In geology, range offset is the time difference between the last fossil occurrence of a taxon and the actual disappearance of this taxon. Range offset can be used as a measure of biostratigraphic precision and determines among others how much information about extinctions can be derived from fossil occurrences.

Definition

The range offset of a taxon is defined as * the time span between the moment in which the highest stratigraphic occurrence of said taxon was deposited and the moment in which the taxon disappeared from the locality or area and/or * the time span between the moment the taxon appears for the first time in the locality or area and the moment in which the lowest stratigraphic occurrence of said taxon was deposited.

Effects of sequence stratigraphy

Range offset is strongly affected by sequence stratigraphy. Simulations show that range offset changes by up to three orders of magnitude dependent on the position in the

systems tract Sequence stratigraphy is a branch of geology, specifically a branch of stratigraphy, that attempts to discern and understand historic geology through time by subdividing and linking sedimentary deposits into unconformity bounded units on a varie ...

References

Biostratigraphy Paleobiology Sequence stratigraphy {{stratigraphy-stub