Age frequency distribution and revised stable isotope curves for New Zealand speleothems: palaeoclimatic implications

The occurrence of speleothems in New Zealand with reversed magnetism indicates that secondary calcite deposition in caves has occurred for more than 780 thousand years (ka). 394 uranium-series dates on 148 speleothems show that such deposition has taken place somewhere in the country with little int...

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Bibliographic Details
Main Authors: Williams Paul W., Neil Helen L., Zhao Jian-Xin
Format: Article
Language:English
Published: University of South Florida Libraries 2010-07-01
Series:International Journal of Speleology
Subjects:
Online Access:http://www.ijs.speleo.it/pdf/73.600.39(2)_Williams.et.al.pdf