In general, tectonic activity is interpreted to be the main driving force for the formation and evolution of these landforms, whilst climate change is suggested to be of minor importance.
Such activity-dependent changes are interpreted to be homeostatic because the direction of the alterations are such that they appear to counteract the imposed change in activity, resulting in stabilization of firing rates within the appropriate ranges [2].
The dynamic patterns of extracellular DA concentrations resulting from these changes in activity are interpreted by MSN through the differential activation of D1 and D2 receptors located primarily in striatonigral and striatopallidal circuits, respectively [ 150, 184].
Decreased parasympathetic activity and increased sympathetic activity are interpreted as a state of autonomic hypervigilance [ 46, 47].
Decreased parasympathetic activity and increased sympathetic activity are interpreted as a state of autonomic hypervigilance [ 34, 35], and sympathoexcitatory subcortical circuits are normally under the inhibitory control of the PFC [ 34- 36].
Another view is that the two pathways act independently to generate and propagate polarity [ 3, 4]: if correct, this raises the question of how gradients of Ft and Ds expression or activity might be interpreted to provide strong cellular polarizing cues and how such cues are propagated from cell to cell.
Cell growth and the β-galactosidase activity assays can be interpreted to mean that the full-length HMT-1 and HMT-1 lacking NTE do not interact, or that interactions are very weak and are at the limit of detection.
Therefore, the hepatoprotective activity was interpreted according to the increase/decrease in AST (aspartate aminotransferase), ALT (alanine aminotransferase) and total bilirubin levels (Table 5).
Thus, the β-activities of radioSr were interpreted to have the same counting efficiency regardless of the β-energy.
Nevertheless, based on all of these arguments and geophysical constraints, we conclude that the plate boundary beneath Kyushu exists at a depth of 40 km, and the tremor activity recorded in this study is interpreted to represent shear slip along the plate interface.
