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67 results for “Saxony”
Parish church (Église Saint-Thomas). The mausoleum of the Marshall of Saxony (Maréchal de Saxe). Sculptor Jean-Baptiste Pigalle. 1776.
<u>File Name</u>: PM_150063_F_Strasbourg <br><u>Sublocation</u>: Église Saint-Thomas <br><u>Location</u>: Strasbourg <br><u>Province</u>: Gand-Est, Bas-Rhin <br><u>Country</u>: France <br><u>Header</u>: Mausolée du maréchal Maurice de Saxe, sculpteur Jean-Baptiste Pigalle, 1776 <br><u>Description</u>: Parish church (Église Saint-Thomas). The mausoleum of the Marshall of Saxony (Maréchal de Saxe). Sculptor Jean-Baptiste Pigalle. 1776. <br><u>Author</u>: Jean-Baptiste Pigalle (1714-1785) <br><u>Author Mail</u>: PMRMaeyaert@gmail.com <br><u>Copyright</u>: © Paul M.R. Maeyaert; pmrmaeyaert@gmail.com <br><u>Keywords</u>: Europe|France; Europe|France|Grand Est; Europe|France|Grand Est|Bas-Rhin; Europe|France|Grand Est|Bas-Rhin|Strasbourg; Cultural heritage|Techniques|Sculpture; Cultural heritage|Styles|Baroque; Cultural heritage|Monuments|Church; Cultural heritage|Monuments; Cultural heritage|Styles; Cultural heritage <br><u>Date of Generation</u>: 2023-08-14T15:59:18+02:00
Grain-size data from the loess profiles Ostrau and Gleina in Saxony (Germany)
<p><strong>Grain-size data from the loess profiles Ostrau and Gleina in Saxony (Germany)</strong></p> <p>The samples were taken between 2009 and 2010 in the framework of the DFG project <a href="https://gepris.dfg.de/gepris/projekt/46526743"><em>"Rekonstruktion der Umweltbedingungen des Spätpleistozäns in Mittelsachsen anhand von Löss-Paläobodensequenze</em>n" (DFG FU 417/7-1 and FA 239/13-1</a>) from the loess records Ostrau and Gleina. Both located in the Saxonian-Loess-Region in Germany. For further details on the project profiles (with further references therein), we refer to Meszner et al. (2011,2013), Kreutzer et al. (2012), Meszner (2015) and Zech et al. (2017). </p> <p>Samples for the data reported here were selected in 2015. 212 samples were taken from the loess profile Ostrau and 269 samples from the loess profile Gleina. Full details on sampling and sample preparation can be found in the Grassl (2016) (unpublished master thesis in Germany, available upon request). The most relevant details are extracted below. </p> <p><strong>Preparation and measurements</strong></p> <p>Sample preparation and measurements were carried out at the GFZ in Potsdam (Germany). Thirty-nine samples from the profile Ostrau were separated into eight equal parts to obtain representative samples. The samples were labeled with "G" for Gleina and "O" for Ostrau. All other samples were sampled without applying this separation method. <br> For samples from the profile Ostrau, the suffix "mT" (with separation) and "oT" (without separation) indicates whether this <br> separation method was used. </p> <p>The samples were treated with HCl (10 %, 12 h to 20 h) and rinsed in the demineralized water. To suspend the samples, NO<sub>3</sub>P0<sub>4</sub> was used on twelve pars of H<sub>2</sub>O<sub>2</sub>. </p> <p>A <em>Retch Laser Scattering Particle Size Distribution Analyzer (HORIBA LA- 950)</em> was used for the grain-size measurements. Details <br> on the settings are reported separately in each file.</p> <p><br> <strong>The data in the repository </strong></p> <p>Grainsize_data.zip This folder contains 4,853 ASCII TXT-files with the raw granulometric data. Filenames are unique timestamps (measurement date and time in the format <em>YYYYMMDDHHMMSS</em> CET). Each file comes with a header with relevant metadata and the measurement data. The metadata also contains the sample name, e.g., <em>O_55_oT</em> reads "O" for Ostrau, "55" sampling depth in cm, and "oT" for "ohne Teiler" (without separator, while "mT", "mit Teiler" would stand for with separator). For files for the profile Gleina, a "G" is used followed by the sampling depth range (two numbers, e.g., <em>G_380_382</em>) in cm. </p> <p>The files <em>Gleina_depth.txt</em>, <em>Ostrau02_depth.txt</em>, and <em>Ostrau03_depth.txt</em> allow a correlation with the profiles graphs published in Meszner (2015). </p> <p><br> <strong>References</strong></p> <p>Grassl, W., 2016. End-Member-Modellierungsanalyse an hochauflösenden Korngrößen der Lössprofile Ostrau und Gleina, Lommatzscher Pflege, Sachsen. unpublished Master thesis, TU Dresden.</p> <p>Kreutzer, S., Fuchs, M., Meszner, S., Faust, D., 2012. OSL chronostratigraphy of a loess-palaeosol sequence in Saxony/Germany using quartz of different grain sizes. Quaternary Geochronology 10, 102–109. doi:10.1016/j.quageo.2012.01.004</p> <p>Meszner, S., Fuchs, M., Faust, D., 2011. Loess-Paleosol-Sequences from the loess area of Saxony (Germany). E & G, Quaternary Science Journal 60, 47–65.</p> <p>Meszner, S., 2015. Loess from Saxony. A reconstruction of the Late Pleistocene landscape evolution and palaeoenvironment based on loess-palaeosol sequences from Saxony (Germany). Dresden. PhD thesis. TU Dresden. </p> <p>Meszner, S., Kreutzer, S., Fuchs, M., Faust, D., 2013. Late Pleistocene landscape dynamics in Saxony, Germany: Paleoenvironmental reconstruction using loess-paleosol sequences. Quaternary International 296, 95–107. doi:10.1016/j.quaint.2012.12.040</p> <p>Zech, M., Kreutzer, S., Zech, R., Goslar, T., Meszner, S., McIntyre, C., Häggi, C., Eglinton, T., Faust, D., Fuchs, M., 2017. Comparative 14C and OSL dating of loess-paleosol sequences to evaluate post-depositional contamination of n-alkane biomarkers. Quaternary Research 87, 180–189. doi:10.1017/qua.2016.7</p>
Where2Test Saxony-Czechia COVID-19 new cases dataset
<p>Data in the repository were used in the study "Fine-scale variation in the effect of national border on COVID-19 spread: A case study of the Saxon-Czech border region", published in <a href="https://www.sciencedirect.com/journal/spatial-and-spatio-temporal-epidemiology">Spatial and Spatio-temporal Epidemiology</a>.</p> <p>This repository consists of two files:</p> <p><strong>saxony-westczechia_cases7</strong></p> <p>Weekly numbers of new COVID-19 cases in all municipalities in Saxony and Northwestern Czechia (Liberec, Ústí nad Labem, and Karlovy Vary regions) in the first half of 2021. Data are extracted from the websites <a href="https://www.coronavirus.sachsen.de">coronavirus.sachsen</a> and <a href="https://onemocneni-aktualne.mzcr.cz/covid-19">onemocneni-aktualne.mzcr.cz/covid-19</a>. The missing values were interpolated, and daily values were recalculated to weekly values.</p> <p><strong>municipalities</strong></p> <p>The second file consists of a list of all municipalities with their names, geometries, and population values. For Germany, we used the dataset <a href="https://hub.arcgis.com/datasets/esri-de-content::gemeindegrenzen-2018-mit-einwohnerzahl/about">"Gemeindegrenzen 2018 mit Einwohnerzahl"</a> (© GeoBasis-DE / BKG, Statistisches Bundesamt (Destatis) (2020), <a href="http://www.govdata.de/dl-de/by-2-0">dl-de/by-2-0</a>) as a source of geometries and population sizes of the municipalities (“<em>Gemeinde”</em>) in Saxony. Czech population numbers on the municipality level ("obec") were taken from the <a href="https://www.czso.cz/csu/czso/population-of-municipalities-1-january-2021">Czech Statistical Office</a>, while the geometries were obtained from <a href="https://www.cuzk.cz/ruian/RUIAN.aspx">RÚIAN</a> (@<a href="http://geoportal.cuzk.cz">Czech Office for Surveying, Mapping and Cadastre</a>, 2021). To keep the same geometry detail on both sides of the borders, we applied the Douglas-Peucker simplification algorithm implemented in the Python library <a href="https://github.com/mattijn/topojson">TopoJSON</a>.</p>
Marteloscope data of the experimental plot, Naundorf 710 b1 (Saxony, Germany 2020)
<p>Yield data (diameter breast height and tree height) of a mixed stand in the Tharandt Forest, Germany. The data was collected for the establishment of a marteloscope site within the I+ network of the European Forest Institute.</p> <p> </p>
Dataset (81 forest parcels) supplementing the publication "Owner attitudes and landscape parameters drive stand structure and valuable habitats in small-scale private forests of Lower Saxony (Germany)"
<p>The dataset about 81 small-scale private forest parcels contains the answer variables and predictors used in the publication "Owner attitudes and landscape parameters drive stand structure and valuable habitats in small-scale private forests of Lower Saxony (Germany)".</p>
OpenDRIVE sample dataset of Test Bed Lower Saxony
<p>This OpenDRIVE dataset models a road network snippet of the motorway A39 near Wolfsburg. It is intended to be used for data evaluation. The data snippet is part of a greater dataset which has been acquired in the context of the project <a href="http://verkehrsforschung.dlr.de/en/projects/test-bed-lower-saxony-automated-and-connected-mobility">Test Bed Lower Saxony</a>. Main application scopes of this OpenDRIVE data are driving simulation, verification and validation. The raw data has been surveyed through mobile mapping end of 2019.</p>
Text-fig. 2. Kaolin clay pit at hill Hasenberg in Wiesa, Saxony, Germany; view of southern high wall, showing deeply weathered late Early Miocene lignite seam by dark brown color in center (photographed 2015). Fossil-bearing strata were reported (e.g., Mai 1964) as below lignite seam, but this horizon does actually not crop out (also evidenced by new drillings, communicated by Dr. Jochen Rascher, GEOMONTAN GmbH company, Freiberg/Sa., Germany). in Assessment Of Phytogeographic Reference Regions For Cenozoic Vegetation: A Case Study On The Miocene Flora Of Wiesa (Germany)
Text-fig. 2. Kaolin clay pit at hill Hasenberg in Wiesa, Saxony, Germany; view of southern high wall, showing deeply weathered late Early Miocene lignite seam by dark brown color in center (photographed 2015). Fossil-bearing strata were reported (e.g., Mai 1964) as below lignite seam, but this horizon does actually not crop out (also evidenced by new drillings, communicated by Dr. Jochen Rascher, GEOMONTAN GmbH company, Freiberg/Sa., Germany).
Fig. 9 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 9. Acanthoceratid ammonoid Spathites (Jeanrogericeras) reveliereanus (Courtiller, 1860) MMG: SaK 16896 from the lower Turonian of the Briessnitz Formation, Leubnitz, Germany. A. Outer whorl in ventral (A1), lateral (A2), and apertural (A3) views; the fracture at which the outer whorl separates from the inner whorl (arrow) and an umbilical tubercle (UT) are marked. B. Inner whorl in lateral (B1, B3) and apertural (B2) views; the umbilical tubercle (UT) and the position of the fracture shown in A2 are marked by arrow.
Fig. 6 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 6. Statistical test of potential dimorphism in Mammites nodosoides (Schlüter, 1871) based on 119 specimens. The repository number of each specimen is given on top of the diagram. A. Classical clustering; the red color characterises particularly small individuals with D = 33–65 mm in between the large group of potential microconchs. B. Linear discriminant analysis (LDA); the color code follows the assignment of the classical clustering above. The dark blue lines are biplots of all variables, an overlaying of a score plot and a loadings plot in a single graph, which enables to visualise high-dimensional data by using a two-dimensional graph.
Fig. 2 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 2. Ammonite morphological terms and key parameters. Modified after Wilmsen and Nagm (2014). Abbreviations: D, maximum diameter; d, larger radius of the shell; e, smaller radius of the shell; UD, diameter of the umbilicus; Wb, whorl breadth of the final whorl; Wh, height of the final whorl; for the suture line: A, adventive lobe; E, external lobe; U, umbilical lobe.
Fig. 1 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 1. Geological framework and stratigraphy of the lower Elbtal Group. A. Distribution of the Elbtal Group (green) in the area between Meissen and the German/Czech Republic border. B. Palaeogeographic setting of the Saxonian Cretaceous Basin (SCB). C. Chrono-, bio- and lithostratigraphy of the lower Elbtal Group in the area between Meissen and Dresden; the stratigraphic position of the ammonite faunas from the Briessnitz Formation is indicated. Supplemented and modified after Wilmsen et al. (2019, 2022) and Niebuhr et al. (2020). Abbreviations: A., Acanthoceras; Cunningt., Cunningtoniceras; M., Metoicoceras; mid., middle; Neocard., Neocardioceras.
Fig. 5 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 5. Photographic illustration of typical large (A) and small (B) specimens of the acanthoceratid ammonoid Mammites nodosoides (Schlüter, 1871) from the lower Turonian of the Briessnitz Formation, Leubnitz, Germany. A. MMG: SaK 5200 in lateral (A1) and apertural (A2) views. B. MMG: SaK 5203 in lateral (B1, B3) and apertural (B2) views.
Fig. 7 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 7. Photographic illustration of typical large (A) and small (B) specimens of the acanthoceratid ammonoid Spathites (Jeanrogericeras) reveliereanus (Courtiller, 1860) from the lower Turonian of the Briessnitz Formation, Leubnitz, Germany. A. MMG: SaK 5230 in lateral (A1) and apertural (A2) views. B. MMG: SaK 5256 in lateral (B1, B3) and ventral (B2) views.
Fig. 4 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 4. Statistical test of potential dimorphism in Lewesiceras peramplum (Mantell, 1822) based on 63 specimens. The repository number of each specimen is given on top of the diagram. A. Classical clustering; the red color characterises particularly small individuals with D <77 mm in between the group of potential microconchs. B. Linear discriminant analysis (LDA); the color code follows the assignment of the classical clustering above. The dark blue lines are biplots of all variables, an overlaying of a score plot and a loadings plot in a single graph, which enables to visualise high-dimensional data by using a two-dimensional graph.
Fig. 10 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 10. Representative antidimorphs: [m] = microconch, [M] = macroconch of the acanthoceratid ammonoid Spathites (Jeanrogericeras) reveliereanus Courtiller, 1860); based on (A) MMG: SaK 5256 in lateral (A1) and apertural (A2) views and (B) MMG: SaK 5230 in lateral (B1) and apertural (B2) views. Key features of both antidimorphs are listed (see text for further explanation).
Fig. 3 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 3. Photographic illustration of typical large (A) and small (B) specimens of the pachydiscid ammonoid Lewesiceras peramplum (Mantell, 1822) from the lower Turonian of the Briessnitz Formation, Dresden, Germany. A. MMG: SaK 5163 from Leubnitz, in lateral (A1) and ventral (A2) views. B. MMG: SaK 5343 from Leutewitz, in lateral (B1, B4), apertural (B2), and ventral (B3) views.
Fig. 8 in Dimorphism in Late Cretaceous ammonites- evidence from early Turonian ammonite faunas of the Briessnitz Formation in Saxony, Germany
Fig. 8. Statistical test of potential dimorphism in Spathites (Jeanrogericeras) reveliereanus (Courtiller, 1860) based on 38 specimens. The repository number of each specimen is given on top of the diagram. A. Classical clustering; inferred macro- and microconchs are marked by blue and red colors, respectively. B. Linear discriminant analysis (LDA); the color code follows the assignment of the classical clustering above. The dark blue lines are biplots of all variables, an overlaying of a score plot and a loadings plot in a single graph, which enables to visualise high-dimensional data by using a two-dimensional graph.
Figure 12 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 12. Columnar section of the Cenomanian–Turonian boundary and the Lower and Middle Turonian part of the Wunstorf core Wu 2010/4 with agglutinated foraminiferal morphogroups, Fisher alpha index, species richness, and foraminiferal events (acmes) indicated by arrows. For log legend, see Fig. 4.
Figure 11 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 11. Columnar section of the Cenomanian part of the Baddeckenstedt quarry with agglutinated foraminiferal morphogroups, Fisher alpha index, species richness, and foraminiferal events (acmes) indicated by arrows. For log legend, see Fig. 3; log redrawn after Wilmsen (2003: Fig. 8).
Figure 6 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 6. Late Albian to Turonian agglutinated foraminifera from the Lower Saxonian Cretaceous; scale bars are 100 µm. (a) Saccammina grzybowski, Wunstorf Wu2010/1, 54.00 m. (b) Psammosphaera fusca, Wunstorf Wu2010/1, 59.05 m. (c) Tipeammina elliptica, Söhlde section, 31.00 m. (d–e) Tipeammina sp. 1, Wunstorf Wu2010/4, 43.30 m. (f) Hyperammina gaultina, Wunstorf Wu 2010/4, 48.20 m. (g–h) Ammolagena clavata, two specimens sticking together, Wunstorf Wu2010/3, 25.50 m. (i) Ammolagena contorta, possibly previously attached on an inoceramid prism, Wunstorf Wu2010/4, 38.20 m. (j) Caudammina ovula, Söhlde section, 31.00 m. (k) Subreophax scalaris, Wunstorf Wu2010/1, 69.10 m. (l) Ammodiscus cretaceus, Wunstorf Wu 2010/4, 48.20 m. (m) Ammodiscus glabratus, Wunstorf Wu2010/1, 54.65 m. (n) Ammodiscus peruvianus, Wunstorf Wu2010/1, 54.00 m. (o) Ammodiscus tenuissimus, Wunstorf Wu2010/4, 43.30 m. (p) Glomospira diffundens, Wunstorf Wu2010/1, 49.05 m. (q) Glomospira gordialis, Wunstorf Wu 2010/3, 66.05 m. (r) Repmanina charoides, Wunstorf Wu2010/4, 38.20 m. (s) Lituotuba lituiformis, Wunstorf Wu 2010/4, 48.95 m. (t) Rzehakina minima, Wunstorf Wu2010/1, 54.80 m.
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