Synthese von Naturstoffen mit Lacton-Strukturen großer und mittlerer Ringgröße: Ein Curvularin-Analogon und Phomol

1.1 Synthese des dreizehngliedrigen (S)-(-)-Curvularin-AnalogonsrnAus biologischen Studien ist bekannt, dass (S)-(-)-Curvularin die Tyrosin-Phosphorylierung von STAT1-Proteinen inhibiert. Die Struktur des biologischen Targets ist jedoch unbekannt. Aus diesem Grund wurde eine Variation des (S)-(-)-Curvularin-Gerüsts vorgenommen werden, indem das zwölfgliedrige Ringgerüst erweitert wurde. Das dreizehngliedrigen (S)-(-)-Curvularin-Analogons konnte aus Acetondicarbonsäuredimethylester, (S)-Hex-5-en-2-ol, und Adipinsäuremonoallylester in 11 Stufen dargestellt werden.rn1.2 PhomolrnDas zweite Ziel dieser Arbeit war die Totalsynthese von Phomol. Zunächst wurden ausgehend von D Mannitol (3S,4R)-3,4-O-Isopropyliden-dec-1-en-5-ol in sechs Stufen und (3R,4R)-3,4-Dibenzyloxy-5-hexensäure in sieben Stufen synthetisiert und anschließend unter Yamaguchi-Bedingungen verestert. Die erhaltenen Ester wurden der Ringschlussmetathese unterworfen. Hierbei entstand das gewünschte Makrolacton lediglich in Spuren, welches spektroskopisch nachgewiesen werden konnten. Daher wurden im weiteren Verlauf (3S,4S,5S)-3-(p-Methoxybenzyl)-4-(triisopropylsilyloxy)-1-decen-5-ol und (3S,4S,5R)-3-(p-Methoxyben-zyl)-4-(triisopropylsilyloxy)-1-decen-5-ol in 10 Stufen aus (+) Xylose synthetisiert. Diese Alkohole wurden mit (3R,4R)-3,4-Di-p-methoxybenzyloxy-5-hexensäure, welche analog (3R,4R)-3,4-Dibenzyloxy-5-hexensäure dargestellt wurden, unter Yamaguchi-Bedingungen verestert und anschließend Studien zur Ringschlussmetathese unterworfen. Hierbei ließ sich nur ein Diastereomer zur Reaktion bringen wodurch sich (4R,5R,8S,9S,10R,E)-4,5,8-Tri(p-methoxybenzyloxy)-10-pentyl-9-(triisopropylsilyloxy)-3,3,5,8,9,10-hexahydro-2H-oxecin-2-on bildete. Nach Spaltung des Silylethers sollte die Seitenkette an C-8 eingeführt werden, was jedoch unter verschiedenen Bedingungen nicht gelungen ist. rnDas Grundgerüst des Phomols konnte in einer 20-stufigen Synthese ausgehend von D Mannitol und (+) Xylose aufgebaut werden. rn

Role of neutral metabolites in microbial conversion of 3beta-acetoxy-19-hydroxycholest-5-ene into estrone

Biotransformation of 3 beta-acetoxy-19-hydroxycholest-5-ene (19-HCA, 6 g) by Moraxella sp. was studied. Estrone (712 mg) was the major metabolite formed. Minor metabolites identified were 5 alpha-androst-1-en-19-ol-3,17-dione (33 mg), androst-4-en-19-ol-3,17-dione (58 mg), androst-4-en-9 alpha,19-diol-3,17-dione (12 mg), and androstan-19-ol-3,17-dione (1 mg). Acidic metabolites were not formed. Time course experiments on the fermentation of 19-HCA indicated that androst-4-en-19-ol-3,17-dione was the major metabolite formed during the early stages of incubation. However with continuing fermentation its level dropped, with a concomitant increase in estrone. Fermentation of 19-HCA in the presence of specific inhibitors or performing the fermentation for a shorter period (48 h) did not result in the formation of acidic metabolites. Resting-cell experiments carried out with 19-HCA (200 mg) in the presence of alpha,alpha'-bipyridyl led to the isolation of three additional metabolites, viz., cholestan-19-ol-3-one (2 mg), cholest-4-en-19-ol-3-one (10 mg), and cholest-5-en-3 beta,19-diol (12 mg). Similar results were also obtained when n-propanol was used instead of alpha,alpha'-bipyridyl. Resting cells grown on 19-HCA readily converted both 5 alpha-androst-1-en-19-ol-3,17-dione and androst-4-en-19-ol-3,17-dione into estrone. Partially purified 1,2-dehydrogenase from steroid-induced Moraxella cells transformed androst-4-en-19-ol-3,17-dione into estrone and formaldehyde in the presence of phenazine methosulfate, an artificial electron acceptor. These results suggest that the degradation of the hydrocarbon side chain of 19-HCA does not proceed via C-22 phenolic acid intermediates and complete removal of the C-17 side chain takes place prior to the aromatization of the A ring in estrone. The mode of degradation of the sterol side chain appears to be through the fission of the C-17-C-20 bond. On the basis of these observations, a new pathway for the formation of estrone from 19-HCA in Moraxella sp. has been proposed.

Age determination of sediment cores from the western Svalbard margin

The deglaciation of the continental shelf to the west of Spitsbergen and the main fjord, Isfjorden, is discussed based on sub-bottom seismic records and sediment cores. The sea floor on the shelf to the west of Isfjorden is underlain by less than 2 m of glaciomarine sediments over a firm diamicton interpreted as till. In central Isfjorden up to 10 m of deglaciation sediments were recorded, whereas in cores from the innermost tributary, Billefjorden, less than a meter of ice proximal sediments was recognized between the till and the 'normal' Holocene marine sediments. We conclude that the Barents Sea Ice Sheet terminated along the shelf break during the Late Weichselian glacial maximum. Radiocarbon dates from the glaciomarine sediments above the till indicate a stepwise deglaciation. Apparently the ice front retreated from the outermost shelf around 14.8 ka. A dramatic increase in the flux of line-grained glaciomarine sediments around 13 ka is assumed to reflect increased melting and/or current activity due to a climatic warming. This second stage of deglaciation was interrupted by a glacial readvance culminating on the mid-shelf area shortly after 12.4 ka. The glacial readvance, which is correlated with a simultaneous readvance of the Fennoscandian ice sheet along the western coast of Norway, is attributed to the so-called 'Older Dryas' cooling event in the North Atlantic region. Following this glacial readvance the outer part of Isfjorden became rapidly deglaciated around 12.3 ka. During the Younger Dryas the inner fjord branches were occupied by large outlet glaciers and possibly the ice front terminated far out in the main fjord. The remnants of the Barents Sea Ice Sheet melted quickly away as a response to the Holocene warming around 10 ka.

Elaboraci??n de plafones y juegos de vocabulario con pictogramas de ARASAAC en franc??s-espa??ol para alumnado de atenci??n a la diversidad de los centros con programa biling??e

Seleccionado en la convocatoria: Licencias por estudios destinadas a funcionarios docentes no universitarios, Gobierno de Arag??n 2010-2011

Gu??a para auxiliares de conversaci??n de espa??ol en el Reino Unido : curso 2014-2015

Gu??a destinada a los auxiliares de conversaci??n en espa??ol, que deseen trabajar como tales en Reino Unido. La gu??a incluye informaci??n sobre el viaje, el alojamiento y aspectos generales de la vida en dicho pa??s. Tambi??n recoge informaci??n sobre temas laborales, concretamente en el ??mbito de la ense??anza.

Buenas pr??cticas para la creaci??n de una comunidad de aprendices en el aula de espa??ol y la aplicaci??n de la metodolog??a de clase invertida

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A comparison between multi-proxy and historical data of drift-ice conditions on the East Greenland shelf

The reduction in sea ice along the SE Greenland coast during the last century has severely impacted ice-rafting to this area. In order to reconstruct ice-rafting and oceanographic conditions in the area of Denmark Strait during the last ~150 years, we conducted a multiproxy study on three short (20 cm) sediment cores from outer Kangerdlugssuaq Trough (~300 m water depth). The proxy-based data obtained have been compared with historical and instrumental data to gain a better understanding of the ice sheet-ocean interactions in the area. A robust chronology has been developed based on 210Pb and 137Cs measurements on core PO175GKC#9 (~66.2°N, 32°W) and expanded to the two adjacent cores based on correlations between calcite weight percent records. Our proxy records include sea-ice and phytoplankton biomarkers, and a variety of mineralogical determinations based on the <2 mm sediment fraction, including identification with quantitative x-ray diffraction, ice-rafted debris counts on the 63-150 µm sand fraction, and source identifications based on the composition of Fe oxides in the 45-250 µm fraction. A multivariate statistical analysis indicated significant correlations between our proxy records and historical data, especially with the mean annual temperature data from Stykkishólmur (Iceland) and the storis index (historical observations of sea-ice export via the East Greenland Current). In particular, the biological proxies (calcite weight percent, IP25, and total organic carbon %) showed significant linkage with the storis index. Our records show two distinct intervals in the recent history of the SE Greenland coast. The first of these (ad 1850-1910) shows predominantly perennial sea-ice conditions in the area, while the second (ad 1910-1990) shows more seasonally open water conditions.

Age determination of sediment cores off western Spitsbergen

The Late Weichselian glacial history of the continental shelf off western Spitsbergen is discussed, based on acoustic sub-bottom records and sediment cores. The outer part of Isfjorden and the inner shelf to the west of this fjord are characterized by a thin veneer (10-20 m) of glacigenic sediments and absence of ice-marginal features. Towards the outer shelf the sediment thickness increases significantly, and exceeds 500 m at the shelf edge. Possible moraine complexes were identified in this outer part. Sediment cores from the inner shelf sampled a firm diamicton, interpreted as till, beneath soft glaciomarine sediments. Radiocarbon dates on shells from the clay resting directly on the till, suggest an age of around 12,500 yrs B.P. for the base of the marine sequence. We argue that grounded ice covered the sites shortly before. In contrast to suggestions that the fjords and coast were partly ice free during the Late Weischselian, we conclude that the ice must have reached out onto the continental shelf.

Seawater carbonate chemistry and processes during experiments with Emiliania huxleyi (PML B92/11), 2000

We have measured the stable carbon isotopic composition of bulk organic matter (POC), alkenones, sterols, fatty acids, and phytol in the coccolithophorid Emiliania huxleyi grown in dilute batch cultures over a wide range of CO2 concentrations (1.1-53.5 micromol L-1). The carbon isotope fractionation of POC (POC) varied by ca. 7 per mil and was positively correlated with aqueous CO2 concentration [CO2aq]. While this result confirms general trends observed for the same alga grown in nitrogen-limited chemostat cultures, considerable differences were obtained in absolute values of POC and in the slope of the relationship of POC with growth rate and [CO2aq]. Also, a significantly greater offset was obtained between the delta13C of alkenones and bulk organic matter in this study compared with previous work (5.4, cf. 3.8 per mil). This suggests that the magnitude of the isotope offset may depend on growth conditions. Relative to POC, individual fatty acids were depleted in 13C by 2.3 per mil to 4.1 per mil, phytol was depleted in 13C by 1.9 per mil, and the major sterol 24-methylcholesta-5,22E-dien-3beta-ol was depleted in 13C by 8.5 per mil. This large spread of delta13C values for different lipid classes in the same alga indicates the need for caution in organic geochemical studies when assigning different sources to lipids that might have delta13C values differing by just a few per mil. Increases in [CO2aq] led to dramatic increases in the alkenone contents per cell and as a proportion of organic carbon, but there was no systematic effect on values of U37k- used for reconstructions of paleo sea surface temperature.