Abstract

The amount of 11s aggregate in phycocyanin, normally stimulated by hydrophobic forces, is dramatically increased by the presence of deuterium oxide. Proteins in which hydrophobic forces are not proposed as a mechanism for aggregation are unaffected by deuterium oxide. These observations are consistent with the lower critical micelle concentration reported for ionic detergents in deuterium oxide. Phycocyanin samples containing a majority of material sedimenting faster than 11s were also investigated in the presence of deuterium oxide with the following findings: the most rapidly sedimenting species in water buffer is 24s; in deuterium oxide more than 10% of the protein sediments at 67s and substantial amounts of other species with sedimentation coefficients larger than 24s are present. These large quantities of species sedimenting faster than 24s are found in deuterium oxide buffers from pD5.5 to 7.0. Sucrose-density-gradient studies in deuterium oxide at pD6.0 confirm the presence of large amounts of more rapidly sedimenting species. Spectrophotometric studies on fractions from the sucrose-density-gradient experiments indicate with the presence of higher aggregates a red shift of the visible-absorption maximum and an enhancement of the E(620)/E(280) ratio. Fluorescence-emission studies show a greater relative fluorescence efficiency for these higher aggregates and are consistent with the suggested enhancement of higher aggregates in deuterium oxide. The existence of phycocyanin aggregates of such a large size is suggested to be of importance in vivo, with phycocyanin playing a role as a structural protein.

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