Range offset

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[1] 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[2]

  • 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 tracts.[2]

gollark: what
gollark: Ħ = ĸ
gollark: Ħ.
gollark: You do realise that friends are mostly a *good* thing, right?
gollark: It's kind of the opposite. I don't know why you'd want it.

References
  1. Patzkowsky, Mark E.; Holland, Steven M. (2012). Stratigraphic Paleobiology. Chicago: University of Chicago University Press. p. 94.
  2. Holland, Steven M. (2000). "The quality of the fossil record: a sequence stratigraphic perspective". Paleobiology. The Paleontological Society. 26 (4): 148–168.
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