The Exxon global cycle chart is now widely used as a stratigraphic cor
relation tool, although it remains a controversial one. It requires co
ntinual testing against new data, but tests are difficult at present b
ecause the assumptions behind the chart have not so far been precisely
specified. Some reasonable assumptions are made here, and a few simpl
e tests are then proposed on the basis of these. Some of these tests a
re appropriate to specific situations in which the test data are estim
ated sequence boundary ages: others are for situations in which sets o
f undated sequence boundaries are available that are only known to lie
within particular parts of the Exxon chart. No general test for the E
xxon chart has yet been developed, and the specifications for such a t
est are discussed.