Signor–Lipps effect

The Signor–Lipps effect can make extinctions appear more extended in time than they actually are.

The Signor–Lipps effect is a paleontological principle proposed by Philip W. Signor and Jere H. Lipps which states that, since the fossil record of organisms is never complete, neither the first nor the last organism in a given taxon will be recorded as a fossil.[1] The Signor–Lipps effect is often applied specifically to cases of the youngest known fossils of a taxon failing to represent the last appearance of an organism. The inverse, regarding the oldest known fossils failing to represent the first appearance of a taxon, is alternatively called the Jaanusson effect after researcher Valdar Jaanusson, or the Sppil–Rongis effect (Signor–Lipps spelled backwards).[2]

The sporadic nature of the fossil record is reflected in huge gaps spanning a number of epochs

One famous example is the coelacanth, which was thought to have become extinct in the very late Cretaceous – until a live specimen was caught in 1938.[3] The animals known as "Burgess Shale type fauna" are best known from rocks of the Early and Middle Cambrian periods. Since 2006, though, a few fossils of similar animals have been found in rocks from the Ordovician, Silurian, and Early Devonian periods, in other words up to 100 million years after the Burgess Shale.[4][5] The particular way in which such animals have been fossilized may depend on types of ocean chemistry that were present for limited periods of time.[6]

But the Signor–Lipps effect is more important for the difficulties it raises in paleontology:

See also

References

  1. Signor III, P. W. and Lipps, J. H. (1982) "Sampling bias, gradual extinction patterns, and catastrophes in the fossil record", in Geological implications of impacts of large asteroids and comets on the Earth (ed. L. T. Silver and P. H. Schultz), Geological Society of America Special Publication, vol. 190, pp. 291-296.
  2. Heads, M. (2012). "Bayesian transmogrification of clade divergence dates: a critique" (PDF). Journal of Biogeography. 39: 1749–1756. doi:10.1111/j.1365-2699.2012.02784.x.
  3. Jewett, S.L. (11 November 1998). "http://www.washingtonpost.com/wp-srv/national/horizon/nov98/fishstory.htm "On the Trail of the Coelacanth, a Living Fossil". The Washington Post. Retrieved 2009-05-18. External link in |title= (help)
  4. Kühl, G.; Briggs, D.E.G.; Rust, J. (February 2009). "A Great-Appendage Arthropod with a Radial Mouth from the Lower Devonian Hunsrück Slate, Germany". Science. 323 (5915): 771–773. Bibcode:2009Sci...323..771K. doi:10.1126/science.1166586. PMID 19197061.
  5. Siveter, Derek J.; Fortey, R.A., Sutton, M.D., Briggs, D.E.G., and Siveter, David J. (2007). "A Silurian "marrellomorph" arthropod". Proceedings of the Royal Society B. 274 (1623): 2223–2229. doi:10.1098/rspb.2007.0712. PMC 2287322Freely accessible. PMID 17646139. Cite uses deprecated parameter |coauthors= (help)
  6. Butterfield, N.J. (1995). "Secular distribution of Burgess-Shale-type preservation". Lethaia. 28 (1): 1–13. doi:10.1111/j.1502-3931.1995.tb01587.x.

External links

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