Tracing 33P-labelled organic phosphorus compounds in two soils: New insights into decomposition dynamics and direct use by microbes

IF 2.1 Q3 SOIL SCIENCE
Daniel Wasner, J. Prommer, D. Zezula, M. Mooshammer, Yuntao Hu, W. Wanek
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引用次数: 0

Abstract

Introduction Organic phosphorus (Po) compounds constitute an important pool in soil P cycling, but their decomposition dynamics are poorly understood. Further, it has never been directly tested whether low molecular weight Po compounds are taken up by soil microbes in an intact form, which reduces the dependence of their P acquisition on extracellular phosphatases. Methods We investigated the short-term fate (24 h) of five 33P-labelled Po compounds (teichoic acids, phospholipids, DNA, RNA and soluble organophosphates) and 33P-labelled inorganic P (Pi) in two soils. Results We found indications that soil microbial breakdown of phosphodiesters was limited by the depolymerization step, and that direct microbial uptake of Po occurred to a substantial extent. Discussion We postulate a trade-off between direct Po uptake and complete extracellular Po mineralization. These findings have profound consequences for our understanding of microbial P cycling in soils.
在两种土壤中追踪33p标记的有机磷化合物:分解动力学和微生物直接利用的新见解
引言有机磷(Po)化合物在土壤磷循环中是一个重要的库,但其分解动力学尚不清楚。此外,从未直接测试过低分子量的Po化合物是否以完整的形式被土壤微生物吸收,这降低了它们获取P对细胞外磷酸酶的依赖性。方法我们研究了5种33P标记的Po化合物(磷壁酸、磷脂、DNA、RNA和可溶性有机磷)和33P标记无机P(Pi)在两种土壤中的短期命运(24小时)。结果我们发现,土壤微生物对磷酸二酯酶的分解受到解聚步骤的限制,并且在很大程度上发生了微生物对Po的直接吸收。讨论我们假设在直接摄取Po和完全的细胞外Po矿化之间进行权衡。这些发现对我们理解土壤中的微生物磷循环具有深远的影响。
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CiteScore
1.90
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