Abstract

We have previously demonstrated that the alpha'-chain of human activated form of the fourth (C4b) and third (C3b) component of C are cleaved by plasma or serum from vertebrate species spanning through 300,000,000 yr of evolution yielding fragments identical with those obtained with human plasma. In this study, we investigated the molecular basis of this reaction. We chose barred sand bass plasma because this is the most primitive species analyzed possessing these activities. Barred sand bass plasma proteins were separated on a Sephadex G-200 column and the eluted samples analyzed for C4b and C3b cleavage. Individual fractions were inactive, but degradation was obtained when proteins of 380 and 155 kDa were combined. In contrast to the human regulatory proteins, the sand bass proteins require Ca2+ ions. K76COOH, an inhibitor of human factor I, inhibited the function of the 155-kDa but not of the 380 kDa-fraction. Thus it appears that the 155-kDa fraction functions as the C4b/C3b cleaving enzyme (I) and the 380-kDa material as its cofactor. Further purification of the 380-kDa fraction yielded a protein that by SDS-PAGE consisted of two noncovalently linked subunits of 110 and 42 kDa at a molecular ratio of 2:1. These two chains were antigenically distinct, and constitute domains of the same protein. The 110-kDa peptide binds C4b and not C3b but it fully expresses the cofactor function for the 155-kDa fraction on the cleavage of both C4b and C3b. Limited tryptic digestion of the 110-kDa domain demonstrated C4b binding activity in fragments of 34, 25, and 23 kDa. The activity of the 34-kDa fragment was the same as that of the undigested protein. Comparison of the amino acid composition of the barred sand bass cofactor and of human C4bp shows similar high content of cysteine and proline but not of tryptophan. It differs from human factor H in cysteine, serine, proline, and tryptophan. These studies indicate that regulatory proteins for the C4b and C3b C fragments may have appeared very early phylogenetically.

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