In biomineralization, living organisms carefully control the crystallization of calcium carbonate to create functional materials and thereby often take advantage of polymorphism by stabilizing a specific phase that is most suitable for a given demand. In particular, the lifetime of usually transient amorphous calcium carbonate (ACC) seems to be thoroughly regulated by the organic matrix, so as to use it either as an intermediate storage depot or directly as a structural element in a permanently stable state. In the present study, we show that the temporal stability of ACC can be influenced in a deliberate manner also in much simpler purely abiotic systems. To illustrate this, we have monitored the progress of calcium carbonate precipitation at high pH from solutions containing different amounts of sodium silicate. It was found that growing ACC particles provoke spontaneous polymerization of silica in their vicinity, which is proposed to result from a local decrease of pH nearby the surface. This leads to the deposition of hydrated amorphous silica layers on the ACC grains, which arrest growth and alter the size of the particles. Depending on the silica concentration, these skins have different thicknesses and exhibit distinct degrees of porosity, therefore impeding to varying extents the dissolution of ACC and energetically favored transformation to calcite. Under the given conditions, crystallization of calcium carbonate was slowed down over tunable periods or completely prevented on time scales of years, even when ACC coexisted side by side with calcite in solution.

Upon slow crystallization from silica-containing solutions or gels at elevated pH, alkaline-earth carbonates spontaneously self-assemble into remarkable nanocrystalline ultrastructures. These so-called silica biomorphs exhibit curved morphologies beyond crystallographic symmetry and ordered textures reminiscent of the hierarchical design found in many biominerals. The formation of these fascinating materials is thought to be driven by a dynamic coupling of the components' speciations in solution, which causes concerted autocatalytic mineralization of silica-stabilized nanocrystals over hours. In the present work, we have studied the precipitation kinetics of this unique system by determining growth rates of individual aggregates using video microscopy, and correlated the results with time-dependent data on the concentration of metal ions and pH acquired online during crystallization. In this manner, insight to the evolution of chemical conditions during growth was gained. It is shown that crystallization proceeds linearly with time and is essentially reaction controlled, which fits well in the proposed morphogenetic scenario, and thus, indirectly supports it. Measurements of the silica concentration in solution, combined with analyses of crystal aggregates isolated at distinct stages of morphogenesis, further demonstrate that the fraction of silica coprecipitated with carbonate during active growth is rather small. We discuss our findings with respect to the role of silica in the formation of biomorphs, and moreover, prove that the external silica skins that occasionally sheath the aggregates--previously supposed to be involved in the growth mechanism--originate from secondary precipitation after growth is already terminated.

The particular structural arrangement of chaperonins probably contributes to their ability to assist in the folding of proteins. The interaction of the oligomeric bacterial chaperonin GroEL and its cochaperonin, GroES, in the presence of adenosine diphosphate (ADP) forms an asymmetric complex. However, in the presence of adenosine triphosphate (ATP) or its nonhydrolyzable analogs, symmetric complexes were found by electron microscopy and image analysis. The existence of symmetric chaperonin complexes is not predicted by current models of the functional cycle for GroE-mediated protein folding. Because complete folding of a nonnative substrate protein in the presence of GroEL and GroES only occurs in the presence of ATP, but not with ADP, the symmetric chaperonin complexes formed during the GroE cycle are proposed to be functionally significant.

Attachment of microorganisms to surfaces is a prerequisite for colonization and biofilm formation. The hyperthermophilic crenarchaeote Sulfolobus solfataricus was able to attach to a variety of surfaces, such as glass, mica, pyrite, and carbon-coated gold grids. Deletion mutant analysis showed that for initial attachment the presence of flagella and pili is essential. Attached cells produced extracellular polysaccharides containing mannose, galactose, and N-acetylglucosamine. Genes possibly involved in the production of the extracellular polysaccharides were identified.In microbiology, organisms are isolated from their natural habitats and typically cultivated in the laboratory as planktonic species. Though this method has been essential for understanding the concept of life, it remains unclear how microbial ecosystems operate. For bacteria, it is well known that they are able to form large cellular communities with highly complex cellular interactions and symbioses between different microbial or eukaryotic species. Biofilm formation is an essential component of such communities, and studies have shown that bacteria within biofilms are physiologically different from planktonic ones (20,21). They can exhibit extensive networks of pili on their surfaces and produce and secrete extracellular polysaccharides (EPS), their growth rate is decreased, and cells are much more resistant to physical stresses and antibiotics (19).The study of surface colonization and cellular communities of archaea is crucial for understanding their ecological properties. The only detailed study showed that the hyperthermophilic organism Archaeoglobus fulgidus produced biofilms when challenged with heavy metals and pentachlorophenol (10). Pyrococcus furiosus was able to adhere to different surfaces, such as mica and carbon-coated gold grids, and cells were connected via cable-like bundles of flagella (12). Methanopyrus kandleri was shown to adhere to glass, but P. furiosus could colonize only by attaching to M. kandleri cells, using flagella and direct cell contacts (16).Here we report on the function of cell surface appendages in initial attachment to surfaces of archaea, using directed gene inactivation mutants. The crenarchaeote Sulfolobus solfataricus P2 is a thermoacidophile which grows optimally at 80°C and pH values of 2 to 4 (22). S. solfataricus possesses cell surface structures such as flagella and UV-induced pili (1, 2). The flagellum operon of S. solfataricus encodes, in addition to the structural subunit FlaB, four proteins of unknown function, the ATPase FlaI, and the only integral membrane protein, FlaJ. Previously, we isolated a ⌬flaJ mutant which was nonflagellated and had lost its ability for surface motility on Gelrite plates (17). Recently, we described UV-inducible pili in S. solfataricus that directed cellular aggregation after UV stress (8). Deletion of the central ATPase UpsE, responsible for pilus assembly, rendered cells devoid of pili and defective in cellular aggregation after UV treatment (8). In this study, wild...