All reactions are accelerated by an increase in temperature, but the magnitude of that effect on very slow reactions does not seem to have been fully appreciated. The hydrolysis of polysaccharides, for example, is accelerated 190,000-fold when the temperature is raised from 25 to 100°C, while the rate of hydrolysis of phosphate monoester dianions increases 10,300,000-fold. Moreover, the slowest reactions tend to be the most heat-sensitive. These tendencies collapse, by as many as five orders of magnitude, the time that would have been required for early chemical evolution in a warm environment. We propose, further, that if the catalytic effect of a "proto-enzyme"-like that of modern enzymes-were mainly enthalpic, then the resulting rate enhancement would have increased automatically as the environment became cooler. Several powerful nonenzymatic catalysts of very slow biological reactions, notably pyridoxal phosphate and the ceric ion, are shown to meet that criterion. Taken together, these findings greatly reduce the time that would have been required for early chemical evolution, countering the view that not enough time has passed for life to have evolved to its present level of complexity.activation energy | thermophilic organisms | pyridoxal phosphate | phosphate ester hydrolysis | amino acid decarboxylation W hereas enzyme reactions ordinarily occur in a matter of milliseconds, the same reactions proceed with half-lives of hundreds, thousands, or millions of years in the absence of a catalyst ( Fig. 1) (1). Yet life is believed to have taken hold within the first 25% of Earth's history (2). How could cellular chemistry, and the enzymes that make life possible, have arisen so quickly? Here, we show that because of an extraordinarily sensitive relationship between temperature and the rates of very slow reactions, the time required for early evolution on a warm earth was very much shorter than it might appear. That sensitivity also suggests some likely properties of an evolvable catalyst, and a testable mechanism by which its ability to enhance rates might have been expected to increase as the environment cooled.Rapid substrate turnover is necessary to support the metabolism of an organism at the enzyme concentrations found in cells, but the same reactions, in the absence of enzymes, proceed vastly more slowly (Fig. 1). For example, the decarboxylation of orotidine 5′-phosphate (OMP), the final step in the biosynthesis of pyrimidines-and thus nucleic acids-proceeds with a half-life of 0.017 s at the active site of OMP decarboxylase. In neutral solution in the absence of the enzyme, the same reaction proceeds with a half-life of 78 million years (1). It is natural to ask how enzymes arose to meet so formidable a challenge.
The Time Required for Primordial Chemistry to Become EstablishedThe rates of simple reactions, even if they are immeasurably slow at ordinary temperatures, can often be estimated by first determining their rates at elevated temperatures. Plots of the logarithm of the observed rate constants a...