d18O (IC00STTY01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC00STTY01A): interpretation1_variable: 'T' has been replaced by 'temperature'
d18O (IC00STTY01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC00STTY01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

d18O (IC00STTY01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC00STTY01A): interpretation1_variable: 'T' has been replaced by 'temperature'
d18O (IC00STTY01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC00STTY01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

d18O (IC00STTY01A): paleoData_longName: '' has been replaced by 'AD'
year (MAT3bd57ce72c): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT3bd57ce72c): paleoData_longName: '' has been replaced by 'AD'

Steig, E. J., Morse, D. L., Waddington, E. D., Stuiver, M., Grootes, P. M., Mayewski, P. A., Twickler, M. S. and Whitlow, S. I.: Wisconsinan and holocene climate history from an ice core at taylor dome, western ross embayment, antarctica, Geografiska Annaler: Series A, Physical Geography, 82(2-3), 213–235, doi:10.1111/j.0435-3676.2000.00122.x, 2000.

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

Finnigan Mat Delta Plus mass spectrometers

correlation to meteorological data, ("...these data provide qualitative support for the hypothesis that temperature, not the amount effect, is the dominant process controlling d18O over the Tibetan Plateau.")

Yao, T., Thompson, L. G., Mosley-Thompson, E., Zhihong, Y., Xingping, Z., and Lin, P.-N.: 1996,Climatological Significance of I´18O in North Tibetan Ice Cores, J. Geophys. Res. 101, 29531a€“29537

isotope interpretation 1 field has an error (move to isotope interpretation 2?) - BK --> TO:corrected

Yao, T., Thompson, L. G., Mosley-Thompson, E., Zhihong, Y., Xingping, Z., and Lin, P.-N.: 1996,Climatological Significance of ?18O in North Tibetan Ice Cores, J. Geophys. Res. 101, 29531?29537