Leben für die Sache. Vera Figner, Vera Zasulič und das radikale Milieu im späten Zarenreich

In der zweiten Hälfte des 19. Jahrhunderts treten in Russland vermehrt Frauen und Männer in die Öffentlichkeit, die durch radikale Veränderungen einen „neuen Menschen“ und mit ihm eine neue Gesellschaft schaffen wollen. Vera Figner und Vera Zasulič, die beiden Protagonistinnen der vorliegenden Untersuchung, sind herausragende Vertreterinnen der radikalen Bewegung im ausgehenden Zarenreich. Während Vera Zasulič mit ihrem Attentat auf den St. Petersburger Stadtkommandanten Fëdor Trepov 1878 am Beginn der ersten terroristischen Welle in Russland steht, ist Vera Figner bei ihrer Verhaftung 1883 das letzte führende Mitglied der Terrororganisation Narodnaja Volja (Volkswille), die am 1./13. März 1881 einen tödlichen Anschlag auf Zar Aleksandr II. verübt. Die beiden Frauen verbindet zwar kein engerer persönlicher Kontakt, dafür aber die Zugehörigkeit zum selben Milieu. Beeinflusst von der progressiven Debatte in der Intelligencija der 1860er Jahre entschlossen sie sich bereits in ihrer Jugend, sich von traditionellen Standes- und Geschlechterrollen zu lösen, ihr Schicksal „in die eigenen Hände zu nehmen“ und sich einer „Sache“ zu verschreiben. Zusammen mit anderen Radikalen gerieten sie dadurch in einen immer heftigeren Konflikt mit der autokratischen Staatsmacht, der sich schließlich zu einem Kampf mit terroristischen Mitteln steigerte. Stephan Rindlisbacher nutzt die Biographien dieser beiden radikalen Frauen als „Scheinwerfer“, um das radikale Milieu mit seinen Merkmalen, Funktionsmechanismen und Handlungsspielräumen auszuleuchten. Aus zwei voneinander unabhängigen aber vergleichbaren Blickwinkeln zeichnet er ein eindrucksvolles Bild nicht nur der radikalen Netzwerkstrukturen, Symbole, Praktiken und Identitätsnarrativen, sondern auch der beteiligten Menschen mit ihren Wünschen, Hoffnungen und Ängsten.

Crystal chemistry and hydrogen bonding of rustumite Ca10(Si2O7)2(SiO4)(OH)2Cl2 with variable OH, Cl, F

Three samples of the skarn mineral rustumite Ca10(Si2O7)2(SiO4)(OH)2Cl2, space group C2/c, a ≈7.6, b ≈ 18.5, c ≈ 15.5 Å, β ≈ 104°, with variable OH, Cl, F content were investigated by electron microprobe, single-crystal X-ray structure refinements, and Raman spectroscopy. “Rust1LCl” is a low chlorine rustumite Ca10(Si2O7)2(SiO4)(OH1.88F0.12)(Cl1.28,OH0.72) from skarns associated with the Rize batholith near Ikizedere, Turkey. “Rust2F” is a F-bearing rustumite Ca10(Si2O7)2(SiO4)(OH1.13F0.87) (Cl1 96OH0.04) from xenoliths in ignimbrites of the Upper Chegem Caldera, Northern Caucasus, Russia. “Rust3LClF” represents a low-Cl, F-bearing rustumite Ca10(Si2O7)2(SiO4)0.87(H4O4)0.13(OH1.01F0.99) (Cl1.00 OH1.00) from altered merwinite skarns of the Birkhin massif, Baikal Lake area, Eastern Siberia, Russia. Rustumite from Birkhin massif is characterized by a significant hydrogarnet-like or fluorine substitution at the apices of the orthosilicate group, leading to specific atomic displacements. The crystal structures including hydrogen positions have been refined from single-crystal X-ray data to R1 = 0.0205 (Rust1_LCl), R1 = 0.0295 (Rust2_F), and R1 = 0.0243 (Rust3_LCl_F), respectively. Depletion in Cl and replacement by OH is associated with smaller unit-cell dimensions. The substitution of OH by F leads to shorter hydrogen bonds O-H⋯F instead of O-H⋯OH. Raman spectra for all samples have been measured and confirm slight strengthening of the hydrogen bonds with uptake of F.This study discusses the complex crystal chemistry of the skarn mineral rustumite and may provide a wider understanding of the chemical reactions related to contact metamorphism of limestones.

Recovery of large carnivores in Europe's modern human-dominated landscapes.

The conservation of large carnivores is a formidable challenge for biodiversity conservation. Using a data set on the past and current status of brown bears (Ursus arctos), Eurasian lynx (Lynx lynx), gray wolves (Canis lupus), and wolverines (Gulo gulo) in European countries, we show that roughly one-third of mainland Europe hosts at least one large carnivore species, with stable or increasing abundance in most cases in 21st-century records. The reasons for this overall conservation success include protective legislation, supportive public opinion, and a variety of practices making coexistence between large carnivores and people possible. The European situation reveals that large carnivores and people can share the same landscape.

Contrasting PT paths within the Barchi-Kol UHP terrain (Kokchetav Complex): Implications for subduction and exhumation of continental crust

The Barchi-Kol terrain is a classic locality of ultrahigh-pressure (UHP) metamorphism within the Kokchetav metamorphic belt. We provide a detailed and systematic characterization of four metasedimentary samples using dominant mineral assemblages, mineral inclusions in zircon and monazite, garnet zonation with respect to major and trace elements, and Zr-in-rutile and Ti-in-zircon temperatures. A typical diamond-bearing gneiss records peak conditions of 49 ± 4 kbar and 950–1000 °C. Near isothermal decompression of this rock resulted in the breakdown of phengite associated with a pervasive recrystallization of the rock. The same terrain also contains mica schists that experienced peak conditions close to those of the diamond-bearing rocks, but they were exhumed along a cooler path where phengite remained stable. In these rocks, major and trace element zoning in garnet has been completely equilibrated. A layered gneiss was metamorphosed at UHP conditions in the coesite field, but did not reach diamond-facies conditions (peak conditions: 30 kbar and 800–900 °C). In this sample, garnet records retrograde zonation in major elements and also retains prograde zoning in trace elements. A garnet-kyanite-micaschist that reached significantly lower pressures (24 ± 2 kbar, 710 ± 20 °C) contains garnet with major and trace element zoning. The diverse garnet zoning in samples that experienced different metamorphic conditions allows to establish that diffusional equilibration of rare earth element in garnet likely occurs at ~900–950 °C. Different metamorphic conditions in the four investigated samples are also documented in zircon trace element zonation and mineral inclusions in zircon and monazite. U-Pb geochronology of metamorphic zircon and monazite domains demonstrates that prograde (528–521 Ma), peak (528–522 Ma), and peak to retrograde metamorphism (503–532 Ma) occurred over a relatively short time interval that is indistinguishable from metamorphism of other UHP rocks within the Kokchetav metamorphic belt. Therefore, the assembly of rocks with contrasting P-T trajectories must have occurred in a single subduction-exhumation cycle, providing a snapshot of the thermal structure of a subducted continental margin prior to collision. The rocks were initially buried along a low geothermal gradient. At 20–25 kbar they underwent near isobaric heating of 200 °C, which was followed by continued burial along a low geothermal gradient. Such a step-wise geotherm is in good agreement with predictions from subduction zone thermal models.