Lan Shubin, Thomas Andrew D, Tooth Stephen, Wu Li, Elliott David R
Earth Surface Processes Research Group, Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth SY23 3DB, UK; Key Laboratory of Algal Biology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China.
Earth Surface Processes Research Group, Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth SY23 3DB, UK.
Sci Total Environ. 2021 Apr 10;764:142847. doi: 10.1016/j.scitotenv.2020.142847. Epub 2020 Oct 9.
Shrub encroachment is occurring in many of the world's drylands, but its impacts on ecosystem structure and function are still poorly understood. In particular, it remains unclear how shrub encroachment affects dryland soil surfaces, including biological soil crust (biocrust) communities. In this study, soil surfaces (0-1 cm depth) were sampled from areas of Grewia flava shrubs and Eragrostis lehmanniana and Schmidtia kalahariensis grasses in the southwest Kalahari during two different seasons (March and November). Our hypothesis is that the presence of different vegetation cover types (shrubs versus grasses) alters the microbial composition of soil surfaces owing to their contrasting microenvironments. The results showed that more significant differences in microclimate (light, soil surface temperatures) and soil surface microbial communities were observed between shrubs and grasses than between sampling seasons. Based on high-throughput 16S rRNA gene sequencing, our findings showed that approximately one third (33.5%) of the operational taxonomic units (OTUs) occurred exclusively in soil surfaces beneath shrubs. Soil surfaces with biocrusts in grass areas were dominated by the cyanobacteria Microcoleus steenstrupii, whereas the soil surfaces beneath shrubs were dominated by the proteobacteria Microvirga flocculans. Soil surfaces beneath shrubs are associated with reduced cyanobacterial abundance but have higher total carbon and total nitrogen contents compared to biocrusts in grass areas. These findings infer changes in the relative contributions from different sources of carbon and nitrogen (e.g. cyanobacterial and non-cyanobacterial fixation, plant litter, animal activity). The distinctive microbial composition and higher carbon and nitrogen contents in soil surfaces beneath shrubs may provide a positive feedback mechanism promoting shrub encroachment, which helps to explain why the phenomenon is commonly observed to be irreversible.
世界上许多旱地都出现了灌木入侵现象,但其对生态系统结构和功能的影响仍知之甚少。特别是,尚不清楚灌木入侵如何影响旱地土壤表面,包括生物土壤结皮(生物结皮)群落。在本研究中,于两个不同季节(3月和11月)从喀拉哈里沙漠西南部的黄花扁担杆灌木、长穗画眉草和卡拉哈里施密草区域采集了土壤表面(0-1厘米深度)样本。我们的假设是,不同植被覆盖类型(灌木与草本)的存在因其截然不同的微环境而改变了土壤表面的微生物组成。结果表明,灌木和草本之间在小气候(光照、土壤表面温度)和土壤表面微生物群落方面的差异比采样季节之间更为显著。基于高通量16S rRNA基因测序,我们的研究结果表明,约三分之一(33.5%)的可操作分类单元(OTU)仅出现在灌木下方的土壤表面。草地区域有生物结皮的土壤表面以蓝细菌斯氏微鞘藻为主,而灌木下方的土壤表面以变形菌门絮凝微小杆菌为主。与草地区域的生物结皮相比,灌木下方的土壤表面蓝细菌丰度降低,但总碳和总氮含量较高。这些发现推断了不同碳氮来源(如蓝细菌和非蓝细菌固氮、植物凋落物、动物活动)相对贡献的变化。灌木下方土壤表面独特的微生物组成以及较高的碳氮含量可能提供了一种促进灌木入侵的正反馈机制,这有助于解释为何通常观察到这种现象是不可逆的。