subaerial biofilm

地下生物膜
  • 文章类型: Journal Article
    这项研究的主要目的,作为计划保护工作的一部分,是为了揭示本土生物膜的各个方面,这些生物膜与在斯洛文尼亚的石灰石RoanecMithraeum纪念碑上发生的许多恶化症状的形成有关。使用最先进的测序技术,将真菌生物组数据与通过大量光和光谱(FTIR和拉曼)显微镜分析进行的观察相结合,指出了上皮性地衣Gyalectajenensis及其光生物,富含类胡萝卜素的Trentepohliaaurea,作为石灰岩表面鲑鱼色色素变化的起源。此外,纪念碑上主要恶化症状的发展,即,活检,是由代表性的疣科科(Verrucariasp。)与草酸介导的石灰石溶解相结合。苔藓真菌的统治,作为主要的变质剂,在浮雕和周围的石灰石上,此外,在FUNGuild分析中,苔藓化和共生生物组的相对丰度较高。获得的结果不仅提高了人们对这种经常发生但经常被忽视的极端性石头遗产变质剂的认识,而且为开发适用于原位保存类似受影响的石灰石古迹的有效生物防治制剂提供了必要的基础。
    The primary purpose of the study, as part of the planned conservation work, was to uncover all aspects of autochthonous biofilm pertaining to the formation of numerous deterioration symptoms occurring on the limestone Rožanec Mithraeum monument in Slovenia. Using state-of-the-art sequencing technologies combining mycobiome data with observations made via numerous light and spectroscopic (FTIR and Raman) microscopy analyses pointed out to epilithic lichen Gyalecta jenensis and its photobiont, carotenoid-rich Trentepohlia aurea, as the origin of salmon-hued pigmented alterations of limestone surface. Furthermore, the development of the main deterioration symptom on the monument, i.e., biopitting, was instigated by the formation of typical endolithic thalli and ascomata of representative Verrucariaceae family (Verrucaria sp.) in conjunction with the oxalic acid-mediated dissolution of limestone. The domination of lichenized fungi, as the main deterioration agents, both on the relief and surrounding limestone, was additionally supported by the high relative abundance of lichenized and symbiotroph groups in FUNGuild analysis. Obtained results not only upgraded knowledge of this frequently occurring but often overlooked group of extremophilic stone heritage deteriogens but also provided a necessary groundwork for the development of efficient biocontrol formulation applicable in situ for the preservation of similarly affected limestone monuments.
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  • 文章类型: Journal Article
    基于颜料的颜色是矿物-空气界面上生物膜最重要的表型特征之一(地下生物膜,SABS),因为它反映了微生物群落的生理学。因为颜色是所有SAB的标志,我们认为,基于色素的颜色可以传达驱动不同陆地环境中微生物适应和共存的机制,并将表型特征与社区适应性和生态动态联系起来。在这个框架内,我们介绍了矿物-空气界面上最相关的微生物色素,并讨论了一些进化景观,这些进化景观需要色素作为资源分配和生存能力的适应性策略。我们报告了几种反映SAB群落结构和功能的色素特征,以及微生物生活史策略和共存理论背景下的色素生态学。最后,我们通过介绍色素生态学的潜在应用和研究中的一些关键挑战来总结色素生态学的研究。
    Pigment-based color is one of the most important phenotypic traits of biofilms at the mineral-air interface (subaerial biofilms, SABs), because it reflects the physiology of the microbial community. Because color is the hallmark of all SABs, we argue that pigment-based color could convey the mechanisms that drive microbial adaptation and coexistence across different terrestrial environments and link phenotypic traits to community fitness and ecological dynamics. Within this framework, we present the most relevant microbial pigments at the mineral-air interface and discuss some of the evolutionary landscapes that necessitate pigments as adaptive strategies for resource allocation and survivability. We report several pigment features that reflect SAB communities\' structure and function, as well as pigment ecology in the context of microbial life-history strategies and coexistence theory. Finally, we conclude the study of pigment-based ecology by presenting its potential application and some of the key challenges in the research.
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  • 文章类型: Journal Article
    在实验室条件下诱导了花岗岩的模拟环境定殖,以开发用于研究生物容受性的实验方案。实验装置被证明适用于通过用天然生物膜衍生的浮游多物种光养培养物接种花岗岩块来生产地下生物膜。通过颜色测量在三个月的生长期内监测四种不同培养物形成生物膜的能力,光合色素和EPS的定量,和CLSM观测。正在研究的文化之一,其中包括几个类群,包括苔藓植物,Charophyta,绿藻和蓝细菌,特别适合作为接种物,主要是因为它的微生物丰富,它对基质的快速适应性和高定殖能力。在拟议的实验装置中使用这种培养物作为接种物,在实验室条件下生产地下生物膜将有助于标准化所涉及的方案。从而可以在进一步的实验中更客观地评估花岗岩的生物容受性。
    Simulated environmental colonisation of granite was induced under laboratory conditions in order to develop an experimental protocol for studying bioreceptivity. The experimental set-up proved suitable for producing subaerial biofilms by inoculating granite blocks with planktonic multi-species phototrophic cultures derived from natural biofilms. The ability of four different cultures to form biofilms was monitored over a three-month growth period via colour measurements, quantification of photosynthetic pigments and EPS, and CLSM observations. One of the cultures under study, which comprised several taxa including Bryophyta, Charophyta, Chlorophyta and Cyanobacteria, was particularly suitable as an inoculum, mainly because of its microbial richness, its rapid adaptability to the substratum and its high colonisation capacity. The use of this culture as an inoculum in the proposed experimental set-up to produce subaerial biofilms under laboratory conditions will contribute to standardising the protocols involved, thus enabling more objective assessment of the bioreceptivity of granite in further experiments.
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  • 文章类型: Historical Article
    在世界遗产的花岗岩历史建筑上形成的天然地下生物膜的微生物群落(圣地亚哥·德孔波斯特拉,NW西班牙)进行表征并在液体BG11培养基中培养。通过下一代测序(PacificBiosciences)进行环境条形码编码表明,生物膜主要由与岩石基质相关的绿藻门(绿藻)和子囊菌(真菌)组成。真菌的丰富度和多样性高于藻类组合,真菌在样品之间显示出更高的异质性。来自天然生物膜的培养物显示建立了稳定的微生物群落,主要由绿藻和蓝细菌组成。尽管在这些文化中发现的大多数分类单元在原始生物膜中并不常见,他们可能是建造石头表面的共同先驱殖民者,包括花岗岩.因此获得了具有已知微生物多样性的稳定的光养多物种培养物,并且应在进一步的实验中证实它们在花岗岩上模拟自然定殖的可靠性。
    Microbial communities of natural subaerial biofilms developed on granitic historic buildings of a World Heritage Site (Santiago de Compostela, NW Spain) were characterized and cultured in liquid BG11 medium. Environmental barcoding through next-generation sequencing (Pacific Biosciences) revealed that the biofilms were mainly composed of species of Chlorophyta (green algae) and Ascomycota (fungi) commonly associated with rock substrata. Richness and diversity were higher for the fungal than for the algal assemblages and fungi showed higher heterogeneity among samples. Cultures derived from natural biofilms showed the establishment of stable microbial communities mainly composed of Chlorophyta and Cyanobacteria. Although most taxa found in these cultures were not common in the original biofilms, they are likely common pioneer colonizers of building stone surfaces, including granite. Stable phototrophic multi-species cultures of known microbial diversity were thus obtained and their reliability to emulate natural colonization on granite should be confirmed in further experiments.
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