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Reconstructing long-term human impacts on plant communities: an ecological approach based on lake sediment DNA

机译:重建人类对植物群落的长期影响:基于湖泊沉积物DNA的生态方法

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Paleoenvironmental studies are essential to understand biodiversity changes over long timescales and to assess the relative importance of anthropogenic and environmental factors. Sedimentary ancient DNA (sedaDNA) is an emerging tool in the field of paleoecology and has proven to be a complementary approach to the use of pollen and macroremains for investigating past community changes. SedaDNA-based reconstructions of ancient environments often rely on indicator taxa or expert knowledge, but quantitative ecological analyses might provide more objective information. Here, we analysed sedaDNA to investigate plant community trajectories in the catchment of a high-elevation lake in the Alps over the last 6400years. We combined data on past and present plant species assemblages along with sedimentological and geochemical records to assess the relative impact of human activities through pastoralism, and abiotic factors (temperature and soil evolution). Over the last 6400years, we identified significant variation in plant communities, mostly related to soil evolution and pastoral activities. An abrupt vegetational change corresponding to the establishment of an agropastoral landscape was detected during the Late Holocene, approximately 4500years ago, with the replacement of mountain forests and tall-herb communities by heathlands and grazed lands. Our results highlight the importance of anthropogenic activities in mountain areas for the long-term evolution of local plant assemblages. SedaDNA data, associated with other paleoenvironmental proxies and present plant assemblages, appear to be a relevant tool for reconstruction of plant cover history. Their integration, in conjunction with classical tools, offers interesting perspectives for a better understanding of long-term ecosystem dynamics under the influence of human-induced and environmental drivers.
机译:古环境研究对于了解长期生物多样性变化以及评估人为和环境因素的相对重要性至关重要。沉积古DNA(sedaDNA)是古生态领域中的一种新兴工具,并且已被证明是使用花粉和大块残留物调查过去群落变化的一种补充方法。基于SedaDNA的古代环境重建通常依赖于指标分类单元或专家知识,但是定量生态分析可能会提供更多客观信息。在这里,我们分析了sedaDNA,以调查过去6400年内阿尔卑斯山高海拔湖泊流域的植物群落轨迹。我们结合了过去和现在植物物种组合的数据以及沉积学和地球化学记录,以评估人类活动通过放牧和非生物因素(温度和土壤演变)的相对影响。在过去的6400年中,我们发现了植物群落的显着变化,主要与土壤演化和牧草活动有关。在全新世晚期(大约4500年前)发现了与农牧业景观建立相对应的突然的植被变化,并用荒地和牧场取代了山林和高草群落。我们的结果突出了山区的人为活动对于本地植物群落的长期进化的重要性。 SedaDNA数据与其他古环境代理和当前的植物组合相关,似乎是重建植物覆盖历史的重要工具。它们的结合以及经典工具的结合,提供了有趣的观点,可以更好地理解在人为和环境驱动因素的影响下的长期生态系统动态。

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