Studi su Cimone. Saggio di storia greca, ca. 478-461 a.C.

La monografia propone un’analisi del periodo ca. 478-461 a.C. della storia ateniese e delle vicende di Cimone figlio di Milziade entro il contesto contemporaneo. Lo studio dell’Atene, e più in generale di varie realtà elleniche affacciate sull’Egeo, negli immediati anni ‘post-persiani’ si articola in due parti: la prima ripercorre in senso cronologico le notizie, essenzialmente letterarie, disponibili in merito alle attività politiche e militari di Atene, quale guida dell’alleanza greca; la seconda trae conclusioni di respiro più ampio, fondate sull’analisi precedente, e cerca una sintesi del periodo e del personaggio nel superamento di stereotipi e condizionamenti letterari. In tale ottica si esprime una riflessione, a partire dalla scarna trattazione tucididea, sui meccanismi attraverso i quali la tradizione ha deformato e sedimentato le informazioni disponibili generando un progressivo arricchimento che ha portato alla definizione, di fatto, di una ‘era cimoniana’ che è possibile mettere in discussione in alcuni tratti essenziali. Si mira dunque a proporre una valutazione del periodo priva di alcuni elementi, in ultimo evidenti soprattutto nell’approccio plutarcheo alla materia, che appaiono alieni al contesto di riferimento per la prima parte del V secolo: i temi principali ai quali si dedica la riflessione sono quelli dell’imperialismo ateniese, del filolaconismo, della bipolarità tra democrazia e oligarchia, della propaganda politico-mitologica. Il rapporto di Atene con Sparta, con gli Ioni e con le altre realtà del mondo egeo viene letto alla luce degli indizi disponibili sul clima di incertezza e di delicati equilibri creatosi all’indomani della ritirata delle forze persiane. Il ritratto di Cimone che si propone è quello di una figura indubbiamente significativa nella politica contemporanea ma, al contempo, fortemente condizionata e talora adombrata da dinamiche in qualche modo condivise all’interno dello scenario politico ateniese, improntato alla soddisfazione di necessità e volontà che la tradizione renderà archetipiche del paradigma democratico.

Funktionelle Analyse der Plasmamembran-Ca 2+-ATPase 2 -PMCA2- in Modellen der Neurodegeneration

Calcium (Ca2+) ist ein ubiquitär vorkommendes Signalmolekül, das an der Regulation zahlreicher zellulärer Prozesse, von der Proliferation bis zum programmierten Zelltod, beteiligt ist. Daher müssen die intrazellulären Ca2+-Spiegel streng kontrolliert werden. Veränderungen der Ca2+-Homöostase während der altersassoziierten Neurodegeneration können dazu beitragen, dass Neuronen vulnerabler sind. So wurden erhöhte Ca2+-Konzentrationen in gealterten Neuronen, begleitet von einer erhöhten Vulnerabilität, beobachtet (Hajieva et al., 2009a). Weiterhin wird angenommen, dass der selektive Untergang von dopaminergen Neuronen bei der Parkinson Erkrankung auf eine erhöhte Ca2+-Last zurückzuführen sein könnte, da diese Neuronen einem ständigen Ca2+-Influx,rnaufgrund einer besonderen Isoform (CaV 1.3) spannungsgesteuerter Ca2+-Kanäle des L-Typs, ausgesetzt sind (Chan et al., 2007). Bislang wurden die molekularen Mechanismen, die einem Ca2+-Anstieg zu Grunde liegen und dessen Auswirkung jedoch nicht vollständig aufgeklärt und daher in der vorliegenden Arbeit untersucht. Um Veränderungen der Ca2+-Homöostase während der altersassoziiertenrnNeurodegeneration zu analysieren wurden primäre Mittelhirnzellen aus Rattenembryonen und SH-SY5Y-Neuroblastomazellen mit dem Neurotoxin 1-Methyl-4-Phenyl-Pyridin (MPP+), das bei der Etablierung von Modellen der Parkinson-Erkrankung breite Anwendung findet, behandelt. Veränderungen der intrazellulären Ca2+-Konzentration wurden mit einem auf dem grün fluoreszierenden Protein (GFP)-basierten Ca2+-Indikator,rn„Cameleon cpYC 3.6“ (Nagai et al., 2004), ermittelt. Dabei wurde in dieser Arbeit gezeigt, dass MPP+ die Abregulation der neuronenspezifischen ATP-abhängigen Ca2+-Pumpe der Plasmamembran (PMCA2) induziert, die mit der Ca2+-ATPase des endoplasmatischen Retikulums (SERCA) und dem Na+/Ca2+-Austauscher (NCX) das zelluläre Ca2+-Effluxsystem bildet, was zu einer erhöhten zytosolischen Ca2+-Konzentration führt. Die PMCA2-Abnahme wurde sowohl auf Transkriptionsebene als auch auf Proteinebene demonstriert, während keine signifikanten Veränderungen der SERCA- und NCX-Proteinmengen festgestellt wurden. Als Ursache der Reduktion der PMCA2-Expression wurde eine Abnahme des Transkriptionsfaktors Phospho-CREB ermittelt, dessen Phosphorylierungsstatus abhängig von der Proteinkinase A (PKA) war. Dieser Mechanismus wurde einerseits unter MPP+-Einfluss und andererseits vermittelt durch endogene molekulare Modulatoren gezeigt. Interessanterweise konnten die durch MPP+ induzierte PMCA2-Abregulation und der zytosolische Ca2+-Anstieg durch die Aktivierung der PKA verhindert werden. Parallel dazu wurde eine MPP+-abhängige verringerte mitochondriale Ca2+-Konzentration nachgewiesen, welche mit einer Abnahme des mitochondrialen Membranpotentials korrelierte. Darüber hinaus kam es als Folge der PMCA2-Abnahme zu einem verminderten neuronalen Überleben.rnVeränderungen der Ca2+-Homöostase wurden auch während der normalen Alterung inrnprimären Fibroblasten und bei Mäusen nachgewiesen. Dabei wurden verringerte PMCA und SERCA-Proteinmengen in gealterten Fibroblasten, einhergehend mit einem Anstieg der zytosolischen Ca2+-Konzentration demonstriert. Weiterhin wurden verringerte PMCA2-Proteinmengen im Mittelhirn von gealterten Mäusen (C57B/6) detektiert.rnDer zelluläre Ca2+-Efflux ist somit sowohl im Zuge der physiologischen Alterung als auch in einem altersbezogenen Krankheitsmodell beeinträchtigt, was das neuronale Überleben beeinflussen kann. In zukünftige Studien soll aufgeklärt werden, welche Auswirkungen einer PMCA2-Reduktion genau zu dem Verlust von Neuronen führen bzw. ob durch eine PMCA2-Überexpression neurodegenerative Prozesse verhindert werden können.

Ca(2+) release from the sarcoplasmic reticulum activated by the low affinity Ca(2+) chelator TPEN in ventricular myocytes

The Ca(2+) content of the sarcoplasmic reticulum (SR) of cardiac myocytes is thought to play a role in the regulation and termination of SR Ca(2+) release through the ryanodine receptors (RyRs). Experimentally altering the amount of Ca(2+) within the SR with the membrane-permeant low affinity Ca(2+) chelator TPEN could improve our understanding of the mechanism(s) by which SR Ca(2+) content and SR Ca(2+) depletion can influence Ca(2+) release sensitivity and termination. We applied laser-scanning confocal microscopy to examine SR Ca(2+) release in freshly isolated ventricular myocytes loaded with fluo-3, while simultaneously recording membrane currents using the whole-cell patch-clamp technique. Following application of TPEN, local spontaneous Ca(2+) releases increased in frequency and developed into cell-wide Ca(2+) waves. SR Ca(2+) load after TPEN application was found to be reduced to about 60% of control. Isolated cardiac RyRs reconstituted into lipid bilayers exhibited a two-fold increase of their open probability. At the low concentration used (20-40muM), TPEN did not significantly inhibit the SR-Ca(2+)-ATPase in SR vesicles. These results indicate that TPEN, traditionally used as a low affinity Ca(2+) chelator in intracellular Ca(2+) stores, may also act directly on the RyRs inducing an increase in their open probability. This in turn results in an increased Ca(2+) leak from the SR leading to its Ca(2+) depletion. Lowering of SR Ca(2+) content may be a mechanism underlying the recently reported cardioprotective and antiarrhythmic features of TPEN.

Intracellular Ca(2+) operates a switch between repair and lysis of streptolysin O-perforated cells

Pore-forming (poly)peptides originating from invading pathogens cause plasma membrane damage in target cells, with consequences as diverse as proliferation or cell death. However, the factors that define the outcome remain unknown. We show that in cells maintaining an intracellular Ca(2+) concentration [Ca(2+)](i) below a critical threshold of 10 microM, repair mechanisms seal off 'hot spots' of Ca(2+) entry and shed them in the form of microparticles, leading to [Ca(2+)](i) reduction and cell recovery. Cells that are capable of preventing an elevation of [Ca(2+)](i) above the critical concentration, yet are unable to complete plasma membrane repair, enter a prolonged phase of [Ca(2+)](i) oscillations, accompanied by a continuous shedding of microparticles. When [Ca(2+)](i) exceeds the critical concentration, an irreversible formation of ceramide platforms within the plasma membrane and their internalisation drives the dying cells beyond the 'point of no return'. These findings show that the extent of [Ca(2+)](i) elevation determines the fate of targeted cells and establishes how different Ca(2+)-dependent mechanisms facilitate either cell survival or death.

Differential Effects on Survival, Humoral Immune Responses and Brain Lesions in Inbred BALB/C, CBA/CA, and C57BL/6 Mice Experimentally Infected with Neospora caninum Tachyzoites

C57BL/6, BALB/c, and CBA/Ca mouse strains with different MHC-I haplotypes were compared with respect to susceptibility to Neospora caninum infection. Groups of 5 mice received , , or tachyzoites of the NC-Liverpool isolate by intraperitoneal injection and were observed for disease symptoms. Humoral responses, splenocyte interferon-γ (IFN-γ) production, cerebral parasite loads, and histopathology were evaluated at human end points or the latest at 34 days postinfection (PI). The mortality rates in C57BL/6 mice were the highest, and relatively high levels of IgG1 antibodies were detected in those mice surviving till 34 days PI. In lymphocyte proliferation assays, spleen cells from C57BL6 mice stimulated with N. caninum antigen extract exhibited large variations in IFN-γ production. In BALB/c mice mortality was 0% at the lowest and 100% at the highest infection dose. Serologically they responded with high levels of both IgG2a and IgG1 subclasses, and lymphocyte proliferation assays of surviving mice yielded lower IFN-γ levels. CBA/Ca mice were the most resistant, with no animal succumbing to infection at a dose of and tachyzoites, but 100% mortality at tachyzoites. High IgG2a levels as well as increased IFN-γ in lymphocyte proliferation assays were measured in CBA/Ca mice infected with tachyzoites.

Hyalotekite, (Ba,Pb,K)(4)(Ca,Y)(2)Si-8(B,Be)(2)(Si,B)(2)O28F, a Tectosilicate Related to Scapolite: New Structure Refinement, Phase Transitions and a Short-Range Ordered 3B Superstructure

Hyalotekite, a framework silicate of composition (Ba,Pb,K)(4)(Ca,Y)(2)Si-8(B,Be)(2) (Si,B)(2)O28F, is found in relatively high-temperature(greater than or equal to 500 degrees C) Mn skarns at Langban, Sweden, and peralkaline pegmatites at Dara-i-Pioz, Tajikistan. A new paragenesis at Dara-i-Pioz is pegmatite consisting of the Ba borosilicates leucosphenite and tienshanite, as well as caesium kupletskite, aegirine, pyrochlore, microcline and quartz. Hyalotekite has been partially replaced by barylite and danburite. This hyalotekite contains 1.29-1.78 wt.% Y2O3, equivalent to 0.172-0.238 Y pfu or 8-11% Y on the Ca site; its Pb/(Pb+Ba) ratio ranges 0.36-0.44. Electron microprobe F contents of Langban and Dara-i-Pioz hyalotekite range 1.04-1.45 wt.%, consistent with full occupancy of the F site. A new refinement of the structure factor data used in the original structural determination of a Langban hyalotekite resulted in a structural formula, (Pb1.96Ba1.86K0.18)Ca-2(B1.76Be0.24)(Si1.56B0.44)Si8O28F, consistent with chemical data and all cations with positive-definite thermal parameters, although with a slight excess of positive charge (+57.14 as opposed to the ideal +57.00). An unusual feature of the hyalotekite framework is that 4 of 28 oxygens are non-bridging; by merging these 4 oxygens into two, the framework topology of scapolite is obtained. The triclinic symmetry of hyalotekite observed at room temperature is obtained from a hypothetical tetragonal parent structure via a sequence of displacive phase transitions. Some of these transitions are associated with cation ordering, either Pb-Ba ordering in the large cation sites, or B-Be and Si-B ordering on tetrahedral sites. Others are largely displacive but affect the coordination of the large cations (Pb, Ba, K, Ca). High-resolution electron microscopy suggests that the undulatory extinction characteristic of hyalotekite is due to a fine mosaic microstructure. This suggests that at least one of these transitions occurs in nature during cooling, and that it is first order with a large volume change. A diffuse superstructure observed by electron diffraction implies the existence of a further stage of short-range cation ordering which probably involves both (Pb,K)-Ba and (BeSi,BB)-BSi.

Vapnikite Ca<SUB>3UO6 – a new double-perovskite mineral from pyrometamorphic larnite rocks of the Jabel Harmun, Palestinian Autonomy, Israel

The new mineral species vapnikite, Ca3UO6, was found in larnite pyrometamorphic rocks of the Hatrurim Formation at Jabel Harmun in the Judean desert, Palestinian Autonomy, Israel. Vapnikite is an analogue of the synthetic ordered double-perovskite β-Ca3UO6 and is isostructural with the natural fluorperovskite – cryolite Na3AlF6. Vapnikite Ca3UO6 (P21/n,Z = 2, a = 5.739(1), b = 5.951(1), c = 8.312(1) Å, β = 90.4(1)°, V = 283.9(1) Å3) forms yellow-brown xenomorphic grains with a strong vitreous lustre. Small grains up to 20 – 30 m m in size are wedged between larnite, brownmillerite and ye'elimite. Vapnikite has irregular fracture, cleavage and parting were not observed. The calculated density is 5.322 g cm–3, the microhardness is VHN25 = 534 kg mm–2 (mean of seven measurements) corresponding to the hardness of ~5 on the Mohs scale. The crystal structure of vapnikite Ca3UO6 differs from that of its synthetic analogue β-Ca3UO6 by having a larger degree of Ca, U disorder. Vapnikite formed at the high-temperature retrograde stage of pyrometamorphism when larnite rocks were altered by fluids/melts of high alkalinity.

The Lord of Heaven in the Inner Chambers: Jesuits, Women, and Domestic Christianity (ca. 1580-1690)

The study focuses on gender norms and practices in Chinese Christian communities established by Jesuit missionary activity during the long seventeenth century. It analyzes how European and Chinese gender norms and practices affected each other in the context of the Sino-Western cultural contact initiated by the missionaries. The thesis consists of two parts. First, it analyzes the ways in which European Jesuits engaged with Chinese gender relations in the course of their mission in China. The study demonstrates that the Jesuits’ adoption of the Chinese scholar-gentry’s habitus entailed a partial adaptation to Confucian gender norms. The latter placed great emphasis on gender segregation and therefore discouraged direct communication between missionaries and Chinese women. This resulted in the emergence of organizational and devotional arrangements of Christian communities specific to China. Second, the study discusses Chinese Christian women's religious culture that emerged in the absence of a strong missionary presence among female devotees. It points out that Chinese Christian women created their own ritual culture and religious sociability in the domestic context, and that they actively took part in shaping Chinese Christianity as masters of domestic rituals.

Dinoflagellate cyst assemblages, oxygen isotope records of foraminifera, and alkenone and Mg/Ca-based SST estimates for the time interval 3.40-3.18 Ma (Late Pliocene) from five North Atlantic and Caribbean sediment cores

The early Late Pliocene (3.6 to ~3.0 million years ago) is the last extended interval in Earth's history when atmospheric CO2 concentrations were comparable to today's and global climate was warmer. Yet a severe global glaciation during marine isotope stage (MIS) M2 interrupted this phase of global warmth ~3.30 million years ago, and is seen as a premature attempt of the climate system to establish an ice-age world. Our geochemical and palynological records from five marine sediment cores along a Caribbean to eastern North Atlantic transect show that increased Pacific-to-Atlantic flow via the Central American Seaway weakened the North Atlantic Current (NAC) and attendant northward heat transport prior to MIS M2. The consequent cooling of the northern high latitude oceans permitted expansion of the Greenland ice sheet during MIS M2, despite near-modern atmospheric CO2 concentrations. Before and after MIS M2, heat transport via the NAC was crucial in maintaining warm climates comparable to those predicted for the end of this century.

Stable oxygen isotope record and Mg/Ca ratios at the Mid-Pleistocene Climate Transition, ODP Site 181-1123

Earth's climate underwent a fundamental change between 1250 and 700 thousand years ago, the Mid-Pleistocene Transition (MPT), when the dominant periodicity of climate cycles changed from 41,000 to 100,000 years in the absence of significant change in orbital forcing. Over this time, an increase occurred in the amplitude of change of deep ocean foraminiferal oxygen isotopic ratios, traditionally interpreted as defining the main rhythm of ice ages although containing large effects of changes in deep-ocean temperature. We have separated the effects of decreasing temperature and increasing global ice volume on oxygen isotope ratios. Our results suggest that the MPT was initiated by an abrupt increase in Antarctic ice volume at 900 ka. We see no evidence of a pattern of gradual cooling but near-freezing temperatures occur at every glacial maximum.