Laboratory-Induced Endolithic Growth in Calcarenites: Biodeteriorating Potential Assessment

被引:27
|
作者
Miller, A. Z. [1 ,2 ]
Rogerio-Candelera, M. A. [3 ]
Laiz, L. [3 ]
Wierzchos, J. [4 ]
Ascaso, C. [4 ]
Sequeira Braga, M. A. [5 ]
Hernandez-Marine, M. [6 ]
Mauricio, A. [1 ]
Dionisio, A. [1 ]
Macedo, M. F.
Saiz-Jimenez, C. [3 ]
机构
[1] Inst Super Tecn, Ctr Petrol & Geoquim, P-1049001 Lisbon, Portugal
[2] Univ Nova Lisboa, Dept Conservacao & Restauro, Fac Ciencias & Tecnol, P-2829516 Monte De Caparica, Caparica, Portugal
[3] CSIC, Inst Recursos Nat & Agrobiol, Seville 41012, Spain
[4] CSIC, Inst Recursos Natur, Ctr Ciencias Medioambientales, E-28006 Madrid, Spain
[5] Univ Minho, Ctr Invest Geol Ordenamento & Valorizacao Recurso, P-4710057 Braga, Portugal
[6] Univ Barcelona, Fac Farm, E-08028 Barcelona, Spain
关键词
MICROORGANISMS; BIORECEPTIVITY; COLONIZATION; ROCK; CYANOBACTERIA; LICHEN; ALGAE;
D O I
10.1007/s00248-010-9666-x
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
This study is aimed to assess the formation of photosynthetic biofilms on and within different natural stone materials, and to analyse their biogeophysical and biogeochemical deterioration potential. This was performed by means of artificial colonisation under laboratory conditions during 3 months. Monitoring of microbial development was performed by image analysis and biofilm biomass estimation by chlorophyll extraction technique. Microscopy investigations were carried out to study relationships between microorganisms and the mineral substrata. The model applied in this work corroborated a successful survival strategy inside endolithic microhabitat, using natural phototrophic biofilm cultivation, composed by cyanobacteria and algae, which increased intrinsic porosity by active mineral dissolution. We observed the presence of mineral-like iron derivatives (e.g. maghemite) around the cells and intracellularly and the precipitation of hausmannite, suggesting manganese transformations related to the biomineralisation.
引用
收藏
页码:55 / 68
页数:14
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