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Alpine Biological Soil Crusts in theWashington North Cascades: a Distribution Study at Select Sites Across a Precipitation Gradient.

机译:华盛顿北部小瀑布的高山生物土壤结壳:跨降水梯度在特定地点的分布研究。

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摘要

One of the least researched phenomena within the alpine regions of mountain biomes is the combination of primitive plants, algae, fungi, and lichens that are generally referred to as biological soil crusts. Sites containing well-developed biological soil crusts were examined in a variety of alpine, non-forested, vegetated landscapes in the North Cascade Mountains of Washington, USA. For each site, data were recorded for percent ground cover of biological soil crusts, slope aspect, and slope gradient of the terrain where the crust communities were located. For all of the sites, biological soil crusts were common, with a percent ground cover median of 29% and a range of 11% to 73%. The arrangement of the biological soil crusts on all sites was quite similar: all were clumped, as opposed to single, and random, as opposed to uniform. All of the soil crusts were found on soil exposed to direct sunlight. Few, if any, crusts were found in the shade of heavy forbs, or forest, or under accumulations of organic litter. When biological soil crusts were found associated with higher-order vegetation, it was with sparse graminoids, ericaceous woody shrubs, and stunted or krummholz Pinaceae trees. The biological soil crusts from this study exist on all locally undisturbed soil slope-gradients from 0% to almost 100%, and occurred on all aspects except for those in the Southwest quadrant. This study contains an extended literature review for desert and high latitude circumpolar crusts, as well as alpine biological soil crusts. Studies of biological soil crusts in subalpine and alpine environments are not common; it is hoped that this study will stimulate more research interest in these often overlooked pioneer biotic communities.
机译:在高山生物群落的高山区域内,研究最少的现象之一是原始植物,藻类,真菌和地衣的组合,这些植物通常被称为生物土壤结皮。在美国华盛顿州北喀斯喀特山脉的各种高山,非森林,植被繁茂的景观中,研究了含有发育良好的生物土壤结皮的场地。对于每个站点,记录的数据包括生物土壤结皮的地面覆盖百分比,坡度和结皮群落所在地形的坡度。在所有地点,生物土壤结皮都很常见,地面覆盖率中位数为29%,范围在11%至73%之间。在所有地点,生物土壤结皮的排列都非常相似:全部都是成团的,而不是单一的,是随机的,而不是均匀的。在暴露于直射阳光下的土壤中发现了所有的土壤结皮。在厚重的前叉,森林或有机垃圾堆积物的阴影下,几乎没有发现结壳。当发现生物土壤硬皮与高阶植被有关时,则是稀疏的类动物类动物,草木的灌木丛,矮化的或克鲁姆松的松科树木。这项研究中的生物土壤结皮存在于从0%到几乎100%的所有局部不受扰动的土壤坡度梯度上,并且除了西南象限的所有方面都存在。这项研究包含有关沙漠和高纬度旋极地壳以及高山生物土壤地壳的扩展文献综述。在亚高山和高山环境中对生物土壤结皮的研究并不普遍;希望这项研究将激发人们对这些经常被忽视的先锋生物群落的更多研究兴趣。

著录项

  • 作者

    Glenn, Steven W.;

  • 作者单位

    Prescott College.;

  • 授予单位 Prescott College.;
  • 学科 Ecology.;Soil sciences.;Environmental science.
  • 学位 Ph.D.
  • 年度 2015
  • 页码 99 p.
  • 总页数 99
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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