average time resolution from 22 years at the top to 5 years at the base.

SUNDQVIST, H. S., HOLMGREN, K., MOBERG, A., SPATL, C. and MANGINI, A.: Stable isotopes in a stalagmite from NW Sweden document environmental changes over the past 4000 years, Boreas, 39(1), 77–86, doi:10.1111/j.1502-3885.2009.00099.x, 2010.

d18O (SP10SUSE01A): interpretation4_scope: '' has been replaced by 'isotope'

Automated individual-carbonate reaction (Kiel) device coupled with a Finnigan MAT252 mass spectrometer at the National Institute of Water and Atmospheric Research (NIWA).

External precission of 0.05 for d18O and 0.02 for d13C.

Replication of the isotope signal in other stalagmites from other caves

not said, but ages were determined by TIMS or alpha-counting (info from Williams et al., 2005)

0.35 per mil of d18O change per degree of Temperature change

this manuscript and Williams et al., 2005

Evident relationship of speleothem ?18O and temperature, which is generally positive (Williams et al. 2004, 2005, Whittaker 2008). It is probable that significant changes to d18Op would have resulted from perturbations in oceanic and atmospheric circulation patterns that altered the relative mix of vapour from subtropical and sub-Antarctic sources

Changes in annual temperature modulated by oceanic circulation and gradients

There is a presend-day positive relationship between ?18O of precipitation and temperature of +0.35? / i¿½C.,Calculations with dripwater d18O values and calcite d18O values,,1 to 10,lamina counting, high resolution sampling to 100 microns,temperature,,year,,,,,,rainfall amount and source,,,,,,,,,,,,,https://docs.google.com/spreadsheets/d/1WNzh05-BveXAV0WvY6duO7iRR_drkRSgmosDu0BBmyU

Calculated initial 234U/U238 in the sub-sample

Analytical uncertainty of calculated 234U/U238 initial

Analytical uncertainty of calculated 234U/U238

Williams, P., Neil, H. and Zhao, J.-X.: Age frequency distribution and revised stable isotope curves for New Zealand speleothems: palaeoclimatic implications, International Journal of Speleology, 39(2), 99–112, doi:10.5038/1827-806x.39.2.5, 2010.