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Archaeobotanical evidence for climate as a driver of ecological community change across the anthropocene boundary

机译:气候作为人类群落界线中生态群落变化驱动力的考古学证据

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摘要

The biodiversity response to climate change is a major focus in conservation research and policy. Predictive models that are used to project the impact of climate change scenarios - such as bioclimatic envelope models - are widely applied and have come under severe scrutiny. Criticisms of such models have focussed on at least two problems. First, there is an assumption that climate is the primary driver of observed species distributions ('climatic equilibrium'), when other biogeographical controls are often reliably established. Second, a species' sensitivity to macroclimate may become less relevant when impacts are down-scaled to a local level, incorporating a modifying effect of species interactions structuring communities. This article examines the role of different drivers (climate, pollution and landscape habitat structure) in explaining spatial community variation for a widely applied bioindicator group: lichen epiphytes. To provide an analysis free of 'legacy effects' (e. g. formerly higher pollution loads), the study focused on hazel stems as a relatively short-lived and recently colonized substratum. For communities during the present day, climate is shown to interact with stem size/age as the most likely explanation of community composition, thus coupling a macroclimatic and community-scale effect. The position of present-day communities was projected into ordination space for eight sites in England and compared to the position of historical epiphyte communities from the same sites, reconstructed using preserved hazel wattles dating mainly to the 16th Century. This comparison of community structure for the late-to post-Mediaeval period, with the post-Industrial period, demonstrated a consistent shift among independent sites towards warmer and drier conditions, concurrent with the end of the Little Ice Age. Long-term temporal sensitivity of epiphyte communities to climate variation thus complements spatial community patterns. If more widely applied, preserved lichen epiphytes have potential to generate new baseline conditions of environment and biodiversity for preindustrial lowland Europe
机译:生物多样性对气候变化的反应是保护研究和政策的主要重点。用于预测气候变化情景影响的预测模型(例如生物气候覆盖模型)已得到广泛应用,并受到了严格的审查。对这种模型的批评至少集中在两个问题上。首先,假设通常可靠建立其他生物地理控制措施时,气候是观测物种分布(“气候平衡”)的主要驱动力。第二,当将影响降低到局部水平时,物种对大气候的敏感性可能会变得不那么重要,并结合了物种相互作用构造社区的影响。本文探讨了不同驱动因素(气候,污染和景观栖息地结构)在解释广泛应用的生物指示剂组:地衣附生植物的空间群落变异中的作用。为了提供没有“遗留效应”(例如以前较高的污染负荷)的分析,该研究集中于榛树茎,其是相对短暂的并且最近定殖的基质。对于当今的社区而言,气候与茎的大小/年龄相互作用是最可能的解释,它是社区组成的最可能的解释,因此结合了宏观气候和社区规模效应。将当今社区的位置投影到英格兰八个地点的协调空间中,并将其与同一地点的历史附生群落的位置进行比较,这些地点是使用保存于16世纪的榛树来重建的。中世纪后期至后期与工业化后时期的社区结构比较表明,在小冰期结束的同时,独立站点之间向温暖和干燥条件的转变是一致的。因此,附生植物群落对气候变化的长期时间敏感性补充了空间群落的格局。如果更广泛地应用,保存的地衣附生植物有可能为工业化前低地欧洲创造新的环境和生物多样性基准条件

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