Helmholtz Zentrum München, Research Unit Comparative Microbiome Analysis, Neuherberg, Germany.
Technische Universität München, TUM School of Life Science, Chair of Environmental Microbiology, Freising, Germany.
Microb Ecol. 2023 Nov;86(4):2882-2893. doi: 10.1007/s00248-023-02285-9. Epub 2023 Aug 25.
Despite its enormous importance for ecosystem services, factors driving microbial recolonization of soils after disturbance are still poorly understood. Here, we compared the microbial recolonization patterns of a disturbed, autoclaved soil using different amounts of the original non-disturbed soil as inoculum. By using this approach, we manipulated microbial biomass, but did not change microbial diversity of the inoculum. We followed the development of a new soil microbiome after reinoculation over a period of 4 weeks using a molecular barcoding approach as well as qPCR. Focus was given on the assessment of bacteria and archaea. We could show that 1 week after inoculation in all inoculated treatments bacterial biomass exceeded the values from the original soil as a consequence of high dissolved organic carbon (DOC) concentrations in the disturbed soil resulting from the disturbance. This high biomass was persistent over the complete experimental period. In line with the high DOC concentrations, in the first 2 weeks of incubation, copiotrophic bacteria dominated the community, which derived from the inoculum used. Only in the disturbed control soils which did not receive a microbial inoculum, recolonization pattern differed. In contrast, archaeal biomass did not recover over the experimental period and recolonization was strongly triggered by amount of inoculated original soil added. Interestingly, the variability between replicates of the same inoculation density decreased with increasing biomass in the inoculum, indicating a deterministic development of soil microbiomes if higher numbers of cells are used for reinoculation.
尽管微生物对生态系统服务具有巨大的重要性,但驱动土壤受扰后微生物再定植的因素仍知之甚少。在这里,我们比较了使用不同数量原始未受扰土壤作为接种物的受扰、高压灭菌土壤的微生物再定植模式。通过这种方法,我们操纵了微生物生物量,但没有改变接种物的微生物多样性。我们使用分子条形码方法和 qPCR 来跟踪再接种后 4 周内新土壤微生物组的发展。重点评估了细菌和古菌。我们可以表明,在接种后 1 周,所有接种处理的细菌生物量都由于受扰土壤中高溶解性有机碳(DOC)浓度而超过原始土壤的值,这种高生物量在整个实验期间持续存在。与高 DOC 浓度一致,在孵育的前 2 周,来自接种物的富营养型细菌主导了群落。只有在未接收微生物接种物的受扰对照土壤中,再定植模式才有所不同。相比之下,古菌生物量在实验期间并未恢复,并且再定植受到添加的原始接种土壤数量的强烈触发。有趣的是,相同接种密度的重复之间的变异性随着接种物中生物量的增加而降低,这表明如果使用更多数量的细胞进行再接种,土壤微生物组的发展具有确定性。