Occurrence of betulinic acid in different callus cultures of Solanum aviculare

Betulinic acid (3β-hydroxy-lup-20(29)-en-28-oic acid) was obtained from in vitro cultures of Solanum aviculare in yields up to 3% of the dry weight. This is a further example of overproduction by cells cultured in vitro of a product not found in the original parent plant.     

Evaluating potential of green alga <Emphasis Type="Italic">Chlorella vulgaris</Emphasis> to accumulate phosphorus and to fertilize nutrient-poor soil substrates for crop plants

Algae are capable of accumulating nutrients from aqueous waste, which makes them a potential fertilizer. The ability of the fast growing Chlorella vulgaris strain IPPAS C1 to accumulate phosphorus (P) was probed in V-shaped plastic foil photobioreactors. The P uptake was 0.13–0.53 g(P)·m^?2·day^?1 when the algal culture densities were kept between 0.1 and 1.0 g(DW)·L^?1 in a typical summer irradiance of Central Europe. The algal biomass can be effectively utilized for soil fertilization only if the algal cells release nutrients into the soil in a form that would be available to roots and at a rate sufficient to support plant growth. To examine this, we compared the growth of wheat, Triticum aestivum L., in two nutrient-deficient substrates: “Null Erde” and sand, with and without fertilization by wet and spray-dried algae. Plants grown in the two nutrient-deficient substrates supplemented by mineral fertilizer served as a control representing optimal nutrient supply. Plants grown in a high-nutrient substrate (SoMi 513) were used as an additional reference representing the maximum growth potential of wheat. Wheat growth was monitored for 8 weeks and measured, including the increase of the leaf area as well as shoot and root dry weight in 10 randomized replicates for each substrate and fertilization variant. After harvest, the biomass and N, P, and C contents of the plant shoots and roots were recorded. Algae fertilization of “Null Erde” led to wheat growth, including root hair production, which was similar to mineral-fertilized “Null Erde” and only slightly less vigorous than in the nutrient-rich SoMi 513 substrate. The plants grown in sand were smaller than the plants in “Null Erde” but fertilization by algae nevertheless led to growth that was comparable to mineral fertilizer. These results unambiguously demonstrate that algal biomass is a viable option for delivering nutrients to support agriculture on marginal soils.     

Refining the late Silurian sea-level history of the Prague Syncline—a case study based on the Přídolí GSSP (Czech Republic)

A 50-m-thick section in the Po?áry quarry, Prague Syncline (Czech Republic) spanning the upper Silurian (uppermost Ludlow and P?ídolí) to the lowermost Devonian (Lochkovian) has been studied using sedimentological and physical stratigraphical (gamma-ray spectrometry) methods combined with conodont biostratigraphy. Conodont data demonstrate the presence of local conodont biozones: “Ozarkodina” crispa (uppermost Ludlow)—Zieglerodina zellmeri (base of P?ídolí)—Zieglerodina ivochlupaci—Delotaxis detorta—“Ozarkodina” eosteinhornensis s.s.—Zieglerodina klonkensis—Icriodus hesperius-optima (lowermost Lochkovian). The studied section represents a transgressive–regressive facies succession characterized by a transition from distal calciturbidites deposited in a distally steepened carbonate platform during transgression and sea-level highstand (crispa to lower ivochlupaci zones) to mixed calciturbidites/coarse-grained bioclastic limestones (falling-stage systems tract, upper ivochlupaci to lower klonkensis zones). The upper part of the succession consists of bioclastic limestones corresponding to a subtidal setting between storm-wave and fair-weather wave base (lowstand systems tract in upper klonkensis and hesperius-optima zones). This interpretation corresponds to the late Silurian global sea-level pattern as recorded in other regions. Thus the depositional system is interpreted as mostly driven by eustasy with short-lived periods of influence from local tectonics.     

Simultaneous determination of the new anticancer agent amidox and its metabolites in rat bile and plasma by high-performance liquid chromatography

A new reversed-phase ion-pair high-performance liquid chromatography method was developed to study the first-pass hepatic metabolism of the anti cancer drug amidox in bile. Separation of the metabolites was achieved on a Spherisorb C₁₈ column after liquid-liquid extraction using a linear gradient system of heptanesulfonic acid in potassium phosphate monobasic (pH 4.0) with increasing amounts of methanol (0–40%). The method was further applied to a pharmacokinetic study of amidox in rats after 200 mg kg⁻¹ intraperitoneal administration. Using 50 μl of rat bile and 300 μl of rat plasma the limit of detection for amidox was 60 ng and 85 ng, respectively, and the assay was linear from 0.1 to 150 μg ml⁻¹. This method appears to be sensitive enough to be used in further pharmacokinetic studies of amidox in human volunteers.     

Structural characterization of photosystem II complex from red alga Porphyridium cruentum retaining extrinsic subunits of the oxygen-evolving complex.

The structure of photosystem II (PSII) complex isolated from thylakoid membranes of the red alga Porphyridium cruentum was investigated using electron microscopy followed by single particle image analysis. The dimeric complexes observed contain all major PSII subunits (CP47, CP43, D1 and D2 proteins) as well as the extrinsic proteins (33 kDa, 12 kDa and the cytochrome c(550)) of the oxygen-evolving complex (OEC) of PSII, encoded by the psbO, psbU and psbV genes, respectively. The single particle analysis of the top-view projections revealed the PSII complex to have maximal dimensions of 22 x 15 nm. The analysis of the side-view projections shows a maximal thickness of the PSII complex of about 9 nm including the densities on the lumenal surface that has been attributed to the proteins of the OEC complex. These results clearly demonstrate that the red algal PSII complex is structurally very similar to that of cyanobacteria and to the PSII core complex of higher plants. In addition, the arrangement of the OEC proteins on the lumenal surface of the PSII complex is consistent to that obtained by X-ray crystallography of cyanobacterial PSII.