Bjelland Torbjørg, Ekman Stefan
Bergen Museum, Natural History Collections - Botany, University of Bergen, Allégaten 41, N-5007 Bergen, Norway.
Microb Ecol. 2005 May;49(4):598-603. doi: 10.1007/s00248-004-0101-z. Epub 2005 Jul 29.
Lichen-forming fungi have been assumed to be more or less restricted to the surface of the substrate on which they grow, Conclusive identification of hyphae or an assessment of the fungal diversity inside lichen-covered rock has not been possible using methods based on direct observation. We circumvented this problem by using a DNA sequencing approach. Cores were drilled from a Devonian arcosic sandstone rock harboring the crustose lichen Ophioparma ventosa (L.) Norman on the surface. The cores were cut vertically, and DNA was extracted from the pulverized rock slices. A series of polymerase chain reactions using fungal-specific primers as well as Ophioparma ventosa specific primers were employed to amplify the internal transcribed spacer region of the nuclear ribosomal DNA. The results show that hyphae of O. ventosa penetrate approximately 10-12 mm into the rock. Consequently, the hyphal layer formed by the lichen fungus inside the rock could be 7-12 times as thick as the symbiotic thallus at the surface of the rock. In addition, eight non-lichenized fungal taxa and five that could not be identified to species were encountered. One fungal species in the order Helotiales occurs in six of the eight cores. The significance of these results to the colonization and weathering of rock by lichenized fungi is discussed.
地衣形成真菌被认为或多或少局限于它们生长的基质表面,使用基于直接观察的方法无法对菌丝进行确凿鉴定或评估地衣覆盖岩石内部的真菌多样性。我们通过使用DNA测序方法规避了这个问题。从一块泥盆纪长石砂岩岩芯上钻孔,该岩石表面生长着壳状地衣Ophioparma ventosa (L.) Norman。将岩芯垂直切割,从粉碎的岩石切片中提取DNA。使用真菌特异性引物以及Ophioparma ventosa特异性引物进行一系列聚合酶链反应,以扩增核糖体DNA的内部转录间隔区。结果表明,O. ventosa的菌丝深入岩石约10 - 12毫米。因此,岩石内部由地衣真菌形成的菌丝层厚度可能是岩石表面共生叶状体的7 - 12倍。此外,还遇到了8个非地衣化真菌类群和5个无法鉴定到种的类群。锤舌菌目中的一个真菌物种出现在8个岩芯中的6个中。讨论了这些结果对地衣化真菌在岩石定殖和风化方面的意义。