Erratum.

Saunders KM, Grosjean M, Hodgson DA (2013) A 950 yr temperature reconstruction from Duckhole Lake, southern Tasmania, Australia. The Holocene 23(6) 771–783. DOI: <named-content>10.1177/0959683612470176</named-content>.Page 771: AbstractThe calibration model was based on a negative, not positive, relationship between trough area (R_570/630) and temperature. The corrected model is: R = −0.56, p_auto < 0.05, root mean squared error of prediction (RMSEP) = 0.21°C, five-year filtered data, calibration period 1911–2000.Page 774 ‘Reflectance spectroscopy’The correlations in this paragraph are negative (not positive as stated in the original paper). The paragraph should read as follows:VIS-RS data are summarized in Figure 3. R_570/630 and R_660/670 fluctuated throughout the core with a slight overall decreasing trend towards the surface. R_570/630 was positively correlated to R_660/670 (R = 0.5, p < 0.05). R_650;700 and RABD_660;670 were highly significantly correlated (R = −0.85, p < 0.05). R_650;700 was weakly correlated to R_660/670 (R = 0.36). R_650;700, RABD_660;670 and R_660/670 were significantly correlated with water content (R = −0.83, 0.60 and –0.53, respectively, p < 0.05). Once corrected for water content, the negative correlation between R_650;700 and R_660/670 increased (R = −0.41, p < 0.05), while there was no longer a correlation between RABD_660;670 and R_660/670.Page 775 ‘Calibration with meteorological data’The R values referred to should be negative:All VIS-RS-derived proxies (R_650;700, RABD_660;670, R_660/670 and R_570/630) were calibrated to monthly and annual temperature (mean, maximum and minimum) and precipitation (total) for the period AD 1911–2000. R_650;700 was most highly and significantly correlated to mean annual (January–December) temperature (R = −0.84, p_auto < 0.05, p_auto after detrending < 0.05).The correlation between R_650;700 and annual temperature was highly significant after applying a five-year triangular filter (non-detrended: R = −0.85, p_auto < 0.001; Figure 4a) and remained significant when detrended (R = −0.29, p_auto < 0.05; Figure 4b).Consequently, as R_650;700 (reflecting chlorophylls and derivatives) correlated best to temperature, it was used to develop an annual temperature calibration model for Duckhole Lake: R = −0.56, p_auto < 0.05, RMSEP = 0.21°C, where both R and p were adjusted for autocorrelation.Page 778 Figure 4The y axes of the lower panels in 4(a) and 4(b) were not correct. The corrected figure is above: <named-content> Comparison of R650;700 and annual mean temperature: (a) non-detrended R650;700 and mean annual temperature; (b) detrended data. All data are five-year triangular filtered. Note: reversed y axes in the lower panels (proxy data) of (a) and (b). </named-content><graphic></graphic> [ABSTRACT FROM AUTHOR]