Abstract
Large uncertainties in estimates of methane (CH4) emissions from tropical inland waters reflect the paucity of information at appropriate temporal and spatial scales. CH4 concentrations, diffusive and ebullitive fluxes, and environmental parameters in contrasting aquatic habitats of Lake Janauacá, an Amazon floodplain lake, measured for two years revealed patterns in temporal and spatial variability related to different aquatic habitats and environmental conditions. CH4 concentrations ranged from below detection to 96 µM, CH4 diffusive fluxes from below detection to 2342 µmol m−2 h−1, and CH4 ebullitive fluxes from 0 to 190 mmol m−2 d−1. Vegetated aquatic habitats had higher surface CH4 concentrations than open water habitats, and no significant differences in diffusive CH4 fluxes, likely due to higher k values measured in open water habitats. CH4 emissions were enhanced after a prolonged low water period, when the exposed sediments were colonized by herbaceous plants that decomposed after water levels rose, possibly fueling CH4 production. Statistical models indicated the importance of variables related to CH4 production (temperature, dissolved organic carbon) and consumption (dissolved nitrogen, oxygenated water column), as well as maximum depth, in controlling surface water CH4 concentrations.
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Acknowledgements
This work was supported by the Conselho Nacional de Pesquisa e Desenvolvimento—Ministério da Ciência Tecnologia (CNPq/MCTI); CNPq/LBA-Edital.68/2013, processo 458036/2013-7, CNPq-Universal processo.482004/2012-6. Post-graduate scholarships were provided to PMB and JHFA by Coordenação de Aperfeiçomento de Pessoal de Nível Superior (CAPES) and CNPq. PMB and JHFA are thankful to CAPES for the grant ‘‘Programa de Doutorado Sanduíche no Exterior − 88881.134945/2016-0100 and ‘‘88881.135203/2016-0100 respectively. During manuscript preparation support was provided to PMB and JHFA by NASA Grant NNX17AK49G. JMM received support from National Aeronautics and Space Administration (NASA), the US Department of Energy (Contract No. DE-0010620), the US National Science Foundation (NSF DEB grant 1753856) and a Fulbright fellowship. VFF is partially supported by a CNPq productivity grant. The authors thank for the logistical support of INPA, João B. Rocha for the field support, and Lúcia Silva for offering a floating house as a research base. We thank Michaela Melo and Jonismar S. da Silva for help in field campaigns, and Nicholas Marino for assistance with statistical analyses.
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Barbosa, P.M., Melack, J.M., Amaral, J.H.F. et al. Dissolved methane concentrations and fluxes to the atmosphere from a tropical floodplain lake. Biogeochemistry 148, 129–151 (2020). https://doi.org/10.1007/s10533-020-00650-1
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DOI: https://doi.org/10.1007/s10533-020-00650-1