Associations between affective disorders, anxiety disorders, and substance use disorders were examined in epidemiological studies conducted in Germany, Switzerland, Puerto Rico, and the mainland US. There was a remarkable degree of similarity across studies in the magnitude and type of specific disorders associated with the affective disorders. Comorbidity with affective disorders was greater for the anxiety disorders than for substance misuse. Panic disorder was the subtype of anxiety that was most highly comorbid with depression. Social phobia was the specific phobic type with the strongest association with the affective disorders. The magnitude of associations between substance misuse and affective disorders generally was quite low and less consistent across sites. No major differences were found in the patterns of comorbidity by gender or age group, affective subtype or prevalence period. The onset of anxiety disorders generally preceded that of depression, whereas alcohol misuse was equally likely to pre- or post-date the onset of affective disorders. Finally, comorbidity was associated with an elevation in treatment ratesacross all sites, confirming Berkson's paradox on an international level.

This study examines the 1 year prevalence rates of headache syndromes in an epidemiologic cohort study of young adults ages 29-30 in Zurich, Switzerland. The 1 year prevalence rates of headache subtypes were 3.3% for migraine with aura and 21.3% of migraine without aura as defined by the International Headache Society (IHS) criteria. The demographic distribution, clinical features, sequelae, and treatment patterns of subjects with specific headache subtypes are described. The rates of migraine are compared to those of other community samples that have employed the IHS criteria for headache subtypes. Subjects with migraine reported pervasive impairment in nearly every life role including occupation, leisure, and social relationships. Despite the substantial degree of impairment in occupational and social functioning that was associated with migraine, an extremely low proportion of subjects had received professional treatment for headache. These results suggest that a concerted effort should be directed towards education regarding the classification of headache and the availability of efficacious treatment for migraine.

This paper reports the results of a systematic assessment of the validity of the specific diagnostic criteria for migraine without aura, as defined by the International Headache Society (IHS), in a longitudinal epidemiologic sample of young adults who were selected from the general population of Zürich, Switzerland. Systematic modification of each of the IHS criteria for migraine without aura yielded one-year weighted prevalence rates ranging from 24% for the unmodified IHS criteria to 9% for the most restrictive definition of migraine. The major implications of the findings for the IHS criteria are: (a) they provide adequate coverage to classify the majority of subjects with headache in the general population; (b) there is little overlap between migraine and tension-type headache, suggesting that the criteria define moderately independent subgroups; (c) the criteria for migraine without aura appear to be too unrestrictive for application in the community, particularly among young adults at the peak period of incidence of migraine; (d) the criteria for "aura" need more precise operationalization; and (e) models of validation of the diagnostic criteria suggest that Criterion D of the IHS criteria for migraine without aura should be modified to require both gastrointestinal symptoms and photophobia and phonophobia.

Early ENE-striking joints (present coordinates) within both Pennsylvanian coal and Devonian black shale of the Central and Southern Appalachians reflect an approximately rectilinear stress field with a dimension Ͼ1500 km. This Appalachian-wide stress field (AWSF) dates from the time of joint propagation, when both the coal and shale were buried to the oil window during the 10-15 m.y. period straddling the Pennsylvanian-Permian boundary. The AWSF was generated during the final assembly of Pangea as a consequence of plate-boundary tractions arising from late-stage oblique convergence, where maximum horizontal stress, S H , of the AWSF was parallel to the direction of closure between Gondwana and Laurentia. After closure, the AWSF persisted during dextral slip of peri-Gondwanan microcontinents, when S H appears to have crosscut plate-scale transcurrent faults at ϳ30؇. Following Ͼ10 m.y. of dextral slip during tightening of Gondwana against Laurentia, the AWSF was disrupted by local stress fields associated with thrusting on master basement decollements to produce the local orocline-shaped Alleghanian map pattern seen today.

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