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Late-Holocene expansion of a south Swedish peatland and its impact on marginal ecosystems: Evidence from dendrochronology, peat stratigraphy and palaeobotanical data

机译:瑞典南部泥炭地的晚全新世扩张及其对边缘生态系统的影响:来自树木年代学,泥炭地层学和古植物学数据的证据

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摘要

In this study, a reconstruction of the long-term development and lateral expansion of a south Swedish peat bog was performed using a multi-proxy approach, including dendrochronology, peat stratigraphy and macrofossil and pollen analyses. By combining mapping of cross-dated subfossil trees with radiocarbon-dated peat sequences, an improved approach to reconstruction of lateral peat expansion was applied. Apart from providing approximate ages of tree burial episodes, the ring-width records offer information on hydrological variations prior to the bog expansion. New bog oak, pine and alder chronologies are presented and their potential as a dating tool for peatland expansion as well as for local to regional environmental interpretations is examined. Our tree-replication records show that increased amounts of bog trees in the central parts can be linked to drier bog-surface conditions, whereas an increase in wood remains in the marginal zone is related to enhanced preservation due to lateral bog expansion. Our reconstructions of the development of the peat deposit and associated changes in the distribution of vegetation communities provide new insight into peatland responses to climate change at the end of the 'Holocene Thermal Maximum' (5000-4000 cal. yr BP).
机译:在这项研究中,瑞典南部泥炭沼泽的长期发展和横向扩展的重建采用了多种代理方法,包括树状年代学,泥炭地层学以及大型化石和花粉分析。通过结合跨日期的化石树与放射性碳日期泥炭序列的映射,应用了一种改进的方法来重建侧向泥炭膨胀。除了提供树木埋葬事件的大概年龄外,环宽记录还提供了沼泽扩展之前的水文变化信息。介绍了新的沼泽橡树,松树和al木的年代,并考察了它们作为泥炭地扩张以及当地到区域环境解释的约会工具的潜力。我们的树木复制记录表明,中部的沼泽树木数量增加可能与较干燥的沼泽地表状况有关,而边缘区域木材残留量的增加与横向沼泽扩张引起的保存增强有关。我们对泥炭矿床开发的重建以及植被群落分布的相关变化为“全新世热最大值”(5000-4000 cal.yr BP)结束时泥炭地对气候变化的响应提供了新的见解。

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