The distribution of field data (e.g., tree basal area, organic layer and fibric horizon thicknesses) within each position class provided additional information for corroborating the assignment of each class to a defined paludification type.
Due to their phylogenetic position, class II and class III ACBPs were suggested to be functionally related [ 32].
Coding sequences for secondary structure scaffolds that position Class I and II catalytic residues also support Sense/Antisense (SAS) ancestry.
The composition of stands within LMUs grouped by slope position class (canyon, mid-slope, ridge) all demonstrated a declining density of trees with increasing dbh size.
In pair-wise comparisons among all four aligners, we find that in both S1 and S2 data sets, suppressing multiple alignments decreases the number of reads aligned to different positions (class 2) in all comparison pairs, while the number of reads aligned to same positions (class 1) stays the same (Tables 5, 6, 7, 8).
While a clear trend regarding grid cell size and window size can be observed with regard to the difference between macro and meso scale topographic positions, the overall classification accuracy regarding the different topographic position classes was less promising.
A semi-automated classification method based on TPI and slope was firstly used to create six initial topographic position classes: deep-depressions, lower-slope depressions, flat surfaces, mid-slopes, upper-slopes, and hilltops.
They were sorted in 35 position classes (Pcls) defined first by the same location in the cox1 CDS sequence.
For each of the 10,000 instances, for each considered window, we permute the footprint counts of the 10 position classes.
In 44 alignment positions, class-specific residues are replaced in the other class with residues having different properties, according to the chemical features of their side-chain group (hydrophobic, polar basic, polar acidic and polar uncharged).
