Speleothem stable isotope records interpreted within a multi-proxy framework and implications for New Zealand palaeoclimate reconstruction (original) (raw)
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This research focuses on the interpretation of speleothem stable isotope records through a multi-proxy framework to reconstruct palaeoclimate conditions in New Zealand. By analyzing the stable oxygen and carbon isotopes from calcite deposits in caves, the study identifies distinct climatic conditions over various periods, demonstrating how these proxies indicate changes in precipitation and temperatures. The findings reveal insights into the past climate regimes and highlight the complexity of New Zealand's climatic history.
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