The extracellular proteinase of
Ps. myxogenes sp. is constitued with Ca as an essential component as shown in the previous paper
1). This paper deals with a study concerning the step of incorporation of Ca in the synthesizing reaction of the proteinase of the bacteria.
A protein or peptide substance constituted from Ca is not found within the cells of the bacteria which have been shaken in the presence of a carbon source and Ca ion, while the proteinase is accumulated at the extracellular site. As it is sure that nitrogen material within the cells (which has been assumed to be a more complicated substance than amino acid, which is a precursor substance) contributes to the enzyme synthesis, the above result might suggest that Ca is not incorporated at the precursor state in the enzyme synthesis, or even if the incorporation really does occur at that state, the precursor substance is immediately secreted in the medium. However, we have not found the precursor material which is secreted in the medium where the material is activated auto-catalytically as seen in
Streptococcal proteinase
6). Accordingly, it is difficult to consider the latter case to occur.
The total amount of organic nitrogen material secreted in the medium containing a carbon source by shaking the bacterial cells aerobically, is found to be identical in both the presence or absence of Ca ion, but the secreted protein content is remarkably diminished (to almost one-fifth) in the absence of Ca ion. Further, it is clear that the removal of Ca from the enzyme molecule, by treatment with EDTA at 50°C, results not only in inactivation of the enzymatic action but also exhibits the autosplitting phenomenon of the enzyme protein.
These results may lead to the assumption that Ca-free proteinase would be secreted in the medium regardless of the existence of Ca ion, and the enzyme is accumulated when it is stabilized by the constitution of Ca ion in the medium, whereas the auto-splitting phenomenon of the enzyme would take place in absence of the Ca ion.
Therefore, the incorporation of Ca in the proteinase synthesis by the bacteria is considered to occur in the completely synthesized Ca-free proteinase secreted in the medium.
The author wishes to express his sincere thanks to Prof. H. Katagiri of Kyoto University for his constant guidance and encouragement throughout this work. Thanks are also due to Mr. E. Masuo of this Laboratory for his assistance.
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