Abstract
A method has been devised which enables the direct measurement of ATP and adenine nucleotide pool turnover. The method is based upon the incorporation of 32 PO 4 into the α-, β-, γ-P positions of ATP. 32 PO 4 uptake time course experiments were conducted in seawater and freshwater samples. Determinations of the ATP concentration and of the specific activities of the α-, β-, and γ-positioned 32 P in ATP at sequential time points enables the calculation of: (1) the pool size of total biologically available P in water samples; (2) the rate of biochemical energy flux; and (3) the mean microbial community specific growth rate. This method is relatively simple, straightforward and extremely sensitive. It has, therefore, the advantage that it can be employed in environments where dissolved P levels are too low to obtain reliable P flux estimates using existing techniques.

This publication has 0 references indexed in Scilit: