Open AccessNon-flooded riparian Amazon trees are a regionally significant methane source
Author(s) -
Vincent Gauci,
Valeska Carvalho Figueiredo,
Nicola Gedney,
Sunitha Rao Pangala,
Tainá Stauffer,
Graham P. Weedon,
Alex EnrichPrast
Publication year - 2021
Publication title -
philosophical transactions - royal society. mathematical, physical and engineering sciences/philosophical transactions - royal society. mathematical, physical and engineering sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.074
H-Index - 169
eISSN - 1471-2962
pISSN - 1364-503X
DOI - 10.1098/rsta.2020.0446
Subject(s) - environmental science , wetland , floodplain , riparian zone , hydrology (agriculture) , ecosystem , amazon rainforest , methane , riparian forest , flux (metallurgy) , water table , global warming , atmosphere (unit) , swamp , aquatic ecosystem , climate change , atmospheric sciences , ecology , geology , groundwater , geography , oceanography , habitat , geotechnical engineering , meteorology , biology , materials science , metallurgy
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 Tg CH4 yr−1 to the atmosphere in addition to inundated tree emissions of approximately 12.7–21.1 Tg CH4 yr−1 . Applying our approach to all tropical wetland broad-leaf trees yields an estimated non-flooded floodplain tree flux of 6.4 Tg CH4 yr−1 which, at 17% of the flooded tropical tree flux of approximately 37.1 Tg CH4 yr−1 , demonstrates the importance of these ecosystems in extending the effective CH4 emitting area beyond flooded lands.This article is part of a discussion meeting issue 'Rising methane: is warming feeding warming? (part 2)'.