索取更多资源

In forested wetlands, inundation-adapted trees have been found to be the primary pathway for soil-produced methane emissions. This challenges existing modeling efforts as it suggests that methane produced deep in the soil can vent to the atmosphere through tree roots even when the water table is below the surface. A study in the Amazon basin revealed that tree stem emissions were significantly higher than emissions from soil or aquatic surfaces, and were closely related to the depth of the water table. Additionally, nonflooded floodplain trees contribute a significant amount to methane emissions, highlighting the importance of these ecosystems in extending the area of methane emission beyond flooded lands.
Inundation-adapted trees were recently established as the dominant egress pathway for soil-produced methane (CH4) in forested wetlands. This raises the possibility that CH4 produced deep within the soil column can vent to the atmosphere via tree roots even when the water table (WT) is below the surface. If correct, this would challenge modelling efforts where inundation often defines the spatial extent of ecosystem CH4 production and emission. Here, we examine CH4 exchange on tree, soil and aquatic surfaces in forest experiencing a dynamic WT at three floodplain locations spanning the Amazon basin at four hydrologically distinct times from April 2017 to January 2018. Tree stem emissions were orders of magnitude larger than from soil or aquatic surface emissions and exhibited a strong relationship to WT depth below the surface (less than 0). We estimate that Amazon riparian floodplain margins with a WT< 0 contribute 2.2-3.6 TgCH(4) yr(-1) to the atmosphere in addition to inundated tree emissions of approximately 12.7-21.1 TgCH(4) yr(-1). Applying our approach to all tropical wetland broad-leaf trees yields an estimated nonflooded floodplain tree flux of 6.4 TgCH(4) yr(-1) which, at 17% of the flooded tropical tree flux of approximately 37.1 TgCH(4) yr(-1), demonstrates the importance of these ecosystems in extending the effective CH4 emitting area beyond flooded lands.

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