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. 2020 Jan 14;26(3):1259–1270. doi: 10.1111/gcb.14952

Table 3.

Results from the four mixed‐effects models used to estimate individual lake stability, and explore between‐lake patterns in stability

Variable DCA 1 South DCA 2 South DCA 1 North DCA 2 North
Effect sizes (β)
Latitude 0.04 (−0.02, 0.1) −0.08 (−0.15, 0) −0.02 (−0.1, 0.06) −0.06 (−0.14, 0.02)
Size 0 (−0.06, 0.05) 0.08 (0.02, 0.14) −0.01 (−0.08, 0.06) 0.10 (0.03, 0.16)
Richness −0.15 (−0.23, −0.06) −0.07 (−0.17, 0.02) −0.26 (−0.36, −0.15) −0.16 (−0.25, −0.06)
Alkalinity 0.02 (−0.06, 0.1) −0.06 (−0.15, 0.03) 0.09 (0, 0.17) −0.01 (−0.08, 0.06)
Total phosphorus −0.04 (−0.13, 0.04) 0.09 (−0.02, 0.19) 0.27 (0.12, 0.42) −0.07 (−0.19, 0.07)
Between‐lake variance in stability 0.07 (0.04, 0.10) 0.12 (0.08, 0.17) 0.09 (0.06, 0.14) 0.07 (0.04. 0.10)

In this table, we present results of effects on the heterogeneous residual variances, used to study the drivers of community stability (inverse of variation in detrended correspondence analysis [DCA] scores). Models were performed separately for DCA axes 1 and 2 and for the two ecoregions (north and south). We present mean and 95% credible intervals. We also depict in bold those estimates where the 95% credible intervals did not overlap zero.