39The Amazonian floodplain forests are dynamic ecosystems of great importance for the regional 40 hydrological and biogeochemical cycles and provide a significant contribution to the global 41 carbon balance. Unique geochemical factors may drive the microbial community composition 42 and, consequently, affect CH4 emissions across floodplain areas. Here we provide the first 43 report of the in situ seasonal dynamics of CH4 cycling microbial communities in Amazonian 44 floodplains. We asked how abiotic factors may affect both overall and CH4 cycling microbial 45 communities and further investigated their responses to seasonal changes. We collected 46 sediment samples during wet and dry seasons from three different types of floodplain forests, 47 along with upland forest soil samples, from the Eastern Amazon, Brazil. We used high-48 resolution sequencing of archaeal and bacterial 16S rRNA genes combined with real-time PCR 49 to quantify Archaea and Bacteria, as well as key functional genes indicative of the 50 methanogenic (methyl coenzyme-M reductase -mcrA) and methanotrophic (particulate51 methane monooxygenase -pmoA) metabolisms. Methanogens were found to be present in 52 high abundance in floodplain sediments and they seem to resist to dramatic seasonal 53 environmental changes. Methanotrophs known to use different pathways to oxidise CH4 were 54 3 detected, including anaerobic archaeal and bacterial taxa, indicating that a wide metabolic 55 diversity may be harboured in this highly variable environment. The floodplain environmental 56 variability, which is affected by the river origin, drives not only the sediment chemistry, but also 57 the composition of the microbial communities. The results presented may contribute to the 58 understanding of the current state of CH4 cycling in this region. 59 60 Quantitative PCR. 62 63 65 et al. , 2015). These ecosystems comprise diversified and dynamic landscapes, which are 66 exposed to seasonal flooding events by the expanding rivers, as a consequence of the periodic 67 excessive rainfalls. Floodplains seem to play a significant role in the regional and global C 68 72 significant process of CH4 transfer through trees (Pangala et al., 2017). Modelling studies have 73 predicted that Amazonian floodplains may contribute up to 7% of total global CH4 emissions 74 (Potter, Melack & Engle, 2014; Wilson et al., 2016).
75In anoxic environments, the CH4 is generated as the final product of the anaerobic 76 respiration by methanogenic archaea, which can use acetate, H2/CO2, formate, CO, or 77 methylated compounds as substrates (Bridgham, Cadillo-Quiroz, Keller & Zhuang, 2013). The 78 ability to use one or more substrates varies across the different methanogenic archaea taxa. 79 Hence, substrate availability, along with other factors (biotic and abiotic), affects the diversity 80 of these organisms in the environment (Barros et al., 2019).81 103 scales. For instance, the riverine origin is a very important factor, as some waters may carry 104 large amounts of inorganic suspensoids, s...