Climatic change at the end of the last glaciation in Japan inferred from pollen in three cores from the Northwest Pacific Ocean
The AA. examine paleoclimatic evidence from northeast Asia. The primary data are pollen time-series from three high sedimentation-rate marine cores from which a cooling event described as coeval with the Younger Dryas Chronozone has been identified
This paper presents the results of a marine geological survey of the South Orkney Plateau. Field work for this project was conducted during the austral summer of 1985 and consisted of piston coring and the acquisition of high-resolution (sparker
reversal in northern Europe and an increase in the vigor of atmospheric circulation recorded by Greenland ice cores. Climatic fluctuations in high latitude areas during Younger Dryas time may reflect variations in the CO2 content of the atmosphere.
The authors measured hydraulic conductivity (saturated and unsaturated) on 127 soil cores, which were taken in different horizons of a wide variety of Belgian soil series. The hot air method and the crust method were combined to obtain the complete