Dendroisotopes is the study of using the isotope values measured in tree rings to obtain and/or use climatic or environmental information archived in the measurement data.

 

TRRC is establishing long-term tree-ring δ18O chronology and using the chronology to reconstruct the paleoclimate. So far, we are focusing on the topic below.

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• Investigating the potential of tree-ring δ18O chronology in dating archaeological woods.

• Investigating the climatic factors being able to be reconstructed using tree-ring δ18O chronology.