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首页> 外文期刊>Biogeosciences >Controls on microalgal community structures in cryoconite holes upon high-Arctic glaciers, Svalbard
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Controls on microalgal community structures in cryoconite holes upon high-Arctic glaciers, Svalbard

机译:对高北极冰川斯瓦尔巴特群岛冰冻洞中微藻群落结构的控制

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摘要

Glaciers are known to harbor surprisingly complex ecosystems. On their surface, distinct cylindrical holes filled with meltwater and sediments are considered hot spots for microbial life. The present paper addresses possible biological interactions within the community of prokaryotic cyanobacteria and eukaryotic microalgae (microalgae) and relations to their potential grazers, such as tardigrades and rotifers, additional to their environmental controls. Svalbard glaciers with substantial allochthonous input of material from local sources reveal high microalgal densities. Small valley glaciers with high sediment coverages and high impact of birds show high biomasses and support a high biological diversity. Invertebrate grazer densities do not show any significant negative correlation with microalgal abundances but rather a positive correlation with eukaryotic microalgae. Shared environmental preferences and a positive effect of grazing are the proposed mechanisms to explain these correlations. Most microalgae found in this study form colonies (< 10 cells, or > 25 mu m), which may protect them against invertebrate grazing. This finding rather indicates grazing as a positive control on eukaryotic microalgae by nutrient recycling. Density differences between the eukaryotic microalgae and prokaryotic cyanobacteria and their high distinction in redundancy (RDA) and principal component (PCA) analyses indicate that these two groups are in strong contrast. Eukaryotic microalgae occurred mainly in unstable cryoconite holes with high sediment loads, high N:P ratios, and a high impact of nutrient input by bird guano, as a proxy for nutrients. In these environments autochthonous nitrogen fixation appears to be negligible. Selective wind transport of Oscillatoriales via soil and dust particles is proposed to explain their dominance in cryoconites further away from the glacier margins. We propose that, for the studied glaciers, nutrient levels related to recycling of limiting nutrients are the main factor driving variation in the community structure of microalgae and grazers.
机译:众所周知,冰川具有令人惊讶的复杂生态系统。在其表面上,充满熔水和沉积物的明显圆柱孔被认为是微生物生命的热点。本文探讨了原核蓝细菌和真核微藻(微藻)群落中可能的生物相互作用,以及与它们潜在的放牧者(如缓坡和轮虫)的关系,以及它们的环境控制。斯瓦尔巴德冰川具有大量来自当地的异源物质输入,显示出较高的微藻类密度。具有高沉积物覆盖率和鸟类影响的小型山谷冰川显示出高生物量,并支持高度生物多样性。无脊椎动物的放牧者密度与微藻的丰度没有显着的负相关,而与真核微藻的正相关。共有的环境偏好和放牧的积极效果是解释这些相关性的拟议机制。在这项研究中发现的大多数微藻形成菌落(<10个细胞,或> 25μm),可以保护它们免受无脊椎动物的放牧。该发现反而表明通过养分循环利用放牧作为真核微藻的阳性对照。真核微藻和原核蓝细菌之间的密度差异以及它们在冗余度(RDA)和主成分(PCA)分析中的高度区别表明,这两组之间存在强烈的对比。真核微藻类主要发生在不稳定的低温暗孔中,其沉积物负荷高,N:P比高,并且鸟粪作为养分的替代物对养分输入的影响很大。在这些环境中,自然氮的固定似乎可以忽略不计。提出了通过土壤和尘埃颗粒进行的颤藻选择性风传输,以解释它们在远离冰川边缘的冰冻土中的优势。我们建议,对于所研究的冰川,与有限养分循环有关的养分水平是驱动微藻和放牧者群落结构变化的主要因素。

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