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Microscale sulfur cycling in the phototrophic pink berry consortia of the Sippewissett Salt Marsh

机译:Sippewissett盐沼的光养性粉红色浆果财团中的微量硫循环

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摘要

Microbial metabolism is the engine that drives global biogeochemical cycles, yet many key transformations are carried out by microbial consortia over short spatiotemporal scales that elude detection by traditional analytical approaches. We investigate syntrophic sulfur cycling in the ‘pink berry’ consortia of the Sippewissett Salt Marsh through an integrative study at the microbial scale. The pink berries are macroscopic, photosynthetic microbial aggregates composed primarily of two closely associated species: sulfide-oxidizing purple sulfur bacteria (PB-PSB1) and sulfate-reducing bacteria (PB-SRB1). Using metagenomic sequencing and 34S-enriched sulfate stable isotope probing coupled with nanoSIMS, we demonstrate interspecies transfer of reduced sulfur metabolites from PB-SRB1 to PB-PSB1. The pink berries catalyse net sulfide oxidation and maintain internal sulfide concentrations of 0–500 μm. Sulfide within the berries, captured on silver wires and analysed using secondary ion mass spectrometer, increased in abundance towards the berry interior, while δ34S-sulfide decreased from 6‰ to −31‰ from the exterior to interior of the berry. These values correspond to sulfate–sulfide isotopic fractionations (15–53‰) consistent with either sulfate reduction or a mixture of reductive and oxidative metabolisms. Together this combined metagenomic and high-resolution isotopic analysis demonstrates active sulfur cycling at the microscale within well-structured macroscopic consortia consisting of sulfide-oxidizing anoxygenic phototrophs and sulfate-reducing bacteria.
机译:微生物代谢是驱动全球生物地球化学循环的引擎,然而微生物联盟在短时空范围内进行了许多关键的转化,而传统的分析方法无法进行检测。通过微生物规模的综合研究,我们研究了Sippewissett盐沼的“粉红浆果”财团中的腐化硫循环。粉色浆果是宏观的光合微生物聚集体,主要由两个紧密相关的物种组成:硫化物氧化的紫色硫细菌(PB-PSB1)和硫酸盐还原的细菌(PB-SRB1)。使用宏基因组测序和 34 S富集的硫酸盐稳定同位素探针,与nanoSIMS结合,我们证明了还原的硫代谢物从PB-SRB1到PB-PSB1的种间转移。粉红色的浆果催化净硫化物的氧化并保持内部硫化物浓度为0–500μm。浆果中的硫化物被银丝捕获并使用二次离子质谱仪进行分析,其向浆果内部的丰度增加,而δ 34 S-硫化物从外部到外部从6‰降低到-31‰。浆果的内部。这些值对应于硫酸盐-硫化物同位素分馏(15-53‰),与硫酸盐还原或还原代谢和氧化代谢的混合物一致。结合起来的宏基因组学和高分辨率同位素分析表明,在结构良好的宏观财团内,硫在微观尺度上具有活跃的硫循环,该财团由硫化物氧化的产氧光养菌和硫酸盐还原的细菌组成。

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