Boak Emily N, Bowen Benjamin P, Louie Katherine B, Northen Trent R, Kroeger Marie E
Microbial and Biome Sciences Group, Bioscience Division, Los Alamos National Laboratory, Los Alamos, NM 87545, United States.
Genomics and Systems Biology, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, United States.
ISME Commun. 2025 May 20;5(1):ycaf084. doi: 10.1093/ismeco/ycaf084. eCollection 2025 Jan.
Soil water repellency (SWR), the reduced affinity of soil for water, is a phenomenon that affects soils globally. With worsening climate change, SWR is expected to increase emphasizing the need to understand the mechanisms driving SWR development and persistence. The importance of the soil microbes in SWR has been postulated for decades, but limited research has been conducted into whole-community interactions and the role of community metabolic activity. To address this gap in knowledge, we investigated the direct effect of microbial community composition, activity, and diversity, as well as their associated metabolites on the development and persistence of SWR by inoculating microcosms containing model soils with 15 different microbial communities and quantified respiration and SWR over time. Six communities that consistently produced either a hydrophobic or hydrophilic phenotype were characterized using metagenomics and metabolomics to determine the impact of microbial and metabolite composition and diversity on SWR. We identified several bacterial genera with significant changes in abundance between SWR phenotypes including and in hydrophilic and and in hydrophobic. We discovered that hydrophilic communities were more positively connected when compared to hydrophobic communities, which could be due to an increase in defense mechanism genes. Additionally, we identified specific metabolites associated with hydrophilic and hydrophobic phenotypes including an increase in the osmolyte ectoine in hydrophilic and an increase in plant-derived decomposition products in hydrophobic communities. Finally, our research suggests that fungi, previously thought to cause hydrophobicity, may actually contribute to hydrophilicity through their preferential consumption of hydrophobic compounds.
土壤斥水性(SWR)是指土壤对水的亲和力降低的现象,这是一种影响全球土壤的现象。随着气候变化的加剧,预计土壤斥水性将会增加,这凸显了了解驱动土壤斥水性发展和持续存在机制的必要性。数十年来,人们一直假定土壤微生物在土壤斥水性中具有重要作用,但针对整个群落相互作用以及群落代谢活动的作用开展的研究有限。为了填补这一知识空白,我们通过向含有模型土壤的微观世界接种15种不同的微生物群落,并随时间量化呼吸作用和土壤斥水性,研究了微生物群落组成、活性和多样性及其相关代谢产物对土壤斥水性发展和持续存在的直接影响。利用宏基因组学和代谢组学对六个始终产生疏水或亲水表型的群落进行了表征,以确定微生物和代谢产物组成及多样性对土壤斥水性的影响。我们鉴定出了几个在土壤斥水性表型之间丰度有显著变化的细菌属,包括亲水表型中的 和 ,以及疏水表型中的 和 。我们发现,与疏水群落相比,亲水群落的连接更为积极,这可能是由于防御机制基因的增加。此外,我们还鉴定出了与亲水和疏水表型相关的特定代谢产物,包括亲水表型中渗透保护剂ectoine的增加以及疏水群落中植物源分解产物的增加。最后,我们的研究表明,以前被认为会导致疏水性的真菌,实际上可能通过优先消耗疏水化合物而促进亲水性。