943 resultados para Thales, ca. 634-ca. 546 B.C.


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Zusammenfassung Das 2,7-Polyfluoren (2,7-PF) wurde in neuer Zeit sowohl wegen seiner einfachen Synthese und hohen Fluoreszenzquantenausbeuten als auch seiner chemischen und thermischen Stabilität intensiv untersucht. Leider liegt das Emissionsmaximum von 2,7-PF in einem Bereich, bei dem das menschliche Auge nicht genügend Sensitivität aufweist. Das Leiter-Poly(p-phenylen) (LPPP) besitzt die optimale Wellenlänge. Jedoch zeigt das LPPP wegen seines steifen Rückgrates große Aggregationstendenz im Film auf, wodurch die Emissionsfarbe bathochrom verschoben und die Photolumineszenzquantenausbeute verringert wird. Es ist deshalb wünschenswert, Polymere zu synthetisieren, die eine längerwellige Emissionsbande als 2,7-PF und eine geringere Aggregationstendenz als LPPP 20 besitzen. Eine Reihe neuer blau emittierender Polymere auf der Basis von Indenofluoren- und Fluoren-Bausteinen mit geringer Aggregationstendenz, hoher thermischer und chemischer Stabilität sowie guter Verarbeitbarkeit wurden dargestellt. Die Polymere weisen eine hohe thermische Stabilität auf (Zersetzung ca.: 310 °C) und sind sehr gut löslich in organischen Lösungsmitteln. Das Absorptionsmaximum des 2,8-Polyindenofluoren (2,8-PIF) in Chloroform liegt bei 416 nm, das Emissionsmaximun bei 432 nm. Die Phasenumwandlungstemperatur beim PIF liegt ca. bei 260 °C. Leider zeigen 2,8-PIF Aggregationstendenzen im Film. Um die Aggregation komplett zu unterbinden, wurden Polyphenylene als Seitenketten an das Dibromfluoren angebracht. Anschließend wurde nach Yamamoto polymerisiert. Das dendritnische PF (DPF) weist die gleiche thermische Stabilität wie die PIFs 28 auf (Zersetzung: 340 °C). Das Polymer 62a ist sehr gut löslich in Toluol, Xylol und chlorierten organischen Lösungsmitteln. Die Absorptions- und Emissionsmaxima des DPFs in Lösung (Chloroform) weisen keine Veränderung gegenüber PF auf. Die Emissionsmaxima des DPFs im Film und nach dem Tempern (100 °C, 24 h) zeigen lediglich eine Verschiebung um 8 nm. Eine Aggregatenbande entsteht jedoch nicht. Dies unterstreicht die abschirmende Eigenschaft der dendritischen Substituenten. Durch Copolymerisation lassen sich die Eigenschaften von Polymeren variieren. Um die Aggregationstendenz der PIF-Derivate zu verringern, wurden die entsprechenden Monomere in verschiedenen Verhältnissen copolymerisiert. Durch die Copolymerisation wurde die PL-Quantenausbeute auf 50 % erhöht. Weiterhin wurden Copolymere von Indenofluoren und 9,10-Dibromanthracen, und erschiedenen Perylenen hergestellt, um zu blau, rot und grün emittierenden Polymeren zu gelangen. Alle blau emittierenden Polymeren wurden in Leuchtdioden untersucht. Das DPF und das Copolymer aus Indenofluoren und Anthracene wiesen die besten Eigenschaften hierfür auf.

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Bis heute ist die Frage nicht geklärt, warum bei der Entstehung des Universums Materie gegenüber der Antimaterie bevorzugt war und das heutige Materieuniversum entstanden ist. Eine Voraussetzung für die Entstehung dieser Materie-Antimaterie-Asymmetrie ist die Verletzung der Kombination von Ladungs- (C) und Punktsymmetrie (P), die CP-Verletzung. CP-Verletzung kann sich unter anderem in den Zerfällen K+- -> pi+- pi0 pi0 zeigen. Die NA48/2"=Kollaboration zeichnete während den Jahren 2003 und 2004 über 200~TB Daten von Zerfällen geladener Kaonen auf. In dieser Arbeit wurde die CP"=verletzende Asymmetrie der Zerfälle K+- -> pi+- pi0 pi0 mit über 90~Millionen ausgewählten Ereignissen aus diesem Datensatz gemessen. Vorhersagen im Standardmodell der Teilchenphysik sagen hier eine CP"=verletzende Asymmetrie in der Größenordnung zwischen $10^{-6}$ und $10^{-5}$ voraus. In Modellen außerhalb des Standardmodells kann es aber auch größere Asymmetrien geben. Das NA48/2"=Experiment war darauf ausgelegt, mögliche systematische Unsicherheiten zu begrenzen. Um dies zu erreichen, wurden positive und negative Kaonen simultan an einem Target erzeugt und ihr Impuls durch ein Strahlsystem mit zwei Strahlengängen auf ca. $60~GeV/c$ begrenzt. Die Strahlen wurden auf wenige Millimeter genau überlagert in die Zerfallsregion geleitet. Die Strahlengänge von positiven und negativen Kaonen sowie die Polarität des Magneten des Impulsspektrometers wurden regelmäßig gewechselt. Dies erlaubte eine Symmetrisierung von Strahlführung und Detektor für positive und negative Kaonen während der Analyse. Durch ein Vierfachverhältnis der vier Datensätze mit den unterschiedlichen Konfigurationen konnte sichergestellt werden, dass alle durch Strahlführung oder Detektor erzeugten Asymmetrien sich in erster Ordnung aufheben. Um die unterschiedlichen Produktionsspektren von positiven und negativen Kaonen auszugleichen wurde in dieser Arbeit eine Ereignisgewichtung durchgeführt. Die Analyse wurde auf mögliche systematische Unsicherheiten untersucht. Dabei zeigte sich, dass die systematischen Unsicherheiten in der Analyse deutlich kleiner als der statistischer Fehler sind. Das Ergebnis der Messung des die CP-verletzende Asymmetrie beschreibenden Parameters $A_g$ ist: begin{equation} A_g= (1,2 pm 1,7_{mathrm{(stat)}} pm 0,7_{mathrm{(sys)}}) cdot 10^{-4}. end{equation} Diese Messung ist fast zehnmal genauer als bisherige Messungen und stimmt innerhalb ihrer Unsicherheit mit dem Standardmodell überein. Modelle, die eine größere CP-Verletzung in diesem Zerfall vorhersagen, können ausgeschlossen werden.

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This work comprises three different types of unconventional correlated systems.rnChapters 3-5 of this work are about the open shell compounds Rb4O6 and Cs4O6. These mixed valent compounds contain oxygen in two different modifications: the closed-shell peroxide anion is nonmagnetic, whereas the hyperoxide anion contains an unpaired electrons in an antibonding pi*-orbital. Due to this electron magnetic ordering is rendered possible. In contrast to theoretical predictions, which suggested half-metallic ferromagnetism for Rb4O6,rndominating antiferromagnetic interactions were found in the experiment. Besidesrna symmetry reduction due to the mixed valency, strong electronic correlations of this highly molecular system determine its properties; it is a magnetically frustrated insulator. The corresponding Cs4O6 was found to show similar properties.rnChapters 6-9 of this work are about intermetallic Heusler superconductors. rnAll of these superconductors were rationally designed using the van Hove scenario as a working recipe. A saddle point in the energy dispersion curve of a solid leads to a van Hove singularity in the density of states. In the Ni-based and Pd-based Heusler superconductors presented in this work this sort of a valence instability occurs at the high-symmetry L point and coincides or nearly coincides with the Fermi level. The compounds escape the high density of states at the Fermi energy through a transition into the correlated superconducting state.rnChapter 10 of this work is about the tetragonally distorted ferrimagnetic DO22 phase of Mn3Ga. This hard-magnetic modification is technologically useful for spin torque transfer applications. The phase exhibits two different crystallographic sites that are occupied by Mn atoms and can thus be written as Mn2MnGa. The competition between the mainly itinerant moments of the Mn atoms at the Wyckoff position 4d and the localized moments of the Mn atoms at the Wyckoff position 2b leads to magnetic correlations. The antiferromagnetic orientation of these moments determines the compound to exhibit a resulting magnetic moment of approximately 1 µB per formula unit in a partially compensated ferrimagnetic configuration.

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Diamant ist das härteste Mineral – und dazu ein Edelstein -, das unter höchstem Druck und hohen Temperaturen in tiefen kontinentalen Regionen der Erde kristallisiert. Die Mineraleinschlüsse in Diamanten werden durch die physikalische Stabilität und chemische Beständigkeit der umgebenden – eigentlich metastabilen -Diamant-Phase geschützt. Aufgrund der koexistierenden Phasenkombination ermöglichen sie, die Mineral-Entwicklung zu studieren, während deren der Einschlüssen und die Diamanten kristallisierten. rnDie Phasenkombinationen von Diamant und Chrom-Pyrop, Chrom-Diopsid, Chromit, Olivin, Graphit und Enstatit nebeneinander (teilweise in Berührungsexistenz) mit Chrom-Pyrop Einschlüssen wurden von neunundzwanzig Diamant-Proben von sechs Standorten in Südafrika (Premier, Koffiefontein, De Beers Pool, Finsch, Venetia und Koingnaas Minen) und Udachnaya (Sibirien/Russland) identifiziert und charakterisiert. Die Mineraleinschlüsse weisen z.T. kubo-oktaedrische Form auf, die unabhängig von ihren eigenen Kristallsystemen ausgebildet werden können. Das bedeutet, dass sie syngenetische Einschlüsse sind, die durch die sehr hohe Formenergie des umgebenden Diamanten morphologisch unter Zwang stehen. Aus zweidiemnsionalen Messungen der ersten Ordnung von charakteristischen Raman-Banden lassen sich relative Restdrucke in Diamanten zwischen Diamant und Einschlussmineral gewinnen; sie haben charakteristische Werte von ca. 0,4 bis 0,9 GPa um Chrom-Pyrop-Einschlüsse, 0,6 bis 2,0 GPa um Chrom-Diopsid-Einschlüsse, 0,3 bis 1,2 GPa um Olivin-Einschlüsse, 0,2 bis 1,0 GPa um Chromit-Einschlüsse, beziehungsweise 0,5 GPa um Graphit Einschlüsse.rnDie kristallstrukturellen Beziehung von Diamanten und ihren monomineralischen Einschlüssen wurden mit Hilfe der Quantifizierung der Winkelkorrelationen zwischen der [111] Richtung von Diamanten und spezifisch ausgewählten Richtungen ihrer mineralischen Einschlüsse untersucht. Die Winkelkorrelationen zwischen Diamant [111] und Chrom-Pyrop [111] oder Chromit [111] zeigen die kleinsten Verzerrungen von 2,2 bis zu 3,4. Die Chrom-Diopsid- und Olivin-Einschlüsse zeigen die Missorientierungswerte mit Diamant [111] bis zu 10,2 und 12,9 von Chrom-Diopsid [010] beziehungsweise Olivin [100].rnDie chemische Zusammensetzung von neun herausgearbeiteten (orientiertes Anschleifen) Einschlüssen (drei Chrom-Pyrop-Einschlüsse von Koffiefontein-, Finsch- und Venetia-Mine (zwei von drei koexistieren nebeneinander mit Enstatit), ein Chromit von Udachnaya (Sibirien/Russland), drei Chrom-Diopside von Koffiefontein, Koingnaas und Udachnaya (Sibirien/Russland) und zwei Olivin Einschlüsse von De Beers Pool und Koingnaas) wurden mit Hilfe EPMA und LA-ICP-MS analysiert. Auf der Grundlage der chemischen Zusammensetzung können die Mineraleinschlüsse in Diamanten in dieser Arbeit der peridotitischen Suite zugeordnet werden.rnDie Geothermobarometrie-Untersuchungen waren aufgrund der berührenden Koexistenz von Chrom-Pyrop- und Enstatit in einzelnen Diamanten möglich. Durchschnittliche Temperaturen und Drücke der Bildung sind mit ca. 1087 (± 15) C, 5,2 (± 0,1) GPa für Diamant DHK6.2 von der Koffiefontein Mine beziehungsweise ca. 1041 (± 5) C, 5,0 (± 0,1) GPa für Diamant DHF10.2 von der Finsch Mine zu interpretieren.rn

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La Tesi Materiale epigrafico per la ricostruzione dei contatti nel Mediterraneo tra il 1200 a.C. e il 500 a.C. si propone di illustrare i complessi rapporti instauratisi tra i vari popoli che si affacciarono sulle rive del Mediterraneo e nelle sue vicinanze, tra il 1200 e il 500 a.C. circa, quali emergono dalle iscrizioni disponibili, principalmente greche e semitiche (soprattutto fenicie, ebraiche, aramaiche e assire), prendendo tuttavia in esame anche iscrizioni ittite, egiziane, frigie, etrusche e celtiche. Le date suddette riguardano due eventi cruciali, che sconvolsero il Mediterraneo: gli attacchi dei Popoli del Mare, che distrussero l'Impero Ittita e indebolirono l'Egitto, e le guerre Persiane. Le iscrizioni riportate sono 1546, quasi sempre traslitterate, tradotte, e accompagnate da un'immagine, da riferimenti bibliografici essenziali e da una breve motivazione del collegamento proposto. Il quadro che si delinea ben testimonia la complessità dei rapporti che si intrecciarono in quel periodo: si pensi alle centinaia di graffiti greci trovati a Naucrati, in Egitto, o alle decine di iscrizioni greche trovate a Gravisca. Anche le iscrizioni aramaiche e assire attestano gli stretti rapporti che si formarono tra Siria e Mesopotamia; ugualmente Iran e Arabia sono, direttamente o indirettamente, collegati a Etruria e Grecia; così troviamo un'iscrizione greca nel cuore dell'Impero Persiano, e un cratere laconico nel centro della Gallia. In realtà lo scopo di questo lavoro è anche quello di mettere in contatto due mondi sostanzialmente separati, ossia quello dei Semitisti e quello dei Grecisti, che solo apparentemente si conoscono e collaborano. Inoltre vorrei soavemente insinuare l'idea che la tesi di Joseph Naveh, che ipotizzò che gli alfabeti greci abbiano tratto origine in prima istanza dalle iscrizioni protocananaiche, nel XII sec. a.C., è valida, e che solo in un secondo tempo i Fenici abbiano dato il loro apporto.

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Chironomids preserved in a sediment core from Lago di Origlio (416 m a.s.l.), a lake in the foreland of the Southern Swiss Alps, allowed quantitative reconstruction of Late Glacial and Early Holocene summer temperatures using a combined Swiss–Norwegian temperature inference model based on chironomid assemblages from 274 lakes. We reconstruct July air temperatures of ca. 10 °C between 17 300 and 16 000 cal yr BP, a rather abrupt warming to ca. 12.0 °C at ca. 16 500–16 000 cal yr BP, and a strong temperature increase at the transition to the Bølling/Allerød interstadial with average temperatures of about 14 °C. During the Younger Dryas and earliest Holocene similar temperatures are reconstructed as for the interstadial. The rather abrupt warming at 16 500–16 000 cal yr BP is consistent with sea-surface temperature as well as speleothem records, which indicate a warming after the end of Heinrich event 1 (sensu stricto) and before the Bølling/Allerød interstadial in southern Europe and the Mediterranean Sea. Pollen records from Origlio and other sites in southern Switzerland and northern Italy indicate an early reforestation of the lowlands 2000–1500 yr prior to the large-scale afforestation of Central Europe at the onset of the Bølling/Allerød period at ca. 14 700–14 600 cal yr BP. Our results suggest that these early afforestation processes in the formerly glaciated areas of northern Italy and southern Switzerland have been promoted by increasing temperatures.

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OBJECTIVE We investigated the skeletal growth profile of female rats from birth to senescence (100weeks) on the basis of sequential radiometrical, hormonal and biochemical parameters. DESIGN Weaning rats entered the study which was divided into two sections: a) sequential measurements of vertebral and tibial growths and bone mineral density (BMD), estimation of mineral content of the entire skeleton (BMC) and chemical analysis of vertebral Ca; and b) determination of basal and pulsatile growth hormone (rGH), insulin-like growth hormone (IGF-I), estradiol (E2), parathyroid hormone (PTH), osteocalcin (OC) and urinary d-pyridinoline (dp) throughout the experimental period. RESULTS Vertebral and tibial growths ceased at week 25 whereas BMD and BMC as well as total vertebral Ca exhibited a peak bone mass at week 40. rGH pulsatile profiles were significantly higher in younger animals coinciding with the period of active growth and IGF-I peaked at 7weeks, slowly declining thereafter and stabilizing after week 60. OC and dp closely paralleled IGF-I coinciding with the period of enhanced skeletal growth, remaining thereafter in the low range indicative of reduced bone turnover. E2 increased during reproductive life but the lower values subsequently recorded were still in the physiological range, strongly suggesting a protective role of this steroid on bone remodeling. PTH followed a similar profile to E2, but the significance of this after completion of growth remains unclear. CONCLUSIONS Mechanisms governing skeletal growth in the female rat appear similar to those in humans. Bone progression and attainment of peak bone mass are under simultaneous control of rGH, IGF-I and calciotropic hormones and are modulated by E2. This steroid seems to protect the skeleton from resorption before senescence whereas the role of PTH in this context remains uncertain.

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The palynostratigraphy of two sediment cores from Soppensee, Central Switzerland (596 m asl) was correlated with nine regional pollen assemblage zones defined for the Swiss Plateau. This biostratigraphy shows that the sedimentary record of Soppensee includes the last 15 000 years, i.e. the entire Late-glacial and Holocene environmental history. The vegetation history of the Soppensee catchment was inferred by pollen and plant-macrofossil analyses on three different cores taken in the deepest part of the lake basin (27 m). On the basis of a high-resolution varve and calibrated radiocarbonchronology it was possible to estimate pollen accumulation rates, which together with the pollen percentage data, formed the basis for the interpretation of the past vegetation dynamics. The basal sediment dates back to the last glacial. After reforestation with juniper and birch at ca. 12 700 B.P., the vegetation changed at around 12 000 B.P. to a pine-birch woodland and at the onset of the Holocene to a mixed deciduous forest. At ca. 7000 B.P., fir expanded and dominated the vegetation with beech becoming predominant at ca. 50014C-years later until sometime during the Iron Age. Large-scale deforestation, especially during the Middle Ages, altered the vegetation cover drastically. During the Late-glacial period two distinct regressive phases in vegetation development are demonstrated, namely, the Aegelsee oscillation (equivalent to the Older Dryas biozone) and the Younger Dryas biozone. No unambiguous evidence for Holocene climatic change was detected at Soppensee. Human presence is indicated by early cereal pollen and distinct pulses of forest clearance as a result of human activity can be observed from the Neolithic period onwards.

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Creatine Kinase (CK) is used as a measure of exercise-induced muscle membrane damage. During acute eccentric (muscle lengthening) exercise, muscle sarcolemma, sarcoplasmic reticulum, and Z-lines are damaged, thus causing muscle proteins and enzymes to leak into the interstitial fluid. Strenuous eccentric exercise produces an elevation of oxygen free radicals, which further increases muscle damage. Muscle soreness and fatigue can be attributed to this membrane damage. Estradiol, however, may preserve membrane stability post-exercise (Brancaccio, Maffulli, & Limongelli, 2007; Carter, Dobridge, & Hackney, 2001; Tiidus, 2001). Because estradiol has a similar structure to Vitamin E, which is known to have antioxidant properties, and both are known to affect membrane structure, researchers have proposed that estrogen acts as an antioxidant to provide a protective effect on the post-exercise muscle of women (Sandoval & Matt, 2002). As a result, it has been postulated that muscles in women incur less damage in response to an acute strenuous exercise as compared to men. PURPOSE: To determine if circulating estrogen concentrations are related to muscle damage, as measured by creatine kinase activity and to determine gender differences in creatine kinase as a marker of muscle damage in response to an acute heavy resistance exercise protocol. METHODS: 7 healthy, resistance-trained, eumenhorrheic women (23±3 y, 169±9.1 cm, 66.4±10.5 kg) and 8 healthy, resistance-trained men (25±5 y, 178±6.7 cm, 82.3±9.33 kg) volunteered to participate in the study. Subjects performed an Acute Resistance Exercise Test (ARET) consisting of 6 sets of 5 repetitions Smith machine squats at 90% of their previously determined 1-RM. Blood samples were taken pre-, mid-, post-, 1 hour post-, 6 hours post-, and 24 hours post-exercise. Samples were stored at -80ºC until analyzed. Serum creatine kinase was measured using an assay kit from Genzyme (Framingham, MA). Serum estradiol was measured by an ELISA from GenWay (San Diego, CA). Estradiol b-receptor presence on granulocytes was measured via flow cytometry using primary antibodies from Abcam (Cambridge, MA) and PeCy7 antibodies (secondary) from Santa Cruz (Santa Cruz, CA). RESULTS: No significant correlations between estrogen and CK response were found after an acute resistant exercise protocol. Moreover, no significant change in estradiol receptors were expressed on granulocytes after exercise. Creatine Kinase response, however, differed significantly between genders. Men had higher resting CK concentrations throughout all time points. Creatine Kinase response increased significantly after exercise in both men and women (p=0.008, F=9.798). Men had a significantly higher CK response at 24 hours post exercise than women. A significant condition/sex/time interaction was exhibited in CK response (p=0.02, F=4.547). Perceived general soreness presented a significant condition, sex interaction (p=0.01, F=9.532). DISCUSSION: Although no estradiol and CK response correlations were found in response to exercise, a significant difference in creatine kinase activity was present between men and women. This discrepancy of our results and findings in the literature may be due to the high variability between subjects in creatine kinase activity as well as estrogen concentrations. The lack of significance in change of estradiol receptor expression on granulocytes in response to exercise may be due to intracellular estradiol receptor staining and non-specific gating for granulocytes rather than additional staining for neutrophil markers. Because neutrophils are the initial cells present in the inflammatory response after strenuous exercise, staining for estrogen receptors on this cell type may allow for a better understanding of the effect of estrogen and its hypothesized protective effect against muscle damage. Furthermore, the mechanism of action may include estradiol receptor expression on the muscle fiber itself may play a role in the protective effects of estradiol rather than or in addition to expression on neutrophils. We have shown here that gender differences occur in CK activity as a marker of muscle damage in response to strenuous eccentric exercise, but may not be the result of estradiol concentration or estradiol receptor expression on granulocytes. Other variables should be examined in order to determine the mechanism involved in the difference in creatine kinase as a marker of muscle damage between men and women after heavy resistance exercise.

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Viral hepatitis is a significant public health problem worldwide and is due to viral infections that are classified as Hepatitis A, B, C, D, and E. Hepatitis B is one of the five known hepatic viruses. A safe and effective vaccine for Hepatitis B was first developed in 1981, and became adopted into national immunization programs targeting infants since 1990 and adolescents since 1995. In the U.S., this vaccination schedule has led to an 82% reduction in incidence from 8.5 cases per 100,000 in 1990 to 1.5 cases per 100,000 in 2007. Although there has been a decline in infection among adolescents, there is still a large burden of hepatitis B infection among adults and minorities. There is very little research in regards to vaccination gaps among adults. Using the National Health and Nutrition Examination Survey (NHANES) question "{Have you/Has SP (Study Participant)} ever received the 3-dose series of the hepatitis B vaccine?" the existence of racial/ethnic gaps using a cross-sectional study design was explored. In this study, other variables such as age, gender, socioeconomic variables (federal poverty line, educational attainment), and behavioral factors (sexual practices, self-report of men having sex with men, and intravenous drug use) were examined. We found that the current vaccination programs and policies for Hepatitis B had eliminated racial and ethnic disparities in Hepatitis B vaccination, but that a low coverage exists particularly for adults who engage in high risk behaviors. This study found a statistically significant 10% gap in Hepatitis B vaccination between those who have and those who do not have access to health insurance.^

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We compare six high-resolution Holocene, sediment cores along a S-N transect on the Norwegian-Svalbard continental margin from ca 60°N to 77.4°N, northern North Atlantic. Planktonic foraminifera in the cores were investigated to show the changes in upper surface and subsurface water mass distribution and properties, including summer sea-surface temperatures (SST). The cores are located below the axis of the Norwegian Current and the West Spitsbergen Current, which today transport warm Atlantic Water to the Arctic. Sediment accumulation rates are generally high at all the core sites, allowing for a temporal resolution of 10-102 years. SST is reconstructed using different types of transfer functions, resulting in very similar SST trends, with deviations of no more than +- 1.0/1.5 °C. A transfer function based on the maximum likelihood statistical approach is found to be most relevant. The reconstruction documents an abrupt change in planktonic foraminiferal faunal composition and an associated warming at the Younger Dryas-Preboreal transition. The earliest part of the Holocene was characterized by large temperature variability, including the Preboreal Oscillations and the 8.2 k event. In general, the early Holocene was characterized by SSTs similar to those of today in the south and warmer than today in the north, and a smaller S-N temperature gradient (0.23 °C/°N) compared to the present temperature gradient (0.46 °C/°N). The southern proxy records (60-69°N) were more strongly influenced by slightly cooler subsurface water probably due to the seasonality of the orbital forcing and increased stratification due to freshening. The northern records (72-77.4°N) display a millennial-scale change associated with reduced insolation and a gradual weakening of the North Atlantic thermohaline circulation (THC). The observed northwards amplification of the early Holocene warming is comparable to the pattern of recent global warming and future climate modelling, which predicts greater warming at higher latitudes. The overall trend during mid and late Holocene was a cooling in the north, stable or weak warming in the south, and a maximum S-N SST gradient of ca 0.7 °C/°N at 5000 cal. years BP. Superimposed on this trend were several abrupt temperature shifts. Four of these shifts, dated to 9000-8000, 5500-3000 and 1000 and ~400 cal. years BP, appear to be global, as they correlate with periods of global climate change. In general, there is a good correlation between the northern North Atlantic temperature records and climate records from Norway and Svalbard.

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La tuna es una fruta presente principalmente en zonas áridas y semiáridas. Su aporte nutricional podría aprovecharse consumiéndola en forma directa, como así también a través de productos elaborados en forma artesanal. Dichos productos podrían incorporarse a la economía del mercado de consumo interno y eventualmente externo. Por tal motivo, se evalúa la posibilidad de desarrollar mermeladas con tres ecotipos de tuna de la misma variedad, considerando la aceptación del producto. Se trabajó con tunas (Opuntia ficus indica f. inerme), cultivadas en el Centro Regional de Investigaciones Científicas y Tecnológicas (CRICYT) ubicado en el Parque General San Martín, Capital, Mendoza. El objetivo general del trabajo estuvo dirigido a la elaboración de mermeladas de tres ecotipos de tuna: tuna roja o morada, tuna anaranjada o amarilla y tuna verde o blanca acorde a la legislación vigente. Los ítems específicos estuvieron conducidos hacia el desarrollo de una mermelada utilizando una fruta no convencional, para determinar el valor nutricional del mismo, y sus características fisicoquímicas, ampliar la producción de subproductos de tuna en la región árida y semiárida, para así finalmente evaluar el grado de aceptabilidad sensorial y comercial del producto. Se caracterizaron los tres ecotipos de tuna y sus respectivas mermeladas mediante determinaciones fisicoquímicas, se verificó el contenido nutricional y se realizaron los análisis microbiológicos de cada una de ellas. Dentro de las determinaciones fisicoquímicas de las mermeladas se incluyó K, P, Ca y vitamina C, teniendo en cuenta que se parte de una materia prima con buenas cantidades de estos minerales y vitamina C con respecto a otras frutas. Se llevaron a cabo pruebas de evaluación sensorial del producto terminado y se consultó el precio que estarían dispuestos a pagar los potenciales consumidores. Los jueces entrenados contribuyeron al diseño de un perfil sensorial para cada una de las mermeladas y evaluaron en forma global al producto obtenido. Los resultados obtenidos en cuanto a la caracterización de la materia prima arrojan un buen contenido en sólidos solubles, vitamina C y en minerales como el fósforo, calcio, potasio y un contenido bajo en sodio con respecto a otras frutas que se consumen habitualmente. Los análisis microbiológicos realizados para evaluar la conservación permiten expresar que se trata de un producto de bajo riesgo microbiológico, bajo las condiciones de conservación que se obtuvieron. En base a lo expuesto, se puede concluir que es técnicamente posible elaborar artesanalmente mermeladas de tres ecotipos de tuna, las cuales poseen un buen aporte nutricional, son aptas para el consumo humano desde el punto de vista bromatológico y aceptadas sensorialmente por los consumidores.

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Este trabajo se propone analizar críticamente algunas teorías recientes sobre las consecuencias sociales de la Segunda Guerra Púnica (218-201 a. C.) en la antigua sociedadáromana. Mientras que laáinterpretación clásica había subrayado el efecto dañino que las guerras de expansión supusieronápara el campesinado romano, los nuevos enfoques en boga se caracterizan por dejar de lado las contradicciones del proceso histórico, adoptando una interpretación malthusiana en la cual laápoblación simplementeáhabría crecido mucho más que los recursos para sostenerla. Considerando que la demografía no es una variable independiente sino que se encuentra enmarcada en un modo de producción específico, se propone estudiar algunasálimitaciones de los enfoques mencionados paraáluego abordar el problema desde una óptica que enfatice en la dinámica contradictoria de la sociedad romana