Two different conceptual models underlie the application of sequence strati
graphy by Exxon stratigraphers and later researchers. One, the global sea-l
evel model (GSM), relates to presumed sea-level behaviour through time; the
other, the sequence stratigraphic model (SSM), relates to the stratigraphi
c record produced during a single cycle of sea-level change. Though the two
models are inter-related they are logically distinct, and it is important
to test them separately. A summary is presented of the nature of the two mo
dels, and of the nomenclature that is used in their description. It is conc
luded (a) that the global sea-level model comprises an assembly of local re
lative sea-level events which are widely recognisable within their parent s
edimentary basin; and (b) that the sequence stratigraphic model is robust,
and its application is therefore an insightful way to approach the interpre
tation of sedimentary rocks. (C) 1998 Elsevier Science B.V. All rights rese
rved.