首页> 外文OA文献 >Fighting carbon loss of degraded peatlands by jump-starting ecosystem functioning with ecological restoration
【2h】

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

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

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。我们在芬兰选择了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C储存的长期影响是什么,ii)可以恢复生态系统功能(表层生长)和结构(植物) iii)是否恢复了生态系统功能所需的原始结构?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,当原始位置的可比短期速率为178.2 g m-2 yr-1(SE 13.3)时,再生表层以116.3 g m-2 yr-1(SE 12.7)的平均速率螯合C。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

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号