Microbial carbon use efficiency: accounting for population, community, and ecosystem-scale controls over the fate of metabolized organic matter

IF 3.9 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Kevin M. Geyer, Emily Kyker-Snowman, A. Stuart Grandy, Serita D. Frey
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引用次数: 227

Abstract

Microbial carbon use efficiency (CUE) is a critical regulator of soil organic matter dynamics and terrestrial carbon fluxes, with strong implications for soil biogeochemistry models. While ecologists increasingly appreciate the importance of CUE, its core concepts remain ambiguous: terminology is inconsistent and confusing, methods capture variable temporal and spatial scales, and the significance of many fundamental drivers remains inconclusive. Here we outline the processes underlying microbial efficiency and propose a conceptual framework that structures the definition of CUE according to increasingly broad temporal and spatial drivers where (1) CUE P reflects population-scale carbon use efficiency of microbes governed by species-specific metabolic and thermodynamic constraints, (2) CUE C defines community-scale microbial efficiency as gross biomass production per unit substrate taken up over short time scales, largely excluding recycling of microbial necromass and exudates, and (3) CUE E reflects the ecosystem-scale efficiency of net microbial biomass production (growth) per unit substrate taken up as iterative breakdown and recycling of microbial products occurs. CUEE integrates all internal and extracellular constraints on CUE and hence embodies an ecosystem perspective that fully captures all drivers of microbial biomass synthesis and decay. These three definitions are distinct yet complementary, capturing the capacity for carbon storage in microbial biomass across different ecological scales. By unifying the existing concepts and terminology underlying microbial efficiency, our framework enhances data interpretation and theoretical advances.

Abstract Image

微生物碳利用效率:考虑种群、群落和生态系统对代谢有机物命运的控制
微生物碳利用效率(CUE)是土壤有机质动态和陆地碳通量的重要调节因子,对土壤生物地球化学模型具有重要意义。虽然生态学家越来越认识到CUE的重要性,但其核心概念仍然模糊不清:术语不一致且令人困惑,方法捕捉可变的时间和空间尺度,许多基本驱动因素的意义仍然没有定论。在此,我们概述了微生物效率的基本过程,并提出了一个概念框架,根据越来越广泛的时空驱动因素来构建CUE的定义,其中:(1)CUE P反映了受物种特异性代谢和热力学约束的微生物的种群尺度碳利用效率;(2) CUE C将群落规模微生物效率定义为短时间内单位底物的总生物量,在很大程度上不包括微生物坏死块和渗出物的再循环。(3) CUE E反映了微生物产品发生迭代分解和循环时,单位基质净微生物生物量生产(增长)的生态系统尺度效率。CUEE整合了CUE的所有细胞内外限制,因此体现了生态系统的观点,充分捕捉了微生物生物量合成和衰变的所有驱动因素。这三个定义是不同的,但互补的,捕获在不同的生态尺度微生物生物量的碳储存能力。通过统一微生物效率的现有概念和术语,我们的框架增强了数据解释和理论进步。
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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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