Elektronenmikroskopische Untersuchungen über Glaskörperrindenzellen und Zonulafasern

Zusammenfassung Es werden folgende Befunde zur Feinstruktur des Glaskörpers beim 16 Tage alten Rattenembryo und der Glaskörperrinde beiderseits der Ora serrata beim 3 Jahre alten, an Retinoblastom erkrankten Kind mitgeteilt:Der Glaskörper des Rattenembryos und die Glaskörperrinde des kindlichen Auges enthalten Fibroblasten. Sie unterscheiden sich nicht von den im Bindegewebe vorkommenden Fibroblasten. Im embryonalen Rattenglaskörper wurden außerdem faserbildende Zellen mit wabiger Struktur des Zytoplasmas beobachtet.Die Fibroblasten der Glaskörperrinde bilden die Fibrillen des Glaskörpergerüstes und der Zonulafasern. Diese Fibrillen zeigen eine deutliche Querstreifung. Die Streifung ist unregelmäßig oder periodisch. Die Länge der Perioden beträgt in unseren Schnitten bei den Glaskörperfibrillen des Rattenembryos und des kindlichen Auges meist etwa 120, seltener 210 A. An den Fibrillenbündeln einer Zonulafaser des kindlichen Auges wurden Perioden von 90–120, 400, 440 und 630 A beobachtet.Die Fibroblasten der Glaskörperrinde des kindlichen Auges liegen im Bereich der Pars plana corporis ciliaris auch tief in den Buchten und Falten des Ciliarepithels. Hierdurch wird eine maximal große Anheftungsfläche für die von ihnen produzierten Fibrillen der Zonulafasern gewährleistet.Die Pars plana corporis ciliaris des kindlichen Auges ist von einem dichten Netz von Fibroblastenfortsätzen überzogen. Auch vereinzelte Makrophagen finden sich hier.Unsere elektronenmikroskopischen Befunde bestätigen die Angaben von Balazs über das Vorkommen von Fibrocyten (Fibroblasten) und Makrophagen in der Glaskörperrinde. Ferner bestätigen sie die bereits von früheren Autoren lichtmikroskopisch gewonnenen Erkenntnisse, wonach es sich beim Glaskörper um mesenchymales Gewebe, bei den Zonulafasern im Bindegewebsfasern handelt.

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Summary The following electron microscopical findings in the vitreous body of 16-day-old rat embryos and in the vitreoretinal border layer on both sides of the ora serrata in a 3-year-old child are reported:The vitreous body of the rat embryo and the vitreoretinal border layer of the infant eye contain fibroblasts. These fibroblasts do not differ from those present in connective tissue. The embryonic vitreous body of the rat contains fibre-forming cells, which show an alveolar structure of the cytoplasm.The fibroblasts in the cortical tissue layer of the vitreous body form the fibrils of the stroma of the vitreous body and the zonula fibres. These fibrils show a marked cross striation. The striation is either irregular or shows periodicity. In the vitreous body of the rat embryo and of the infant eye the lenght of these periods has been measured with 120 and 210 A. Periods of 90–120, 400, 440 and 630 A could be shown in the fibrillar bundles of a zonula fibre of the infant eye. In the region of the pars plana corporis ciliaris the fibroblasts of the cortical tissue layer of the vitreous body of the infant eye are also found deep down in the sinus and folds of the ciliary epithelium. Thus they guarantee an as large as possible area for the attachment of the fibrils of the zonula fibres which they produce.The pars plana corporis ciliaris of the infant eye is covered with a dense network of fibroblast processes. Also cells of the macrophage type may be found in this region.Our electron microscopical findings confirm those of earlier light microscopists and lately by Balazs. The vitreous body of the eye is formed by mesenchymal tissue, whereas the zonula fibres are formed by connective tissue.

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Mit dankenswerter Unterstützung durch den Schweizerischen Nationalfonds zur Förderung der Wissenschaftlichen Forschung.     

Purification of thymocyte growth peptide (TGP) from sheep thymus. Relationship to FTS/thymulin

Thymocyte growth peptide (TGP) initiates DNA synthesis in immature thymocytes and has previously been characterized as an acidic peptide isolated from calf thymus. We now report the isolation of TGP from sheep thymus and show it to be a nonapeptide with a large N-terminal blocking moiety characterized by high UV absorbance. The amino acid composition is identical to FTS, consisting of 2 Gly, 2 Ser, 2 Glx, 1 Ala, 1 Lys, 1 Asx. In contrast to FTS, TGP is acidic with an apparent isoelectric point of 4.2 and a high UV absorbance at 270–280 nm. Reverse phase chromatography of TGP at an acidic pH results in a change of the molecule and the appearance of two new compounds TGP-A and TGP-B, both with less than 50% of the original TGP activity. Full activity could be restored by the addition of ZnCl₂ to TGP-A. Both TGP-A and B have some amino acid composition and high UV absorbance as native TGP. We propose that TGP consists of a non-peptide moiety bound to the N-terminal of the nonapeptide Glu-Ala-Lys-Ser-Gln-Gly-Gly-Ser-Asn and that the active molecule is stabilized by Zn²⁺.     

Microbial oxidation of ebastine

The microbial oxidation of ebastine to carebastine was investigated. Among the 15 micro-organisms examined, only theCunninghamella strains showed the desired biotransformation.Cunninghamella blakesleeana oxidised the substrate within 7 days, via the intermediates alcohol and aldehyde, mainly to carebastine, the corresponding carboxylic acid. Optimisation of the culture conditions increased the yield from initially 10% up to a reproducible 40%. For the synthesis of carebastine a substrate concentration of 200 mg/l, a starting pH of 5.0 and the addition of 1% poly(vinyl alcohol) is favourable. The results achieved in experiments with shaking flasks are transferable to the fermentation scale and yielded 270 mg carebastine in a 3-l fermentation of 600 mg ebastine. The progress of the reaction was detected by TLC and HPLC, the products were identified by mass spectrometry and NMR.     

Xylitol production by immobilized recombinant Saccharomyces cerevisiae in a continuous packed-bed bioreactor

Continuous xylitol production with two different immobilized recombinant Saccharomyces cerevisiae strains (H475 and S641), expressing low and high xylose reductase (XR) activities, was investigated in a lab-scale packed-bed bioreactor. The effect of hydraulic residence time (HRT; 1.3-11.3 h), substrate/cosubstrate ratio (0.5 and 1), recycling ratio (0, 5, and 10), and aeration (anaerobic and oxygen limited conditions) were studied. The cells were immobilized by gel entrapment using Ca-alginate as support and the beads were treated with Al(3+) to improve their mechanical strength. Xylose was converted to xylitol using glucose as cosubstrate for regeneration of NAD(P)H required in xylitol formation and for generation of maintenance energy. The stability of the recombinant strains after 15 days of continuous operation was evaluated by XR activity and plasmid retention analyses. Under anaerobic conditions the volumetric xylitol productivity increased with decreasing HRT with both strains. With a recycling ratio of 10, volumetric productivities as high as 3.44 and 5.80 g/L . h were obtained with the low XR strain at HRT 1.3 h and with the high XR strain at HRT 2.6 h, respectively. However, the highest overall xylitol yields on xylose and on cosubstrate were reached at higher HRTs. Lowering the xylose/cosubstrate ratio from 1 to 0.5 increased the overall yield of xylitol on xylose, but the productivity and the xylitol yield on cosubstrate decreased. Under oxygen limited conditions the effect of the recycling ratio on production parameters was masked by other factors, such as an accumulation of free cells in the bioreactor and severe genetic instability of the high XR strain. Under anaerobic conditions the instability was less severe, causing a decrease in XR activity from 0.15 to 0.10 and from 3.18 to 1.49 U/mg with the low and high XR strains, respectively. At the end of the fermentation, the fraction of plasmid bearing cells in the beads was close to 100% for the low XR strain; however, it was significantly lower for the high XR strain, particularly for cells from the interior of the beads. (c) 1996 John Wiley & Sons, Inc.     

The upper cretaceousLacazina limestone in the Basco-Cantabrian and Iberian basins of northern Spain: Cold-water grain associations in warm-water environments

Summary The Upper Santonian to Lower CampanianLacazina Limestone consists of massive, often amalgamated beds of packstones and grainstones which were deposited in a shallow marine environment. The most abundant skeletal components are miliolid foraminifera, echinoderm, bivalve and bryozoan fragments, peloids and sparse red algae. Small, solitary corals only occur sporadically. Hermatypic corals, sponges and green algae are missing. The series which reaches thicknesses between 60 m and 160 m, was sampled at intervals of 0.5 m at five localities. The petrographic features throughout the series are mainly a product of changing depositional energy. The limestones are well cemented. Diagenesis is characterized by a transition from marine phreatic to burial cementation. Syntaxial and blocky calcite cements predominate over early acicular to bladed and microgranular cements. The faunal association within theLacazina Limestone exhibits features typical for temperate water i.e.foramol carbonates. On the other hand, oxygen (δ¹⁸O =-1.7 to −6.3 ‰ PDB) and carbon (δ¹³C to 3.0‰ PDB) isotope values of diagentically unaltered bivalve shells indicate warm surface waters corresponding better to the palaeogeographical situation of theLacazina Limestone. Nutrient-surplus is proposed as a limiting factor preventing the development of reefs and finally ofchlorozoan sediments. In the sense of sequence stratigraphy, theLacazina Limestone is interpreted to contain transgressive and highstand systems tracts. This interpretation fits well into theHaq-Vail-curve. The series shows no visible high-frequency cyclicity in the field. Several cycles were found by means of principle component analysis and spectral analysis. Their relationships to the Milankovitch spectrum are discussed. The ammonite fauna of the unit and of preceding sediments (late Coniacian to early Campanian) is described and some inoceramids are figured. They permit—for the first time—the exact dating of theLacazina Limestone in the Basco-Cantabrian Basin (BCB) and throw light on a prominent faunal change at the Coniacian/Santonian boundary. The Cenomanian to Coniacian ammonite faunas which were dominated by endemic Tethyan pseudoceratitic faunas are replaced by cosmopolitan species dominated by Madagascan elements. This drastic change permits speculations about the installation of a new oceanic current system in the Santonian.     

Enumeration and characterization of the soil microflora from hydrocarbon-contaminated soil sites able to mineralize polycyclic aromatic hydrocarbons (PAH)

The use of a plate screening technique allowed the direct isolation and quantification of polycylic aromatic hydrocarbon (PAH)-degrading bacteria from different soil sites. Bacteria that were able to grow on anthracene, phenanthrene, fluoranthene or pyrene as a sole carbon source were found with numbers between 10³ and 10⁵ colony-forming units (cfu)/g of soil dry weight, but only in samples that originated from PAH-contaminated sites. No isolates were found that could grow on perylene, triphenylene, benzo(a)pyrene or chrysene as sole carbon source. Bacteria that had been selected on the same PAH substrate showed a related degradation pattern for both other PAH and oil compounds and carbohydrate substrates even if they had been collected at distant soil sites. Based on these findings the isolates could be clustered into four different catabolic and taxonomic similarity groups. Taxonomic determination of representative isolates suggested that nocardioform actinomycetes of the genera Mycobacterium, Rhodococcus and Gordona represented a major part of the soil microflora able to mineralize PAH. Three new isolates able to grow on anthracene, pyrene or fluoranthene as the sole carbon source, respectively, have been isolated and identified (Sphingomonas paucimobilis BA2, Gordona sp. BP9, Mycobacterium sp. VF1). The ubiquitous presence of a potent and versatile mineralizing microflora in PAH-contaminated soils indicated that the microflora is not the limiting factor for the degradation of PAH with up to four rings.     

Nutrient balances and phytoplankton dynamics in two agriculturally loaded shallow lakes

The impact of agriculture was estimated on two shallow, eutrophic lakes, Lake Kotojärvi and Lake Villikkalanjärvi in southern Finland. The main emphasis was on phosphorus and nitrogen budgets and on the phytoplankton dynamics. Special attention was paid to internal P loading and blue-green algal blooms. The mean Tot-P load from agricultural land was 1.2 kg ha^-1 a^-1 in both basins and Tot-N loads were 19 kg ha^-1 a^-1 in L. Villikkalanjärvi and 12 kg ha^-1 a^-1 in L. Kotojärvi. The Tot-P input to L. Kotojärvi was on an average 0.62 g m^-2 a^-1 (per lake surface area), and the Tot-N input 9.1 g m^-2 a^-1. The corresponding inputs to L. Villikkalanjärvi were 3.1 and 57 g m^-2 a^-1, respectively. The annual variation followed the runoff volumes. About half of the Tot-P and one third of the Tot-N load was retained in L. Kotojärvi. In L. Villikkalanjärvi the retention was only 24% for Tot-P and 19% for Tot-N. The difference was very probably due to a longer theoretical retention time in L. Kotojärvi. In L. Villikkalanjärvi the mean concentration of Tot-P was 120 µg 1^-1 and that of Tot-N 1700 µg 1^-1 and the corresponding figures in L. Kotojärvi 67 and 990 µg 1^-1, respectively. The mean chlorophyll a concentration was, however, higher in L. Kotojärvi (26 µg 1^-1) than in L. Villikkalanjärvi (20 µg 1^-1). This was probably due to an internal P load in L. Kotojärvi: in 1988 the internal load of dissolved P was estimated to be as much as twofold the external load. In L. Villikkalanjärvi the internal dissolved P load was only up to 50% of the external input. In L. Kotojärvi the high internal P load coupled with a low DIN:DIP ratio resulted in a strong blue-green algal bloom in the summer of 1988. In L. Villikkalanjärvi blue-green algae were observed only in small amounts. Even in August 1990, when the DIN:DIP ratio was low enough to favor the occurrence of blue-green algae, they contributed only up to 10–15% of the total phytoplankton biomass.