Table 1: Results from Creno LandClim fire and vegetation simulations. Simulation runs were based on an unlimited fire size and 10,000 permutations of randomization tests performed per time period. Proportion of the species set and abundances matching the plant macroremain assemblages (plant parts preserved in the sediment core of Creno Lake, more details in Leys, et al. 2014 [15] are reported. Simulations were performed using three temperature permutations (0 ℃, + 1 ℃, + 2 ℃) compared with current mean temperature, and 6 fire-frequency treatments (from no fire to extreme). The age reported are expressed in age calibrated before present (with 0 corresponding to 1950 AD), and correspond to a time span of 1000 years. The shaded cells highlight the highest proportion values per line.
| Model | Temperature | 0 | 1 | 2 | |||||||||||||||
| Model | Fire frequency | extreme | high | medium | low | very low | No fire | extreme | high | medium | low | very low | No fire | extreme | high | medium | low | very low | No fire |
| 400 | 0.50 | 0.20 | 0.08 | 0.08 | 0.05 | 0.05 | 0.04 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | |
| 1400 | 0.52 | 0.18 | 0.10 | 0.07 | 0.05 | 0.03 | 0.04 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | |
| 2400 | 0.23 | 0.07 | 0.01 | 0.01 | 0.01 | 0.00 | 0.25 | 0.12 | 0.06 | 0.05 | 0.04 | 0.05 | 0.10 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 | |
| 3400 | 0.46 | 0.21 | 0.08 | 0.07 | 0.07 | 0.06 | 0.05 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | |
| 4400 | 0.50 | 0.21 | 0.09 | 0.08 | 0.05 | 0.03 | 0.04 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | |
| 5400 | 0.45 | 0.20 | 0.10 | 0.07 | 0.06 | 0.04 | 0.05 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | |
| 6400 | 0.49 | 0.20 | 0.10 | 0.07 | 0.05 | 0.03 | 0.06 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | |