d18O (IC08VI7701A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC08VI7701A): interpretation4_scope: '' has been replaced by 'isotope'

d18O (IC08VI7901A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC08VI7901A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRdCUSZK7JY9X7BRO8', with variable name 'yearEnsemble', was added to the dataset

d18O (IC08VI8401A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC08VI8401A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRgyd0UgkRU3DtrWto', with variable name 'yearEnsemble', was added to the dataset

d18O (IC08VI8701A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC08VI8701A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRLiwZ3NvGQutcambR', with variable name 'yearEnsemble', was added to the dataset

d18O (IC08VIRE01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC08VIRE01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRQiba1JIFGEoWWAcJ', with variable name 'yearEnsemble', was added to the dataset

isotope interpretation direction missing - HRS -->TO: corrected

chronology based on annual layer counting, bomb reference horizon

d18O (IC08VISV01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC08VISV01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRlpwBQCWFLPXII44e', with variable name 'yearEnsemble', was added to the dataset

Vimeux, F., de Angelis, M., Ginot, P., Magand, O., Casassa, G., Pouyaud, B., Falourd, S. and Johnsen, S.: A promising location in Patagonia for paleoclimate and paleoenvironmental reconstructions revealed by a shallow firn core from Monte San Valentin (Northern Patagonia Icefield, Chile), Journal of Geophysical Research, 113(D16), doi:10.1029/2007jd009502, 2008.

age model based on volcanic horizons, beta activity and counting of annual layers (seasonal variations of stable isotopes)

correlation to meteorological data: "A good correlation between 10-year averaged d18O data and Marcha€“November Barnaul temperatures was found (Figure S3, r = 0.83, p < 0.001 for the period 1850a€“1980), suggesting that d18O in precipitation at Belukha glacier is suitable as a proxy of atmospheric temperature, which is in good agreement with previous studies."