甲烷菌素对硫化铜矿物中铜的活化作用:pH、氧和天然有机物的影响

IF 2.7 2区 地球科学 Q2 BIOLOGY
Geobiology Pub Date : 2022-06-18 DOI:10.1111/gbi.12505
Danielle D. Rushworth, Iso Christl, Naresh Kumar, Kevin Hoffmann, Ruben Kretzschmar, Moritz F. Lehmann, Walter D. C. Schenkeveld, Stephan M. Kraemer
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引用次数: 2

摘要

需氧甲烷氧化(MOx)主要取决于铜(Cu)的可用性,铜是颗粒甲烷单加氧酶(MOx的主要酶之一)金属中心的重要组成部分。一些甲烷氧化菌已经发展出了Cu获取策略,在低Cu可用性的条件下,它们会分泌出被称为白团的Cu结合配体。一种特征明显的白团是甲烷菌(mb),由微嗜气的产甲烷菌Methylosinus trichosporium OB3b分泌。好氧甲烷氧化菌通常位于环境氧-缺氧界面附近,由于其溶解度低,硫化铜相的形成会加剧生物可利用铜的限制。对这些硫化铜矿物相的反应活性尚未进行研究。在这项研究中,结合溶解实验和平衡模型,研究了在mb存在下,受pH值、氧气和天然有机物的影响,块状和纳米颗粒硫化铜矿物的溶解和溶解度。总的来说,我们发现在多种可能限制Cu生物利用度的Cu硫化物相存在的情况下,mb在增加溶解Cu浓度方面是有效的。与晶体良好的大块钴岩相相比,每摩尔硫化铜纳米颗粒中调动了更多的铜。一般来说,mb从Cu硫化物中动员Cu的功效与ph值有关。在较低的pH下,例如pH为5时,mb对Cu没有溶解作用。在pH值为7到8.5之间,mb的存在增加了溶解的Cu浓度,在有氧和无氧的情况下,所有Cu硫化物的溶解度通常都很低。这些结果表明,在氧化-缺氧界面,特别是在中性至微碱性pH范围内,白垩团促进Cu从硫化物相的动员是增加溶解Cu浓度的有效胞外机制。这表明,在Cu的生物利用度受到非常稳定的Cu硫化物相限制的自然环境中,好氧甲烷氧化菌可能能够通过mb的渗出来满足它们对Cu的需求。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Copper mobilisation from Cu sulphide minerals by methanobactin: Effect of pH, oxygen and natural organic matter

Aerobic methane oxidation (MOx) depends critically on the availability of copper (Cu) as a crucial component of the metal centre of particulate methane monooxygenase, one of the main enzymes involved in MOx. Some methanotrophs have developed Cu acquisition strategies, in which they exude Cu-binding ligands termed chalkophores under conditions of low Cu availability. A well-characterised chalkophore is methanobactin (mb), exuded by the microaerophilic methanotroph Methylosinus trichosporium OB3b. Aerobic methanotrophs generally reside close to environmental oxic–anoxic interfaces, where the formation of Cu sulphide phases can aggravate the limitation of bioavailable Cu due to their low solubility. The reactivity of chalkophores towards such Cu sulphide mineral phases has not yet been investigated. In this study, a combination of dissolution experiments and equilibrium modelling was used to examine the dissolution and solubility of bulk and nanoparticulate Cu sulphide minerals in the presence of mb as influenced by pH, oxygen and natural organic matter. In general, we show that mb is effective at increasing the dissolved Cu concentrations in the presence of a variety of Cu sulphide phases that may potentially limit Cu bioavailability. More Cu was mobilised per mole of mb from Cu sulphide nanoparticles compared with well-crystalline bulk covellite (CuS). In general, the efficacy of mb at mobilising Cu from Cu sulphides is pH-dependent. At lower pH, e.g. pH 5, mb was ineffective at solubilizing Cu. The presence of mb increased dissolved Cu concentrations between pH 7 and 8.5, where the solubility of all Cu sulphides is generally low, both in the presence and absence of oxygen. These results suggest that chalkophore-promoted Cu mobilisation from sulphide phases is an effective extracellular mechanism for increasing dissolved Cu concentrations at oxic–anoxic interfaces, particularly in the neutral to slightly alkaline pH range. This suggests that aerobic methanotrophs may be able to fulfil their Cu requirements via the exudation of mb in natural environments where the bioavailability of Cu is constrained by very stable Cu sulphide phases.

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来源期刊
Geobiology
Geobiology 生物-地球科学综合
CiteScore
6.80
自引率
5.40%
发文量
56
审稿时长
3 months
期刊介绍: The field of geobiology explores the relationship between life and the Earth''s physical and chemical environment. Geobiology, launched in 2003, aims to provide a natural home for geobiological research, allowing the cross-fertilization of critical ideas, and promoting cooperation and advancement in this emerging field. We also aim to provide you with a forum for the rapid publication of your results in an international journal of high standing. We are particularly interested in papers crossing disciplines and containing both geological and biological elements, emphasizing the co-evolutionary interactions between life and its physical environment over geological time. Geobiology invites submission of high-quality articles in the following areas: Origins and evolution of life Co-evolution of the atmosphere, hydrosphere and biosphere The sedimentary rock record and geobiology of critical intervals Paleobiology and evolutionary ecology Biogeochemistry and global elemental cycles Microbe-mineral interactions Biomarkers Molecular ecology and phylogenetics.
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