Boessenkool Sanne, McGlynn Gayle, Epp Laura S, Taylor David, Pimentel Manuel, Gizaw Abel, Nemomissa Sileshi, Brochmann Christian, Popp Magnus
National Centre for Biosystematics, Natural History Museum, University of Oslo, P.O. Box 1172, Blindern, NO-0318, Oslo, Norway.
Conserv Biol. 2014 Apr;28(2):446-55. doi: 10.1111/cobi.12195. Epub 2013 Dec 26.
Conservation of biodiversity may in the future increasingly depend upon the availability of scientific information to set suitable restoration targets. In traditional paleoecology, sediment-based pollen provides a means to define preanthropogenic impact conditions, but problems in establishing the exact provenance and ecologically meaningful levels of taxonomic resolution of the evidence are limiting. We explored the extent to which the use of sedimentary ancient DNA (sedaDNA) may complement pollen data in reconstructing past alpine environments in the tropics. We constructed a record of afro-alpine plants retrieved from DNA preserved in sediment cores from 2 volcanic crater sites in the Albertine Rift, eastern Africa. The record extended well beyond the onset of substantial anthropogenic effects on tropical mountains. To ensure high-quality taxonomic inference from the sedaDNA sequences, we built an extensive DNA reference library covering the majority of the afro-alpine flora, by sequencing DNA from taxonomically verified specimens. Comparisons with pollen records from the same sediment cores showed that plant diversity recovered with sedaDNA improved vegetation reconstructions based on pollen records by revealing both additional taxa and providing increased taxonomic resolution. Furthermore, combining the 2 measures assisted in distinguishing vegetation change at different geographic scales; sedaDNA almost exclusively reflects local vegetation, whereas pollen can potentially originate from a wide area that in highlands in particular can span several ecozones. Our results suggest that sedaDNA may provide information on restoration targets and the nature and magnitude of human-induced environmental changes, including in high conservation priority, biodiversity hotspots, where understanding of preanthropogenic impact (or reference) conditions is highly limited.
生物多样性的保护未来可能越来越依赖于获取科学信息以设定合适的恢复目标。在传统古生态学中,基于沉积物的花粉提供了一种界定人类活动前影响条件的方法,但在确定证据的确切来源以及具有生态意义的分类分辨率水平方面存在问题,限制了其应用。我们探讨了利用沉积古DNA(sedaDNA)在重建热带地区过去高山环境中补充花粉数据的程度。我们构建了一份从东非艾伯丁裂谷两个火山口遗址沉积物岩芯中保存的DNA中检索到的非洲高山植物记录。该记录远远超出了人类对热带山区产生重大影响的起始时间。为了确保从sedaDNA序列进行高质量的分类推断,我们通过对经分类验证的标本进行DNA测序,建立了一个涵盖大部分非洲高山植物区系的广泛DNA参考文库。与来自相同沉积物岩芯的花粉记录进行比较表明,利用sedaDNA恢复的植物多样性通过揭示更多分类群并提供更高的分类分辨率,改进了基于花粉记录的植被重建。此外,将这两种方法结合有助于区分不同地理尺度上的植被变化;sedaDNA几乎只反映当地植被,而花粉可能来自广泛区域,特别是在高地,可能跨越几个生态区。我们的结果表明,sedaDNA可能提供有关恢复目标以及人类引起的环境变化的性质和程度的信息,包括在高度优先保护的生物多样性热点地区,在这些地区,对人类活动前影响(或参考)条件的了解非常有限。