Spatially resolved denitrification coupled with methane and arsenite oxidation at the millimeter-scale straw–soil interface

反硝化 甲烷厌氧氧化 产甲烷 生物地球化学循环 亚砷酸盐 化学 环境化学 甲烷 好氧反硝化 稻草 氮气循环 固氮 微生物种群生物学 氮气 缺氧水域 氧化还原 有机质 温室气体 土壤水分 曝气 溶解有机碳 硝酸盐 矿化(土壤科学) 环境科学 一氧化二氮 生态系统 微生物 生物量(生态学) 生物地球化学 固碳 富营养化 碳循环
作者
Xin-Di Zhao,Ya-Qin Wang,Sha Zhang,S. Y. Zhang,Yu-Jia Cai,Yu-Jia Cai,Xiao Shu,Zheng Chen,Si-Yu Zhang,Si-Yu Zhang
出处
期刊:Proceedings of the National Academy of Sciences of the United States of America [National Academy of Sciences]
卷期号:123 (8): e2521285123-e2521285123
标识
DOI:10.1073/pnas.2521285123
摘要

Straw return reshapes the biogeochemical processes in paddy soils by driving microbial transformation of key elements. Despite growing awareness of these individual processes, the integration of these processes under millimeter-scale spatiotemporal heterogeneity remains unclear. Combining high-resolution geochemical profiling with multiomics, we revealed that straw addition altered the depth-dependent dynamics of arsenic, carbon, and nitrogen, establishing a sophisticated three-layer microbial stratification. We identified 1) an 18 mm organic matter (OM)-rich layer extending from the straw layer, which serves as a methanogenic epicenter co-occurring with active nitrogen fixation microbes; 2) an overlying layer dominated by aerobic methane oxidation and denitrification microbes; and 3) a deeper substraw layer dominated by anaerobic arsenite oxidation and denitrification microbes. Significantly positively correlated abundances of transcribed mcrA with nifH genes and pmoA or aioA/arxA with denitrification genes were identified. Corroboratively, intensified co-occurrence patterns of mcrA with nifH, pmoA with denitrification, and aioA/arxA with denitrification genes were observed in the OM-rich, upper, and lower layers, respectively. Moreover, the co-occurred mcrA-nifH and aioA-nirS/arxA-narG genes in different metagenome-assembled genomes presented 80.6 to 260.8- and 1.55 to 6.85-fold greater transcriptional activity in the OM-rich and lower layers than in the other layers, respectively. Our results demonstrated that straw incorporation established a dynamic soil redox zone, restructuring millimeter-scale microbial networks and promoting potentially coupled denitrification with arsenite or methane oxidation, as well as methanogenesis with nitrogen fixation. These findings provide a mechanistic basis for optimizing subsurface straw placement and nitrate application to enhance nutrient cycling and mitigate environmental risks.
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