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首页> 外文期刊>Hydrobiologia >Multiproxy study of anthropogenic and climatic changes in the last two millennia from a small mire in central Poland
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Multiproxy study of anthropogenic and climatic changes in the last two millennia from a small mire in central Poland

机译:最近两千年来波兰中部一个小泥潭的人为和气候变化的多代理研究

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摘要

The Żabieniec kettle hole is the first peatland in central Poland analyzed quantitatively with four biotic proxies (plant macrofossils, pollen, testate amoebae and chironomids) to reconstruct the past environmental change. Palaeoecological data were supported by historical and archaeological records. We focused on autogenic vegetation change and human impact in relation to climatic effects. The aims of our study were (a) to describe the development history of the mire during the last 2,000 years, (b) to date and reconstruct the anthropogenic land-use changes and (c) to discuss a possible climatic signal in the peat archive. The combination of proxies revealed dramatic shifts that took place in the peatland since the Roman Period. Żabieniec was a very wet telmatic habitat until ca. AD 600. Then, the water table declined, and the site transformed into a Sphagnum-dominated mire. This dry shift took place mainly during the Early Medieval Period. Human impact was gradually increasing, and it was particularly emphasized by deforestation since AD 1250 (beginning of the Late Medieval Period). Consequently, surface run-off and aeolian transport from the exposed soils caused the eutrophication of the mire. Furthermore, chironomids and testate amoebae reveal the beginning of a wet shift ca. AD 1350. Openness considerably increased in the Late Medieval and the Modern Periods. The highest water table during the last 1,000 years was recorded between AD 1500 and 1800. This wet event is connected with deforestation, but it could be also associated with the Little Ice Age. Our study shows plant succession in the Żabieniec peatland, which can be explained with the recent landscape transformation. However, such changes are also possibly linked with the major climatic episodes during the last two millennia, such as the Medieval Warm Period and the Little Ice Age. Keywords Central Poland - Kettle hole - Testate amoebae - Pollen - Macrofossils - Human impact - Climate - Environmental archaeology Guest editors: K. Buczkó, J. Korponai, J. Padisák & S. W. Starratt Palaeolimnological Proxies as Tools of Environmental Reconstruction in Fresh Water
机译:Żabieniec壶洞是波兰中部的第一个泥炭地,使用四种生物代理(植物大化石,花粉,睾丸变形虫和奇虫)进行定量分析,以重建过去的环境变化。历史和考古记录支持了古生态数据。我们关注与气候影响有关的自生植被变化和人类影响。我们研究的目的是(a)描述过去2000年泥潭的发展历史;(b)迄今为止并重建人为土地利用方式的变化;(c)讨论泥炭档案库中可能的气候信号。代理人的组合揭示了自罗马时代以来泥炭地发生的巨大变化。 Żabieniec是一个非常潮湿的遥远生境,直到大约公元前。公元600年。然后,地下水位下降,该地点变成了以泥炭藓为主的泥潭。这种干燥的转变主要发生在中世纪初期。自从公元1250年(中世纪晚期开始)以来,森林砍伐尤其突出了对人类的影响。因此,地表径流和来自裸露土壤的风沙运输导致泥潭富营养化。此外,尺虫和睾丸变形虫揭示了湿移的开始。公元1350年。开放性在中世纪晚期和现代时期大大增加。在公元1500年至1800年之间,记录了近1000年中最高的地下水位。这一湿事件与森林砍伐有关,但也可能与小冰期有关。我们的研究表明Żabieniec泥炭地植物的演替,可以用最近的景观改造来解释。但是,这样的变化也可能与最近两千年的主要气候事件有关,例如中世纪的暖期和小冰期。关键字波兰中部-壶孔-睾丸生物-花粉-大化石-人类影响-气候-环境考古客座编辑:K.Buczkó,J。Korponai,J。Padisák和S. W. Starratt古生物学代表作为淡水环境重建的工具

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