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Oxidative mitigation of aquatic methane emissions in large Amazonian rivers
Author(s) -
Sawakuchi Henrique O.,
Bastviken David,
Sawakuchi André O.,
Ward Nicholas D.,
Borges Clovis D.,
Tsai Siu M.,
Richey Jeffrey E.,
Ballester Maria Victoria R.,
Krusche Alex V.
Publication year - 2016
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/gcb.13169
Subject(s) - environmental science , amazonian , sink (geography) , tributary , methane , flux (metallurgy) , hydrology (agriculture) , water column , ecosystem , greenhouse gas , environmental chemistry , aquatic ecosystem , atmospheric sciences , ecology , chemistry , amazon rainforest , geology , biology , cartography , geotechnical engineering , geography , organic chemistry
The flux of methane ( CH 4 ) from inland waters to the atmosphere has a profound impact on global atmospheric greenhouse gas ( GHG ) levels, and yet, strikingly little is known about the dynamics controlling sources and sinks of CH 4 in the aquatic setting. Here, we examine the cycling and flux of CH 4 in six large rivers in the A mazon basin, including the A mazon R iver. Based on stable isotopic mass balances of CH 4 , inputs and outputs to the water column were estimated. We determined that ecosystem methane oxidation ( MOX ) reduced the diffusive flux of CH 4 by approximately 28–96% and varied depending on hydrologic regime and general geochemical characteristics of tributaries of the Amazon River. For example, the relative amount of MOX was maximal during high water in black and white water rivers and minimal in clear water rivers during low water. The abundance of genetic markers for methane‐oxidizing bacteria ( pmoA ) was positively correlated with enhanced signals of oxidation, providing independent support for the detected MOX patterns. The results indicate that MOX in large Amazonian rivers can consume from 0.45 to 2.07 Tg CH 4 yr −1 , representing up to 7% of the estimated global soil sink. Nevertheless, climate change and changes in hydrology, for example, due to construction of dams, can alter this balance, influencing CH 4 emissions to atmosphere.