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Survival and colonisation potential of photoautotrophic microorganisms within a glacierised catchment on Svalbard, High Arctic

机译:高北极地区斯瓦尔巴特群岛冰川集水区中光合自养微生物的存活和定殖潜力

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摘要

The survival and colonisation potential of photoautotrophic microbes (cyanobacteria and microalgae) were investigated in three terrestrial environments within a glacierised catchment on Svalbard: old vegetation-covered soil, recently deglaciated barren soil and subglacial sediments. One-year reciprocal transplant incubations of photoautotrophic microbial communities from the three soil/ sediment environments were conducted in order to reveal the autochthonous or allochthonous origin of the present photoautotrophs. The abundance and taxonomic composition of photoautotrophic microbes and their changes over time and between soil/sediment types and physico-chemical characteristics of the soils/sediments were determined. The recovery time of a photoautotrophic community by import of cells was between several months in subglacial and vegetated soils and up to 27 years in proglacial soils. No active growth was recorded in subglacial sediments, whilst positive growth, and so the potential for autochthonous recovery, was found in proglacial and vegetated soils. The most suitable environment for the survival of transplanted microbes was provided in proglacial soil. Wernshow here that the new proglacial substrata can be successfully colonised by photoautotrophic microbes, and that input of allochthonous cells may, in some cases, exceed in situ microbial growth. Whilst the subglacial environment is rather a conduit for photoautotrophic microbes than a place of growth and production, the supply of viable photoautotrophs in it is relatively high and may serve as a significant resource of nutrients for subglacial microbial communities.
机译:在斯瓦尔巴特群岛冰川集水区的三个陆地环境中,研究了光合自养微生物(蓝细菌和微藻)的存活和定殖潜力:老植被覆盖的土壤,最近冰川消融的贫瘠土壤和冰下沉积物。为了揭示本光合自养生物的自生或异源起源,对来自三种土壤/沉积物环境的光合自养微生物群落进行了为期一年的相互移植培养。确定了光合自养微生物的丰度和分类学组成,以及它们随时间以及土壤/沉积物类型与土壤/沉积物的理化特性之间的变化。通过输入细胞,光自养群落的恢复时间在冰下和植被土壤中要花费几个月,而在冰原土壤中要长达27年。在冰川下的沉积物中没有记录到活跃的生长,而在正面的生长中,则发现了正增长,因此在冰川覆盖的和植被覆盖的土壤中发现了土体恢复的潜力。在冰原土壤中提供了最适合移植微生物生存的环境。 Wernshow在此表示,新的泌乳基层可以被光合自养微生物成功定殖,在某些情况下,异源细胞的输入可能会超过原位微生物的生长。尽管冰下环境是光合自养微生物的通道,而不是生长和生产的场所,但其中的存活光合自养生物的供应相对较高,可以作为冰川下微生物群落的重要营养资源。

著录项

  • 来源
    《Polar biology》 |2010年第6期|737-745|共9页
  • 作者单位

    Institute of Botany, Czech Academy of Sciences, Dukelska 135, Trebon 379 82, Czech Republic;

    Institute of Botany, Czech Academy of Sciences, Dukelska 135, Trebon 379 82, Czech Republic Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol, UK;

    Institute of Botany, Czech Academy of Sciences, Dukelska 135, Trebon 379 82, Czech Republic Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, USA;

    Speleo-Rehak, Semily, Czech Republic;

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

    colonisation; photoautotrophic microorganisms; arctic; soil; transplant experiment; svalbard;

    机译:殖民光合自养微生物;北极;泥;移植实验;斯瓦尔巴特群岛;

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