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冰岛两处地热温泉中光养微生物席的真核微生物多样性。

Eukaryotic microbial diversity of phototrophic microbial mats in two Icelandic geothermalhot springs.

机构信息

Center of Astrobiology, National Institute for Aerospace Technology-CSIC, Torrejon de Ardoz, Spain.

出版信息

Int Microbiol. 2010 Mar;13(1):21-32. doi: 10.2436/20.1501.01.109.

Abstract

The composition of the eukaryotic community and the three-dimensional structure of diverse phototrophic microbial mats from two hot springs in Iceland (Seltun and Hveradalir geothermal areas) were explored by comparing eukaryotic assemblages from microbial mats. Samples were collected in July 2007 from 15 sampling stations along thermal and pH gradients following both hot springs. Physicochemical data revealed high variability in terms of pH (ranging from 2.8 to 7), with high concentrations of heavy metals, including up to 20 g Fe/l, 80 mg Zn/l, 117 mg Cu/l, and 39 mg Ni/l at the most acidic sampling points. Phylogenetic analysis of 18S rDNA genes revealed a diversity of sequences related to several taxa, including members of the Bacillariophyta, Chlorophyta, Rhodophyta, and Euglenophyta phyla as well as ciliates, amoebae, and stramenopiles. The closest relatives to some of the sequences detected came from acidophilic organisms, even when the samples were collected at circumneutral water locations. Electron microscopy showed that most of the microecosystems analyzed were organized as phototrophic microbial mats in which filamentous cyanobacteria usually appeared as a major component. Deposits of amorphous minerals rich in silica, iron, and aluminium around the filaments were frequently detected.

摘要

通过比较微生物席中的真核生物组合,探索了来自冰岛两个温泉(Seltun 和 Hveradalir 地热区)的真核生物群落组成和各种光养微生物席的三维结构。2007 年 7 月,在这两个温泉沿线的热梯度和 pH 梯度上的 15 个采样点采集了样本。理化数据显示 pH 值变化很大(范围从 2.8 到 7),重金属浓度很高,在最酸性的采样点,铁浓度高达 20 g/L,锌浓度为 80 mg/L,铜浓度为 117 mg/L,镍浓度为 39 mg/L。18S rDNA 基因的系统发育分析揭示了与多个分类群相关的序列多样性,包括硅藻门、绿藻门、红藻门和眼虫门的成员,以及纤毛虫、变形虫和不等鞭毛门的成员。一些检测到的序列的最接近的亲缘关系来自嗜酸生物,即使样本是在近中性水的位置采集的。电子显微镜显示,大多数分析的微型生态系统都是由丝状蓝细菌通常作为主要成分的光养微生物席组织而成。在丝状物周围经常检测到富含硅、铁和铝的无定形矿物沉积物。

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