A Speleothem Record of Younger Dryas Cooling, Klamath Mountains, Oregon, USA

@article{Vacco2005ASR,
  title={A Speleothem Record of Younger Dryas Cooling, Klamath Mountains, Oregon, USA},
  author={David A. Vacco and Peter U. Clark and Alan C. Mix and Hai Cheng and Richard Lawrence Edwards},
  journal={Quaternary Research},
  year={2005},
  volume={64},
  pages={249 - 256}
}
Abstract A well-dated δ 18O record in a stalagmite from a cave in the Klamath Mountains, Oregon, with a sampling interval of 50 yr, indicates that the climate of this region cooled essentially synchronously with Younger Dryas climate change elsewhere in the Northern Hemisphere. The δ 18O record also indicates significant century-scale temperature variability during the early Holocene. The δ 13C record suggests increasing biomass over the cave through the last deglaciation, with century-scale… 
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