Streptococcal pyrogenic exotoxin type B purified from culture filtrates of either the NY-5 or T-19 strain of group A streptococcus was found to be heterogeneous in charge. Three protein fractions with isoelectric points of 8.0, 8.4, and 9.0 were isolated by differential solubility in ethanol and acetate-buffered saline followed by isoelectric focusing and shown to be antigenically identical to streptococcal pyrogenic exotoxin type B. The molecular weights of all three fractions were approximately 17,500, as determined by sodium dodecyl sulfate-polyacrylamide gel electrophoresis, with aggregates forming in the presence of hyaluronic acid. Only the pI 8.4 fraction showed the characteristic activities of streptococcal pyrogenic exotoxin in rabbits: pyrogenicity and ability to enhance susceptibility to lethal endotoxin shock. The pI 8.0 and pl 9.0 fractions were not pyrogenic, but could be used to immunize against pyrogenicity. These two fractions failed either to enhance lethal endotoxin shock or to immunize against enhancement activity. When the isolated fractions were electrofocused again they appeared heterogeneous, suggesting an instability of the B toxin molecular forms.
Patterns of dispersal of distinctive Proterozoic and Paleozoic erratics across terrain formed on Archean and Aphebian crystalline rocks indicate that (1) ice never flowed from Hudson Bay into Keewatin in the region from the Manitoba border (lat 60°N) northward at least to lat 65°N; (2) westward-southwestward flow out of the bay, probably from a Labradorean dispersal center, interfaced with southward-and southeastwardflowing ice from the Keewatin dispersal center somewhere between Nelson River and Churchill; and (3) at least 300 km of dispersal of distinctive erratics observed from the vicinity of the last position of the Keewatin Ice Divide to the present coast of Hudson Bay required considerably more time than the 1,000 to 3,000 yr that the divide has traditionally been thought to have existed. In fact, the Keewatin Ice Divide and its precursors represent the centers of an independent, land-based ice sheet that probably existed throughout the period of Wisconsin Glaciation.
Streptococcal pyrogenic exotoxin (SPE) isolated from culture filtrates of strain NY-5 (type 10), and separated from other extracellular enzymes by differential solubility in ethanol and acetate-buffered saline, has previously been shown to exhibit a wide range of biological activities including erythrogenic activity, pyrogenicity, enhancement of susceptibility to endotoxin shock, blockage of the reticuloendothelial system, immunosuppression, and lymphocyte mitogenicity. Toxin prepared in this way was found to consist of hyaluronic acid and several proteins which could be distinguished by thin-layer polyacrylamide isoelectric focusing (IEF). SPE has been further purified by ion exchange chromatography on QAE-Sephadex columns. One of the fractions isolated from QAE-Sephadex, and shown to be a homogeneous protein by thin-layer IEF and Ouchterlony with hyperimmune serum, was highly active erythrogenically, pyrogenically, and in enhancing susceptibility to endotoxin. This fraction was identified as exotoxin A. A second, less active fraction identified as SPE B showed similar activities, but differed from the other fraction antigenically and in net charge and molecular weight. These findings indicate that a single highly purified protein can mediate at least three of the biological activities attributed to SPE and that NY-5 produces pyrogenic exotoxins A and B in vitro as well as in vivo.
The effect of purified streptococcal pyrogenic exotoxins (SPE) on the antibody response to sheep erythrocytes was studied in cultures of mouse spleen cells. Purified SPE types A, B, and C shared the ability to suppress the day 4 direct plaque-forming cell response when added to cultures. SPE A and C were most suppressive at concentrations of 0.1 to 1 ng per culture, while SPE B was active at 1 microgram per culture. Pretreatment of mice with SPE A, 3 h before removal of their spleens for culture, also produced suppression. Cell populations were separated from spleens of normal and toxin-treated mice and recombined in culture to test the cellular site of action of SPE immunosuppression. When nonadherent cells (lymphocytes) and adherent cells (macrophages) from control and SPE-treated mice were separated and recombined, the plaque-forming cell response depended on the source of lymphocytes. Macrophages from toxin-treated mice functioned normally in the presence of control lymphocytes. In a further experiment, toxin pretreatment failed to suppress the plaque-forming cell response of spleen cells that were T-cell depleted and reconstituted with control thymocytes. When the T lymphocytes were removed from toxin-treated spleen cell suspensions, the remaining cells were able to respond normally to antigen if normal helper T cells were provided. The results suggest that the suppressive activity of SPE on antibody production is mediated by altered activity of T lymphocytes.
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