首页> 外文学位 >Ecosystem consequences of forest fragmentation in the Pacific Northwest: Biogeochemical edge effects within old-growth forest remnants.
【24h】

Ecosystem consequences of forest fragmentation in the Pacific Northwest: Biogeochemical edge effects within old-growth forest remnants.

机译:西北太平洋地区森林破碎化的生态系统后果:旧森林残留物中的生物地球化学边缘效应。

获取原文
获取原文并翻译 | 示例

摘要

Possible mechanisms are presented for biogeochemical edge effects observed within oldgrowth Douglas-fir/western hemlock forests fragmented by timber harvests in the U.S. Pacific Northwest. In a systematic manner with distance into remnant forest, I tested the general hypothesis that edge-altered microclimate and structure initiate positive feedbacks linking abiotic and biotic responses. Mixed-effects statistical models and Spearman correlations were used to describe spatiotemporal patterns and interactions among these variables.; By modifying material and energy flows, structural changes near edges impact forest microclimate. I found reductions in cover and live-crown volume of plant canopies to be the most significant structural changes near edges. As evidenced by distance effects on basal area and relative importance, altered competition among dominant tree species may affect succession in edge environments. Extreme variability in temperature and reductions in both floor moisture and snow retention were the most notable microclimatic effects near forest edges. The results include significant negative correlations between tree live-crown volume and microclimatic variability. Relative to other forest types, the longer persistence of abiotic edge effects in north temperate coniferous forest may result from the tall stature and slow side-canopy closure of the long-lived tree species.; As identified in the conceptual model, the dynamics of soil organic matter at the soil-plant interface provide key information for understanding how abiotic effects influence basic biogeochemical processes near forest edges. I investigated mechanisms for edge effects on soil organic matter by focusing on the major above-ground fluxes of litter fall and decomposition. Reduced litter fall near edges appears largely due to depleted forest canopies. The interplay of microclimatic variability and the quantity and quality of the litter fall may be responsible for the more complex patterning of litter decomposition rates with distance into remnant forest. The decoupling of basic ecosystem processes near edges, including litter fall and decomposition, predicate the polymodal distance effects observed for biologically available nitrogen, uptake of nitrogen by plants, and forest productivity. These results indicate an accurate quantification of edge effects is required within fragmented forest landscapes, in order to assess the cumulative impact of land use on the processing of organic matter and nutrients important to ecosystem sustainability and conservation planning.
机译:提出了可能的机制,用于在美国太平洋西北部的古老生长的花旗松/西部铁杉林中观察到的生物地球化学边缘效应,这些森林因木材砍伐而破碎。我以系统的方式进入残留森林,并检验了一般假设,即边缘改变的微气候和结构会引发将非生物和生物反应联系起来的积极反馈。混合效应统计模型和Spearman相关性用于描述时空模式以及这些变量之间的相互作用。通过改变物质和能量流,边缘附近的结构变化会影响森林的小气候。我发现减少植物冠层的覆盖率和减少其活动量是边缘附近最显着的结构变化。距离对基础面积和相对重要性的影响证明,优势树种之间竞争的改变可能会影响边缘环境的演替。温度的极端可变性以及地板水分和积雪的减少都是森林边缘附近最明显的微气候影响。结果包括树木活冠量与微气候变异性之间的显着负相关。相对于其他森林类型,北温带针叶林中非生物边缘效应的持续存在时间较长,可能是由于长寿树种的身高较高且侧盖关闭较慢。正如在概念模型中确定的那样,土壤-植物界面的土壤有机质动态为了解非生物作用如何影响森林边缘附近的基本生物地球化学过程提供了关键信息。我通过关注凋落物掉落和分解的主要地上通量,研究了对土壤有机质的边缘效应机制。边缘附近的凋落物减少的现象在很大程度上归因于林冠层的枯竭。小气候变异性与凋落物下降的数量和质量之间的相互作用可能是导致凋落物分解速率随进入残留森林的距离而更复杂的模式。边缘附近的基本生态系统过程的解耦,包括凋落物的下落和分解,预测了生物可利用的氮,植物对氮的吸收以及森林生产力所观察到的多峰距离效应。这些结果表明,在零散的森林景观中需要对边缘效应进行准确的量化,以便评估土地利用对有机物质和营养素加工的累积影响,这对生态系统可持续性和保护规划很重要。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

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