Ammonoids and Quantitative Biochronology—A Unitary Association Perspective

Chapter
Part of the Topics in Geobiology book series (TGBI, volume 44)

Abstract

Ammonoid evolutionary changes have long been recognized to be excellent time markers. They are the major macrofossil group to date and correlate Paleozoic and Mesozoic marine strata. Originations and extinctions of ammonoid species are commonly used to define GSSPs and build high resolution biozonations. Biochronology is now an advanced field with the recent development of computerized, quantitative methods yielding robust biochronological schemes. It has been demonstrated that such quantitative biochronological methods are very efficient to resolve (often complex) biostratigraphic contradictions and produce accurate and high resolution biozonations, thus enabling precise dating and correlations at various spatial scales. Among the available methods, Unitary Associations is the only one that does not violate the integrity of the data by breaking real coexistences or generating spurious coexistences of species. It has been most commonly applied to ammonoids and is thus reviewed here.

Keywords

Ammonoids Biochronology Biostratigraphy Correlation Quantitative methods 

Notes

Acknowledgments

This work is a contribution to the team BioME of the UMR CNRS 6282; it was funded by the CNRS INSU Interrvie. We thank Spencer Lucas and Jean Guex for insightful comments on this manuscript.

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© Springer Science+Business Media Dordrecht 2015

Authors and Affiliations

  1. 1.UMR CNRS 8217 Géosystèmes, UFR des Sciences de la Terre (SN5)Université de Lille 1Villeneuve dAscq cedexFrance
  2. 2.UMR CNRS 6282 BiogéosciencesUniversité de BourgogneDijonFrance
  3. 3.Paläontologisches Institut und MuseumUniversität ZürichZürichSwitzerland

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