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The slopes of flexural horizons revealed in seismic reflection lines are consistent with this, indicating a Te of 2 km to 5 km, although the depths to these horizons are not consistent, perhaps due to a northwards slope, or step, in the pre-flexural surface.
The simulations described here are in agreement with this, indicating that the Ci-VSP C2 domain binds to the membrane via a Ca2+-independent mechanism as is the case for PTEN and auxilin.
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To begin with this indicates that the lack of concern with the Volcano is not primarily a result of ignorance about Cotopaxi.
However, only 9% of questionnaires were returned with this indicated.
Together with the fact that their numbers did not accumulate with time, this indicates survival and eventual re-entry into the cell cycle to complete mitosis.
As neither the hypercapnia nor hypoxemia changed with time, this indicates continued respiratory depression.
In line with expectations, this indicates that sharing of regulatory elements enhances co-expression.
In addition, the effect of a retreat on RT and DDM parameters decreased as a function of prior experience with MT. This indicates that MT creates lasting changes in cognition.
Together with Figure 3, this indicates that Rosetta performs better on alpha-helical proteins.
Moreover, several predicted genetic interactions coincided with existing pathways; this indicates the potential of PARE in predicting partial pathway components.
We obtain qualitatively similar results with this model indicating that our results are robust to this change in grouping rules (see Results section).
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CEO of Professional Science Editing for Scientists @ prosciediting.com