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Controls on microalgal community structures in cryoconite holes uponhigh-Arctic glaciers, Svalbard

机译:斯瓦尔巴德对低温冰川孔的微藻群落结构对微藻群落结构进行控制

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Glaciers are known to harbor surprisingly complex ecosystems. On theirsurface, distinct cylindrical holes filled with meltwater and sediments areconsidered hot spots for microbial life. The present paper addressespossible biological interactions within the community of prokaryoticcyanobacteria and eukaryotic microalgae (microalgae) and relations to theirpotential grazers, such as tardigrades and rotifers, additional to theirenvironmental controls. Svalbard glaciers with substantial allochthonousinput of material from local sources reveal high microalgal densities. Smallvalley glaciers with high sediment coverages and high impact of birds showhigh biomasses and support a high biological diversity. Invertebrate grazerdensities do not show any significant negative correlation with microalgalabundances but rather a positive correlation with eukaryotic microalgae. Sharedenvironmental preferences and a positive effect of grazing are the proposedmechanisms to explain these correlations. Most microalgae found in this studyform colonies (?25?μm), whichmay protect them against invertebrate grazing. This finding rather indicatesgrazing as a positive control on eukaryotic microalgae by nutrient recycling.Density differences between the eukaryotic microalgae and prokaryoticcyanobacteria and their high distinction in redundancy (RDA) and principal component (PCA) analyses indicatethat these two groups are in strong contrast. Eukaryotic microalgae occurredmainly in unstable cryoconite holes with high sediment loads, high N?:?Pratios, and a high impact of nutrient input by bird guano, as a proxy fornutrients. In these environments autochthonous nitrogen fixation appears tobe negligible. Selective wind transport of Oscillatoriales via soil and dustparticles is proposed to explain their dominance in cryoconites further awayfrom the glacier margins. We propose that, for the studied glaciers, nutrientlevels related to recycling of limiting nutrients are the main factor drivingvariation in the community structure of microalgae and grazers.
机译:众所周知,冰川叫令人惊讶的复杂生态系统。在他们的脸上,填充熔融水和沉积物的独特圆柱孔,又是微生物寿命的热点。本文涉及原核细菌和真核微藻(微藻)群落内的生物相互作用以及与周转加剧的关系,如Tardirdes和Rotifers,其他环境控制。 Svalbard冰川具有来自本地来源的大量血管基因材料,揭示了高微观的密度。 Smallvalley冰川具有高沉积物覆盖范围和鸟类展示高影响的生物测量,并支持高生物多样性。无脊椎动物的格拉塞特不显示与微藻碱性的任何显着的负相关性,而是与真核微藻的正相关性。 Shareden环境的偏好和放牧的积极效果是解释这些相关性的拟议机制。在该研究中发现的大多数微藻(<?10个细胞,或>?25Ωμm),其中将它们保护它们免受无脊椎动物放牧。这种发现相当指出作为通过营养回收的真核微藻对真核微藻的阳性控制。在冗余(RDA)和主要成分(PCA)分析中,真核微藻和原核细菌的密度差异及其高分分析表明这两组具有强烈的对比度。真核微藻发生在不稳定的低温孔孔中,高沉积物负荷,高N?:?PRATIOS,以及鸟鸟类的营养投入的高影响力,作为代理营养不良。在这些环境中,自动加速的氮固定出现在忽略不计。提出了通过土壤和灰尘颗粒的选择性风传输,以解释冰川边缘的冷冻膜中的优势。我们提出,对于学习的冰川,与限制营养素的回收相关的营养素是在微藻和格拉泽的社区结构中的主要因素驱动。

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