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Effect of freshwater mussels on the vertical distribution of anaerobic ammonia oxidizers and other nitrogen-transforming microorganisms in upper Mississippi river sediment

机译:淡水贻贝对密西西比河上游沉积物中厌氧氨氧化剂和其他氮转化微生物的垂直分布的影响

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摘要

Targeted qPCR and non-targeted amplicon sequencing of 16S rRNA genes within sediment layers identified the anaerobic ammonium oxidation (anammox) niche and characterized microbial community changes attributable to freshwater mussels. Anammox bacteria were normally distributed (Shapiro-Wilk normality test, W-statistic =0.954, p = 0.773) between 1 and 15 cm depth and were increased by a factor of 2.2 (p < 0.001) at 3 cm below the water-sediment interface when mussels were present. Amplicon sequencing of sediment at depths relevant to mussel burrowing (3 and 5 cm) showed that mussel presence reduced observed species richness (p = 0.005), Chao1 diversity (p = 0.005), and Shannon diversity (p < 0.001), with more pronounced decreases at 5 cm depth. A non-metric, multidimensional scaling model showed that intersample microbial species diversity varied as a function of mussel presence, indicating that sediment below mussels harbored distinct microbial communities. Mussel presence corresponded with a 4-fold decrease in a majority of operational taxonomic units (OTUs) classified in the phyla Gemmatimonadetes, Actinobacteria, Acidobacteria, Plantomycetes, Chloroflexi, Firmicutes, Crenarcheota, and Verrucomicrobia. 38 OTUs in the phylum Nitrospirae were differentially abundant (p < 0.001) with mussels, resulting in an overall increase from 25% to 35%. Nitrogen (N)-cycle OTUs significantly impacted by mussels belonged to anammmox genus Candidatus Brocadia, ammonium oxidizing bacteria family Nitrosomonadaceae, ammonium oxidizing archaea genus Candidatus Nitrososphaera, nitrite oxidizing bacteria in genus Nitrospira, and nitrate- and nitrite-dependent anaerobic methane oxidizing organisms in the archaeal family “ANME-2d” and bacterial phylum “NC10”, respectively. Nitrosomonadaceae (0.9-fold (p < 0.001)) increased with mussels, while NC10 (2.1-fold (p < 0.001)), ANME-2d (1.8-fold (p < 0.001)), and Candidatus Nitrososphaera (1.5-fold (p < 0.001)) decreased with mussels. Co-occurrence of 2-fold increases in Candidatus Brocadia and Nitrospira in shallow sediments suggests that mussels may enhance microbial niches at the interface of oxic–anoxic conditions, presumably through biodeposition and burrowing. Furthermore, it is likely that the niches of Candidatus Nitrososphaera and nitrite- and nitrate-dependent anaerobic methane oxidizers were suppressed by mussel biodeposition and sediment aeration, as these phylotypes require low ammonium concentrations and anoxic conditions, respectively. As far as we know, this is the first study to characterize freshwater mussel impacts on microbial diversity and the vertical distribution of N-cycle microorganisms in upper Mississippi river sediment. These findings advance our understanding of ecosystem services provided by mussels and their impact on aquatic biogeochemical N-cycling.
机译:沉积层内16S rRNA基因的靶向qPCR和非靶向扩增子测序确定了厌氧铵氧化(anammox)生态位,并表征了淡水贻贝引起的微生物群落变化。 Anammox细菌呈正态分布(Shapiro-Wilk正态性检验,W统计= 0.954,p = 0.773)在1至15厘米深度之间,并在水-沉积物界面以下3厘米处增加2.2倍(p <0.001)当贻贝存在时。在与贻贝挖洞有关的深度(3和5 cm)处对沉积物进行扩增子测序表明,贻贝的存在降低了观察到的物种丰富度(p = 0.005),Chao1多样性(p = 0.005)和Shannon多样性(p <0.001),更明显在5厘米深度处减小。一个非度量的多维标度模型显示样本间微生物物种多样性随贻贝的存在而变化,这表明贻贝以下的沉积物具有独特的微生物群落。贻贝的存在对应于归类为双子叶植物门,放线菌,酸性细菌,植物菌,绿叶弯曲菌,Firmicutes,Crenarcheota和Verrucomicrobia的大多数操作分类单位(OTU)降低4倍。硝化螺菌门中的38个OTU有贻贝的差异丰富(p <0.001),导致总体从25%增至35%。受贻贝严重影响的氮(N)循环OTU属于溴化假丝酵母念珠菌属,铵氧化菌科亚硝菌,硝化古细菌念珠菌,亚硝化属亚硝酸盐氧化菌,硝化螺菌属和亚硝酸盐-亚硝酸盐菌古细菌家族“ ANME-2d”和细菌门“ NC10”。亚贻贝科(0.9倍(p <0.001))与贻贝一起增加,而NC10(2.1倍(p <0.001)),ANME-2d(1.8倍(p <0.001))和白色念珠菌(1.5倍(p p 0.001))随着贻贝而减少。浅底沉积物中的念珠菌和硝化螺旋藻共同出现2倍的增加表明,贻贝可能通过有氧沉积和穴居来增强有氧-缺氧条件下的微生物壁ni。此外,贻贝生物沉积法和沉积物通气法可能抑制了 Candidatus 亚硝化球菌的壁ni以及依赖于亚硝酸盐和硝酸盐的厌氧甲烷氧化剂,因为这些系统型分别需要低铵浓度和缺氧条件。据我们所知,这是第一项研究淡水贻贝对密西西比河上游沉积物中微生物多样性和N循环微生物垂直分布的影响的研究。这些发现提高了我们对贻贝提供的生态系统服务及其对水生生物地球化学氮循环的影响的理解。

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