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Fungal–bacterial dynamics and their contribution to terrigenous carbon turnover in relation to organic matter quality

机译:真菌-细菌动力学及其对与有机质相关的陆生碳转换的贡献

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摘要

Ecological functions of fungal and bacterial decomposers vary with environmental conditions. However, the response of these decomposers to particulate organic matter (POM) quality, which varies widely in aquatic ecosystems, remains poorly understood. Here we investigated how POM pools of substrates of different qualities determine the relative contributions of aquatic fungi and bacteria to terrigenous carbon (C) turnover. To this end, surface sediments were incubated with different POM pools of algae and/or leaf litter. 13C stable-isotope measurements of C mineralization were combined with phospholipid analysis to link the metabolic activities and substrate preferences of fungal and bacterial heterotrophs to dynamics in their abundance. We found that the presence of labile POM greatly affected the dominance of bacteria over fungi within the degrader communities and stimulated the decomposition of beech litter primarily through an increase in metabolic activity. Our data indicated that fungi primarily contribute to terrigenous C turnover by providing litter C for the microbial loop, whereas bacteria determine whether the supplied C substrate is assimilated into biomass or recycled back into the atmosphere in relation to phosphate availability. Thus, this study provides a better understanding of the role of fungi and bacteria in terrestrial–aquatic C cycling in relation to environmental conditions.
机译:真菌和细菌分解剂的生态功能随环境条件而变化。但是,这些分解者对水生生态系统中差异很大的颗粒有机物(POM)质量的反应仍然知之甚少。在这里,我们研究了不同质量底物的POM库如何确定水生真菌和细菌对陆生碳(C)转换的相对贡献。为此,将表面沉积物与藻类和/或枯枝落叶的不同POM库一起孵育。碳矿化的 13 C稳定同位素测量结果与磷脂分析相结合,将真菌和细菌异养生物的代谢活性以及底物偏好与其丰富的动态联系起来。我们发现不稳定的POM的存在极大地影响了降解菌群落中细菌对真菌的优势,并主要通过代谢活性的增加刺激了山毛榉凋落物的分解。我们的数据表明,真菌通过为微生物环提供凋落物C来主要促进陆源C的转换,而细菌则决定了所提供的C底物是否与磷酸盐有效利用同化或再循环回大气中。因此,本研究更好地了解了真菌和细菌在与环境条件相关的陆生水碳循环中的作用。

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