depth (chron1): The chronData_values have changed
age (chron15): The chronData_values have changed
SD (chron16): The chronData_values have changed
age14C (chron2): The chronData_values have changed
SD (chron3): The chronData_values have changed
labID (chron9): The chronData_values have changed

Rosqvist, G. C. , Leng, M. J. , Jonsson, C.

North Atlantic region atmospheric circulation dynamics inferred from a late-Holocene lacustrine carbonate isotope record, northern Swedish Lapland

Rosqvist, G. C., Leng, M. J. and Jonsson, C.: North Atlantic region atmospheric circulation dynamics inferred from a late-Holocene lacustrine carbonate isotope record, northern Swedish Lapland, The Holocene, 17(7), 867–873, doi:10.1177/0959683607080508, 2007.

GV IsoPrime IRMS coupled with an online carbonate preparation system (MultiPrep)

Precipitation amount (as a function of temperature)

I just moved this from the Rejected list - not sure why it was there and not here? Data also published in Yan et al 2011 (Nat Comms) and data on NOAA from that paper, but from what I can tell, isotope data are same as in 2008 paper

Liu, X., Sun, L., Wei, G., Wang., Y., Liu, K., Wu, X.

Liu, X., Sun, L., Wei, G., Wang, Y., Yan, H., Liu, K. and Wu, X.: A 1,100-year palaeoenvironmental record inferred from stable isotope and trace element compositions of ostracode and plant caryopses in sediments of Cattle Pond, Dongdao Island, South China Sea, Journal of Paleolimnology, 40(4), 987–1002, doi:10.1007/s10933-008-9211-9, 2008.

LS08LICA01a: updated 'useInAgeModel' values to match publication

d18O (LS08LICA01a): interpretation3_scope: '' has been replaced by 'isotope'
d18O (LS08LICA01a): interpretation4_scope: '' has been replaced by 'isotope'

Finnigan MAT 252 massspectrometer coupled to a Kiel II carbonate sampling device

sample was  homogenized  prior to division into aliquots for isotope and diatom  analyses; Sediment for isotopic analysis was reacted with 2% sodium hypochlorite to remove organic matter and rinsed five times. The sediment was then sieved at 63 mm to remove ostracodes, shell material, and charaphyte sheaths. The flowthrough from the sieve was collected, freezedried, homogenized, and analyzed for carbon and oxygen isotopes