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A long‐term field experiment of soil transplantation demonstrating the role of contemporary geographic separation in shaping soil microbial community structure

机译:土壤移植的长期野外实验证明了当代地理分离在塑造土壤微生物群落结构中的作用

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AbstractThe spatial patterns of microbial communities are largely determined by the combined effects of historical contingencies and contemporary environmental disturbances, but their relative importance remains poorly understood. Empirical biogeographic data currently available are mostly based on the traditional method of observational survey, which typically involves comparing indigenous microbial communities across spatial scales. Here, we report a long-term soil transplantation experiment, whereby the same two soils (red Acrisol and purple Cambisol from Yingtan) were placed into two geographic locations of ~1000 km apart (i.e., Yingtan in the mid-subtropical region and Fengqiu in warm-temperate region; both located in China). Twenty years after the transplantation, the resulting soil microbial communities were subject to high-throughput 454 pyrosequencing analysis of 16S and 18S rRNA genes. Additionally, bacteria and archaea involved in nitrogen cycling were estimated using clone library analysis of four genes: archaeal amoA, bacterial amoA, nirK, and nifH. Data of subsequent phylogenetic analysis show that bacteria, fungi, and other microbial eukaryotes, as well as the nitrogen cycling genes, are grouped primarily by the factor of geographic location rather than soil type. Moreover, a shift of microbial communities toward those in local soil (i.e., Chao soil in Fengqiu) has been observed. The results thus suggest that the historical effects persistent in the soil microbial communities can be largely erased by contemporary disturbance within a short period of 20 years, implicating weak effects of historical contingencies on the structure and composition of microbial communities in the soil.
机译:摘要微生物群落的空间格局在很大程度上取决于历史偶然事件和当代环境干扰的综合作用,但对它们的相对重要性仍然知之甚少。当前可获得的经验生物地理数据主要基于传统的观察调查方法,该方法通常涉及在空间尺度上比较土著微生物群落。在这里,我们报告了一项长期的土壤移植实验,其中将相同的两种土壤(来自鹰潭的红色阿克里斯索和紫色坎比索)放置在相距约1000公里的两个地理位置(即亚热带中部的鹰潭和南亚的封丘)温带地区;均位于中国)。移植二十年后,对所得土壤微生物群落进行了16S和18S rRNA基因的高通量454焦磷酸测序分析。此外,使用四个基因的克隆文库分析来估计参与氮循环的细菌和古细菌:古细菌amoA,细菌amoA,nirK和nifH。随后的系统发育分析数据表明,细菌,真菌和其他微生物真核生物以及氮循环基因主要根据地理位置而不是土壤类型进行分组。此外,已经观察到微生物群落向局部土壤(即,封丘的潮土)迁移。因此,结果表明,在短短20年内,当代的干扰可以大大消除土壤微生物群落中持久的历史影响,这意味着历史偶然性对土壤微生物群落的结构和组成的影响较弱。

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