首页> 外文期刊>Biology and fertility of soils: Cooperating Journal of the International Society of Soil Science >Soil pH and plant diversity drive co-occurrence patterns of ammonia and nitrite oxidizer in soils from forest ecosystems
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Soil pH and plant diversity drive co-occurrence patterns of ammonia and nitrite oxidizer in soils from forest ecosystems

机译:森林生态系统土壤中氨和亚硝酸盐氧化剂的土壤pH与植物多样性促进

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In this study, we investigated how co-occurrence patters of ammonia and nitrite oxidizers, which drive autotrophic nitrification, are influenced by tree species composition as well as soil pH in different forest soils. We expected that a decline of ammonia oxidizers in coniferous forests, as a result of excreted nitrification inhibitors and at acidic sites with low availability of ammonia, would reduce the abundance of nitrite-oxidizing bacteria (NOB). To detect shifts in co-occurrence patterns, the abundance of key players was measured at 50 forest plots with coniferous respectively deciduous vegetation and different soil pH levels in the region Schwabische Alb (Germany). We found ammonia-oxidizing archaea (AOA) and Nitrospira-like NOB (NS) to be dominating in numbers over their counterparts across all forest types. AOA co-occurred mostly with NS, while bacterial ammonia oxidizers (AOB) were correlated with Nitrobacter-like NOB (NB). Co-occurrence patterns changed from tight significant relationships of all ammonia and nitrite oxidizers in deciduous forests to a significant relationship of AOB and NB in coniferous forests, where AOA abundance was reduced. Surprisingly, no co-occurrence structures between ammonia and nitrite oxidizers could be determined at acidic sites, although abundances were correlated to the respective nitrogen pools. This raises the question whether interactions with heterotrophic nitrifiers may occur, which needs to be addressed in future studies.
机译:在这项研究中,我们研究了如何通过树种组成以及不同森林土壤中的土壤pH来影响氨和亚硝酸亚硝酸盐氧化剂的共同发生的平台和亚硝酸盐氧化剂。我们预计,由于排出的硝化抑制剂和具有低可用性氨的酸性部位,因此对针叶林氨氧化剂的下降将减少亚硝酸盐氧化细菌(NOB)的丰富。为了检测共同发生模式的变化,在50个森林地块中测量了关键球员的丰度,其中具有针叶树的落叶植被和不同土壤pH水平的施瓦布斯契(德国)。我们发现氨氧化archaea(AOA)和尼硝基类似的nob(ns)在所有森林类型的对应物上都以数量的数量支配。 AOA主要与NS一起发生,而细菌氨氧化剂(AOB)与氮杆菌的NOB(NB)相关。共同发生模式从落叶林中所有氨和亚硝酸盐氧化剂的紧张显着关系变为AOB和NB在针叶林中的显着关系,其中AOA丰度降低。令人惊讶的是,可以在酸性位点确定氨和亚硝酸盐氧化剂之间的共发生结构,但是与相应的氮气池相关的丰富。这提出了可能发生与异养硝化符的相互作用的问题,需要在未来的研究中解决。

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