S��fer miktev�� ��ivr��t oder ebrei��er und dai�����er brief�����eller : ... in rein und laich��� fer�����endlich lo��n ha-koide�� und dai����� ...

fon M����e ��em��'��l Neiman

An die Hohe Verfassunggebende Versammlung der Freien Stadt Frankfurt: Gehorsamste dringliche Beschwerde und Bitte des Orientalisten L. H. Loewenstein aus Steinbach in W��rttemberg, derzeit in R��delheim, seine, mit Umgehung jeder rechtlichen Formalit��t erfolgte polizeiliche Ausweisung und nachmalige Verhaftung betreffend: Hohe Verfassunggebende Versammlung! I. Die Ausweisung: Seit dem Jahre 1827 hatte ich mich (mit einer Unterbrechung von 3 1/2 Jahren) in Frankfurt aufgehalten ...

Boberach: Ein j��discher Einwohner Frankfurts, dem nach einem Aufenthalt von 21 Jahren zun��chst das Frankfurter B��rgerrecht in Aussicht gestellt worden war, beschwert sich dar��ber, da�� er wegen seines Auftretens in Volksversammlungen verhaftet und ausgewiesen wurde und verlangt ein Gerichtsverfahren oder Genugtuung, nachdem er sich um Schutz durch seine w��rttembergische Heimatbeh��rde bem��ht hat

Meine Assisen-Rede, gehalten vor den Geschwornen zu D��sseldorf am 3. Mai 1849, gegen die Anklage, die B��rger zur Bewaffnung gegen die K��nigl. Gewalt aufgereizt zu haben

Boberach: Zur Rechtfertigung der Proteste gegen die Regierung im November 1848 werden deren Rechtsbr��che und ungesetzliche Ma��nahmen der Lokalbeh��rden dargestellt. - Welsch (Projektbearbeiter): Verfa��t von dem Publizisten und Politiker Lassalle, dem sp��teren (1863) Gr��nder des 'Allgemeinen Deutschen Arbeitervereins', "Durch einen Act der Willk��hr ... wurde es dem Angeklagten nicht gestattet, die vorstehende Rede vor dem ... Publikum ... zu halten ... [worauf] der Angeklagte erkl��rte: Er halte es [f��r] unter seiner W��rde, ... seine Rede zu halten, er verzichte auf's Wort. Dennoch erfolgte die Freisprechung durch die Geschwornen." [Aus der Vorlage]

Kundmachung an die Arbeiter: Der unterzeichnete Ausschu�� kann heute nur wiederholen, was er Euch Samstag schon bekannt gegeben hat ...

Welsch (Projektbearbeiter): Bekr��ftigung der bestehenden L��hne und Sachleistungen f��r die bei den ��ffentlichen Arbeiten Besch��ftigten: bei witterungsbedingter Arbeitsunterbrechung am Vormittag wird ein halber Tag, am Nachmittag ein ganzer bezahlt. F��llt ein Arbeitstag witterungsbedingt v��llig aus, besteht Anspruch auf 6 Kreuzer Aushilfe (in Brot oder in Geld). Fallen mehrere Arbeitstage aus, so steigt die Aushilfe auf 9 Kreuzer t��glich (ab dem zweiten Tag; entweder in bar oder als Anweisung auf 6 Kreuzer in Brot plus 3 Kreuzer Zulage). Arbeiter, denen aufgrund eines Mi��verst��ndnisses ein halber Tag zuviel ausgezahlt wurde sind verpflichtet, dies durch Mehrarbeit oder Lohnverzicht auszugleichen

Ms.Ff.F.Stoltze 3. 67 - Brief von Friedrich August Finger an Friedrich Stoltze

Wilhelm Sauerwein: "Der Gr��ff, wie er leibt und lebt", Georg Friedrich Gr��ff, Samuel Friedrich Hassel

Ms.Ff.F.Stoltze 3. 141 - Brief von Karl Friedrich Holbach an F��licie Louise Schalck de la Faverie

Ernst Schalck soll aus dem Nassauischen zur��ckgeholt werden, da er dort wegen des preu��ischen Urteils gegen die Latern-Redakteure in Verhaftungsgefahr schwebt

Ms.Ff.F.Stoltze 3. 336 - Brief von Friedrich Stoltze an Friedrich August Finger

Frankfurter Dialekttheater, Wilhelm Sauerwein: "Der Gr��ff, wie er leibt und lebt", "Gr��ff im Gr��nen", "Der Amerikaner", Carl Mal��, Pfeifer: "Die Brunnenfahrt", Sauerwein: Briefe an Wilhelm Rieger (verloren), Collegzeitung, Geplante Sauerwein-Gesamtausgabe

Panorama dramatique. Walter de Montbarey. D��coration des 1.er et 2e Actes. Par Gu��

Signatur des Originals: S 36/G02653

Evaluating the Harris County TexHealth 3-Share Plan: An exploratory study

An important health issue in the United States today is the large number of people who have problems accessing needed health care because they lack health insurance coverage. Providing health insurance coverage for the working uninsured is a particularly significant challenge in Texas, which has the highest percentage of uninsured in the nation. In response to the low rate of employer-sponsored coverage in the Houston area and the growing numbers of uninsured, the Harris County Health Care Alliance (HCHA) developed and implemented the Harris County 3-Share Plan. A 3-Share Plan is not insurance, but provides health coverage in the form of a benefits package to employers who subscribe to the program and offer it to their employees. ^ A cross sectional study design was conducted to describe 3-Share employer and employee participants and evaluate their outcomes after its first year of operation. Between September and December 2011, 85% of employers enrolled in the 3-Share Plan completed a survey about the affordability of the 3-Share Plan, their satisfaction with the Plan, and the Plan's impact on employee recruitment, retention, productivity, and absenteeism. Forty-five percent of employees enrolled in the 3-Share Plan responded to a survey asking about the affordability of the 3-Share plan, accessibility of health care, availability of providers on the plan, health plan availability, utilization of primary care providers and the ER, and satisfaction with the plan. ^ A summary of the findings shows employers and employees say that they joined the plan because of the low-cost, and once they had participated in the Plan, the majority of employers and employees found that it is affordable for them. The majority of employees say they are getting access easily and without delay, but for those who aren't able to get access, or are delayed, the main cause is related to non-financial barriers to care. Ultimately, employees are satisfied with the 3-Share, and they plan to continue with health coverage under the 3-Share Plan. The 3-Share Plan will keep people in a system of care, and promote health, which will benefit the individuals, the businesses and the community of Harris County.^

Evaluating the Harris County TexHealth 3-Share plan: An exploratory study

An important health issue in the United States today is the large number of people who have problems accessing needed health care because they lack health insurance coverage. Providing health insurance coverage for the working uninsured is a particularly significant challenge in Texas, which has the highest percentage of uninsured in the nation. In response to the low rate of employer-sponsored coverage in the Houston area and the growing numbers of uninsured, the Harris County Health Care Alliance (HCHA) developed and implemented the Harris County 3-Share Plan. A 3-Share Plan is not insurance, but provides health coverage in the form of a benefits package to employers who subscribe to the program and offer it to their employees. ^ A cross sectional study design was conducted to describe 3-Share employer and employee participants and evaluate their outcomes after its first year of operation. Between September and December 2011, 85% of employers enrolled in the 3-Share Plan completed a survey about the affordability of the 3-Share Plan, their satisfaction with the Plan, and the Plan's impact on employee recruitment, retention, and productivity. Forty-five percent of employees enrolled in the 3-Share Plan responded to a survey asking about the affordability of the 3-Share plan, accessibility of providers on the plan, satisfaction, and utilization of primary care providers and the ER. ^ A summary of the findings shows employers and employees say that they joined the plan because of the low-cost, and once they had participated in the Plan, the majority of employers and employees found that it is affordable for them. The majority of employees say they are getting access easily and without delay, but for those who aren't able to get access, or are delayed, the main cause is related to non-financial barriers to care. Ultimately, employees are satisfied with the 3-Share, and they plan to continue with health coverage under the 3-Share Plan. The 3-Share Plan will keep people in a system of care, and promote health, which will benefit the individuals, the businesses and the community of Harris County.^

Chemical and Sr isotopic compositions of 3 step leachates and residues of bulk samples, zeolites, and smectites from Lower Miocene sediments at ODP Site 166-1007

Massive clinoptilolite authigenesis was observed at about 1105 meters below sea floor (mbsf) in lower Miocene wellcompacted carbonate periplatform sediments from the Great Bahama Bank [Ocean Drilling Program, ODP Leg 166, Site 1007]. The diagenetic assemblage comprises abundant zeolite crystallized within foraminifer tests and sedimentary matrix, as well as Mg smectites. In carbonate-rich deposits, the formation of the zeolite requires a supply of silica. Thus, the objective of the study is to determine the origin of the silica supply, its diagenetic evolution, and consequently the related implications on interpretation of the sedimentary record, in terms of local or global paleoceanographic change. For lack of evidence for any volcaniclastic input or traces of Si-enriched deep fluids circulation, an in situ biogenic source of silica is validated by isotopic data and chemical modeling for the formation of such secondary minerals in shallow-water carbonate sequences. Geochemical and strontium isotopic data clearly establish the marine signature of the diagenetic zeolite, as well as its contemporaneous formation with the carbonate deposition (Sr model ages of 19.6-23.2 Ma). The test of saturation for the pore fluids specifies the equilibrium state of the present mineralogical assemblage. Seawater-rock modeling specifies that clinoptilolite precipitates from the dissolution of biogenic silica, which reacts with clay minerals. The amount of silica (opal-A) involved in the reaction has to be significant enough, at least 10 wt.%, to account for the observed content of clinoptilolite occurring at the most zeolite-rich level. Modeling also shows that the observed amount of clinoptilolite (~19%) reflects an in situ and short-term reaction due to the high reactivity of primary biogenic silica (opal-A) until its complete depletion. The episodic occurrence of these well-lithified zeolite-rich levels is consistent with the occurrence of seismic reflectors, particularly the P2 seismic sequence boundary located at 1115 mbsf depth and dated as 23.2 Ma. The age range of most zeolitic sedimentary levels (biostratigraphic ages of 21.5-22 Ma) correlates well with that of the early Miocene glaciation Mi-1 and Mi-1a global events. Thus, the clinoptilolite occurrence in the shallow carbonate platform environment far from volcanogenic supply, or in other sensitive marine areas, is potentially a significant new proxy for paleoproductivity and oceanic global events, such as the Miocene events, which are usually recognized in deep-sea pelagic sediments and high latitude deposits.

(Table 7) Fe**3+/Fe**2+ ratios in selected nontronite samples at DSDP Leg 70 Holes

Since its discovery in 1974 (Klitgord and Mudie, 1974), the Galapagos mounds hydrothermal field has received much attention. Sediment samples were taken during Leg 54 of the Deep Sea Drilling Project (DSDP) and by other expeditions to the area (e.g., Corliss et al., 1978). While a hydrothermal origin for the mounds sediments has been generally accepted, several different theories of origin for the mounds themselves have been proposed (e.g., Corliss et al., 1978; Natland et al., 1979; Williams et al., 1979). One of the aims of DSDP Leg 70 was to return to the mounds field and, using the new hydraulic piston cor er described elsewhere in this volume, to obtain more complete recovery of mounds sediments than had previously been possible. It was our hope that this would help in our understanding of the nature and origin of these deposits. In this chapter, we describe the results of chemical analysis of over 250 sediment samples taken during the course of Leg 70.

Chemical composition of sediment core GeoB12309-5 from the northern Arabian Sea, its pore water profile and age depth relationship as well as CTD data obtained during cruise M74/3

The Arabian Sea off the Pakistan continental margin is characterized by one of the world's largest oxygen minimum zones (OMZ). The lithology and geochemistry of a 5.3 m long gravity core retrieved from the lower boundary of the modern OMZ (956 m water depth) were used to identify late Holocene changes in oceanographic conditions and the vertical extent of the OMZ. While the lower part of the core (535 - 465 cm, 5.04 - 4.45 cal kyr BP, Unit 3) is strongly bioturbated indicating oxic bottom water conditions, the upper part of the core (284 - 0 cm, 2.87 cal kyr BP to present, Unit 1) shows distinct and well-preserved lamination, suggesting anoxic bottom waters. The transitional interval from 465 to 284 cm (4.45 - 2.87 cal kyr BP, Unit 2) contains relicts of lamination which are in part intensely bioturbated. These fluctuations in bioturbation intensity suggest repetitive changes between anoxic and oxic/suboxic bottom-water conditions between 4.45 - 2.87 cal kyr BP. Barium excess (Baex) and total organic carbon (TOC) contents do not explain whether the increased TOC contents found in Unit 1 are the result of better preservation due to low BWO concentrations or if the decreased BWO concentration is a result of increased productivity. Changes in salinity and temperature of the outflowing water from the Red Sea during the Holocene influenced the water column stratification and probably affected the depth of the lower boundary of the OMZ in the northern Arabian Sea. Even if we cannot prove certain scenarios, we propose that the observed downward shift of the lower boundary of the OMZ was also impacted by a weakened Somali Current and a reduced transport of oxygen-rich Indian Central Water into the Arabian Sea, both as a response to decreased summer insolation and the continuous southward shift of the Intertropical Convergence Zone during the late Holocene.