For entries where we have calculated a mean paleointensity, the associated uncertainty is one standard deviation.
Second, we calculated a mean IQV for each of the 26 questions (mean IQV per question) for all the participating centers (see Additional file 1).
Third, we calculated a mean IQV per center (based on 26 IQVs) to assess the global variability for each center (Additional file 1).
We therefore calculated a mean FNI value for each map comparison with values ranging from 0 (perfect dissimilarity) to 1 (perfect similarity).
For each modelling scenario (i.e., NFI- and LiDAR-calibrated AGB models), we calculated a mean AGB value from 100 Monte Carlo realizations.
By comparing DAT KD mice to wildtype (WT) littermates in every experiment, we calculated effect sizes for each of the four outcomes and then calculated a mean effect size using a random effects model.
Note that for the analysis of implicit theory, we reverse-scored the fixed theory of ability items and calculated a mean theory of ability score with the incremental items – thus higher scores represented stronger agreement with incremental theory of ability.
Baritz and Strich [30] calculated a mean C content in the humus layer of 20.7 t C/ha for Germany which is slightly above the concentration calculated for the forests of North Rhine-Westphalia.
When the ROM evaluations were considered, we calculated a mean loss of about 5° for flexion extension and 2° for pronation supination. Several studies in the literature evaluated the ROM in patients who had been surgically treated for medial epicondyle fractures.
When the same process was measured for two years we first calculated a mean value for this process over the two years.
Combining the two sets, we calculated a mean crossing time of 0.55 sec (S.D.±0.19 sec), compared to a mean time between crossings of 1.71 sec (S.D.±1.23).
