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Resilience of plant and testate amoeba communities after climatic and anthropogenic disturbances in a Baltic bog in Northern Poland: Implications for ecological restoration

机译:在波兰北部的波罗的海沼泽中,气候和人为干扰后植物和睾丸变形虫的恢复力:对生态恢复的影响

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摘要

This study explores the history of the development of Sphagnum communities in an ombrotrophic peatland - Bagno Kusowo - over the past 650years, based on high-resolution plant macrofossil and testate amoebae analysis. Our research provided information related to the length of peatland existence and the characteristics of its natural/pristine state before the most recent human impacts. Changes in the Sphagnum communities before human impact could have resulted from climate cooling during the Little Ice Age' (LIA). In this cold and unstable hydrological period, among vascular plants, Eriophorum vaginatum and Baeothryon caespitosum dominated in the peatland vegetation. Peat-forming Sphagnum communities survived the drainage conducted during the 20th century at the Bagno Kusowo bog. We provide three important messages through this study: (1) testate amoebae reflect similar hydrological trends in two peat cores despite considerable microhabitat variability, (2) average long-term water level 10cm below the surface should be a target for active bog conservation and (3) sites like Bagno Kusowo are extremely important to preserve the remains of pristine biodiversity (including genetic diversity of plants and protists) that was completely removed from most of the raised bogs in Europe due to human activities, for example, drainage.
机译:这项研究基于高分辨率的植物化石和有遗迹的变形虫分析,探索了过去650年的营养养护泥炭地-Bagno Kusowo泥炭藓群落的发展历史。我们的研究提供了有关泥炭地的存在时间及其在最近的人类影响之前的自然/原始状态特征的信息。小冰河时代”(LIA)的气候变冷可能导致人为影响之前,泥炭藓群落的变化。在这个寒冷而不稳定的水文时期,脉管植物中,泥炭地植被中占主导地位的是阴道Eriophorumtumum和Baeothryon caespitosum。形成泥炭的泥炭藓群落在20世纪Bagno Kusowo沼泽进行的排水中幸存下来。在这项研究中,我们提供了三个重要信息:(1)尽管微生境差异很大,但遗留的遗留物在两个泥炭岩心中反映出相似的水文趋势;(2)地表以下10cm处的长期平均水位应作为主动保护沼泽的目标;( 3)Bagno Kusowo之类的遗址对于保护原始生物多样性(包括植物和原生生物的遗传多样性)的遗迹极为重要,该遗留由于人类活动(例如排水)而被从欧洲大部分抬高的沼泽中完全清除。

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