Abstract

The change in the distribution of the phosphate species containing 0 to 4 18O oxygens per Pi was investigated during medium Pi equilibrium HOH exchange catalyzed by myosin subfragment 1. At 25 degrees C, a Pi molecule once bound loses an average of 3.9 of its original 4 oxygens prior to release which means that at least 100 reversals of the exchange reaction must have occurred. At 0 degrees C, only 3.4 of the 4 oxygens are lost prior to release indicating an average of 17 reversals. Distribution patterns are consistent with equivalent participation in the exchange reactions of all 4 oxygens of bound Pi. The intermediate exchange of Pi oxygens during hydrolysis of 18O-labeled ATP by myosin has also been investigated. The distribution of the product Pi species shows that there is an ATPase component in myosin preparations which hydrolyzes ATP without intermediate exchange. Presence of this component, which is likely a contaminating ATPase, provides a simple explanation of the apparent nonequivalence of phosphate oxygens which has been observed. When correction is made for this contaminant, characteristics of the myosin intermediate Pi equilibrium HOH exchange are similar to those of myosin subfragment 1 medium exchange, and intermediate exchange data are in much closer agreement with other kinetic measurements.

Highlights

  • I and II show the results of myosin subfragment l-catalyzed medium P, s HOH exchange experiments at 25” and O”C, respectively

  • Possible interference by adenylate kinase was eliminated by use of column-purified

  • P’“OI and I”‘O$ species which dominate the distribution at zero time are converted directly to the I”‘O, species during the exchange process with little accumulation of intermediates

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Summary

Introduction

The intermediate exchange of Pi oxygens during hydrolysis of l”O-labeled ATP by myosin has been investigated. The distribution of the product Pi species shows that there is an ATPase component in myosin preparations which hydrolyzes ATP without intermediate exchange.

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Conclusion
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