Earth and Biological Sciences Directorate, Pacific Northwest National Laboratory, Richland, WA, USA.
National Security Directorate, Pacific Northwest National Laboratory, Richland, WA, USA.
Microbiome. 2023 Feb 27;11(1):34. doi: 10.1186/s40168-022-01427-4.
Microbiomes contribute to multiple ecosystem services by transforming organic matter in the soil. Extreme shifts in the environment, such as drying-rewetting cycles during drought, can impact the microbial metabolism of organic matter by altering microbial physiology and function. These physiological responses are mediated in part by lipids that are responsible for regulating interactions between cells and the environment. Despite this critical role in regulating the microbial response to stress, little is known about microbial lipids and metabolites in the soil or how they influence phenotypes that are expressed under drying-rewetting cycles. To address this knowledge gap, we conducted a soil incubation experiment to simulate soil drying during a summer drought of an arid grassland, then measured the response of the soil lipidome and metabolome during the first 3 h after wet-up.
Reduced nutrient access during soil drying incurred a replacement of membrane phospholipids, resulting in a diminished abundance of multiple phosphorus-rich membrane lipids. The hot and dry conditions increased the prevalence of sphingolipids and lipids containing long-chain polyunsaturated fatty acids, both of which are associated with heat and osmotic stress-mitigating properties in fungi. This novel finding suggests that lipids commonly present in eukaryotes such as fungi may play a significant role in supporting community resilience displayed by arid land soil microbiomes during drought. As early as 10 min after rewetting dry soil, distinct changes were observed in several lipids that had bacterial signatures including a rapid increase in the abundance of glycerophospholipids with saturated and short fatty acid chains, prototypical of bacterial membrane lipids. Polar metabolites including disaccharides, nucleic acids, organic acids, inositols, and amino acids also increased in abundance upon rewetting. This rapid metabolic reactivation and growth after rewetting coincided with an increase in the relative abundance of firmicutes, suggesting that members of this phylum were positively impacted by rewetting.
Our study revealed specific changes in lipids and metabolites that are indicative of stress adaptation, substrate use, and cellular recovery during soil drying and subsequent rewetting. The drought-induced nutrient limitation was reflected in the lipidome and polar metabolome, both of which rapidly shifted (within hours) upon rewet. Reduced nutrient access in dry soil caused the replacement of glycerophospholipids with phosphorus-free lipids and impeded resource-expensive osmolyte accumulation. Elevated levels of ceramides and lipids with long-chain polyunsaturated fatty acids in dry soil suggest that lipids likely play an important role in the drought tolerance of microbial taxa capable of synthesizing these lipids. An increasing abundance of bacterial glycerophospholipids and triacylglycerols with fatty acids typical of bacteria and polar metabolites suggest a metabolic recovery in representative bacteria once the environmental conditions are conducive for growth. These results underscore the importance of the soil lipidome as a robust indicator of microbial community responses, especially at the short time scales of cell-environment reactions. Video Abstract.
微生物组通过转化土壤中的有机物来提供多种生态系统服务。环境的剧烈变化,如干旱期间的干湿循环,通过改变微生物的生理学和功能,可能会影响有机物的微生物代谢。这些生理反应部分受到脂质的调节,脂质负责调节细胞与环境之间的相互作用。尽管脂质在调节微生物对压力的反应方面起着至关重要的作用,但我们对土壤中的微生物脂质和代谢物知之甚少,也不知道它们如何影响在干湿循环下表达的表型。为了弥补这一知识空白,我们进行了一项土壤培养实验,模拟干旱草原夏季干旱期间的土壤干燥,然后在湿化后的头 3 小时测量土壤脂类组和代谢组的响应。
土壤干燥期间养分获取减少导致膜磷脂的替代,导致多种富含磷的膜脂质丰度降低。炎热干燥的条件增加了鞘脂和含有长链多不饱和脂肪酸的脂质的流行,这两者都与真菌中的热和渗透胁迫缓解特性有关。这一新颖的发现表明,真菌等真核生物中常见的脂质可能在支持干旱土地土壤微生物组在干旱期间表现出的群落恢复力方面发挥重要作用。在重新润湿干燥土壤后的短短 10 分钟内,就观察到了具有细菌特征的几种脂质的明显变化,包括具有饱和和短脂肪酸链的甘油磷脂的丰度迅速增加,这是细菌膜脂质的典型特征。极性代谢物,包括二糖、核酸、有机酸、肌醇和氨基酸,在重新润湿后也增加了丰度。这种快速的代谢再激活和重新润湿后的生长与厚壁菌门相对丰度的增加相吻合,表明该门的成员受到了再润湿的积极影响。
我们的研究揭示了在土壤干燥和随后再润湿过程中,适应压力、利用底物和细胞恢复的特定脂质和代谢物变化。干旱引起的养分限制反映在脂类组和极性代谢组中,两者都在数小时内(hours)迅速变化。在干燥土壤中,由于缺乏营养物质,甘油磷脂被无磷脂质取代,并阻碍了资源密集型渗透调节剂的积累。在干燥土壤中,神经酰胺和含有长链多不饱和脂肪酸的脂质水平升高表明,在能够合成这些脂质的微生物类群中,脂质可能在耐旱性方面发挥重要作用。细菌甘油磷脂和三酰基甘油的丰度增加,其脂肪酸具有细菌的典型特征,以及极性代谢物的增加,表明一旦环境条件有利于生长,代表性细菌就会出现代谢恢复。这些结果强调了土壤脂类组作为微生物群落反应的一个强有力指标的重要性,特别是在细胞-环境反应的短时间尺度上。视频摘要。