Coastal and Freshwater Group, Cawthron Institute, Nelson, New Zealand.
Victoria University of Wellington, Wellington, New Zealand.
PLoS One. 2021 May 3;16(5):e0250783. doi: 10.1371/journal.pone.0250783. eCollection 2021.
Lake sediments are natural archives that accumulate information on biological communities and their surrounding catchments. Paleolimnology has traditionally focussed on identifying fossilized organisms to reconstruct past environments. In the last decade, the application of molecular methodologies has increased in paleolimnological studies, but further research investigating factors such as sample heterogeneity and DNA degradation are required. In the present study we investigated bacterial community heterogeneity (16S rRNA metabarcoding) within depth slices (1-cm width). Sediment cores were collected from three lakes with differing sediment compositions. Samples were collected from a variety of depths which represent a period of time of approximately 1,200 years. Triplicate samples were collected from each depth slice and bacterial 16S rRNA metabarcoding was undertaken on each sample. Accumulation curves demonstrated that except for the deepest (oldest) slices, the combination of three replicate samples were insufficient to characterise the entire bacterial diversity. However, shared Amplicon Sequence Variants (ASVs) accounted for the majority of the reads in each depth slice (max. shared proportional read abundance 96%, 86%, 65% in the three lakes). Replicates within a depth slice generally clustered together in the Non-metric multidimensional scaling analysis. There was high community dissimilarity in older sediment in one of the cores, which was likely due to the laminae in the sediment core not being horizontal. Given that most paleolimnology studies explore broad scale shifts in community structure rather than seeking to identify rare species, this study demonstrates that a single sample is adequate to characterise shifts in dominant bacterial ASVs.
湖泊沉积物是自然档案,可积累有关生物群落及其周围集水区的信息。古湖沼学传统上专注于识别化石生物,以重建过去的环境。在过去的十年中,分子方法在古湖沼学研究中的应用有所增加,但需要进一步研究,例如调查样本异质性和 DNA 降解等因素。在本研究中,我们研究了不同沉积组成的三个湖泊中深度切片(1 厘米宽)内的细菌群落异质性(16S rRNA 代谢组学)。从三个具有不同沉积物组成的湖泊中采集沉积物岩芯。从各种深度采集样本,这些样本代表了大约 1200 年的时间段。从每个深度切片采集了三个重复样本,并对每个样本进行了细菌 16S rRNA 代谢组学分析。积累曲线表明,除了最深(最古老)的切片外,三个重复样本的组合不足以描述整个细菌多样性。但是,共享的扩增子序列变异(ASV)占每个深度切片中大部分读长(三个湖泊中最大共享比例读长丰度分别为 96%、86%和 65%)。深度切片内的重复样本通常在非度量多维尺度分析中聚类在一起。一个核心中的较老沉积物中的群落差异很大,这可能是由于沉积物岩芯中的层不是水平的。鉴于大多数古湖沼学研究探索群落结构的广泛变化,而不是试图识别稀有物种,因此本研究表明,单个样本足以描述主要细菌 ASV 的变化。