Aeration and mineral composition of soil determine microbial CUE

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE
Soil Pub Date : 2025-02-21 DOI:10.5194/egusphere-2025-481
Jolanta Niedźwiecka, Roey Angel, Petr Čapek, Ana Catalina Lara, Stanislav Jabinski, Travis B. Meador, Hana Šantrůčková
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Abstract

Abstract. Microbial carbon use efficiency (CUE) in soils is used to estimate the balance of CO2 respired by heterotrophs versus the accumulation of organic carbon (C). While most CUE studies assume that aerobic respiration is the predominant degradation process of organic C, anoxic microniches are common inside soil aggregates. Microorganisms in these microniches carry out fermentation and anaerobic respiration using alternative electron acceptors, e.g. NO3-, Fe, SO42-. Extracellular metabolites are also not traditionally accounted for but may represent a significant C flux. Moreover, climate change may modulate soil microbial activity by altering soil aeration status on a local level due to warming and elevated frequency of extreme precipitation events. Therefore, CUE should be measured under more realistic assumptions regarding soil aeration. This study focused on the effect of oxygen and Fe on C mineralisation in forest soils and quantified C distribution between biomass and different extracellular metabolites. Forest soils were collected from two Bohemian Forest (Czechia) sites with low and high Fe content and incubated under oxic and anoxic conditions. A solution of 13C-labelled glucose was used to track stable isotope incorporation into the biomass, respired CO2, and extracellular metabolites. We estimated CUE based on microbial respiration, glucose consumption, biomass growth, and extracellular metabolites. RNA-SIP was used to identify the active bacteria under each treatment. As expected, the oxic incubation showed a rapid utilisation and immediate production of biomass and CO2. Under anoxic conditions, 90 % of the added glucose was still present after 72 h, and anoxic soils showed significantly lower microbial activity. The low-Fe soil samples were more active under oxic conditions, while the high-Fe samples were more active under anoxia. Our findings confirm that anoxia in soils enhances short-term C preservation. Accordingly, excluding exudates in mass flux calculations would underestimate apparent CUE values.
土壤的通气性和矿物组成决定微生物CUE
摘要。土壤微生物碳利用效率(CUE)用于估算异养生物呼吸的CO2与有机碳(C)积累的平衡。尽管大多数CUE研究认为有氧呼吸是有机碳的主要降解过程,但在土壤团聚体中,缺氧微生境是常见的。这些微生态系统中的微生物利用NO3-、Fe、SO42-等替代电子受体进行发酵和厌氧呼吸。细胞外代谢物传统上也没有考虑,但可能代表一个重要的碳通量。此外,由于气候变暖和极端降水事件频率的增加,气候变化可能通过改变局部水平的土壤通气状况来调节土壤微生物活动。因此,CUE应在更现实的土壤通气性假设下测量。本文主要研究了氧和铁对森林土壤碳矿化的影响以及生物量和不同细胞外代谢物之间碳的定量分布。在捷克两个低铁和高铁的波西米亚森林地区采集森林土壤,在缺氧和缺氧条件下进行培养。13c标记的葡萄糖溶液用于跟踪稳定同位素在生物质、呼吸二氧化碳和细胞外代谢物中的掺入。我们根据微生物呼吸、葡萄糖消耗、生物量生长和细胞外代谢物来估计CUE。采用RNA-SIP对各处理下的活性菌进行鉴定。正如预期的那样,氧培养显示出生物质和二氧化碳的快速利用和即时生产。在缺氧条件下,添加的葡萄糖在72 h后仍有90%存在,缺氧土壤的微生物活性显著降低。低铁土壤样品在氧化条件下活性更高,而高铁土壤样品在缺氧条件下活性更高。我们的研究结果证实,土壤中的缺氧增强了短期的碳保存。因此,在质量通量计算中排除渗出物会低估表观CUE值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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