In vitro receptivity of carbonate rocks to endolithic lichen-forming aposymbionts

Sergio E. Favero-Longo , Alessandro Borghi , Mauro Tretiach , Rosanna Piervittori
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引用次数: 37

Abstract

Sterile cultured isolates of lichen-forming aposymbionts have not yet been used to investigate lichen–rock interactions under controlled conditions. In this study mycobionts and photobiont of the endolithic lichens Bagliettoa baldensis and Bagliettoa marmorea were isolated and inoculated with coupons of one limestone and four marbles commonly employed in the Cultural Heritage framework. After one year of incubation, microscopic observations of polished cross-sections were performed to verify if the typical colonization patterns observed in the field may be reproduced in vitro and to evaluate the receptivity of the five lithotypes to endolithic lichens. The mycobionts of the two species developed both on the surface of and within all the lithotypes, showing different penetration pathways which depend on mineralogical and structural features and highlight different receptivity. By contrast, algae inoculated with the coupons did not penetrate them. Observations suggest that the hyphal penetration along intrinsic discontinuities of rocks is a relatively fast phenomenon when these organisms are generally considered as slow-growing. Samples from limestone outcrops and abandoned marble quarries, colonized by the same species or other representatives of Verrucariaceae, showed penetration pathways intriguingly similar to those reproduced in vitro and highlighted that lichen-driven erosion processes only increase the availability of hyphal passageways after a long-term colonization. These results show that in vitro incubation of sterile cultured lichen-forming ascomycetes with rock coupons is a practicable experimental system to investigate the lichen–rock interactions under controlled conditions and, together with analysis in situ, may support decisions on conservative treatments of historical and cultural significant stone substrata.

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碳酸盐岩对内生地衣形成共生体的体外接受性
无菌培养的地衣形成共生体尚未用于研究地衣与岩石在受控条件下的相互作用。在本研究中,分离了内石器地衣(Bagliettoa baldensis和Bagliettoa marmorea)的分枝生物和光生物,并用文化遗产框架中常用的一种石灰石和四种大理石接种。经过一年的孵育,对抛光的横截面进行显微镜观察,以验证在野外观察到的典型定植模式是否可以在体外复制,并评估五种石型对内生地衣的接受性。两种菌体均发育在所有岩性的表面和内部,并根据矿物学和构造特征表现出不同的渗透途径,突出了不同的接受性。相比之下,接种了优惠券的藻类没有穿透它们。观察结果表明,菌丝沿着岩石的内在不连续面渗透是一个相对较快的现象,而这些生物通常被认为是生长缓慢的。来自石灰岩露头和废弃大理石采石场的样本,由同一物种或其他疣状菌科代表定殖,显示出与体外繁殖的渗透途径有趣地相似,并强调地衣驱动的侵蚀过程只会增加长期定殖后菌丝通道的可用性。这些结果表明,无菌培养的形成地衣的子囊菌与岩石片的体外培养是一种可行的实验系统,可以在受控条件下研究地衣与岩石的相互作用,并结合现场分析,可能支持对具有历史和文化意义的岩石基质进行保守处理的决策。
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