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In light of this, searches for prophage-like elements revealed that B. longum subsp. longum NCIMB 8809 and B. longum subsp. longum CCUG 30698 harbor prophage-like elements (Table 2).
Detection of genes encoded on mobile elements revealed that none of the isolates contained a SCCmec cassette or the phage-encoded Panton-Valentine leukocidin gene.
Analysis of the variable region of Hatvine-6 elements revealed that these sequences often share high sequence identity to genic (introns and exons) as well as non-genic grapevine sequences (Figure 5).
An analysis of repetitive elements revealed that 39.8%% of the end sequences consisted of repetitive DNA.
The phylogenetic analysis of the reverse transcriptase (RT) sequences from these elements revealed that they consist of two major subgroups.
More detailed analyses of these repetitive elements revealed that many of them are actually special cases of TEs.
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Being zero, the next pair of elements reveals that the intermediate node 2 is not used in the route.
The analysis of the orbital elements reveals that the loss of the initial configuration is mostly due to variations of RAAN.
The present study of the mutual interaction effect between the array elements reveals that the interaction effects are relatively less for a 120° segmented circular array.
It is shown that the solubilities strongly depend on the C-activity and binder matrix elements, revealing that Ni dissolves most W and Fe most C out of the investigated systems.
Geochemical discrimination systematics built on immobile trace elements reveal that the basaltic units of the Phanerozoic ophiolites are dominantly subduction-related (75%), linked to backarc processes and characterized by a strong MORB component, similar to ophiolites in Precambrian greenstone sequences (85%).
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