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Temperature Controls Crystalline Iron Oxide Utilization by Microbial Communities in Methanic Ferruginous Marine Sediment Incubations

机译:温度控制甲烷氧化性铁质海洋沉积物中微生物群落对结晶氧化铁的利用

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摘要

Microorganisms can use crystalline iron minerals for iron reduction linked to organic matter degradation or as conduits for direct interspecies electron transfer (mDIET) to syntrophic partners, e.g., methanogens. The environmental conditions that lead either to reduction or conduit use are so far unknown. We investigated microbial community shifts and interactions with crystalline iron minerals (hematite and magnetite) in methanic ferruginous marine sediment incubations during organic matter (glucose) degradation at varying temperatures. Iron reduction rates increased with decreasing temperature from 30°C to 4°C. Both hematite and magnetite facilitated iron reduction at 4°C, demonstrating that microorganisms in the methanic zone of marine sediments can reduce crystalline iron oxides under psychrophilic conditions. Methanogenesis occurred, however, at higher rates with increasing temperature. At 30°C, both hematite and magnetite accelerated methanogenesis onset and maximum process rates. At lower temperatures (10°C and 4°C), hematite could still facilitate methanogenesis but magnetite served more as an electron acceptor for iron reduction than as a conduit. Different temperatures selected for different key microorganisms: at 30°C, members of genus Orenia, Halobacteroidaceae, at 10°C, Photobacterium and the order Clostridiales, and at 4°C Photobacterium and Psychromonas were enriched. Members of the order Desulfuromonadales harboring known dissimilatory iron reducers were also enriched at all temperatures. Our results show that crystalline iron oxides predominant in some natural environments can facilitate electron transfer between microbial communities at psychrophilic temperatures. Furthermore, temperature has a critical role in determining the pathway of crystalline iron oxide utilization in marine sediment shifting from conduction at 30°C to predominantly iron reduction at lower temperatures.
机译:微生物可以使用结晶性铁矿物质来还原与有机物降解相关的铁,或用作将种间电子直接传递给同养伴侣(如产甲烷菌)的管道(mDIET)。迄今为止,导致减少或使用导管的环境条件尚不清楚。我们调查了在不同温度下有机物(葡萄糖)降解过程中,甲烷化铁质海洋沉积物中的微生物群落迁移以及与结晶铁矿物(赤铁矿和磁铁矿)的相互作用。铁的还原率随温度从30°C降低到4°C而增加。赤铁矿和磁铁矿都促进了4°C下的铁还原,这表明海洋沉积物甲烷化区中的微生物在嗜冷条件下可以还原结晶性铁氧化物。然而,随着温度升高,甲烷生成发生的速率更高。在30°C时,赤铁矿和磁铁矿都加快了甲烷生成的速度,并加快了最大加工速度。在较低的温度(10°C和4°C)下,赤铁矿仍可促进甲烷生成,但磁铁矿作为铁还原的电子受体比起管道更能起到作用。为不同的关键微生物选择了不同的温度:在30°C时,富集了Orenia属,盐杆菌科的成员,在10°C,光细菌和梭状芽胞杆菌以及在4°C时,光细菌和Psychromonas富集。在所有温度下,富含已知异化铁还原剂的Desulfuromonadales订单的成员也被富集。我们的研究结果表明,在某些自然环境中,主要存在的结晶性氧化铁可以促进在嗜冷温度下微生物群落之间的电子转移。此外,温度在确定海洋沉积物中晶体氧化铁利用从30°C的传导转变为较低温度下的主要铁还原的途径中起着至关重要的作用。

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