Socioeconomic, Temporal and Regional Variation in Body Mass Index among 188,537 Swiss Male Conscripts Born between 1986 and 1992

BACKGROUND Rising levels of overweight and obesity are important public-health concerns worldwide. The purpose of this study is to elucidate their prevalence and trends in Switzerland by analyzing variations in Body Mass Index (BMI) of Swiss conscripts. METHODS The conscription records were provided by the Swiss Army. This study focussed on conscripts 18.5-20.5 years of age from the seven one-year birth cohorts spanning the period 1986-1992. BMI across professional status, area-based socioeconomic position (abSEP), urbanicity and regions was analyzed. Two piecewise quantile regression models with linear splines for three birth-cohort groups were used to examine the association of median BMI with explanatory variables and to determine the extent to which BMI has varied over time. RESULTS The study population consisted of 188,537 individuals. Median BMI was 22.51 kg/m2 (22.45-22.57 95% confidence interval (CI)). BMI was lower among conscripts of high professional status (-0.46 kg/m2; 95% CI: -0.50, -0.42, compared with low), living in areas of high abSEP (-0.11 kg/m2; 95% CI: -0.16, -0.07 compared to medium) and from urban communities (-0.07 kg/m2; 95% CI: -0.11, -0.03, compared with peri-urban). Comparing with Midland, median BMI was highest in the North-West (0.25 kg/m2; 95% CI: 0.19-0.30) and Central regions (0.11 kg/m2; 95% CI: 0.05-0.16) and lowest in the East (-0.19 kg/m2; 95% CI: -0.24, -0.14) and Lake Geneva regions (-0.15 kg/m2; 95% CI: -0.20, -0.09). Trajectories of regional BMI growth varied across birth cohorts, with median BMI remaining high in the Central and North-West regions, whereas stabilization and in some cases a decline were observed elsewhere. CONCLUSIONS BMI of Swiss conscripts is associated with individual and abSEP and urbanicity. Results show regional variation in the levels and temporal trajectories of BMI growth and signal their possible slowdown among recent birth cohorts.

Ms. hebr. oct. 188 - ha-Shemesh ba

Vorbesitzer: Eljāqīm Carmoly

Na 1 Nachlass Max Horkheimer, 6 - Korrespondenzen u.a. mit Célestin Bouglé (p. I 3, 188-402)

66 Briefe zwischen Célestin Bouglé, C. Bouglé, Jeanne Bouglé und Max Horkheimer, 1933-1940; 2 Briefe von Henri Bergson an Célestin Bouglé, 1933, 1935; 1 Brief von Bouvier & Beale an Max Horkheimer, 19.08.1936; 8 Briefe zwischen C. M. Bowra und Max Horkheimer, 1936-1937; 13 Briefe zwischen Ralph Raoul Boyer und Max Horkheimer, 1943-1946; 1 Brief von Max Horkheimer an Justice Louis Brandeis, 18.06.1940; 1 Brief von Karl Brandt von der Notgemeinschaft Deutscher Wissenschaftler im Ausland New York an Max Horkheimer, 27.11.1935; 4 Briefe zwischen Alfred Braunthal und Max Horkheimer, 03.08.1938, 1936-1938; 1 Brief von Trude Briess an Max Horkheimer, 07.06.1938; 4 Briefe zwsichen Lilly Brill und Max Horkheimer, 1947-1948; 1 Brief von Max Horkheimer an Chandis H. Brauchler, 03.09.1949; 1 Brief von Max Horkheimer an Lilian Broadwin, 07.03.1939; 4 Briefe zwischen Lola Bronstein und Max Horkheimer, 1940; 1 Brief von Ferdinand Bruckner an Max Horkheimer, 02.02.1938; 6 Briefe zwischen Paul Bruell udn Max Horkheimer, 1939; 1 Brief von H. Brungs an Max Horkheimer, 20.07.1949; 2 Briefe zwischen Fritz Brupbacher und Max Horkheimer, 31.03.1940, 17.04.1940; 4 Briefe zwischen Gerhard Bry und Max Horkheimer, 1937-1940, 26.01.1940; 1 Brief von Max Horkheimer an Richard Büchner, 29.06.1937; 2 Briefe zwischen Erika Buhlmann und Max Horkheimer, 1949; 13 Briefe zwischen Else Buki und Max Horkheimer, 1940-1941; 1 Brief von Max Horkheimer an Hans Buki, 14.07.1943; 1 Brief von Max Horkheimer an Friedrich Burschell, 29.08.1938; 7 Briefe und 5 Entwürfe zwischen dem Präsident der Columbia University Nicholas Murray Butler und Max Horkheimer, 1938-1941; 1 Brief von Max Horkheimer an Pierce Butler, 03.05.1938;

Na 1 Nachlass Max Horkheimer, 36 - Korrespondenzen u.a. mit Karl Menninger vom The Menninger Clinic, The Menninger Sanatorium, Topeka, Kansas (p. I 18, 188-334)

15 Brief zwischen Heinrich Meng und Max Horkheimer sowie Briefwechsel mit The Johns Hopkins Hospital, Baltimore Maryland, 1935-1940; 4 Briefe zwischen dem The Johns Hopkins Hospital, Baltimore, Maryland und Max Horkheimer, 1940; 1 Brief von Werner Münsterberger an Max Horkheimer, 13.03.1940; 44 Briefe zwischen Karl Menninger vom The Menninger Clinic, The Menninger Sanatorium, Topeka, Kansas und Max Horkheimer, 1938-1941;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 188 - Freudige Kenntnisnahme der Entscheidung Schopenhauers zur Habilitation

u.a.: Schreiben Schopenhauers an Philipp August Boeckh vom 31. Januar 1820; Vorlesung Schopenhauers an der Universität Berlin;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1165 - Übernahme der Preisaufgabe "Darlegung und Kritik der Principien der Schopenhauerschen Philosophie"

Philosophische Fakultät der Universität Leipzig; Privatbibliothek Karl Bährs;

Ms. Praed. 188 - Biblia sacra utriusque testamenti ex vulgata editione

Vorbesitzer: Jakob Heller; Dominikanerkloster Frankfurt am Main

Ms.Ff.F.Stoltze 3. 188 - Brief von Feodor Loewe an Friedrich Stoltze

Zu einem Beitrag für "Hessenland"

Ausst. 188 - Psalmi poenitentiales et confessionales

Vorbesitzer: [Louise] Oehler-Jaeger

Ms. lat. oct. 188 - Instrutione utile alla republica Christiana

Vorbesitzer: Franciscus Deyarza

Organic matter C and N composition and N. pachyderma stable isotope ratios of ODP Hole 188-1166A sediments

We report the results of downhole stable isotopic (d13Corg [organic carbon] and d15N) and elemental measurements (total organic carbon [TOC], total nitrogen [TN], and carbon/nitrogen [C/N]) of sedimentary organic matter (SOM) along with stable isotopic measurements (d18O and d13C) of left-coiling Neogloboquadrina pachyderma planktonic foraminifers from Ocean Drilling Program Site 1166. TOC and TN measurements indicate a large change from organic-rich preglacial sediments with primary organic matter to organic-poor early glacial and glacial sediments, with mainly recycled organic matter. Results of the stable isotopic measurements of SOM show a range of values that are typical of both marine and terrestrial organic matter, probably reflecting a mixture of the two. However, C/N values are mostly high (>15), suggesting greater input and/or preservation of terrestrial organic matter. Foraminifers are only present in glacial/glaciomarine sediments of latest Pliocene to Pleistocene age at Site 1166 (lithostratigraphic Unit I). The majority of this unit has d13Corg and TOC values that are similar to those of glacial sediments recovered at Site 1167 (lithostratigraphic Unit II) on the slope and may have the same source(s). Although the low resolution of the N. pachyderma (s.) d18O and d13C data set precludes any specific paleoclimatic interpretation, downcore variations in foraminifer d18O and d13C values of 0.5 per mil to 1 per mil amplitude may indicate glacial-interglacial changes in ice volume/temperature in the Prydz Bay region.

Ice-rafted debris record in the Prydz Bay

Ice-rafted debris mass accumulation rates (IRD MAR) at a drill site on the Antarctic continental margin are investigated to evaluate the linkages between East Antarctic Ice Sheet extent and Southern Ocean temperatures in the early to mid-Pliocene. ODP Site 1165 is within 400 km of the Antarctic coastline and in the direct pathway of icebergs released by the Amery Ice Shelf. The Amery Ice Shelf is the largest ice shelf in East Antarctica and it buttresses the Lambert Glacier drainage system, which accounts for 14% of the outflow from the East Antarctic Ice Sheet. IRD MAR were low during peak Southern Ocean warming in the early Pliocene. After a brief precursor, a tenfold increase in IRD MAR at 3.3 Ma marks the termination of the early Pliocene ice sheet minimum, coincident with the M2 glacial. For the mid-Pliocene, a strong correlation exists between the high-amplitude signal in the LR04 benthic stack and IRD MAR, suggesting linkages between East Antarctic ice extent, global ice volume and deep-water temperatures. The IRD record at Site 1165 provides evidence of greater sensitivity of the Lambert Glacier-Amery Ice Shelf system to Southern Ocean warming than is currently predicted by ice sheet models, which may relate to uncertainties in the understanding of ocean heat uptake, poleward heat transport and ice sheet-ocean interactions.