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For example, Levallois technology is shown to be optimal in terms of raw material economy and flake utility (17), and Levallois flakes detached from preferential Levallois cores form a statistically robust group with morphologically desirable characteristics that are distinguishable from those of other flakes (19).
These cores form a bulge-helix-bulge (BHB) motif (Fig. 4 b-e) post-transcription that is very similar to the characterized BHB motifs of intron-containing archaeal tRNAs [ 41] and 23S rRNAs [ 23], both of which are excised by the same splicing endoribonuclease [ 23, 42– 42].
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N- and C-cores form a nucleotide-binding pocket within which are arrayed conserved amino acid helicase motifs.
In particular, the side chain of K431 in the ZIKV helicase points to the inner core, forming a salt bridge with the side chain of D410 and a weak hydrogen bond with N3 atom of the adenine base (Fig. 4C).
The shell grew at the expense of the Ni-core, forming a passivating layer of NiO, as confirmed and estimated by the X-ray absorption near-edge structure (XANES) measurements.
The flower-like Co3O4 shell on the surface of the CNF core formed a highly porous three-dimensional (3D) structure with a large surface area of 332 m2 g−1 and a mesoporous surface area of 176 m2 g−176
The collapsed core formed a neutron star, an extremely compact and highly magnetized object with roughly the mass of the Sun, but with a radius of only about six miles.
In a metabolic network, the core forms a giant cluster, where the nodes are densely interconnected.
Cell encapsulation in a semi-permeable membrane differs from bead immobilization in that the cells grow inside a liquid core, forming a dense cell pellet inside the capsule rather than being dispersed in the pores of the alginate matrix [ 10].
Key functional amino acid residues, identified by site-directed mutagenesis, reside in the three amphipathic and conserved transmembrane helices II, V and VI, which are supposed to constitute an inner core forming a channel [ 14, 18, 29, 30].
In all cases, Fe will crystallize at the top of the core, forming an iron "snow" (Stewart et al. 2007).
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CEO of Professional Science Editing for Scientists @ prosciediting.com