Department of Biology, Washington College, Chestertown, Maryland, USA.
Department of Ecology and Evolutionary Biology, University of Michigan, Ann Arbor, Michigan, USA.
Ecology. 2022 Apr;103(4):e3656. doi: 10.1002/ecy.3656. Epub 2022 Mar 3.
Interactions between plants and soil microbes influence plant nutrient transformations, including nitrogen (N) fixation, nutrient mineralization, and resource exchanges through fungal networks. Physical disturbances to soils can disrupt soil microbes and associated processes that support plant and microbial productivity. In low resource drylands, biological soil crusts ("biocrusts") occupy surface soils and house key autotrophic and diazotrophic bacteria, non-vascular plants, or lichens. Interactions among biocrusts, plants, and fungal networks between them are hypothesized to drive carbon and nutrient dynamics; however, comparisons across ecosystems are needed to generalize how soil disturbances alter microbial communities and their contributions to N pools and transformations. To evaluate linkages among plants, fungi, and biocrusts, we disturbed all unvegetated surfaces with human foot trampling twice yearly from 2013-2019 in dry conditions in cyanobacteria-dominated biocrusts in the Chihuahuan Desert grassland and shrubland ecosystems. After 5 years, disturbance decreased the abundances of cyanobacteria (especially Microcoleus steenstrupii clade) and N-fixers (Scytonema sp., and Schizothrix sp.) by >77% and chlorophyll a by up to 55% but, conversely, increased soil fungal abundance by 50% compared with controls. Responses of root-associated fungi differed between the two dominant plant species and ecosystem types, with a maximum of 80% more aseptate hyphae in disturbed than in control plots. Although disturbance did not affect N tracer transfer from biocrusts to the dominant grass, Bouteloua eriopoda, disturbance increased available soil N by 65% in the shrubland, and decreased leaf N of B. eriopoda by up to 16%, suggesting that, although rapid N transfer during peak production was not affected by disturbance, over the long-term plant nutrient content was disrupted. Altogether, the shrubland may be more resilient to detrimental changes due to disturbance than grassland, and these results demonstrated that disturbances to soil microbial communities have the potential to cause substantial changes in N pools by reducing and reordering biocrust taxa.
植物与土壤微生物之间的相互作用影响着植物养分的转化,包括氮(N)固定、养分矿化以及通过真菌网络进行的资源交换。土壤的物理干扰会破坏支持植物和微生物生产力的土壤微生物和相关过程。在资源匮乏的干旱地区,生物土壤结皮(“biocrusts”)占据着地表土壤,并且是关键的自养和固氮细菌、非维管束植物或地衣的栖息地。生物结皮、植物和它们之间的真菌网络之间的相互作用被假设为驱动碳和养分动态;然而,需要在不同的生态系统中进行比较,以概括土壤干扰如何改变微生物群落及其对 N 库和转化的贡献。为了评估植物、真菌和生物结皮之间的联系,我们在 2013 年至 2019 年期间,在以蓝藻为主的生物结皮覆盖的干旱条件下,每年两次用人类踩踏的方式干扰所有无植被的表面,这些结皮位于奇瓦瓦沙漠草原和灌木生态系统中。经过 5 年的干扰,与对照相比,干扰使蓝藻(尤其是 Microcoleus steenstrupii 组)和固氮生物(Scytonema sp. 和 Schizothrix sp.)的丰度减少了>77%,叶绿素 a 减少了高达 55%,但土壤真菌的丰度却增加了 50%。与对照相比,两种主要植物物种和生态系统类型的根相关真菌的反应不同,在受干扰的样地中,无菌丝的真菌菌丝增加了最多 80%。虽然干扰并没有影响 N 示踪剂从生物结皮到优势草种 Bouteloua eriopoda 的转移,但在灌木生态系统中,干扰增加了 65%的土壤可利用氮,B. eriopoda 的叶片氮含量最多减少了 16%,这表明,尽管在高峰期生产过程中快速的 N 转移不受干扰的影响,但从长期来看,植物的营养含量还是会受到干扰的破坏。总的来说,与草原相比,灌木可能对土壤微生物群落的干扰有更强的恢复能力,这些结果表明,土壤微生物群落的干扰有可能通过减少和重新排列生物结皮类群,导致 N 库发生重大变化。