Note that depths are cm without intervening turbidites - absolute depth estimates are therefore larger

SW Chinese calibration dataset (Zhang et al 2016); human impact and dating should not be a major issue for this site

reliable (R1fh5PMjNja): paleoData_proxyGeneral: '' has been replaced by 'chironomid'
uncertainty (RIzvUYvkjbJ): paleoData_proxyGeneral: '' has been replaced by 'chironomid'
uncertainty (RycHLoobRmE): paleoData_proxyGeneral: '' has been replaced by 'chironomid'

Chang, Jie; Zhang, Enlou; Liu, Enfeng; Shulmeister, James

Summer temperature variability inferred from subfossil chironomid assemblages from the south-east margin of the Qinghai   Tibetan Plateau for the last 5000 years

Variable name changed from (230Th/232Th)b to 230Th/232Th b during update from DKs csv files.

Variable name changed from (230Th/232Th)b_error to 230Th/232Th b_error during update from DKs csv files.

Variable name changed from (230Th/238Th)b to 230Th/238Th b during update from DKs csv files.

Variable name changed from (230Th/238Th)b_error to 230Th/238Th b_error during update from DKs csv files.

Variable name changed from Age(raw)c to Age raw c during update from DKs csv files.

Variable name changed from Age(raw)c_error to Age raw c_error during update from DKs csv files.

Variable name changed from Age(corr)d to age during update from DKs csv files.

Variable name changed from Age(corr)d_error to Age error during update from DKs csv files.

Variable name changed from depth to type during update from DKs csv files.

Wang, Canfa; Bendle, James A.; Zhang, Hongbin; Yang, Yi; Liu, Deng; Huang, Junhua; Cui, Jingwei; Xie, Shucheng

Holocene temperature and hydrological changes reconstructed by bacterial 3-hydroxy fatty acids in a stalagmite from central China

Where midpoint is n.25 or n.75, sample is 0.5cm thick. Where midpoint is n.5, sample is 1cm thick. Where midpoint is whole number, sample is 2cm thick.

44-lake surface water temperature training set from Sierra Nevada (Porinchu et al. 2002)

two separate curves for different portions of core (see Potito et al. 2006)