原位冠层 13CO2 富集条件下毛竹通过根瘤沉积增加活性有机碳库的微生物机制

IF 4.8 2区 农林科学 Q1 SOIL SCIENCE
Man Shi , Hang Chen , Junbo Zhang, Zhenxiong Chen, Zhikang Wang, Tingting Cao, Quan Li, Xinzhang Song
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引用次数: 0

摘要

植物根系沉积在很大程度上介导了植物-土壤-微生物之间的相互作用,并对土壤活性有机碳库产生影响。然而,人们对根状茎沉积影响土壤活性有机碳库的机制仍然知之甚少。本研究调查了根状茎沉积对毛竹(Phyllostachys edulis)活性有机碳库和微生物群落的影响。用 13CO2 富集母株的树冠,以追踪根状茎的沉积,并评估不同根系(秆根和根茎根)在关键生长阶段(初期、高峰期、分枝期和落叶期)土壤有机碳库和微生物群落的变化。结果表明,树冠二氧化碳富集增加了根圈中δ13C和微生物生物量C、溶解有机C和可溶性有机C的含量(增加了22.08%至43.67%),从而显著改变了细菌群落的组成。在冠层二氧化碳富集条件下,与难分解 C 相关的细菌类群和基因的丰度分别下降了 29.08 %-77.38 % 和 30.75 %-56.85 %;而与二氧化碳固定相关的类群和基因则分别增加了 51.22 %-267.00 % 和 92.52 %-331.46 %。这些微生物的变化导致了土壤活性有机碳库的增加。此外,生长阶段而非根系对根瘤沉积的影响更大,与生长高峰期和分枝期相比,早期和落叶期的δ13C更高。总之,我们的研究结果表明,活性有机碳库的增加主要是由碳根瘤沉积的增强、参与二氧化碳固定的微生物的刺激和参与难分解碳的细菌的抑制所驱动的,同时与生长阶段有很大关系。这项研究为了解植物根系沉积、微生物功能和土壤活性有机碳动态之间的相互作用提供了宝贵的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Microbial mechanisms underlying active organic carbon pool increases via rhizodeposition by Moso bamboo under in situ crown 13CO2 enrichment

Microbial mechanisms underlying active organic carbon pool increases via rhizodeposition by Moso bamboo under in situ crown 13CO2 enrichment
Plant rhizodeposition strongly mediates plant-soil-microbe interactions and impacts the soil active organic carbon (C) pool. However, the mechanisms by which rhizodeposition affects the modulation of soil active organic C pool remain poorly understood. In this study, we investigated the effects of rhizodeposition on active organic C pool and microbial communities in Moso bamboo (Phyllostachys edulis), a clonal plant with rhizome-connected mother and offspring ramets. The crown of the mother ramet was enriched with 13CO2 to trace rhizodeposition and assess changes in soil organic C pool and the microbial community across different root systems (culm roots and rhizome roots) during key growth stages (early, peak, branching, and leafing). Our results showed that crown CO2 enrichment increased δ13C and the contents of microbial biomass C, dissolved organic C, and labile organic C (by 22.08 % to 43.67 %) in the rhizosphere, which significantly altered the bacterial community composition. Under crown CO2 enrichment, the abundance of bacterial taxa and genes associated with recalcitrant C decomposition decreased by 29.08 %–77.38 % and 30.75 %–56.85 %, respectively; while taxa and genes related to CO2 fixation increased by 51.22 %–267.00 % and 92.52 %–331.46 %, respectively. These microbial shifts contributed to an increase in the soil active organic C pool. In addition, the growth stage, rather than the root system, had a greater influence on rhizodeposition, with higher δ13C observed during the early and leafing stages compared to the peak and branching stages. In conclusion, our findings suggest that increases in the active organic C pool were primarily driven by enhanced C rhizodeposition, the stimulation of microbes involved in CO2 fixation, and the suppression of bacteria involved in recalcitrant C decomposition, while being highly dependent on the growth stage. This study provides valuable insights into the interactions between plant rhizodeposition, microbial functions, and soil active organic C dynamics.
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来源期刊
Applied Soil Ecology
Applied Soil Ecology 农林科学-土壤科学
CiteScore
9.70
自引率
4.20%
发文量
363
审稿时长
5.3 months
期刊介绍: Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.
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