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Fighting carbon loss of degraded peatlands by jump-starting ecosystem functioning with ecological restoration

机译:通过启动生态系统功能和生态恢复来应对退化泥炭地的碳损失

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摘要

Degradation of ecosystems is a great concern on the maintenance of biodiversity and ecosystem services. Ecological restoration fights degradation aiming at the recovery of ecosystem functions such as carbon (C) sequestration and ecosystem structures like plant communities responsible for the C sequestration function. We selected 38 pristine, drained and restored boreal peatland sites in Finland and asked ⅰ) what is the long-term effect of drainage on the peatland surface layer C storage, ⅱ) can restoration recover ecosystem functioning (surface layer growth) and structure (plant community composition) and ⅲ) is the recovery of the original structure needed for the recovery of ecosystem functions? We found that drainage had resulted in a substantial net loss of C from surface layer of drained sites. Restoration was successful in regaining natural growth rate in the peatland surface layer already within 5 years after restoration. However, the regenerated surface layer sequestered C at a mean rate of 116.3 g m~(-2) yr~(-1) (SE 12.7), when a comparable short-term rate was 178.2 g m~(-2) yr~(-1) (SE 13.3) at the pristine sites. The plant community compositions of the restored sites were considerably dissimilar to those of pristine sites still 10 years after restoration. We conclude that ecological restoration can be used to jump-start some key peatland ecosystem functions even without the recovery of original ecosystem structure (plant community composition). However, the re-establishment of other functions like C sequestration may require more profound recovery of conditions and ecosystem structure. We discuss the potential economic value of restored peatland ecosystems from the perspective of their C sequestration function.
机译:生态系统的退化是维护生物多样性和生态系统服务的重大关切。生态恢复与退化作斗争,旨在恢复诸如碳(C)隔离的生态系统功能和负责C隔离功能的植物群落等生态系统结构。我们选择了芬兰的38个原始,排水和恢复的北方泥炭地,并询问ⅰ)排水对泥炭表层碳储量的长期影响是什么,ⅱ)可以恢复生态系统功能(表层生长)和结构(植物)社区组成)和ⅲ)是恢复生态系统功能所需的原始结构吗?我们发现,排水导致排水站点表层的碳大量净损失。在恢复后的5年内,恢复成功地恢复了泥炭表层的自然生长率。然而,当可比较的短期速率为178.2 gm〜(-2)yr〜(-)时,再生的表层以116.3 gm〜(-2)yr〜(-1)的平均速率螯合C(SE 12.7)。 1)(SE 13.3)在原始位置。恢复的地点的植物群落组成与恢复10年后的原始地点的植物群落组成明显不同。我们得出的结论是,即使不恢复原始生态系统结构(植物群落组成),生态恢复也可以用于启动一些重要的泥炭地生态系统功能。但是,重新建立诸如碳封存等其他功能可能需要更深刻地恢复条件和生态系统结构。我们从固碳功能的角度讨论了恢复的泥炭地生态系统的潜在经济价值。

著录项

  • 来源
    《The Science of the Total Environment》 |2015年第15期|268-276|共9页
  • 作者单位

    University of Jyvaeskylae, Department of Biological and Environmental Science, P.O. Box 35, 40014, Finland,Metsaehallitus, Parks and Wildlife Finland, P.O. Box 36, 40101 Jyvaeskylae, Finland;

    University of Jyvaeskylae, Department of Biological and Environmental Science, P.O. Box 35, 40014, Finland,Metsaehallitus, Parks and Wildlife Finland, P.O. Box 36, 40101 Jyvaeskylae, Finland;

    University of Jyvaeskylae, Department of Biological and Environmental Science, P.O. Box 35, 40014, Finland,Metsaehallitus, Parks and Wildlife Finland, P.O. Box 8016, 96101 Rovaniemi, Finland;

    University of Jyvaeskylae, Department of Chemistry, P.O. Box 35, 40014, Finland;

    University of Eastern Finland, Department of Biology, P.O. Box 111, 80101 Joensuu, Finland;

    University of Jyvaeskylae, Department of Biological and Environmental Science, P.O. Box 35, 40014, Finland,Natural History Museum, University of Jyvaeskylae, P.O. Box 35, 40014, Finland;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Carbon sequestration; Plant community composition; Ecosystem degradation; Ecosystem recovery; Ecosystem structure-function relationship; Peat;

    机译:碳汇;植物群落组成;生态系统退化;生态系统恢复;生态系统结构-功能关系;泥炭;

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