首页> 外文期刊>Mycological Research >LICHENIZED ASSOCIATION BETWEEN SEPTONEMA TORMES SP. NOV., A COCCOID CYANOBACTERIUM, AND A GREEN ALGA WITH AN UNFORESEEN BIOPRESERVATION EFFECT OF VILLAMAYOR SANDSTONE AT CASA LIS OF SALAMANCA, SPAIN
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LICHENIZED ASSOCIATION BETWEEN SEPTONEMA TORMES SP. NOV., A COCCOID CYANOBACTERIUM, AND A GREEN ALGA WITH AN UNFORESEEN BIOPRESERVATION EFFECT OF VILLAMAYOR SANDSTONE AT CASA LIS OF SALAMANCA, SPAIN

机译:SEPTONEMA TORMES SP之间经过许可的协会。 11月,一种藻类藻类细菌和一种绿色藻类,在西班牙萨拉曼卡的卡利亚斯具有未曾预料到的维拉马约斯沙石的生物保存作用

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'Casa Lis' is the most characteristic building in Salamanca, Spain, belonging to the modernist trend. It was built with Villamayor sandstone from nearby Salamanca, which has high porosity providing an easy medium for water absortion and capillarity. During a restoration process on the southern wall, near an underground water flow, two well defined, naturally developed layers were observed on the sandstone surface: an outer, hard crust with greyish shades and whitish salt patches resulting from rising damp, and an inner, green layer with organic material linking the sandstone to the inorganic crust. The microbiological study of this biofilm showed an ecologically obligate, stable mutualism between a dematiaceous mitosporic fungus (Septonema tormes sp. nov.), a coccoid cyanobacterium (Cyanothece-group) and a green alga (Gloeocystis rupestris), with the accumulation of different metabolites excreted by these microorganisms. The case reported here is one of the few studies where a microbial mat, in association with the external crust, avoids a further weathering of the stone because of an unforeseen biopreservation-effect due to the maintenance of humidity at constant levels under the crust avoids changes in clay swelling and subsequent surface arenization of the sandstone. The lichenized complex of a mitosporic mycobiont and two photobionts, in this case, has not been reported before as a stable association on this kind of substrate.
机译:“ Casa Lis”是西班牙萨拉曼卡最具特色的建筑,属于现代主义潮流。它是用附近萨拉曼卡(Salamanca)的Villamayor砂岩建造的,它具有高孔隙率,为水的吸收和毛细作用提供了一种简便的介质。在南壁的修复过程中,在地下水流附近,在砂岩表面观察到了两个界限分明的,自然发育的层:外层硬壳,灰白色阴影,由于潮湿增加而形成白色盐斑,内层绿色层,有机材料将砂岩与无机地壳相连。对该生物膜的微生物学研究显示,皮病性线粒体真菌(Septonema tormes sp。nov。),球状蓝藻细菌(蓝藻菌群)和绿藻(Gloeocystis rupestris)之间存在生态专一的,稳定的共生关系。被这些微生物排泄。此处报道的病例是为数不多的研究之一,其中微生物垫与外部地壳相关联,避免了石头的进一步风化,这是由于不可预见的生物保存效应所致,因为在地壳下将湿度保持在恒定水平可避免变化粘土膨胀和随后的砂岩表面芳构化。在这种情况下,以前没有报道过线粒体分枝杆菌和两种光致生物剂的地衣化复合物是这种底物上的稳定缔合体。

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