Asian continental isoscapes of tree-ring δ18O: implications for paleoclimate and paleoenvironment

Continental-scale isoscapes of tree-ring oxygen isotopes (δ¹⁸O_TR) are crucial for understanding atmospheric circulation dynamics, interpreting climatic significance, and tracing wood provenance. However, continental-scale δ¹⁸O_TR isoscapes remain underdeveloped. We compiled 313 multi-year averaged δ¹⁸O_TR records across Asia and generated isoscapes using two machine learning approaches: XGBoost and Random Forest. Results reveal a 'sandwich' pattern: depleted values at high (>50°N) and low (<30°N) latitudes, enriched values at mid-latitudes (30°N-50°N). This pattern closely resembles the distribution of precipitation δ¹⁸O (δ¹⁸O_P). Correlation and commonality analyses confirm δ¹⁸O_P as the primary driver of δ¹⁸O_TR isoscape patterns across Asia. Continental-scale δ¹⁸O_TR-elevation relationships are generally insignificant, except in Indian Summer Monsoon regions showing significant negative correlations (<i>r</i> = -0.69, <i>p</i> < 0.05). These findings suggest that δ¹⁸O-based paleoaltimetry reconstructions work best in regions with dominant moisture sources such as Indian Summer Monsoon regions. This study provides Asia's first continental-scale δ¹⁸O_TR isoscapes, establishing a foundation for atmospheric circulation and dendroprovenancing research.