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Depth matters: effects of precipitation regime on soil microbial activity upon rewetting of a plant-soil system

机译:深度问题:植物-土壤系统再湿润后降水制度对土壤微生物活性的影响

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摘要

Changes in frequency and amplitude of rain events, that is, precipitation patterns, result in different water conditions with soil depth, and likely affect plant growth and shape plant and soil microbial activity. Here, we used 18O stable isotope probing (SIP) to investigate bacterial and fungal communities that actively grew or not upon rewetting, at three different depths in soil mesocosms previously subjected to frequent or infrequent watering for 12 weeks (equal total water input). Phylogenetic marker genes for bacteria and fungi were sequenced after rewetting, and plant-soil microbial coupling documented by plant 13C-CO2 labeling. Soil depth, rather than precipitation pattern, was most influential in shaping microbial response to rewetting, and had differential effects on active and inactive bacterial and fungal communities. After rewetting, active bacterial communities were less rich, more even and phylogenetically related than the inactive, and reactivated throughout the soil profile. Active fungal communities after rewetting were less abundant and rich than the inactive. The coupling between plants and soil microbes decreased under infrequent watering in the top soil layer. We suggest that differences in fungal and bacterial abundance and relative activity could result in large effects on subsequent soil biogeochemical cycling.
机译:降雨事件的频率和幅度的变化(即降水模式)导致土壤深度不同的水条件,并可能影响植物的生长以及植物和土壤微生物活动的形状。在这里,我们使用了 18 O稳定同位素探测(SIP),研究了在以前经历过频繁或不频繁浇水12周的土壤中膜的三种不同深度下,细菌和真菌群落在重新润湿后是否活跃生长。 (等于总水输入量)。重新润湿后,对细菌和真菌的系统发生标记基因进行测序,并通过植物 13 C-CO2标记记录植物-土壤微生物的耦合。土壤深度而不是降水模式对塑造微生物对再润湿的反应影响最大,并且对活跃和不活跃的细菌和真菌群落具有不同的影响。重新湿润后,活跃的细菌群落比不活跃的细菌群落更少,更均匀,与系统发育相关,并且在整个土壤剖面中都被重新激活。重新润湿后的活跃真菌群落比不活跃的真菌群落丰富和丰富。在表层土壤不经常浇水的情况下,植物与土壤微生物之间的耦合降低。我们建议真菌和细菌丰度和相对活性的差异可能会对随后的土壤生物地球化学循环产生重大影响。

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