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Stable isotope ratios in tree rings have become an important proxy for palaeoclimatology, particularly in temperate regions. Yet temperate forests are often characterized by heterogeneous stand structures, and the effects of stand dynamics on carbon (δ13C) and oxygen isotope ratios (δ18O) in tree rings are not well explored.
In this study, we investigated long‐term trends and offsets in δ18O and δ...
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