Physicochemical characteristics of the mineral-forming S-layer from the cyanobacterium Synechococcus strain GL24

作者：Susanne Schultze-Lam, Terry J. Beveridge · 发表于：Canadian Journal of Microbiology · 年份：1994 · DOI：10.1139/m94-035 · 被引用次数：50 · 研究领域：Microbial Community Ecology and Physiology、Diatoms and Algae Research、Genomics and Phylogenetic Studies

The hexagonal S-layer from the unicellular cyanobacterium Synechococcus strain GL24 can act as a template for sulfate and carbonate mineral formation by providing regularly spaced, chemically identical nucleation sites. This novel ability is a reflection of the S-layer's chemistry in addition to its structure. Few, if any, other cyanobacterial S-layers have been subjected to detailed chemical analysis and no other reports of the involvement of an S-layer in mineral formation can be found. We have investigated the surface charge and chemical characteristics of the Synechococcus strain GL24 S-layer in an attempt to unravel the mechanism(s) of mineral formation on this proteinaceous surface layer. The constituent proteins of the S-layer show up as two bands (Mr = 109 000 and 104 000) on SDS-PAGE gels. When assembled, the S-layer confers a net neutral charge on the cell surface with negatively charged sites (which can bind cations) exposed in the large holes of the array. Treatment of whole cells with a wide range of chemical agents failed to disrupt intralayer bonding and binding of the S-layer to the underlying outer membrane, indicating that this is a remarkably resilient S-layer in comparison to those found on other bacteria.Key words: S-layer, cyanobacteria, chemistry, carbonate minerals.