d18O (SP08ZHCN01A): interpretation4_scope: '' has been replaced by 'isotope'

Finnigan Delta V Advantage mass spectrometer equipped with an automated carbonate preparation system (Gas Bench-II) at the Institute of Geological Sciences, University of Bern.

Precision of d13C and d18O measurements is 0.06% and 0.07% (1s-error) respectively.

Isotope profiles of all stalagmites are very similar, indicating that So-1 d18O and d13C values are not biased by site-, cave- or sample-specific effects (e.g., kinetic fractionation effects), and furthermore that the So-1 record can be used with confidence for environmental and climatic reconstructions.

TP: elevation estimate from Google Earth. ZK, BM 04/01/2019:  we thought we have to change 'Moisture source' to 'precipitation_Isotope' in column BG; but we can not add a single term to the interpretation, even the direction of the interpretation is problematic ... so one possible solution would be to change this record from 'primary timeseries' to non 'primary timeseries'? but discussed with Bronwen during and we have to discuss this further before qualifying as  'FALSE' in column CB (intended mainly for sites with 2 possible records ans flagging the one to be used)

Fleitmann, D., Cheng, H., Badertscher, S., Edwards, R. L., Mudelsee, M., Goektuerk, O. M., Fankhauser, A., Pickering, R., Raible, C. C., Matter, A., Kramers, J. and Tueysuez, O.: Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey, Geophysical Research Letters, 36(19), doi:10.1029/2009gl040050, 2009.

d18O (SP09FLTR01A): interpretation2_scope: '' has been replaced by 'isotope'
d18O (SP09FLTR01A): interpretation3_scope: '' has been replaced by 'isotope'

LR06-B1 - continuous-flow GV2003 gas-source isotope ratio mass spectrometer at the University of Newcastle, Australia; LR06-B3 - automated individual-carbonate reaction Kiel device coupled to a Finnigan MAT-251 dual-inlet stable isotope mass spectrometer at the Research School of Earth Sciences, ANU.