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Quaternary marine terrace chronology, North Canterbury, New Zealand, using amino acid racemization and infrared-stimulated luminescence

Published online by Cambridge University Press:  06 February 2017

David O.S. Oakley ,
Darrell S. Kaufman ,
Thomas W. Gardner ,
Donald M. Fisher  and
Rebecca A. VanderLeest
David O.S. Oakley*
Affiliation:
Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States
Darrell S. Kaufman
Affiliation:
School of Earth Sciences & Environmental Sustainability, Northern Arizona University, Flagstaff, AZ 86011, United States
Thomas W. Gardner
Affiliation:
Department of Geosciences, Trinity University, One Trinity Place, San Antonio, TX 78212, United States
Donald M. Fisher
Affiliation:
Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States
Rebecca A. VanderLeest
Affiliation:
Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States
*
*Corresponding author at: Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States. E-mail address: doo110@psu.edu (D.O.S. Oakley).
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Abstract

Extensive marine terraces along the North Canterbury coast of the South Island of New Zealand record uplift in this tectonically active area. Although the terraces have been studied previously, applications of Quaternary geochronological techniques to the region have been limited. We use infrared-stimulated luminescence (IRSL), amino acid racemization (AAR), and radiocarbon to determine ages of terraces at three locations—Glenafric, Motunau Beach, and Haumuri Bluff. We develop an AAR calibration curve for the mollusk species Tawera spissa from sites of known age, including the sedimentary sequence of the Whanganui Basin. Bayesian model averaging of the results is used to estimate ages of marine shells from the North Canterbury terraces. By using both IRSL and AAR, we are able to confirm ages using two independent dating methods and to identify one IRSL result that is likely in error. We develop new age estimates for the marine terraces of North Canterbury and propose correlations between sites. This terrace chronology differs significantly from most previous studies, highlighting the importance of numerical dating. The most extensive terraces are from marine isotope stages (MISs) 5a and 5c, with partial reoccupation of one terrace during MIS 3, whereas MIS 5e terraces are notably lacking among those dated.

Keywords

Quaternary geochronologyMarine terracesNew ZealandAmino acid racemizationLuminescence
Type
Research Article
Information
Quaternary Research , Volume 87 , Issue 1 , January 2017 , pp. 151 - 167
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2017 

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