首页> 外文期刊>Soil Biology & Biochemistry >Bacterial communities in soil mimic patterns of vegetative succession and ecosystem climax but are resilient to change between seasons.
【24h】

Bacterial communities in soil mimic patterns of vegetative succession and ecosystem climax but are resilient to change between seasons.

机译:土壤中的细菌群落模拟了植物演替和生态系统高潮的模式,但可以适应季节之间的变化。

获取原文
获取原文并翻译 | 示例
           

摘要

Organism succession during ecosystem development has been researched for aboveground plant communities, however, the associated patterns of change in below-ground microbial communities are less described. In 2008, a study was initiated along a developmental sand-dune soil chronosequence bordering northern Lake Michigan near Wilderness Park (WP). It was hypothesized that soil bacterial communities would follow a pattern of change that is associated with soil, plant, and ecosystem development. This study included 5 replicate sites along 9 soils (n=45) ranging in age from ~105 to 4010 years since deposition. Soil bacterial community composition and diversity were studied using bacterial tag-encoded FLX amplicon pyrosequencing of the 16S rRNA gene. Bray-Curtis ordination indicated that bacterial community assembly changed along the developmental soil and plant gradient. The changes were not affected by seasonal differences, despite likely differences in plant root C (e.g. exudates), temperature, and water availability in soil. Soil base cations (Ca, Mg) and pH declined, showing log-linear correlations with soil age (r ~ 0.83, 0.84 and 0.81; P<0.01). Bacterial diversity (Simpson's 1/D) declined rapidly during the initial stages of soil development (~105-450 y) and thereafter (>450 y) did not change. Turnover of plant taxa was also more rapid early during ecosystem development and correlated with bacterial community structural change (P<0.000001; r=0.56). It is hypothesized that plants help to drive pedogenic change during early (<450 y) soil development (e.g. pH decline, cation leaching) which drive selection of soil bacterial communities. In mature soils (~450-4000 y), resilient and stable soil bacterial community structures developed, mimicking steady-state climax communities that were observed during latter stages of primary plant succession. These relationships point to possible feedbacks between plant and bacterial communities during ecosystem development.
机译:对于地上植物群落,已经研究了生态系统发展过程中的生物演替,但是,地下微生物群落的相关变化模式很少描述。 2008年,沿着密歇根湖北部荒野公园(WP)附近的发育沙丘土壤时间序列开始了一项研究。据推测,土壤细菌群落将遵循与土壤,植物和生态系统发展相关的变化模式。这项研究包括沿9个土壤(n = 45)分布的5个重复点,年龄从沉积开始约105至4010年。土壤细菌群落组成和多样性进行了研究,使用细菌标签编码的FLX扩增子焦磷酸测序的16S rRNA基因。 Bray-Curtis整理指示细菌群落组装随着发育土壤和植物梯度的变化而变化。尽管植物根系C(例如渗出液),温度和土壤中的水分利用率可能存在差异,但这些变化不受季节差异的影响。土壤基础阳离子(Ca,Mg)和pH下降,与土壤年龄呈对数线性相关性(r〜0.83、0.84和0.81; P <0.01)。在土壤发育的初始阶段(〜105-450 y),细菌多样性(Simpson's 1 / D)迅速下降,此后(> 450 y)没有变化。在生态系统发展的早期,植物类群的周转也更快,并且与细菌群落结构的变化相关(P <0.000001; r ​​= 0.56)。据推测,植物在土壤发育的早期(<450 y)(例如pH下降,阳离子浸出)过程中有助于推动土壤成因的变化,从而驱动土壤细菌群落的选择。在成熟的土壤(约450-4000 y)中,形成了有弹性且稳定的土壤细菌群落结构,模仿了在植物初生演替后期观察到的稳态高潮群落。这些关系指出了生态系统发展过程中植物和细菌群落之间可能的反馈。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号