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end{aligned}In Appendix 1, we have noticed the basic features of trend (and cycle), seasonal and irregular components: the trend-cycle or permanent component corresponds to large values close to (f=0) (e.g. in Fig. 5, left part or in Fig. 6, right part).
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This unique feature of Trend I organisms seems to have a major contribution to the PAS.
Another distinct feature of Trend I is that the pairs of instantaneous GC-skew and AT-skew values exhibit significant positive correlations for both oriC-ter (blue points) and ter-oriC (red points) regions along the plus strand.
Although not part of our study, high-resolution paleoclimate data from the past ~130 years have been compiled from various geological archives, and confirm the general features of warming trend over this time interval (Anderson, D.M. et al., 2013, Geophysical Research Letters, v. 40, p. 189-193).
In Figure 9, we illustrate how some key features of misclassified trends diverge from the majority of the trends that are correctly classified.
Panel b) of Fig. 11 uncovers interesting features of these trends.
This map (Fig. 9) shows more relative regular contour lines with local features of different trends and amplitudes.
Specific features of the trends of these dependencies allowed also for an evaluation of presence of the second type of charge carrying species diamagnetic bipolarons and the effects of their interactions with polarons at different potentials.
Let us explore the roles and importance of different features for trend detection.
A more recent feature of this trend has been the increased movement of livestock during the dry season toward the southeast into Mali Kayes Regionn).
Mercifully, violence has not been a significant feature of this trend -- but it has not been absent.
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