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The effect of tree mortality on biogeochemical response after mountain pine beetle forest infestation.

机译:树木死亡率对山地甲虫森林侵染后生物地球化学响应的影响。

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摘要

Pine species in the American West are experiencing large-scale, bark beetleinduced mortality in association with a changing climate. As resulting terrestrial biogeochemical responses to this ecosystem disturbance are unclear, we hypothesized that a threshold of localized tree mortality must be exceeded before disruption of carbon and nitrogen biogeochemical cycling is observed. In order to isolate the compensatory effects of proximal healthy trees and intertwined hydrologic, energetic and rhizospheric processes, microbiological and geochemical parameters within three near-surface soil horizons were contrasted between healthy and deceased lodgepole pines (Pinus contorta) surrounded by varying extents of tree mortality. Bark beetle impact altered N cycling, as an increased proportion of the total N pool was inorganic ammonium, as opposed to more stable and less mobile organic N, which dominates in healthy systems. This change in N cycling was dependent on the extent of surrounding tree mortality in the upper soil horizons, but not in the mineral soil. The different response in the upper and lower soil horizons is likely a reflection of how altered inputs after bark beetle infestation are different in each horizon. A threshold response in the upper horizons was found for ammonium, which accumulated only under trees surrounded by at least 40% tree mortality. The elevated ammonium response was associated with increased C recalcitrance and increased relative abundance of N. Concurrently, surrounding tree mortality also affected the soil bacterial community structure with associated increases in alpha diversity and overall community structure. However, functional processes tended to correlate better with changes in C:N ratio. Collectively, these biogeochemical and microbial indicators suggest that high degrees of beetle-induced mortality shift the terrestrial environment of Colorado Rocky Mountain lodgepole pine forests from an N-limited ecosystem to one where N is in excess.
机译:美国西部的松树物种正经历着大规模的,由树皮甲虫引起的死亡以及气候变化。由于对这种生态系统扰动产生的陆地生物地球化学反应尚不清楚,我们假设在观察到碳和氮生物地球化学循环破坏之前,必须超过局部树木死亡率的阈值。为了隔离近端健康树木和水文,能量和根际相互作用的补偿作用,对比了健康和已故的寄宿松(松树)周围三个不同地表土壤视野内的微生物和地球化学参数,这些松树被不同程度的树木死亡率包围。树皮甲虫的影响改变了氮的循环,因为在总氮库中增加的比例是无机铵,而在健康系统中占主导地位的是更稳定,流动性更弱的有机氮。氮循环的这种变化取决于上部土壤层中周围树木的死亡程度,而不取决于矿物土壤中树木的死亡率。上层和下层土壤层位的不同响应可能反映了树皮甲虫侵染后每个层位的输入变化如何不同。在较高的视野中发现了铵的阈值响应,铵仅在树木死亡率至少为40%的树木下积累。较高的铵盐响应与C的抗拒性增加和N的相对丰度增加有关。同时,周围树木的死亡也影响了土壤细菌群落结构,并伴随着α多样性和整体群落结构的增加。但是,功能过程倾向于与C:N比的变化更好地相关。总的来说,这些生物地球化学和微生物指标表明,甲虫引起的高度死亡将科罗拉多洛矶山黑松林的陆地环境从限氮生态系统转移到了氮过多的生态系统。

著录项

  • 作者

    Bokman, Chelsea M.;

  • 作者单位

    Colorado School of Mines.;

  • 授予单位 Colorado School of Mines.;
  • 学科 Biogeochemistry.;Climate change.;Forestry.
  • 学位 M.S.
  • 年度 2016
  • 页码 55 p.
  • 总页数 55
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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