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Some skull and scale features indicate derivation from palaeonisciform ancestors.
These features indicate extensive chemical exchange with seawater.
These features indicate that IL-25, but not IL-33 and/or TSLP, is essential for resistance to infection.
Additional microstructural features indicate that powder particles have been subjected to different modifications during spraying.
These features indicate the improvement of osseointegration for this sort of load bearing Ti implants.
These features indicate that form II should be a high entropy, conformationally disordered phase.
These features indicate intermittent and generally unchannelized stream flow, with repeated exposure to air.
Several morphological features indicate a change in water flux direction after the main erosive phase.
Together, these features indicate that non-classical monocytes comprise the most senescent subset, followed sequentially by the intermediate and then the classical subset.
In sum, all these petrographical and geochemical features indicate that North Aït Ahmane serpentinites endured an abyssal black smoker-type hydrothermalism before the obduction of the ophiolitic sequence.
Keratinous claws, however, are rare in living amphibians; their microstructure and other features indicate that they probably originated independently from those in amniotes.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com