Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution
journal contributionposted on 05.07.2018 by Anieke Brombacher, Paul A. Wilson, Ian Bailey, Thomas H. G. Ezard
Any type of content formally published in an academic journal, usually following a peer-review process.
S1: Study species Globoconella puncticulata (a) and Truncorotalia crassaformis (b). The scale bars represent 100 μm. S2: Map of study site IODP Site U1313 in the North Atlantic. S3: Autocorrelation plots for traits of Globoconella puncticulata showing autocorrelation in the original time series (a-c) but not in the first differences (d-f). S4: Autocorrelation plots for traits of Truncorotalia crassaformis showing autocorrelation in the original time series (a-c) but not in the first differences (d-f ). Only area in T. crassaformis still contained a small amount of autocorrelation in the first differences time series. However, comparison of two Generalized Least Squares models with and without autocorrelation (by setting the continuous auto-correlation parameter phi=0.3 and phi=0.1, which converges to 0 under maximum likelihood, respectively) show lower AIC values for the model without autocorrelation, implying that the model with temporal autocorrelation is actually a poorer fit to the data than that without. S5: ΔAIC values showing the added relative importance of each environmental parameter or combination of parameters to the total model.