Item talk:Q250466
From geokb
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"abstract": "A 1000-yr history of climate change in the central Yukon Territory, Canada, is inferred from sediment composition and isotope geochemistry from small, groundwater fed, Seven Mile Lake. Recent observations of lake-water \u03b418O, lake level, river discharge, and climate variations, suggest that changes in regional effective moisture (precipitation minus evaporation) are reflected by the lake\u2019s hydrologic balance. The observations indicate that the lake is currently\u00a018O-enriched by summer evaporation and that during years of increased precipitation, when groundwater inflow rates to the lake increase, lake-water \u03b418O values decrease. Past lake-water \u03b418O values are inferred from oxygen isotope ratios of fine-grained sedimentary endogenic carbonate. Variations in carbonate \u03b418O, supplemented by those in carbonate and organic \u03b413C, C/N ratios, and organic carbon, carbonate and biogenic silica accumulation rates, document changes in effective moisture at decadal time scales during the early Little Ice Age period to present. Results indicate that between \u223cAD 1000 and 1600, effective moisture was higher than today. A shift to more arid climate conditions occurred after \u223cAD 1650. The 19th and 20th centuries have been the driest of the past millennium. Temporal variations correspond with inferred shifts in summer evaporation from Marcella Lake \u03b418O, a similarly small, stratified, alkaline lake located \u223c250\u00a0km to the southwest, suggesting that the combined reconstructions accurately document the regional paleoclimate of the east-central interior. Comparison with regional glacial activity suggests differing regional moisture patterns during early and late Little Ice Age advances.",
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