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Climatic implications of D/H ratios of meteoric water over North America (9500–22,000 B.P.) as inferred from ancient wood cellulose CH hydrogen

HydrometeorologyEngineeringEnvironmental GeochemistryPaleoenvironmental ChangeMeteoric WaterD/h RatiosIsotope GeochemistryGeochemistryPaleoclimatologyNorth AmericaEarth ScienceEarth's ClimateClimate Change