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Tortuosity distribution indicated two populations of data points one of which corresponded to the oolitic and skeletal-intraclastic lithofacies, referred to as "granular electro-facies"; and the other to the muddy and the dolomitic lithofacies, named "dolomitic-muddy electro-facies".
Provided one keeps in mind the limitations of the technique, this can be a highly effective tool in analyzing large populations of data.
Significant differences between different populations of data were tested with Student t-test for unpaired observations.
This means that there were 2 populations of data pixels in the CA3 cell layer that have different sensitivities to kainate (Fig. 4e).
Comparisons between two populations of data were made using the Student's unpaired t-test with a confidence limit for significance set at 0.05 or less.
ANOVA was used to test statistical significance between different populations of data.
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In both data sets there appears to be a population of data that have a decreased Fe/Se ratio.
The corsets are the small set of points that represent the larger population of data and maintain the actual properties of overall population.
This suggests that the transition between PE and HFA is represented by one single population of data, likely reflecting a unique process characterized by a continuum of thermal energy release.
Conversely, the transition from HFA to SE is represented by the occurrence of a new population of data, likely related to a change in the source of the anomalies, i.e., hydrothermal versus magmatic origin.
Each set of detected proteins each forms a three-lobed histogram, with the central population of data points containing proteins observed in both states, while the outer histograms contain proteins observed only in one state, but not the other.
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