Sg. Pemberton et al., Significance of ichnofossils to genetic stratigraphy - Examples from the Cretaceous of Alberta, Canada, SCI CHINA D, 43(5), 2000, pp. 541-560
Trace fossils represent both sedimentological and paleontological entities,
representing a unique blending of potential environmental indicators in th
e rock record. Trace fossils and trace fossil suites can be employed effect
ively to aid in the recognition of various discontinuity types and to assis
t in their genetic interpretation. Ichnology may be employed to resolve sur
faces of stratigraphic significance in two main ways: 1) through the identi
fication of discontinuities using substrate-controlled ichnofacies, and 2)
through careful analysis of vertical softground (penecontemporaneous) ichno
logic successions (analogous to facies successions). Ichnological analysis
is a valuable tool in genetic stratigraphic studies. Integrating the data d
erived from substrate-controlled ichnofacies with paleoecological data from
vertical ichnologic successions greatly enhances the recognition and inter
pretation of a wide variety of stratigraphic surfaces. When this is coupled
with conventional facies analysis and sequence stratigraphy, a powerful ap
proach to the interpretation of the rock record is generated.