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These length scales may not be sufficiently small to estimate the pore-fluid pressures in a limited local region.
These length scales are typically dominated by the magnetic field created by the spatial variation in structure and composition of the Earth's crust and upper mantle (Thébault et al., 2010 for a review).
These length and nucleotide variants constitute more than 50% of the total EBV miRNA reads, and many sequences show significant deviation from the miRBase reference sequence.
These length variations have been mainly attributed to enzymatic modification such as RNA editing [18], 3'-editing [19], exonuclease activities [20], [21], etc. Presently, there is little understanding of the functional role of these homologs of highly abundant miRNAs.
These length scales bridge from molecular scale to microscale and finally to the macroscale.
These length expansions are caused by large insertions consisting of tandemly repeated motifs.
These length convergences are easily amenable to homology establishment using secondary structure as a guide.
These length and mismatch criteria were selected based on our search parameters as described in the Materials and methods section.
These length changes through the cell cycle are consistent with previous descriptions of procyclic T. brucei [ 18].
These length differences, ddBS, were calculated for all monophyletic groupings of extant taxa supported by the 74-OTU supermatrix.
These length polymorphisms are mostly due to variation in the numbers of different internal subrepeats present in the IGS.
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