首页> 外文期刊>Biogeosciences >Sedimentary ancient DNA and pollen reveal the composition of plant organic matter in Late Quaternary permafrost sediments of the Buor Khaya Peninsula (north-eastern Siberia)
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Sedimentary ancient DNA and pollen reveal the composition of plant organic matter in Late Quaternary permafrost sediments of the Buor Khaya Peninsula (north-eastern Siberia)

机译:古老的沉积DNA和花粉揭示了Buor Khaya半岛(东北西伯利亚)第四纪多年冻土后期沉积物中的有机质组成。

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Organic matter deposited in ancient, ice-rich permafrost sediments is vulnerable to climate change and may contribute to the future release of greenhouse gases; it is thus important to get a better characterization of the plant organic matter within such sediments. From a Late Quaternary permafrost sediment core from the Buor Khaya Peninsula, we analysed plant-derived sedimentary ancient DNA (sedaDNA) to identify the taxonomic composition of plant organic matter, and undertook palynological analysis to assess the environmental conditions during deposition. Using sedaDNA, we identified 154 taxa and from pollen and non-pollen palynomorphs we identified 83 taxa. In the deposits dated between 54 and 51?kyr?BP, sedaDNA records a diverse low-centred polygon plant community including recurring aquatic pond vegetation while from the pollen record we infer terrestrial open-land vegetation with relatively dry environmental conditions at a regional scale. A fluctuating dominance of either terrestrial or swamp and aquatic taxa in both proxies allowed the local hydrological development of the polygon to be traced. In deposits dated between 11.4 and 9.7?kyr?BP (13.4–11.1?cal?kyr?BP), sedaDNA shows a taxonomic turnover to moist shrub tundra and a lower taxonomic richness compared to the older samples. Pollen also records a shrub tundra community, mostly seen as changes in relative proportions of the most dominant taxa, while a decrease in taxonomic richness was less pronounced compared to sedaDNA. Our results show the advantages of using sedaDNA in combination with palynological analyses when macrofossils are rarely preserved. The high resolution of the sedaDNA record provides a detailed picture of the taxonomic composition of plant-derived organic matter throughout the core, and palynological analyses prove valuable by allowing for inferences of regional environmental conditions.
机译:沉积在古老的,富含冰的多年冻土沉积物中的有机物易受气候变化的影响,并可能有助于将来释放温室气体;因此,重要的是要更好地表征此类沉积物中的植物有机质。从Buor Khaya半岛的晚第四纪多年冻土沉积岩心中,我们分析了植物来源的古代沉积DNA(sedaDNA),以识别植物有机物的分类学组成,并进行了孢粉学分析以评估沉积过程中的环境条件。使用sedaDNA,我们鉴定出154个分类单元,并从花粉和非花粉的palynomorphs中鉴定出83个分类单元。在日期为54至51?kyr?BP的矿床中,sedaDNA记录了一个多样化的低中心多边形植物群落,包括周期性的水生池塘植被,而从花粉记录中我们推断出一个区域规模相对干燥的环境条件下的陆地开阔地植被。两个代理中陆地或沼泽和水生生物类群的波动优势使得可以追踪多边形的当地水文发展。在日期为11.4至9.7?kyr?BP(13.4-11.1?cal?kyr?BP)的沉积物中,sedaDNA显示出与湿润灌木冻原的分类学周转率,并且比较早的样本具有较低的分类学丰富度。花粉还记录了一个灌木苔原群落,主要被看作是最主要的分类单元的相对比例的变化,而与sedaDNA相比,分类学丰富度的降低并不那么明显。我们的结果表明,在很少保存大型化石的情况下,将sedaDNA与昆虫学分析结合使用的优势。 sedaDNA记录的高分辨率提供了整个核心植物来源有机物的分类学组成的详细图片,并且通过进行区域环境条件的推断,孢粉学分析证明是有价值的。

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