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Temperature signal instability of tree-ring δ13C chronology in the northeastern Qinghai-Tibetan Plateau
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文摘

A millennium-long tree-ring δ13C chronology was developed in the northeastern Qinghai–Tibetan Plateau.

Tree-ring δ13C responded instability to temperature variations in the last millennium.

Correlations of tree-ring δ13C and δ18O series were also temporal instability over the last thousand years.

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