Biofilms formed by the archaeon Haloferax volcanii exhibit cellular differentiation and social motility, and facilitate horizontal gene transfer

被引:66
作者
Chimileski, Scott [1 ]
Franklin, Michael J. [2 ,3 ]
Papke, R. Thane [1 ]
机构
[1] Univ Connecticut, Dept Mol & Cell Biol, Storrs, CT 06269 USA
[2] Montana State Univ, Dept Microbiol, Bozeman, MT 59717 USA
[3] Montana State Univ, Ctr Biofilm Engn, Bozeman, MT 59717 USA
基金
美国国家科学基金会;
关键词
biofilm; Haloferax volcanii; microbial development; archaeal genetics; archaeal biofilm; horizontal gene transfer; amyloid; collective behavior; swarming; haloarchaea; EXTRACELLULAR DNA; CONGO RED; BACILLUS-SUBTILIS; HALOBACTERIUM-VOLCANII; AMYLOID PLAQUES; POPULATION; BACTERIA; MATRIX; GROWTH; POLYSACCHARIDE;
D O I
10.1186/s12915-014-0065-5
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Background: Archaea share a similar microbial lifestyle with bacteria, and not surprisingly then, also exist within matrix-enclosed communities known as biofilms. Advances in biofilm biology have been made over decades for model bacterial species, and include characterizations of social behaviors and cellular differentiation during biofilm development. Like bacteria, archaea impact ecological and biogeochemical systems. However, the biology of archaeal biofilms is only now being explored. Here, we investigated the development, composition and dynamics of biofilms formed by the haloarchaeon Haloferax volcanii DS2. Results: Biofilms were cultured in static liquid and visualized with fluorescent cell membrane dyes and by engineering cells to express green fluorescent protein (GFP). Analysis by confocal scanning laser microscopy showed that H. volcanii cells formed microcolonies within 24 h, which developed into larger clusters by 48 h and matured into flake-like towers often greater than 100 mu m in height after 7 days. To visualize the extracellular matrix, biofilms formed by GFP-expressing cells were stained with concanavalin A, DAPI, Congo red and thioflavin T. Stains colocalized with larger cellular structures and indicated that the extracellular matrix may contain a combination of polysaccharides, extracellular DNA and amyloid protein. Following a switch to biofilm growth conditions, a sub-population of cells differentiated into chains of long rods sometimes exceeding 25 mu m in length, compared to their planktonic disk-shaped morphology. Time-lapse photography of static liquid biofilms also revealed wave-like social motility. Finally, we quantified gene exchange between biofilm cells, and found that it was equivalent to the mating frequency of a classic filter-based experimental method. Conclusions: The developmental processes, functional properties and dynamics of H. volcanii biofilms provide insight on how haloarchaeal species might persist, interact and exchange DNA in natural communities. H. volcanii demonstrates some biofilm phenotypes similar to bacterial biofilms, but also has interesting phenotypes that may be unique to this organism or to this class of organisms, including changes in cellular morphology and an unusual form of social motility. Because H. volcanii has one of the most advanced genetic systems for any archaeon, the phenotypes reported here may promote the study of genetic and developmental processes in archaeal biofilms.
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