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Testing the precision of bioevents

Published online by Cambridge University Press:  15 May 2009

C. R. C. PAUL  and
M. A. LAMOLDA
C. R. C. PAUL*
Affiliation:
Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK
M. A. LAMOLDA
Affiliation:
Departarmento de Estratigrafía y Paleontología, Facultad de Ciencias, Universidad de Granada, Avenida de Fuentenueva s/n, 18002, Granada, Spain
*
*Author for correspondence: [email protected]
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Abstract

Deciding which of two bioevents is the less diachronous is a common problem in biostratigraphy. The most accurate correlation uses the finest timescale available. Chemostratigraphy or cyclostratigraphy offer a potential precision of about 10 ka. Graphic correlation can then be used to test the precision of bioevents and to quantify any mismatch. It can also be used to determine in which section any event occurs earlier. Application of these ideas to correlation of the Cenomanian–Turonian and Coniacian–Santonian boundaries demonstrates that some bioevents are as precise as chemo- and cyclostratigraphy, but that most are not. Two problems occur with bioevents. First they may not be recognizable in all sections. Second, where they are recognizable, they may be diachronous. In the former case, calculating confidence intervals on known ranges in sections where the relevant fossil has been recorded is an alternative test. Large confidence intervals suggest that both first and last occurrences of a fossil may be diachronous bioevents. At the Cenomanian–Turonian boundary the following bioevents (in stratigraphic order) appear to be reliable time planes for international correlation. The last occurrences of (1) Corolithion kennedyi, (2) Rotalipora greenhornensis, (3) Axopodorhabdus albianus, (4) Rotalipora cushmani, (5) Lithraphidites acutus, (6) Microstaurus chiastius and (7) the first occurrence of Quadrum gartneri. At the Coniacian–Santonian boundary only the first and last occurrences of Platyceramus undulatoplicatus, and the first occurrences of Platyceramus cycloides and Lucianorhabdus cayeuxii have been identified as potentially reliable bioevents.

Keywords

stratigraphic precisiongraphic correlationCenomanian–Turonian boundaryConiacian–Santonian boundarybioevents
Type
Original Article
Information
Geological Magazine , Volume 146 , Issue 5 , September 2009 , pp. 625 - 637
Copyright
Copyright © Cambridge University Press 2009

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