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Creators/Authors contains: "Rubin, Kenneth H."

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  1. Background

    Given the robust evidence base for the efficacy of evidence‐based treatments targeting youth anxiety, researchers have advanced beyond efficacy outcome analysis to identifymechanismsof change and treatment directionality. Grounded in developmental transactional models, interventions for young children at risk for anxiety by virtue of behaviorally inhibited temperament often target parenting and child factors implicated in the early emergence and maintenance of anxiety. In particular, overcontrolling parenting moderates risk for anxiety among highly inhibited children, just as child inhibition has been shown to elicit overcontrolling parenting. Although longitudinal research has elucidated the temporal unfolding of factors that interact to place inhibited children at risk for anxiety, reciprocal transactions between these child and parent factors in the context of early interventions remain unknown.

    Method

    This study addresses these gaps by examining mechanisms of change and treatment directionality (i.e., parent‐to‐child vs. child‐to‐parent influences) within a randomized controlled trial comparing two interventions for inhibited preschoolers (N = 151): the multicomponent Turtle Program (‘Turtle’) and the parent‐only Cool Little Kids program (‘CLK’). Reciprocal relations between parent‐reported child anxiety, observed parenting, and parent‐reported accommodation of child anxiety were examined across four timepoints: pre‐, mid‐, and post‐treatment, and one‐year follow‐up (NCT02308826).

    Results

    Hypotheses were tested via latent curve models with structured residuals (LCM‐SR) and latent change score (LCS) models. LCM‐SR results were consistent with the child‐to‐parent influences found in previous research on cognitive behavioral therapy (CBT) for older anxious youth, but only emerged in Turtle. LCS analyses revealed bidirectional effects ofchangesin parent accommodation and child anxiety during and after intervention, but only in Turtle.

    Conclusion

    Our findings coincide with developmental transactional models, suggesting that the development of child anxiety may result from child‐to‐parent influences rather than the reverse, and highlight the importance of targeting parentandchild factors simultaneously in early interventions for young, inhibited children.

     
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  2. null (Ed.)
    The transition from subduction to transform motion along horizontal terminations of trenches is associated with tearing of the subducting slab and strike-slip tectonics in the overriding plate. One prominent example is the northern Tonga subduction zone, where abundant strike-slip faulting in the NE Lau back-arc basin is associated with transform motion along the northern plate boundary and asymmetric slab rollback. Here, we address the fundamental question: how does this subduction-transform motion influence the structural and magmatic evolution of the back-arc region? To answer this, we undertake the first comprehensive study of the geology and geodynamics of this region through analyses of morphotectonics (remote-predictive geologic mapping) and fault kinematics interpreted from ship-based multibeam bathymetry and Centroid-Moment Tensor data. Our results highlight two notable features of the NE Lau Basin: 1) the occurrence of widely distributed off-axis volcanism, in contrast to typical ridge-centered back-arc volcanism, and 2) fault kinematics dominated by shallow-crustal strike slip-faulting (rather than normal faulting) extending over ∼120 km from the transform boundary. The orientations of these strike-slip faults are consistent with reactivation of earlier-formed normal faults in a sinistral megashear zone. Notably, two distinct sets of Riedel megashears are identified, indicating a recent counter-clockwise rotation of part of the stress field in the back-arc region closest to the arc. Importantly, the Riedel structures identified in this study directly control the development of complex volcanic-compositional provinces, which are characterized by variably-oriented spreading centers, off-axis volcanic ridges, extensive lava flows, and point-source rear-arc volcanoes. This study adds to our understanding of the geologic and structural evolution of modern backarc systems, including the association between subduction-transform motions and the siting and style of seafloor volcanism. 
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  3. null (Ed.)