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

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 TgCH₄ yr^-1 to the atmosphere in addition to inundated tree emissions of approximately 12.7-21.1 TgCH₄ yr^-1. Applying our approach to all tropical wetland broad-leaf trees yields an estimated nonflooded floodplain tree flux of 6.4 TgCH₄ yr^-1 which, at 17% of the flooded tropical tree flux of approximately 37.1 TgCH₄ yr^-1, demonstrates the importance of these ecosystems in extending the effective CH₄ emitting area beyond flooded lands. [ABSTRACT FROM AUTHOR]