联合国教科文组织世界遗产地波斯波利斯石灰石上内生白斑藓属植物(地衣化疣状藓科)的生物降解效应

IF 3.5 2区 综合性期刊 0 ARCHAEOLOGY
Mahsa Esmaeillou , Mohammad Sohrabi , Hamideh Ofoghi , Miguel Blázquez , Sergio Pérez-Ortega , Asunción de los Ríos
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引用次数: 0

摘要

本研究考察了地衣形成真菌Bagliettoa sp.(一种明显未被描述的物种)的内生菌体在伊朗联合国教科文组织世界遗产波斯波利斯(Persepolis)生物退化过程中所起的作用。这个物种产生大量的大型生殖体(周鞘),产生具有美学影响的微坑,即使在地衣不再存在后也会持续存在。这项研究的目的是深入了解这些微坑是如何发展的,以及它们对殖民石灰岩的影响。通过光镜和电子显微镜,研究了微坑发育的各个阶段,从石头表面的周鞘出现到它们的腐烂。通过元条形码分析,还评估了其他微生物在这些微坑和周围石头上定殖的可能性。我们的研究结果表明,周鞘的形成和出现对石灰岩造成的结构破坏比已知的生物地球化学过程更明显,这些过程归因于石头内共生细胞的内生扩散。随着菌体和被周分解,微坑充满了矿物碎片,而泥晶层和藻类层则消失了。这最终导致去除高达0.5毫米的石头表面,留下一个空洞的表面,浅微坑。在所有确定的阶段都观察到细菌菌落,最初与泥晶层有关,后来与周被残余有关。石灰石上没有特定的生物变质活性迹象可以归因于这些细菌菌落。元条形码结果显示,与空微坑或仅含有周包膜残留物的微坑相比,具有健康周包膜的微坑中细菌多样性较低,蓝藻丰富度更高。然而,在不同的微坑阶段,细菌群落结构没有显著差异,这表明在微坑发育过程中很少建立新的分类群。我们的研究为内生地衣对鞘周微坑形成的影响提供了新的见解。了解这种生物退化机制对波斯波利斯和其他地衣优势遗址的保护策略设计至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Biodeterioration effects of the endolithic Bagliettoa sp. (lichenized verrucariaceae) on the limestones of persepolis, UNESCO world heritage site
This study examines the role played by the endolithic thallus of the lichen-forming fungi Bagliettoa sp., an apparently undescribed species, in the biodeterioration of Persepolis, a UNESCO World Heritage Site in Iran. This species produces abundant large reproductive bodies (perithecia) creating micropits with aesthetic impacts that persist even after the lichen is no longer present. The aim of this study was to gain insight into how these micropits develop and their effects on colonized limestone. By both light and electron microscopy, the various stages of micropit development were examined from the emergence of perithecia on the stone surface until their decay. The potential for other microorganisms to colonize these micropits and the surrounding stone was also assessed through metabarcoding analysis. Our results indicate that the formation and emergence of perithecia caused more pronounced structural damage to the limestone than reported biogeochemical processes attributed to the endolithic spread of symbiont cells within the stone. As the thallus and perithecium disintegrate, micropits fill with mineral fragments, while micrite and algal layers vanish. This eventually leads to the removal of up 0.5 mm of stone surface, leaving behind a surface marked by empty, shallow micropits. Bacterial colonies were observed at all defined stages, initially associated with the micrite layer and later with perithecium remnants. No specific signs of biodeterioration activity on the limestone could be attributed to these bacterial colonies. Metabarcoding results revealed a lower bacterial diversity in micropits with healthy perithecia and a greater abundance of cyanobacteria compared to empty micropits or those containing only perithecium remnants. However, no significant differences in bacterial community structure were detected across the different micropit stages, suggesting that new taxa rarely become established during micropit development. Our study provides new insight into the effects of endolithic lichens associated with perithecium micropit formation. Knowledge of this biodeterioration mechanism is essential for the design of preservation strategies for Persepolis and other sites featuring the dominance of these lichens.
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来源期刊
Journal of Cultural Heritage
Journal of Cultural Heritage 综合性期刊-材料科学:综合
CiteScore
6.80
自引率
9.70%
发文量
166
审稿时长
52 days
期刊介绍: The Journal of Cultural Heritage publishes original papers which comprise previously unpublished data and present innovative methods concerning all aspects of science and technology of cultural heritage as well as interpretation and theoretical issues related to preservation.
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