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Neuropsychological data have provided important evidence for models of this process, particularly from case reports; however, the quality and extent of the data varies widely between studies.
The presence of high As groundwaters with recharge derived from both local precipitation and relatively evaporated surface water sources, such as ponds or flooded wetlands, are consistent with (but do not provide direct evidence for) models of a potential dual role of surface-derived and sedimentary organic matter in As mobilization.
This suggests that the evidence for Models 1 6 did not improve when increasing complexity (i.e., B, C, or D vs. A).
In the absence of evidence for Models B1 or B2, Model B3 becomes the most likely candidate but positive evidence for Model B3 may require intracellular recordings.
As shown in Table 3, there was stronger evidence for Models 1 6 in configuration A (noted 1A 6A) even when the comparison included Models 25 and 26.
Based on these results, there is strong evidence for models with a top-down connection between middle occipital areas (first level) and IT/F (third level), but there is no evidence for lateral connections between lMO and mMO (first level).
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In that respect our focus will be on supporting evidence for Model 2 testing if the factor loadings were equal.
Especially in the last two specifications of the LL model (15 and 10%) and the last specification of the TL model (10%), there is ample evidence for model misspecification.
These procedures are deployed in a synergistic manner to provide mutually corroborating evidence for model correction.
If we compare model 2 with model 3 there is evidence for model 3 consistently over all 3 years.
Thus BF 01 greater than 2 represent positive evidence for model M 1, and greater than 6 provide strong evidence.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com