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首页> 外文期刊>The holocene >Disturbance and resilience of a Sphagnum peatland in western Russia (Western Dvina Lakeland) during the last 300 years: A multiproxy, high-resolution study
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Disturbance and resilience of a Sphagnum peatland in western Russia (Western Dvina Lakeland) during the last 300 years: A multiproxy, high-resolution study

机译:在过去的300年期间,俄罗斯西部(西德维纳州莱克兰州)的泥炭泥(Western Dvina Lakeland)的干扰和复原力:多分,高分辨率研究

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This paper presents the results of multiproxy research (pollen, charcoal, plant macrofossil and testate amoebae) on the biogenic deposits core from Gorodetsky Moch, an ombrotrophic peatland in western Russia (Western Dvina Lakeland). We reconstructed the impact of disturbance on peatland development in the last 300 years by using chronology of the records based on~(14)C and~(210)Pb data set. The multiproxy reconstruction was compared with changes in the land cover using historical maps and Corona images, which provides a unique spatial analysis of past ecological and land-use changes. We aimed to determine the effect of local disturbances (drainage) and land-use changes (landscape openness) on the development of the peatland during the last 300 years. Our study suggests that human activity had a crucial impact on the development of the peatland in the last centuries. The analysis of testate amoebae and plant macrofossils revealed a clear disturbed layer in the second half of the 20th century CE. Most probably, the drainage of the peatland triggered changes in the community of testate amoebae and plants, thereby causing a functional shift in Sphagnum peatland ecosystem. The hydrological stress and vegetation composition shift led to the collapse of mixotrophic testate amoebae. However, the peatland showed strong resilience and recovered toward the end of the 20th century CE and the beginning of the 21st century CE, despite the lower water table. Our study shows an example of the peatland ecosystem that experienced a considerable stress but finally sustained the former function.
机译:本文介绍了来自Gorodetsky Moch的生物沉积物核心,俄罗斯西部的令人幕府泥炭地生物沉积物(Pollen,木炭,植物大甲酰胺和睾丸Baoebae)的结果。我们通过使用基于〜(14)C和〜(210)PB数据集的记录的年代学,重建了在过去300年中对泥炭地发展的影响。使用历史地图和电晕图像与土地覆盖的变化进行了多分X重建,这提供了对过去生态和土地利用变化的独特空间分析。我们旨在确定当地扰动(排水)和土地利用变化(景观开放)在过去300年期间泥炭地发展的影响。我们的研究表明,人类活动对过去几个世纪对泥炭地发展的影响至关重要。睾丸Amoebae和植物大甲酸的分析显示了20世纪的下半年明确令人不安的层。最重要的是,泥炭地的排水引发了睾丸群和植物群落的变化,从而导致泥炭泥泥泥生态系统的功能转变。水文应激和植被组成转变导致混合营养睾丸的塌陷。然而,泥炭地表现出强烈的复原力,并恢复到20世纪末的CE和21世纪的初期,尽管水位桌。我们的研究显示了泥炭地生态系统的一个例子,其经历了相当大的压力,但最终持续了前职能。

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