Finn Damien Robert, Ziv-El Michal, van Haren Joost, Park Jin Gyoon, Del Aguila-Pasquel Jhon, Urquiza-Muñoz Jose David, Cadillo-Quiroz Hinsby
School of Life Sciences, Arizona State University, Tempe, AZ, United States.
Swette Center for Environmental Biotechnology, Biodesign Institute, Arizona State University, Tempe, AZ, United States.
Front Microbiol. 2020 Apr 24;11:746. doi: 10.3389/fmicb.2020.00746. eCollection 2020.
Tropical peatlands are globally important carbon reservoirs that play a crucial role in fluxes of atmospheric greenhouse gases. Amazon peatlands are expected to be large source of atmospheric methane (CH) emissions, however little is understood about the rates of CH flux or the microorganisms that mediate it in these environments. Here we studied a mineral nutrient gradient across peatlands in the Pastaza-Marañón Basin, the largest tropical peatland in South America, to describe CH fluxes and environmental factors that regulate species assemblages of methanogenic and methanotrophic microorganisms. Peatlands were grouped as minerotrophic, mixed and ombrotrophic categories by their general water source leading to different mineral nutrient content (rich, mixed and poor) quantified by trace elements abundance. Microbial communities clustered dependent on nutrient content (ANOSIM < 0.001). Higher CH flux was associated with minerotrophic communities compared to the other categories. The most dominant methanogens and methanotrophs were represented by , and , respectively. Weighted network analysis demonstrated tight clustering of most methanogen families with minerotrophic-associated microbial families. Populations of were present across all peatlands. Null model testing for species assemblage patterns and species rank distributions confirmed non-random aggregations of methanotroph and methanogen families ( < 0.05). We conclude that in studied amazon peatlands increasing mineral nutrient content provides favorable habitats for , while populations seem to broadly distribute independent of nutrient content.
热带泥炭地是全球重要的碳库,在大气温室气体通量中起着关键作用。亚马逊泥炭地预计是大气甲烷(CH)排放的重要来源,然而,对于这些环境中CH通量的速率或介导其产生的微生物,人们了解甚少。在这里,我们研究了南美洲最大的热带泥炭地帕斯塔萨 - 马拉尼翁盆地泥炭地的矿质养分梯度,以描述CH通量以及调节产甲烷和甲烷氧化微生物物种组合的环境因素。根据其一般水源,泥炭地被分为矿质营养型、混合型和雨养型类别,这导致了通过微量元素丰度量化的不同矿质养分含量(丰富、混合和贫乏)。微生物群落根据养分含量聚类(ANOSIM < 0.001)。与其他类别相比,矿质营养型群落的CH通量更高。最主要的产甲烷菌和甲烷氧化菌分别由 和 代表。加权网络分析表明,大多数产甲烷菌家族与矿质营养相关的微生物家族紧密聚类。 在所有泥炭地中均有分布。对物种组合模式和物种排名分布的零模型测试证实了甲烷氧化菌和产甲烷菌家族的非随机聚集(< 0.05)。我们得出结论,在所研究的亚马逊泥炭地中,矿质养分含量的增加为 提供了有利的栖息地,而 种群似乎广泛分布,与养分含量无关。