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Anaerobic decomposition of humic substances by Clostridium from the deep subsurface

机译:梭菌从深地下厌氧分解腐殖质

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摘要

Decomposition of humic substances (HSs) is a slow and cryptic but non-negligible component of carbon cycling in sediments. Aerobic decomposition of HSs by microorganisms in the surface environment has been well documented; however, the mechanism of anaerobic microbial decomposition of HSs is not completely understood. Moreover, no microorganisms capable of anaerobic decomposition of HSs have been isolated. Here, we report the anaerobic decomposition of humic acids (HAs) by the anaerobic bacterium Clostridium sp. HSAI-1 isolated from the deep terrestrial subsurface. The use of 14C-labelled polycatechol as an HA analogue demonstrated that the bacterium decomposed this substance up to 7.4% over 14 days. The decomposition of commercial and natural HAs by the bacterium yielded lower molecular mass fractions, as determined using high-performance size-exclusion chromatography. Fourier transform infrared spectroscopy revealed the removal of carboxyl groups and polysaccharide-related substances, as well as the generation of aliphatic components, amide and aromatic groups. Therefore, our results suggest that Clostridium sp. HSAI-1 anaerobically decomposes and transforms HSs. This study improves our understanding of the anaerobic decomposition of HSs in the hidden carbon cycling in the Earth’s subsurface.
机译:腐殖质(HSs)的分解是沉积物中碳循环的缓慢而隐秘但不可忽略的组成部分。在表面环境中,微生物对HSs的好氧分解已有很好的记录。但是,尚不完全了解HSs的厌氧微生物分解机理。此外,尚未分离出能够对HS进行厌氧分解的微生物。在这里,我们报告由厌氧细菌梭状芽孢杆菌的腐殖酸(HAs)的厌氧分解。从深层地下分离出的HSAI-1。使用 14 C标记的聚儿茶酚作为HA类似物表明,细菌在14天内分解了该物质的比例高达7.4%。如使用高效尺寸排阻色谱法所确定的,细菌对商业和天然HA的分解产生了较低的分子量分数。傅立叶变换红外光谱法揭示了羧基和多糖相关物质的去除,以及脂肪族成分,酰胺和芳香族基团的产生。因此,我们的结果表明梭状芽孢杆菌。 HSAI-1厌氧分解和转化HS。这项研究提高了我们对地球地下地下隐藏碳循环中HSs厌氧分解的理解。

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