d18O (LS04JOCH): interpretation3_scope: '' has been replaced by 'isotope'
d18O (LS04JOCH): interpretation4_scope: '' has been replaced by 'isotope'

year (LPDd737d3bd): The paleoData_values have changed

Column 'addR93rCKknZaUPZ9tiN', with variable name 'ageEnsemble', was added to the dataset
Column 'addRhUv8fSOSCFYy7mX0', with variable name 'age.rangeHigh', was added to the dataset
Column 'addRlimbiPF3BANHUkhe', with variable name 'age', was added to the dataset
Column 'addRsvshkzzx3sf5bNzu', with variable name 'age.rangeLow', was added to the dataset
Column 'addRVwQ0BEUz3EuaHslb', with variable name 'depth', was added to the dataset
Column 'addRYC9guemEr95BfmpD', with variable name 'depth', was added to the dataset
Column 'LS04JOCH-chron-NA1', with variable name 'depth', was added to the dataset
Column 'LS04JOCH-chron-NA2', with variable name 'age.rangeLow', was added to the dataset
Column 'LS04JOCH-chron-NA3', with variable name 'age.rangeHigh', was added to the dataset
Column 'LS04JOCH-chron-NA4', with variable name 'age', was added to the dataset

Jones, Vivienne J. , Leng, Melanie J. , Solovieva, Nadia , Sloane, Hilary J. , Tarasov, Pavel

Holocene climate of the Kola Peninsula; evidence from the oxygen isotope record of diatom silica

Jones, V. J., Leng, M. J., Solovieva, N., Sloane, H. J. and Tarasov, P.: Holocene climate of the Kola Peninsula; evidence from the oxygen isotope record of diatom silica, Quaternary Science Reviews, 23(7-8), 833–839, doi:10.1016/j.quascirev.2003.06.014, 2004.

Micromass Optima gas-source mass spectrometer with a MultiPrep automated sample preparation device

Piston cores were split, described, and one half of the core was slab sampled at 1-cm intervals. The boxcore was extruded vertically and sampled every 0.5 cm. Samples were washed in deionized water, oven dried, and homogenized prior to coulometric and isotopic analyses [Yuan, 2003]

The unusual dry climate in the MWE was previously attributed to a contraction of the circumpolar vortex that resulted in the atmospheric jet stream remaining to the north of California throughout much of the MWE [Stine, 1994]. Our results support this hypothesis.