1,868 research outputs found
Éléments d'anatomie comparée des animaux invertébrés / par le professeur Th. H. Huxley,... ; traduit de l'anglais par le Dr G. Darin ; avec une préface, des notes et un chapitre sur les principes généraux de la biologie, par le professeur A. Giard
No full textContient une table des matièresAvec mode texteOuvrages de référenc
Die Hohe Majestät der Frommen/ Woher man sie erlange/ Wer sie empfange/ Wie man darin prange/ Aus den Worten Pauli Rom. VIII. v. 31. 32. 33. 34.
No full textDIE HOHE MAJESTÄT DER FROMMEN/ WOHER MAN SIE ERLANGE/ WER SIE EMPFANGE/ WIE MAN DARIN PRANGE/ AUS DEN WORTEN PAULI ROM. VIII. V. 31. 32. 33. 34.
Die Hohe Majestät der Frommen/ Woher man sie erlange/ Wer sie empfange/ Wie man darin prange/ Aus den Worten Pauli Rom. VIII. v. 31. 32. 33. 34. ( - )
Binding ( - )
Title page ( - )
Dedication ( - )
I. N. I. A. (1)
Hohe Leidtragende/ Heilige und Geliebte Gottes. (2)
Höchstbetrübte / Hohe Leidtragende. (4)
Die zu dieser Leichen-Rede erwehlte Text-Worte sind zu finden in dem Briefe Pauli an die Römer Cap. VIII. v.31.32.33.34. und lauten also: (8)
Hohe Leidtragende / Heilige und Geliebte Gottes. (9)
Jura Majestatis Christianæ. Die hohe Majestät der Frommen: Woher man sie Erlange/ Wer Sie Empfange/ Wie man darin prange. (17)
I. Woher man sie erlange. (17)
II. Wer diese Majestät erlange. (35)
Wie man darin Prange. (45)
Ehren-Gedächtnisz. ([1])
Binding ( - )
Section ( -
The V-Dem Party Institutionalization Index: a new global indicator (1900-2015)
No full textBecause levels of party institutionalization may affect the availability of good data, existing datasets have limited reliability and coverage. To overcome these problems, we introduce the V-Dem Party Institutionalization Index, the first global country-level index on the issue. It covers – as of May 2017 – 173 countries for 116 years (1900-2016). Its geographical coverage, timespan, and conceptual reach are larger than any existing alternative. We offer an additive index that measures the scope and depth of party institutionalization in a country every year. Scope is measured by the proportion of parties that reach a threshold of minimal institutionalization, while the linkages party establish with the masses and the elites define the depth. Exploring a set of well-known cases, we show that: the index has extensive face validity, is consistent across regime types, and is comparable to other established indicators of institutionalization.This research project was supported by Riksbankens Jubileumsfond, Grant M13-0559:1, PI: Staffan I. Lindberg, V-Dem Institute, University of Gothenburg, Sweden; by Knut and Alice Wallenberg Foundation to Wallenberg Academy Fellow Staffan I. Lindberg, Grant 2013.0166, V-Dem Institute, University of Gothenburg, Sweden; as well as by internal grants from the Vice-Chancellor’s office, the Dean of the College of Social Sciences, and the Department of Political Science at University of Gothenburg. We performed simulations and other computational tasks using resources provided by the Notre Dame Center for Research Computing (CRC) through the High Performance Computing section and the Swedish National Infrastructure for Computing (SNIC) at the National Supercomputer Centre in Sweden, SNIC 2016/1-382 and 2017/1-68. We specifically acknowledge the assistance of In-Saeng Suh at CRC and Johan Raber at SNIC in facilitating our use of their respective systems
Geochemical composition (XRF SR uncorrected) of the Late Holocene sediments core LV66-3 (Amur Bay of the Sea of Japan)
No full textSediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur Bay of the Sea of Japan using a gravity core. The sampling location was chosen in the zone of maximum bottom water hypoxia (Tishchenko et al., 2011), which ensured minimal bioturbation of sediments due to oppression of benthic fauna. Continuous seismic profiling data at this site revealed a homogeneous structure of the sedimentary strata, with no visible breaks in sedimentation and no inclusions of sediments of a different composition (Karnaukh et al., 2016). The sediments of core LV66-3 are represented by monotonous clays and silty clays of black or dark gray color without visible stratification, with slightly varying density and humidity (Akulichev et al., 2015; Karnaukh et al., 2016). The analysis of the prepared samples was performed in the Budker Institute of Nuclear Physics (Novosibirsk) using a scanning X-ray fluorescence analyzer with the synchrotron radiation (XRF SR ) at the VEPP-3 storage ring as the excitation source according to previously developed methods (Darin et al., 2005; 2015; Kalugin et al., 2007; 2015). The scanning step was 0.5-0.8 mm. The concentrations of Ca, K, Ti, Mn, Fe, V, Cr, Ni, Cu, Zn, Mo, Pb, Rb, Ba, Sr, Y, Br, As, and Nb were determined. The detection limits for the elements were (mg/g): 0.5 (Br, Rb, Sr, Nb), 1 (Zr, Y), 2 (Zn, Ni, Mn, Pb), 10 (Fe), 15 (Ti), and 100 (Ca, K) (Kalugin et al., 2015). Rubidium-normalized elements were used for dimensionless variation. The age model of core LV66-3 was based on radiocarbon dates, tephrochronological data, and chemostratigraphy. Calibration of the 14C dates to obtain the calendar age of the studied samples was performed with the Calib program (Stuiver and Reimer, 1993) using the Marine13 calibration curve (Reimer et al., 2013). Correction of the reservoir effect was made using the dating of shells from Novik Bay in the eastern part of the Amur Bay (Kuzmin et al., 2001).
Geochemical time-series were created using a methodology previously developed for Siberian lakes (Kalugin et al., 2007; 2013; Darin et al., 2005; 2015; Hildebrandt wet al., 2015; Babich et al., 2015; Rudaya et al., 2016) based on the results of XRF SR scanning of the core in the 0-466 cm interval and its age model with some additions that have been used in paleoreconstructions of shelf sediments in the Arctic seas (Astakhov et al., 2019; 2020; 2023).
Considering the feature accumulation of sediment in the Amur Bay (Tishchenko et al., 2006; 2011, Akulichev et al., 2016;, Kalugin et al., 2015) and the experience construction of transfer geochemical functions for other areas (Kalugin et al., 2005; 2013; Babich et al., 1980; 2023; Astakhov et al., 2019; 2023), some elements were removed from the initial feature space: Zr, Nb, and Y are significantly enriched in the tephra of the Baitoushan volcano and overlying sediments, molybdenum is the element with maximum response to redox conditions, lead and zinc are possible anthropogenic contaminants in the surface sediment layer (Kalugin et al., 2015), and elements with very low content and weak variability
Annual mean and mean summer/winter air temperature at weather station Vladivostok
No full textSediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur Bay of the Sea of Japan using a gravity core. The sampling location was chosen in the zone of maximum bottom water hypoxia (Tishchenko et al., 2011), which ensured minimal bioturbation of sediments due to oppression of benthic fauna. Continuous seismic profiling data at this site revealed a homogeneous structure of the sedimentary strata, with no visible breaks in sedimentation and no inclusions of sediments of a different composition (Karnaukh et al., 2016). The sediments of core LV66-3 are represented by monotonous clays and silty clays of black or dark gray color without visible stratification, with slightly varying density and humidity (Akulichev et al., 2015; Karnaukh et al., 2016). The analysis of the prepared samples was performed in the Budker Institute of Nuclear Physics (Novosibirsk) using a scanning X-ray fluorescence analyzer with the synchrotron radiation (XRF SR ) at the VEPP-3 storage ring as the excitation source according to previously developed methods (Darin et al., 2005; 2015; Kalugin et al., 2007; 2015). The scanning step was 0.5-0.8 mm. The concentrations of Ca, K, Ti, Mn, Fe, V, Cr, Ni, Cu, Zn, Mo, Pb, Rb, Ba, Sr, Y, Br, As, and Nb were determined. The detection limits for the elements were (mg/g): 0.5 (Br, Rb, Sr, Nb), 1 (Zr, Y), 2 (Zn, Ni, Mn, Pb), 10 (Fe), 15 (Ti), and 100 (Ca, K) (Kalugin et al., 2015). Rubidium-normalized elements were used for dimensionless variation. The age model of core LV66-3 was based on radiocarbon dates, tephrochronological data, and chemostratigraphy. Calibration of the 14C dates to obtain the calendar age of the studied samples was performed with the Calib program (Stuiver and Reimer, 1993) using the Marine13 calibration curve (Reimer et al., 2013). Correction of the reservoir effect was made using the dating of shells from Novik Bay in the eastern part of the Amur Bay (Kuzmin et al., 2001).
Geochemical time-series were created using a methodology previously developed for Siberian lakes (Kalugin et al., 2007; 2013; Darin et al., 2005; 2015; Hildebrandt wet al., 2015; Babich et al., 2015; Rudaya et al., 2016) based on the results of XRF SR scanning of the core in the 0-466 cm interval and its age model with some additions that have been used in paleoreconstructions of shelf sediments in the Arctic seas (Astakhov et al., 2019; 2020; 2023).
Considering the feature accumulation of sediment in the Amur Bay (Tishchenko et al., 2006; 2011, Akulichev et al., 2016;, Kalugin et al., 2015) and the experience construction of transfer geochemical functions for other areas (Kalugin et al., 2005; 2013; Babich et al., 1980; 2023; Astakhov et al., 2019; 2023), some elements were removed from the initial feature space: Zr, Nb, and Y are significantly enriched in the tephra of the Baitoushan volcano and overlying sediments, molybdenum is the element with maximum response to redox conditions, lead and zinc are possible anthropogenic contaminants in the surface sediment layer (Kalugin et al., 2015), and elements with very low content and weak variability
Annual mean and mean summer/winter precipitation at weather station Vladivostok
No full textSediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur Bay of the Sea of Japan using a gravity core. The sampling location was chosen in the zone of maximum bottom water hypoxia (Tishchenko et al., 2011), which ensured minimal bioturbation of sediments due to oppression of benthic fauna. Continuous seismic profiling data at this site revealed a homogeneous structure of the sedimentary strata, with no visible breaks in sedimentation and no inclusions of sediments of a different composition (Karnaukh et al., 2016). The sediments of core LV66-3 are represented by monotonous clays and silty clays of black or dark gray color without visible stratification, with slightly varying density and humidity (Akulichev et al., 2015; Karnaukh et al., 2016). The analysis of the prepared samples was performed in the Budker Institute of Nuclear Physics (Novosibirsk) using a scanning X-ray fluorescence analyzer with the synchrotron radiation (XRF SR ) at the VEPP-3 storage ring as the excitation source according to previously developed methods (Darin et al., 2005; 2015; Kalugin et al., 2007; 2015). The scanning step was 0.5-0.8 mm. The concentrations of Ca, K, Ti, Mn, Fe, V, Cr, Ni, Cu, Zn, Mo, Pb, Rb, Ba, Sr, Y, Br, As, and Nb were determined. The detection limits for the elements were (mg/g): 0.5 (Br, Rb, Sr, Nb), 1 (Zr, Y), 2 (Zn, Ni, Mn, Pb), 10 (Fe), 15 (Ti), and 100 (Ca, K) (Kalugin et al., 2015). Rubidium-normalized elements were used for dimensionless variation. The age model of core LV66-3 was based on radiocarbon dates, tephrochronological data, and chemostratigraphy. Calibration of the 14C dates to obtain the calendar age of the studied samples was performed with the Calib program (Stuiver and Reimer, 1993) using the Marine13 calibration curve (Reimer et al., 2013). Correction of the reservoir effect was made using the dating of shells from Novik Bay in the eastern part of the Amur Bay (Kuzmin et al., 2001).
Geochemical time-series were created using a methodology previously developed for Siberian lakes (Kalugin et al., 2007; 2013; Darin et al., 2005; 2015; Hildebrandt wet al., 2015; Babich et al., 2015; Rudaya et al., 2016) based on the results of XRF SR scanning of the core in the 0-466 cm interval and its age model with some additions that have been used in paleoreconstructions of shelf sediments in the Arctic seas (Astakhov et al., 2019; 2020; 2023).
Considering the feature accumulation of sediment in the Amur Bay (Tishchenko et al., 2006; 2011, Akulichev et al., 2016;, Kalugin et al., 2015) and the experience construction of transfer geochemical functions for other areas (Kalugin et al., 2005; 2013; Babich et al., 1980; 2023; Astakhov et al., 2019; 2023), some elements were removed from the initial feature space: Zr, Nb, and Y are significantly enriched in the tephra of the Baitoushan volcano and overlying sediments, molybdenum is the element with maximum response to redox conditions, lead and zinc are possible anthropogenic contaminants in the surface sediment layer (Kalugin et al., 2015), and elements with very low content and weak variability
Mall re-imagined reconsidering a Cape Town shopping centre
No full textIncludes abstract.Includes bibliographical references.There is a common assumption that shopping malls are "bad" buildings. But this thesis aims to contest this assumption and offer a new way to approach shopping centre design. The shopping mall is not bad in the sens that it functions highly effieciently and serves the retail requirements of both shopper and tenant. The way in which the shopping mall is bad is the thinking behind their design often as a result of developer control, being one of the most commercially driven building types. This can often result in buildings that have a negative impact on their surroundings. Shopping malls tend to isolate their surroundings by creating inward-facing arcades. This is observed as the only profitable way to deal with shop fronts in shopping malls which results in the creation of large blank facades on the exterior
Franšízing v České republice
No full textDie vorliegende Arbeit befasst sich mit dem Franchising in der Tschechischen Republik. Die
Autorin beschränkt sich darauf, die Situation in Tschechien zu untersuchen. Das Ziel dieser
Arbeit besteht darin, die Entstehung und die weitere Entwicklung des Franchisings in diesem
Land darzustellen und näher zu analysieren.This thesis deals with the franchising in the Czech Republic. The author describes the present situation in the country. The aim of this thesis is to analyze the steady progress and the development of the franchising in the Czech Republic.Tato práce se zabývá franšízingem v České republice. Studentka analyzuje situaci v této zemi. Cíl této práce spočívá v popisu vzniku a dalšího vývoje franšízingu v České republice.Katedra cizích jazykůDokončená práce s úspěšnou obhajobo
OH LOOK AT ME NOW / Bobby Darin, chant, avec Orchestre dir. Billy May
No full textComprend : ALL BY MYSELF / Irving Berlin - MY BUDDY / Walter Donaldson et Gus Kahn - THERE'S A RAINBOW 'ROUND MY SHOULDER / Jolson ; Rose et Dreyer - ROSES OF PICARDY / Haydn Wood et Fred E. Weatherly - YOU'LL NEVER KNOW / Harry Warren et Mack Gordon - BLUE SKIES / Irving Berlin - ALWAYS / Irving Berlin - YOU MADE ME LOVE YOU / James V. Monaco et Joe Mc Carthy - A NIGHTINGALE SANG IN BERKELEY SQUARE / Eric Maschwitz ; Manning et Sherwin - I'M BEGINNING TO SEE THE LIGHT / James ; Ellington ; Hodges et George - OH ! LOOK AT ME NOW / Joe Bushkin et John de Vries - THE PARTY'S OVER / Styne ; Comden et GreenBnF-Partenariats, Collection sonore - BelieveContient une table des matière
Geochemical data of the Late Holocene sediments core LV66-3 (Amur Bay of the Sea of Japan) and results of air temperature and precipitation reconstructions for summer and winter by transfer functions
No full textSediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur Bay of the Sea of Japan using a gravity core. The sampling location was chosen in the zone of maximum bottom water hypoxia (Tishchenko et al., 2011), which ensured minimal bioturbation of sediments due to oppression of benthic fauna. Continuous seismic profiling data at this site revealed a homogeneous structure of the sedimentary strata, with no visible breaks in sedimentation and no inclusions of sediments of a different composition (Karnaukh et al., 2016). The sediments of core LV66-3 are represented by monotonous clays and silty clays of black or dark gray color without visible stratification, with slightly varying density and humidity (Akulichev et al., 2015; Karnaukh et al., 2016). The analysis of the prepared samples was performed in the Budker Institute of Nuclear Physics (Novosibirsk) using a scanning X-ray fluorescence analyzer with the synchrotron radiation (XRF SR ) at the VEPP-3 storage ring as the excitation source according to previously developed methods (Darin et al., 2005; 2015; Kalugin et al., 2007; 2015). The scanning step was 0.5-0.8 mm. The concentrations of Ca, K, Ti, Mn, Fe, V, Cr, Ni, Cu, Zn, Mo, Pb, Rb, Ba, Sr, Y, Br, As, and Nb were determined. The detection limits for the elements were (mg/g): 0.5 (Br, Rb, Sr, Nb), 1 (Zr, Y), 2 (Zn, Ni, Mn, Pb), 10 (Fe), 15 (Ti), and 100 (Ca, K) (Kalugin et al., 2015). Rubidium-normalized elements were used for dimensionless variation. The age model of core LV66-3 was based on radiocarbon dates, tephrochronological data, and chemostratigraphy. Calibration of the 14C dates to obtain the calendar age of the studied samples was performed with the Calib program (Stuiver and Reimer, 1993) using the Marine13 calibration curve (Reimer et al., 2013). Correction of the reservoir effect was made using the dating of shells from Novik Bay in the eastern part of the Amur Bay (Kuzmin et al., 2001). Geochemical time-series were created using a methodology previously developed for Siberian lakes (Kalugin et al., 2007; 2013; Darin et al., 2005; 2015; Hildebrandt wet al., 2015; Babich et al., 2015; Rudaya et al., 2016) based on the results of XRF SR scanning of the core in the 0-466 cm interval and its age model with some additions that have been used in paleoreconstructions of shelf sediments in the Arctic seas (Astakhov et al., 2019; 2020; 2023). Considering the feature accumulation of sediment in the Amur Bay (Tishchenko et al., 2006; 2011, Akulichev et al., 2016;, Kalugin et al., 2015) and the experience construction of transfer geochemical functions for other areas (Kalugin et al., 2005; 2013; Babich et al., 1980; 2023; Astakhov et al., 2019; 2023), some elements were removed from the initial feature space: Zr, Nb, and Y are significantly enriched in the tephra of the Baitoushan volcano and overlying sediments, molybdenum is the element with maximum response to redox conditions, lead and zinc are possible anthropogenic contaminants in the surface sediment layer (Kalugin et al., 2015), and elements with very low content and weak variability.
The final processing of the remaining 14-element XRF SR scan data matrix (Table S3, doi:10.1594/PANGAEA.987515) for the construction of transfer functions and paleoclimatic reconstructions was carried out in the following order:
- removal of sampling intervals containing instrumental errors, coinciding with layers of different composition (pyroclastics), and showing signs of intense diagenetic transformations; for these reasons, geochemical data for layers 352-363, 372-380 and 426-466 cm were removed;
- correction of the content of elements that give anomalous extremes due to the presence of fragments of plant remains, shells and minerals in the sedimentary layers; in these cases, the anomalous contents of chemical elements were replaced by the values obtained by interpolation taking into account their contents in the four nearest sampling points (two from above, two from below);
- generate fractional time-scale geochemical series by transferring geochemical information from the linear scale to the time scale corresponding to the age model of the core (Fig. 2);
- reduction of time series with a fractional time scale to an integral annual time scale with their subsequent smoothed using an 11-year moving average (hereafter referred to as decadal averages);
- rubidium normalization of the chemical elements content (Table S3, doi:10.1594/PANGAEA.987515);
- minimax normalization of chemical elements (Table S3; doi:10.1594/PANGAEA.987515), which makes it possible to bring them into a comparable form, regardless of the scale of their measurement
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