McNamara Christopher J, Perry Thomas D, Bearce Kristen A, Hernandez-Duque Guillermo, Mitchell Ralph
Laboratory of Microbial Ecology, Division of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138, USA.
Microb Ecol. 2006 Jan;51(1):51-64. doi: 10.1007/s00248-005-0200-5. Epub 2006 Jan 3.
Biodeterioration of archaeological sites and historic buildings is a major concern for conservators, archaeologists, and scientists involved in preservation of the world's cultural heritage. The Maya archaeological sites in southern Mexico, some of the most important cultural artifacts in the Western Hemisphere, are constructed of limestone. High temperature and humidity have resulted in substantial microbial growth on stone surfaces at many of the sites. Despite the porous nature of limestone and the common occurrence of endolithic microorganisms in many habitats, little is known about the microbial flora living inside the stone. We found a large endolithic bacterial community in limestone from the interior of the Maya archaeological site Ek' Balam. Analysis of 16S rDNA clones demonstrated disparate communities (endolithic: >80% Actinobacteria, Acidobacteria, and Low GC Firmicutes; epilithic: >50% Proteobacteria). The presence of differing epilithic and endolithic bacterial communities may be a significant factor for conservation of stone cultural heritage materials and quantitative prediction of carbonate weathering.
考古遗址和历史建筑的生物劣化是参与世界文化遗产保护的文物保护者、考古学家和科学家主要关注的问题。墨西哥南部的玛雅考古遗址是西半球一些最重要的文化遗迹,由石灰石建造而成。高温和潮湿导致许多遗址的石头表面出现大量微生物生长。尽管石灰石具有多孔性,并且在许多栖息地中内生微生物普遍存在,但对于生活在石头内部的微生物群落却知之甚少。我们在玛雅考古遗址埃克·巴拉姆内部的石灰石中发现了一个大型内生细菌群落。对16S rDNA克隆的分析表明,(内生:放线菌、酸杆菌和低GC含量的厚壁菌门占比>80%;石表:变形菌门占比>50%)存在不同的群落。石表和内生细菌群落的差异可能是保护石材文化遗产材料以及定量预测碳酸盐风化的一个重要因素。