Die Dankeskirche in Berlin und deren feierliche Einweihung am 3. Januar 1884

DIE DANKESKIRCHE IN BERLIN UND DEREN FEIERLICHE EINWEIHUNG AM 3. JANUAR 1884 Die Dankeskirche in Berlin und deren feierliche Einweihung am 3. Januar 1884 / Brückner, ... (Public Domain) ( - ) ColorChart ( - ) Cover front ( - ) Endsheet ( - ) Illustration: Die Dankeskirche in Berlin auf dem Weddingplatz ( - ) Title page ( - ) Einweihungsfeier der Dankeskirche in Berlin (3) Weiheact (4) Liturgie (8) Fest-Predigt (8) Schluß-Liturgie (12) Gebet, Vaterunser, Segen (13) Die Dankeskirche auf dem Weddingplatz in Berlin (14) Illustration: Die Dankeskirche in Berlin auf dem Weddingplatz (Situationsplan) (14) Illustration: Die Dankeskirche in Berlin auf dem Weddingplatz (Grundriß) (15) Illustration: Die Dankeskirche in Berlin auf dem Weddingplatz (Durchschnitts-Ansicht) ([16]) Nachsatzblatt ( - ) Cover back ( -

How are soil use and management reflected by soil organic matter characteristics: a spectroscopic approach

We studied the quantitative and qualitative changes of soil organic matter (SOM) due to different land uses (arable versus grassland) and treatments (organic manure and mineral fertilizer) within an agricultural crop rotation in a long-term field experiment, conducted since 1956 at Ultuna, Sweden, on a Eutric Cambisol. The organic carbon (OC) content of the grassland plot was 1.8 times greater than that of the similarly fertilized Ca(NO3) 2 treated cropped plots. The comparison of two dispersion techniques (a lowenergy sonication and a chemical dispersion which yield inherent soil aggregates) showed that increasing OC contents of the silt-sized fractions were not matched by a linear increase of silt-sized aggregates. This indicated saturation of the aggregates with OC and a limited capacity of particles to protect OC physically. Thermogravimetric analyses suggested an increase of free organic matter with increasing OC contents. Transmission FT-IR spectroscopy showed relative enrichment of carboxylic, aromatic, CH and NH groups in plots with increasing OC contents. The silt-sized fractions contained the largest SOM pool and, as revealed by 13C NMR spectroscopy, were qualitatively more influenced by the plant residue versus manure input than the clay fractions. Alkyl and O-alkyl C in the silt-sized fractions amounted to 57.4% of organic carbon in the animal manure treated plots and 50–53% in the other treatments.We thank the Austrian Science Fund (Fonds zur FÖrderung der wissenschaftlichen Forschung) for funding this bilateral project.Peer reviewe

High-speed 850 nm VCSELs with 28 GHz modulation bandwidth operating error-free up to 44 Gbit/s

A new generation of high-speed oxide confined 850 nm vertical cavity surface-emitting lasers is presented. A record high modulation bandwidth of 28 GHz is achieved and error-free data transmission at bit-rates up to 44 Gbit/s is demonstrated

Organische Bodensubstanz in sulfatsauren Böden

Sulfatsaure Böden sind Böden und Sedimente, die Eisensulfide enthalten und verbreitet in Küstenregionen und Binnenländern vorkommen. Unter wassergesättigten Bedingungen sind sie produktive Böden der Feuchtgebiete. Eine Austrocknung dieser Böden (durch Entwässerung oder Dürreperioden) führt zur Oxidation der Eisensulfide und damit zu einer starken Versauerung aufgrund der Freisetzung von Schwefelsäure. Nach Wiedervernässung und Wiedereinsetzen reduzierender Bedingungen führt die Aktivität sulfatreduzierender Bakterien zur Bildung von Pyrit und damit zur pH-Erhöhung. Sulfatreduzierende Bakterien sind heterotroph und benötigen ausreichend verfügbares organisches Material. In vielen Regionen kommt es jedoch nach Wiedervernässung solcher Standorte nicht zum erwarteten pH-Anstieg. Dies weist auf eine geringe Aktivität sulfatreduzierender Bakterien hin, obwohl die Gesamtmenge an organischer Bodensubstanz (OBS) in diesen Böden oft hoch ist. Wir vermuten daher, dass eine geringe Verfügbarkeit von OBS die Aktivität der Sulfatreduzierer in wiedervernässten sulfatsauren Böden limitiert. In unserer Studie wurden Menge und Zusammensetzung der OBS in Bodenprofilen zweier wiedervernässter sulfatsaurer Böden in Südaustralien untersucht. Hierbei wurde das Augenmerk besonders auf die verfügbare, nicht-mineralassoziierte OBS gelegt. Bei beiden Standorten handelte es sich um Flußsedimente, die während einer extremen Dürreperiode zwischen 2008 und 2010 tiefgründig austrockneten und stark versauerten (pH <4). Seit dem Ende der Dürreperiode sind beide Standorte wieder vollständig vernässt. In einem Standort erholte sich der pH-Wert vollständig und zeigte 2015 neutrale pH-Werte, während der andere Standort im Unterboden noch immer deutlich versauert war. In den Bodenproben wurde die Menge der OBS bestimmt und mittels Dichtefraktionierung der Anteil der nicht-mineralassoziierten OBS analysiert. Die chemische Zusammensetzung der OBS wurde mittels Festkörper 13C NMR Spektroskopie und Neutralzuckeranalytik untersucht. Es zeigte sich, dass die sulfatsauren Böden zwar hohe OBS-Mengen, jedoch niedrige Anteile an leicht abbaubaren Kohlenhydraten und Proteinen und hohe Anteile an schwer abbaubaren Lipiden und Lignin enthalten. Die geringsten Gehalte an Kohlenhydraten und Proteinen fanden sich im immer noch stark versauerten Boden. Schwer abbaubare OBS ist kaum als Substrat für Sulfatreduzierer geeignet und erschwert somit die pH-Erhöhung in wiedervernässten sulfatsauren Böden

Microscale spatial distribution and soil organic matter persistence in top and subsoil

The spatial distribution of organic substrates and microscale soil heterogeneity significantly influence organic matter (OM) persistence as constraints on OM accessibility to microorganisms. However, it is unclear how changes in OM spatial heterogeneity driven by factors such as soil depth affect the relative importance of substrate spatial distribution on OM persistence. This work evaluated the decomposition and persistence of 13C and 15N labeled water-extractable OM inputs over 50 days as either hotspot (i.e., pelleted in 1 – 2 mm-size pieces) or distributed (i.e., added as OM < 0.07 µm suspended in water) forms in topsoil (0-0.2 m) and subsoil (0.8-0.9 m) samples of an Andisol. We observed greater persistence of added C in the subsoil with distributed OM inputs relative to hotspot OM, indicated by a 17% reduction in cumulative mineralization of the added C and a 10% higher conversion to mineral-associated OM. A lower substrate availability potentially reduced mineralization due to OM dispersion throughout the soil. NanoSIMS (nanoscale secondary ion mass spectrometry) analysis identified organo-mineral associations on cross-sectioned aggregate interiors in the subsoil. On the other hand, in the topsoil, we did not observe significant differences in the persistence of OM, suggesting that the large amounts of particulate OM already present in the soil outweighed the influence of added OM spatial distribution. Here, we demonstrated under laboratory conditions that the spatial distribution of fresh OM input alone significantly affected the decomposition and persistence of OM inputs in the subsoil. On the other hand, spatial distribution seems to play a lower role in topsoils rich in particulate OM. The divergence in the influence of OM spatial distribution between the top and subsoil is likely driven by differences in soil mineralogy and OM composition.Microscale spatial distribution and soil organic matter persistence in top and subsoilpublishedVersio

Biotic and abiotic controls on carbon storage in aggregates in calcareous alpine and prealpine grassland soils

Alpine and prealpine grasslands provide various ecosystem services and are hotspots for the storage of soil organic C (SOC) in Central Europe. Yet, information about aggregate-related SOC storage and its controlling factors in alpine and prealpine grassland soils is limited. In this study, the SOC distribution according to the aggregate size classes large macroaggregates (> 2000 μm), small macroaggregates (250–2000 μm), microaggregates (63–250 μm), and silt-/clay-sized particles (< 63 μm) was studied in grassland soils along an elevation gradient in the Northern Limestone Alps of Germany. This was accompanied by an analysis of earthworm abundance and biomass according to different ecological niches. The SOC and N stocks increased with elevation and were associated with relatively high proportions of water-stable macroaggregates due to high contents of exchangeable Ca$^{2+}$ and Mg$^{2+}$. At lower elevations, earthworms appeared to act as catalyzers for a higher microaggregate formation. Thus, SOC stabilization by aggregate formation in the studied soils is a result of a joined interaction of organic matter and Ca$^{2+}$ as binding agents for soil aggregates (higher elevations), and the earthworms that act as promoters of aggregate formation through the secretion of biogenic carbonates (low elevation). Our study highlights the importance of aggregate-related factors as potential indices to evaluate the SOC storage potential in other mountainous grassland soils

Rab3D is critical for secretory granule maturation in PC12 cells.

Neuropeptide- and hormone-containing secretory granules (SGs) are synthesized at the trans-Golgi network (TGN) as immature secretory granules (ISGs) and complete their maturation in the F-actin-rich cell cortex. This maturation process is characterized by acidification-dependent processing of cargo proteins, condensation of the SG matrix and removal of membrane and proteins not destined to mature secretory granules (MSGs). Here we addressed a potential role of Rab3 isoforms in these maturation steps by expressing their nucleotide-binding deficient mutants in PC12 cells. Our data show that the presence of Rab3D(N135I) decreases the restriction of maturing SGs to the F-actin-rich cell cortex, blocks the removal of the endoprotease furin from SGs and impedes the processing of the luminal SG protein secretogranin II. This strongly suggests that Rab3D is implicated in the subcellular localization and maturation of ISGs

Italy’s Path to Very Low Fertility: The Adequacy of Economic and Second Demographic Transition Theories: Le cheminement de l’Italie vers les très basses fécondités: Adéquation des théories économique et de seconde transition démographique

The deep drop of the fertility rate in Italy to among the lowest in the world challenges contemporary theories of childbearing and family building. Among high-income countries, Italy was presumed to have characteristics of family values and female labor force participation that would favor higher fertility than its European neighbors to the north. We test competing economic and cultural explanations, drawing on new nationally representative, longitudinal data to examine first union, first birth, and second birth. Our event history analysis finds some support for economic determinants of family formation and fertility, but the clear importance of regional differences and of secularization suggests that such an explanation is at best incomplete and that cultural and ideational factors must be considered