Revisiting soil microbial biomass: Considering changes in composition with growth rate

IF 9.8 1区 农林科学 Q1 SOIL SCIENCE
Petr Čapek , Michal Choma , Eva Kaštovská , Karolina Tahovská , Helen C. Glanville , Hana Šantrůčková
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Abstract

Soil microbial biomass is assumed to have stable chemical composition. Various components of the biomass such as DNA, ATP, or chloroform-labile organic carbon are measured in soil and converted into total microbial biomass using experimentally derived conversion factors, which are also assumed to be constant. However, several observations suggest the opposite. The composition of soil microbial biomass is likely changing with specific growth rate as observed in pure cultures of single microbial species. In this study, we define a “sub-Microbial” model that explicitly represents changes in composition of soil microbial biomass associated with changes in specific growth rate. We calibrate the model with published data and compare its performance with the simpler Monod and Pirt models, which consider microbial biomass as a single pool with invariant chemical composition. The model explains well the variability in chloroform-labile content of microbial biomass following organic substrate additions as well as variability in ratios of different components of microbial biomass. Changes in composition of soil microbial biomass are quantitatively significant and occur over hours and days resulting in our sub-Microbial model outperforming both the Monod and Pirt models. Our results further indicate that the composition of soil microbial biomass changes consistently with growth rate across various soils. Here, we provide a methodological recommendation how to determine total soil microbial biomass and its physiological characteristics such as growth rate, turnover rate and substrate use efficiency as accurately as possible. In light of the presented results, we would like to initiate a discussion about the methodological issues associated with measurement of soil microbial biomass as these measurements are expected to inform a new generation of microbially-explicit soil biogeochemical models predicting development of terrestrial ecosystems under various scenarios.

重新审视土壤微生物生物量:考虑其组成随生长速率的变化
土壤微生物生物量被认为具有稳定的化学组成。在土壤中测量生物量的各种成分,如DNA、ATP或氯仿不稳定的有机碳,并使用实验推导的转换因子转化为总微生物生物量,这些转换因子也被假设为恒定的。然而,一些观察结果表明情况恰恰相反。在单一微生物种的纯培养物中观察到,土壤微生物生物量的组成可能随特定生长速率而变化。在这项研究中,我们定义了一个“亚微生物”模型,明确表示土壤微生物生物量组成的变化与特定生长速率的变化相关。我们使用已发表的数据对模型进行校准,并将其性能与更简单的Monod和Pirt模型进行比较,后者将微生物生物量视为具有不变化学成分的单一池。该模型很好地解释了添加有机底物后微生物生物量氯仿不稳定含量的变异性以及微生物生物量不同组分比例的变异性。土壤微生物生物量组成的变化在数量上是显著的,并且发生在数小时和数天内,导致我们的亚微生物模型优于Monod和Pirt模型。我们的研究结果进一步表明,土壤微生物生物量的组成变化与生长速率一致。本文就如何尽可能准确地测定土壤微生物总量及其生长率、周转率和基质利用效率等生理特性提出了方法学建议。鉴于上述结果,我们希望开始讨论与土壤微生物生物量测量相关的方法问题,因为这些测量有望为新一代微生物明确的土壤生物地球化学模型提供信息,预测不同情景下陆地生态系统的发展。
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 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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