水稻土细菌坏死物分解和启动效应依赖于长期施肥

IF 10.3 1区 农林科学 Q1 SOIL SCIENCE
Qi Liu , Zhenke Zhu , Liang Wei , Wenju Zhang , Shuang Wang , Hongzhao Yuan , Jianping Chen , Tida Ge , Minggang Xu , Yakov Kuzyakov
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引用次数: 0

摘要

长期施肥会改变土壤养分有效性和微生物群落组成,从而调节微生物坏死块的分解及其对土壤有机碳(SOC)周转的影响。然而,在稻田中,驱动坏死团循环的微生物分类以及它们的活动如何转化为对有机碳矿化的正或负启动效应(PEs)仍然知之甚少。采用13C同位素探测和高通量测序相结合的方法,研究了施用34年矿肥和鸡粪的水稻土中参与尸块分解的微生物群及其对有机碳矿化的影响。在添加13C标记的细菌坏死块后,在210天内,50-60%的13C被矿化成二氧化碳,与未施肥的土壤相比,施肥土壤释放的13C-CO2多15%。从坏死块中摄取13C的微生物顺序发生:最初(5天内)革兰氏阳性(革兰氏+)细菌占主导地位,随后是革兰氏阴性(革兰氏−)细菌的二次摄取,然后是放线菌和真菌的二次摄取。在未施肥的碳限制土壤中,革兰氏菌(Gram+ bacteria)、γ -变形菌(γ -proteobacteria)、Patescibacteria和担子菌(Basidiomycota)等k -策略菌群通过挖掘顽固的有机碳来满足其养分需求,从而产生强烈的正PE。相反,在接受矿物和有机混合输入的土壤中,包括革兰氏菌、α -变形菌和子囊菌在内的r-策略分类群优先分解新形成的微生物坏死块,而不是有机碳,导致负PE和净有机碳积累。这些发现表明,施肥驱动的微生物生活史策略的转变控制着坏死块的周转及其引发的后果,突出了坏死块的循环是促进有机碳稳定的关键杠杆。因此,管理肥料制度以支持目标微生物协会为加强水稻生态系统的碳固存和维持土壤健康提供了一条有希望的途径。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Bacterial necromass decomposition and priming effects in paddy soils depend on long-term fertilization
Long-term fertilization alters nutrient availability and microbial community composition in soil, thereby modulating the decomposition of microbial necromass and its influence on soil organic carbon (SOC) turnover. However, the microbial taxa that drive necromass recycling and how their activity translates into positive or negative priming effects (PEs) on SOC mineralization in rice paddies remain unknown. We combined 13C isotope probing and high-throughput sequencing to investigate the microbial groups involved in necromass decomposition and their associated PEs on SOC mineralization in paddy soils subjected to 34 years of mineral fertilization or chicken manure application as compared to unfertilized control soil. Following the addition of 13C-labeled bacterial necromass, 50–60 % of the 13C was mineralized to CO2 within 210 days, with fertilized soils releasing 15 % more 13C–CO2 compared to unfertilized soils. Microbial uptake of 13C from necromass occurred sequentially: Gram-positive (Gram+) bacteria dominated initial incorporation (within 5 days), followed by uptake by Gram-negative (Gram) bacteria and thereafter by actinomycetes and fungi after 40 days. In unfertilized carbon-limited soils, K-strategist taxa, such as Gram+ bacteria, Gamma-proteobacteria, Patescibacteria, and Basidiomycota, mined recalcitrant SOC to fulfill their nutrient demands, thus generating a strong positive PE. Conversely, in soils receiving combined mineral and organic inputs, r-strategist taxa, including Gram bacteria, Alpha-proteobacteria, and Ascomycota, preferentially decomposed newly formed microbial necromass rather than SOC, resulting in a negative PE and net SOC accumulation. These findings demonstrate that fertilization-driven shifts in microbial life-history strategies as well as SOC availability govern necromass turnover and its priming consequences, highlighting necromass recycling as a key lever to raise SOC stabilization. Thus, managing fertilizer regimes to favor targeted microbial guilds offers a promising pathway to increase carbon sequestration and sustain soil health in paddy ecosystems.
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来源期刊
Soil Biology & Biochemistry
Soil Biology & Biochemistry 农林科学-土壤科学
CiteScore
16.90
自引率
9.30%
发文量
312
审稿时长
49 days
期刊介绍: Soil Biology & Biochemistry publishes original research articles of international significance focusing on biological processes in soil and their applications to soil and environmental quality. Major topics include the ecology and biochemical processes of soil organisms, their effects on the environment, and interactions with plants. The journal also welcomes state-of-the-art reviews and discussions on contemporary research in soil biology and biochemistry.
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