Addizioni organocatalitiche asimmetriche di 1,3-dicarbonili a orto-chinoni metidi. Un nuovo metodo per la sintesi di 3,4-diidrocumarine e 4h-cromeni otticamente attivi

Questa tesi descrive lo sviluppo di una nuova metodologia che prevede l’utilizzo degli orto-chinoni metidi (o-QMs) in reazioni organocatalitiche asimmetriche. A causa della loro elevata instabilità e reattività, gli o-QMs sono stati impiegati in trasformazioni di sintesi asimmetrica solo di recente. Il metodo sviluppato prevede l’utilizzo di catalizzatori bifunzionali in grado di promuovere la generazione in situ degli intermedi reattivi a partire dai rispettivi 2-solfonilalchil fenoli, tramite eliminazione di acido solfinico. L’utilizzo di condizioni blandamente basiche sia per generare gli o-QMs che per l’attivazione dei partner nucleofili, risulta innovativo e permette non solo di ovviare all’intrinseca instabilità di questi intermedi, ma anche di impiegarli efficacemente in reazioni organocatalitiche con una varietà di nucleofili, come, ad esempio, l’acido di Meldrum, il malononitrile e vari composti 1,3 dicarbonilici. Le reazioni catalitiche portano alla formazione di 3,4-diidrocumarine, 4H-cromeni e xantenoni enantioarricchiti. Alcuni di questi composti sono dei precursori sintetici di composti naturali o sintetici biologicamente attivi e per avvalorare questa metodologia sono state proposte le sintesi formali di tre composti di interesse biologico: la (R)-tolterodina (il principio attivo del farmaco antimuscarinico Detrol®), (S)-4-metossidalbergione (allergene della Dalbergia Nigra) and SB-209670 / SB-217242 (due potenti antagonisti dell’endotelina).

Synoptic drivers of 400 years of summer temperature and precipitation variability on Mt. Olympus, Greece

The Mediterranean region has been identified as a global warming hotspot, where future climate impacts are expected to have significant consequences on societal and ecosystem well-being. To put ongoing trends of summer climate into the context of past natural variability, we reconstructed climate from maximum latewood density (MXD) measurements of Pinus heldreichii (1521–2010) and latewood width (LWW) of Pinus nigra (1617–2010) on Mt. Olympus, Greece. Previous research in the northeastern Mediterranean has primarily focused on inter-annual variability, omitting any low-frequency trends. The present study utilizes methods capable of retaining climatically driven long-term behavior of tree growth. The LWW chronology corresponds closely to early summer moisture variability (May–July, r = 0.65, p < 0.001, 1950–2010), whereas the MXD-chronology relates mainly to late summer warmth (July–September, r = 0.64, p < 0.001; 1899–2010). The chronologies show opposing patterns of decadal variability over the twentieth century (r = −0.68, p < 0.001) and confirm the importance of the summer North Atlantic Oscillation (sNAO) for summer climate in the northeastern Mediterranean, with positive sNAO phases inducing cold anomalies and enhanced cloudiness and precipitation. The combined reconstructions document the late twentieth—early twenty-first century warming and drying trend, but indicate generally drier early summer and cooler late summer conditions in the period ~1700–1900 CE. Our findings suggest a potential decoupling between twentieth century atmospheric circulation patterns and pre-industrial climate variability. Furthermore, the range of natural climate variability stretches beyond summer moisture availabilityobserved in recent decades and thus lends credibility to the significant drying trends projected for this region in current Earth System Model simulations.

Long-term forest fire ecology and dynamics in southern Switzerland

1 Pollen and charcoal analysis at two lakes in southern Switzerland revealed that fire has had a prominent role in changing the woodland composition of this area for more than 7000 years. 2 The sediment of Lago di Origlio for the period between 5100 and 3100 bc cal. was sampled continuously with a time interval of about 10 years. Peaks of charcoal particles were significantly correlated with repeated declines in pollen of Abies, Hedera, Tilia, Ulmus, Fraxinus excelsior t., Fagus and Vitis and with increases in Alnus glutinosa t., shrubs (e.g. Corylus, Salix and Sambucus nigra t.) and several herbaceous species. The final disappearance of the lowland Abies alba stands at around 3150 bc cal. may be an example of a fire-caused local extinction of a fire-intolerant species. 3 Forest fires tended to diminish pollen diversity. The charcoal peaks were preceded by pollen types indicating human activity. Charcoal minima occurred during periods of cold humid climate, when fire susceptibility would be reduced. 4 An increase of forest fires at about 2100 bc cal. severely reduced the remaining fire-sensitive plants: the mixed-oak forest was replaced by a fire-tolerant alder–oak forest. The very strong increase of charcoal influx, and the marked presence of anthropogenic indicators, point to principally anthropogenic causes. 5 We suggest that without anthropogenic disturbances Abies alba would still form lowland forests together with various deciduous broadleaved tree taxa.

Why does low dose morphine augment fentanyl analgesia?

Opioids dominate the field of pain management because of their ability to provide analgesia in many medical circumstances. However, side effects including respiratory depression, constipation, tolerance, physical dependence, and the risk of addiction limit their clinical utility. Fear of these side effects results in the under-treatment of acute pain. For many years, research has focused on ways to improve the therapeutic index (the ratio of desirable analgesic effects to undesirable side effects) of opioids. One strategy, combining opioid agonists that bind to different opioid receptor types, may prove successful.^ We discovered that subcutaneous co-administration of a moderately analgesic dose of the mu-opioid receptor (MOR) selective agonist fentanyl (20μg/kg) with subanalgesic doses of the less MOR-specific agonist morphine (100ng/kg-100μg/kg), augmented acute fentanyl analgesia in rats. Parallel [35S]GTPγS binding studies using naïve rat substantia gelatinosa membrane treated with fentanyl (4μM) and morphine (1nM-1pM) demonstrated a 2-fold increase in total G-protein activation. This correlation between morphine-induced augmentation of fentanyl analgesia and G-protein activation led to our proposal that interactions between MORs and DORs underlie opioid-induced augmentation. We discovered that morphine-induced augmentation of fentanyl analgesia and G-protein activity was mediated by DORs. Adding the DOR-selective antagonist naltrindole (200ng/kg, 40nM) at doses that did not alter the analgesic or G-protein activation of fentanyl, blocked increases in analgesia and G-protein activation induced by fentanyl/morphine combinations. Equivalent doses of the MOR-selective antagonist cyprodime (20ng/kg, 4nM) did not block augmentation. Substitution of the DOR-selective agonist SNC80 for morphine yielded similar results, further supporting our conclusion that interactions between MORs and DORs are responsible for morphine-induced augmentation of fentanyl analgesia and G-protein activation. Confocal microscopy of rat substantia gelatinosa showed that changes in the rate of opioid receptor internalization did not account for these effects.^ In conclusion, fentanyl analgesia augmentation by subanalgesic morphine is mediated by increased G-protein activation resulting from functional interactions between MORs and DORs, not changes in MOR internalization. Additional animal and clinical studies are needed to determine whether side effect incidence changes following opioid co-administration. If side effect incidence decreases or remains unchanged, these findings could have important implications for clinical pain treatment. ^

Pollen and macroremains from sediment core Aschenhütte

The Upper Pleistocene sediments of the Aschenhütte sink-hole (west of Herzberg am Harz, Lower Saxony) enable one to make interesting correlations between palynological and geological results. The sequence is composed of limnic-telmatic deposits (Eemain to Lower Weichselian) and loess with paleosoils (Weichselian). Sedimentation started during the hornbeam-dominated phase of the Eemian interglacial period and continued throughout the Eemian, the Weichselian Brörup interstadial (sensu Andersen) and parts of the preceding and the following stadial phases, the Herning and the Rederstall stadials. As opposed to most of the known Eemian sites spruce was a major tree species during the hornbeam-dominated phase of the Eemian. The vegetational development during the interstadial phase does not show a period of climatic deterioration as is the case for the Brörup interstadial when considering regions with a more demanding vegetation or regions close to the natural boundaries of the tree species concerned. Pollen or seeds of Bruckenthalia and Picea omoricoides have not been found in the Aschenhütte cores. The limnic-telmatic sediments interlock with loess-paleosoils (Eemian soil and Lower Weichselian bleaching soils) at the lake shore. They are overlaid by loess paleosoils of the Stillfried-B interstadial (Hattorf soil and Lohne soil). Lake level fluctuations were determined by means of the facies distribution and isochrones as defined by pollen analysis. A relatively high stand of the lake level existed after the end of the Eemian interglacial and during the Brörup interstadial periods. In the course of the Herning stadial period the water level dropped, whereas during the Rederstall stadial phase the lake basin was covered by sediments and therefore dried up.

Comportamiento de coníferas bajo riego : Mendoza, Argentina

La provincia de Mendoza, ubicada en el centro-oeste de la Argentina, tiene una extensión de 150 830 km2. Prácticamente todas las actividades agropecuarias y forestales están concentradas en el 3 % de su territorio que es posible irrigar. Al oeste, en el límite con Chile, está la cadena montañosa que forma parte de la región fitogeográfica del Desierto Andino que se extiende por más de 500 km, con un ancho promedio de 100 km. El objetivo del trabajo fue introducir algunas especies de coníferas y evaluar su comportamiento en dicha región fitogeográfica, con la finalidad de lograr un aprovechamiento forestal, proteger el suelo contra la erosión hídrica y/o eólica, modificar el paisaje y desarrollar áreas de explotación turística. Las especies seleccionadas en esta primera etapa fueron: Cedrus deodara, Cupressus arizonica, Cupressus macrocarpa, Juniperus virginiana, Pinus griffithii, Pinus halepensis, Pinus nigra, Pinus pinaster, Pinus pinea y Pinus radiata. Las experiencias se llevaron a cabo en dossitios, separados por más de 150 km, y situados a 1 050 y 2 000 msnm, respectivamente. Se tomaron datos de supervivencia, altura y diámetro de los individuos, y se efectuaron observaciones sobre su hábito de crecimiento y condiciones fitosanitarias. Las principales conclusiones fueron las siguientes: 1. Todas las especies mostraron buen estado fitosanitario sin haberse detectado ninguna plaga o enfermedad de importancia. 2. El hábito de crecimiento fue el correspondiente a cada especie; sólo hubo fustes bifurcados en algunos individuos de Pinus pinea. 3. Las especies que evidenciaron mayor aptitud fueron: Juniperus virginiana, Cupressus arizonica, Pinus pinea, Pinus pinaster y Cupressus macrocarpa.

Evaluación de clones de Populus spp., a los dos años de edad, en dos micrositios de la región pampeana, Argentina

La producción de álamos en la pampa ondulada de la provincia de Buenos Aires podría constituir una actividad alternativa y/o complementaria, debido a zonas ecológicas favorables para su cultivo. En este contexto es importante conocer el comportamiento de los clones en los diversos ambientes para poder definir cuáles de ellos podrían presentar mayor estabilidad para los diferentes sitios. El objetivo del trabajo fue estudiar la interacción existente entre los parámetros de crecimiento y supervivencia de 16 clones de Populus spp. en dos micrositios geomorfológicamente diferentes en la región pampeana, Argentina. Los clones en estudio provienen de cruzamientos intraespecíficos de P. deltoides e interespecíficos de P. deltoides x P. nigra (Populus x canadensis). Se plantaron en dos ensayos, uno por cada situación geomórfica: loma y bajo, y se completó con un análisis estadístico comparando los ensayos en forma individual y conjunta. Cada ensayo se instaló con un diseño de bloques completos al azar. Las variables analizadas fueron la supervivencia, la altura media y el área basal al concluir el segundo año de crecimiento. Para el sitio regional evaluado, la interacción entre los clones y los micrositios fue significativa para las variables altura y supervivencia. La mayor disponibilidad de agua en el micrositio bajo produjo mayores crecimientos clonales con diferencias significativas respecto del micrositio loma. La estabilidad de los atributos de supervivencia y crecimiento frente a los micrositios es un objetivo fundamental en las plantaciones clonales. Siendo los micrositios una realidad ambiental importante, propia como variable no controlable, la reducción de la variabilidad de respuesta ante ellos permitiría la constitución de unidades de manejo más homogéneas.

Susceptibilidad a Septoria musiva de híbridos inter e intraespecíficos de Populus spp. implantados en dos micrositios de la Pampa Húmeda Argentina

En los álamos, una de las enfermedades con mayor influencia en la cantidad y calidad de la madera producida es la cancrosis originada por Septoriamusiva Peck . El objetivo del trabajo fue determinar en clones híbridos de álamos (Populus spp.) la incidencia y la severidad de la enfermedad producida por Septoria, en dos micrositios de un mismo sitio regional, en Alberti, Buenos Aires, Argentina. Los clones utilizados fueron obtenidos de cruzamientos intraespecíficos de Populus deltoides e interespecíficos de P. deltoides x P. nigra (= P. x canadensis). Se determinó la susceptibilidad a la enfermedad para cada clon/micrositio mediante la estimación de la incidencia, del número de cancros en guías y ramas, y la severidad de daños (ID). Los híbridos inter e intraespecíficos de P. deltoides presentaron respuesta clonal diferencial en la susceptibilidad a la cancrosis en ambas situaciones geomórficas: los híbridos provenientes de cruzamientos intraespecíficos resultaron resistentes, y los provenientes de cruzamientos interespecíficos susceptibles a la enfermedad. Las diferencias significativas entre clones, determinadas para el número de lesiones totales por posición en ambas situaciones geomórficas, no determinaron ID diferentes. El número de cancros identificados en cada posición constituye una herramienta de estimación de la susceptibilidad clonal a la cancrosis más exacta, teniendo en cuenta que los mayores perjuicios ocurren cuando las lesiones se presentan en las guías.

Evaluación del crecimiento inicial de clones de álamo en el norte de la Patagonia

En los valles irrigados de Río Negro y Neuquén, el cultivo de álamos acompañó históricamente la producción agrícola, utilizándose clones de Populus nigra L. en cortinas rompeviento y clones de Populus xcanadensis Moench. para las forestaciones en macizo. Buscando ampliar la disponibilidad de genotipos para los diferentes sitios de cultivo, se instaló un ensayo comparativo con trece clones de álamo en la localidad de Pomona, Provincia de Río Negro. Se evaluaron seis clones de P. xcanadensis ('Triplo', 'Ragonese 22 INTA', "Pangui INTA", "Pudú INTA", y los testigos comerciales 'Conti 12' e 'I-214'), seis clones de P. deltoides ('Harvard', 'Onda', 'Stoneville 67', 'Carabelas INTA', "20-82" y "C-657") y un clon de P. xcanescens. Se utilizó un diseño experimental de bloques completos al azar (DBCA) con quince repeticiones y parcelas de una planta. Luego de cuatro períodos de crecimiento, 'I-214' y 'Triplo' tuvieron los mayores incrementos de DAP, no encontrándose diferencias significativas con los valores de 'Conti 12', 'Ragonese 22 INTA', "Pangui INTA", "Pudú INTA", "20-82" y P. xcanescens. Los menores crecimientos fueron observados en los deltoides 'Stoneville 67' y "C- 657". Los clones 'Ragonese 22 INTA', 'Triplo' y "20-82" constituyen alternativas para el cultivo de álamos en macizos y cortinas rompeviento.

Palynology on a profile from the Krusné Hory Mountains

Site details: The raised bog Fláje-Kiefern (50°429N, 13°329 E; 760 m a.s.l.; size ca. 500x500 m) lies in the Krusné Hory Mountains (Erzgebirge), Czech Republic, about 10 km from Georgenfelder Moor in Germany. Hejny and Slavík (1988) described the phytogeographic region of the Krusne Hory Mountains as 'a region of mountain flora and vegetation, with thermophilous species largely missing. In the natural forests, conifers, especially spruce (Picea excelsa) prevail. The deforested areas have been converted into meadows and pastures'. The climate is cool with annual average temperatures of about 5°C and annual precipitation of about 900 mm. The bedrock is Precambrian crystallinicum.

Palynology on sediment profile Tso Kar in Ladakh

Palynological investigation of a 410 cm long core section from Tso Kar (33°10'N, 78°E, 4527 m a.s.l.), an alpine lake situated in the arid Ladakh area of NW India at the limit of the present-day Indian summer monsoon, was performed in order to reconstruct post-glacial regional vegetation and climate dynamics. The area was covered with alpine desert vegetation from ca. 15.2 to 14 kyr BP (1 kyr=1000 cal. years), reflecting dry and cold conditions. High influx values of long-distance transported Pinus sylvestris type pollen suggest prevailing air flow from the west and northwest. The spread of alpine meadow communities and local aquatic vegetation is a weak sign of climate amelioration after ca. 14 kyr BP. Pollen data (e.g. influx values of Pinus roxburghii type and Quercus) suggest that this was due to a strengthening of the summer monsoon and the reduced activity of westerly winds. The further spread of Artemisia and species-rich meadows occurred in response to improved moisture conditions between ca. 12.9 and 12.5 kyr BP. The subsequent change towards drier desert-steppe vegetation likely indicates more frequent westerly disturbances and associated snowfalls, which favoured the persistence of alpine meadows on edaphically moist sites. The spread of Chenopodiaceae-dominated vegetation associated with an extremely weak monsoon occurred at ca. 12.2-11.8 kyr BP during the Younger Dryas interstadial. A major increase in humidity is inferred from the development of Artemisia-dominated steppe and wet alpine meadows with Gentianaceae after the late glacial/early Holocene transition in response to the strengthening of the summer monsoon. Monsoonal influence reached maximum activity in the Tso Kar region between ca. 10.9 and 9.2 kyr BP. The subsequent development of the alpine meadow, steppe and desert-steppe vegetation points to a moderate reduction in the moisture supply, which can be linked to the weaker summer monsoon and the accompanying enhancement of the winter westerly flow from ca. 9.2 to 4.8 kyr BP. The highest water levels of Tso Kar around 8 kyr BP probably reflect combined effect of both monsoonal and westerly influence in the region. An abrupt shift towards aridity in the Tso Kar region occurred after ca. 4.8 kyr BP, as evidenced by an expansion of Chenopodiaceae-dominated desert-steppe. Low pollen influx values registered ca. 2.8-1.3 kyr BP suggest scarce vegetation cover and unfavourable growing conditions likely associated with a further weakening of the Indian Monsoon.

Age determination and pollen profile of sediment core Trentelmoor, Peine, northern Germany

The filling up of the lake which existed in the basin of the Trentelmoor (40 km E of Hannover, Germany) - in Preboreal times was finished 2000 years ago. Since then fen vegetation has covered the former lake's surface. The postglacial development of the vegetation follows the pattern which is typical of Central Europe. However, due to the poorness of the soils around the Trentelmoor, the frequencies of some tree species differ. Beech for example never reached - for the benefit of oak - that importance which this tree species usually gains on better soils. Human impact becomes recognisable in the upper Neolithic for the first time. The area has been settled continuously, but with changing intensities, throughout the last 3000 years. When the manuscript of this paper went to press the results of two radiocarbon age determinations only were completed. An additional three determinations were completed somewhat later. See the accompanying table for results.

AMS radiocarbon dates and pollen analysis from Zugspitzplatt

On the strongly karstified and almost unvegetated surface of the Zugspitzplatt, at an altitude of about 2290 m in the Wettersteingebirge, there is a doline within which over a period of several thousand years a bed of fine loess-like sediment, almost 1m thick, has accumulated. Notwithstanding the situation of this locality far above the present tree-line, this infill contains quantities of pollen and spores sufficient for pollen analysis without use of any enrichment techniques. Despite poor pollen preservation, it was possible to date the basal layers of this profile on the basis of their pollen assemblages. AMS dating (7415 ± 30 BP) has confirmed that the oldest sediments were laid down during the early Atlantic period, the time of the thermal optimum of the Holocene. At least since that time this site has never been overridden by a glacier. The moraine associated with the Löbben Oscillation between 3400 and 3100 BP - here represented by the so-called Platt Stillstand (Plattstand) - did not quite reach the doline. A diagram shows known Holocene glacial limits. The composition of the pollen assemblages from the two oldest levels with high pollen concentrations strongly suggests that the distance between the doline and the forest was much less during the Atlantic than at present.