Abscisic acid and the induction of desiccation tolerance in the extremely xerophilic liverwortExormotheca holstii

Abscisic acid (ABA) induces formation of a set of proteins in the xerophilic liverwortExormotheca holstii. Some of them have immunological properties similar to the dehydrins of desiccated corn embryos and the desiccation-related proteins ofCraterostigma plantagineum. The fluctuations of endogenous ABA during cycles of desiccation and rehydration seem to be sufficiently high to indicate a role for ABA as a stress hormone and there by as an endogenous inductor of stress-related protein synthesis. Desiccation tolerance disappears when thalli are cultivated for a longer period under well-watered conditions; such thalli are not able to increase stress-dependent ABA biosynthesis sufficiently, or to form the desiccation-related proteins unless they are treated with external ABA. The rehydrated thalli cannot recover from a rapid water loss, while ABA-treated, non-hardened thalli regain their photosynthetic activity within two hours.Abbreviations ABA abscisic acid - F_o initial fluorescence yield - F_m maximum fluorescence yield - Q_A primary quinone receptor of PSII We are grateful to Deutsche Forschungsgemeinschaft for financial support (SFB 251, TP3, Graduiertenkolleg Ka 456/5-1), to Prof. E.W. Weiler (Lehrstuhl für Pflanzenphysiologie, Ruhr-Universität, Bochum, Germany), Dr. D. Bartels (Max-Planck-Institut für Züchtungsforschung, Köln, Germany) and Dr. T.J. Close (Department of Botany and Plant Science, University of California, Riverside, Calif., USA) for generous gifts of immunochemicals for ABA assay and antibodies 6–19, 37-31 and Rb-2b, to Miss. B. Dierich for skilful technical assistance and to Mrs. E.M. Arnold, Omaruru, Namibia for the generous supply ofExormotheca thalli.     

Two mechanisms of recovery from photoinhibition in vivo: Reactivation of photosystem II related and unrelated to D1-protein turnover

Recovery (at 20° C) of spinach (Spinacia oleracea L.) leaf sections from photoinhibition of photosynthesis was monitored by means of the fluorescence parameter F_V/F_M of intact leaf tissue and of PSII-driven electron-transport activity of isolated thylakoids. Different degrees of photoinactivation of PSII were obtained by preillumination in ambient air (at 4 or 20° C), CO₂-free air or at low and high O₂ levels (2 or 41 %) in N₂. The kinetics of recovery exhibited two distinct phases. The first phase usually was completed within about 20-60 min and was most pronounced after preillumination in low O₂. The slow phase proceeded for several hours leading to almost complete reactivation of PSII. Preincubation of the leaves with streptomycin (SM), which inhibits chloroplast-encoded protein synthesis, inhibited the slow recovery phase only, indicating the dependence of this phase on resynthesis of the reaction-centre protein, D1. The fast recovery phase remained largely unaffected by SM. Both phases were strongly but not totally dependent on irradiation of the leaf with low light. When SM was absent, net degradation of the D1 protein could neither be detected upon photoinhibitory irradiation nor during following incubation of the leaf sections in low light or darkness. In the presence of SM, net D1 degradation was seen and tended to increase with O₂ concentration during photoinhibition treatment. Based on these data, we suggest that photoinactivation of PSII in vivo occurs in at least two steps. From the first step, reactivation appears possible in low light without D1 turnover (fast recovery phase). Action of oxygen then may lead to a second step, in which the D1 protein is affected and reactivation requires its removal and replacement (slow phase).Abbreviations Chl chlorophyll - F₀, F_M and F_V initial, maximum total and maximum variable chlorophyll fluorescence yield, respectively - PFD photon flux density - SM streptomycin We thank Professor P. Böger (Department of Plant Physiology and Biochemistry, University of Konstanz, Germany) for a gift of D1-specific antibodies. The paper contains part of the thesis work of J.L. The study was supported by the Deutsche Forschungs-gemeinschaft (SFB 189).     

Embryonic expression of muscle-specific antigens in the grasshopper Schistocerca gregaria

Monoclonal antibodies (MAbs) are used to investigate molecules that are expressed during embryonic muscle differentiation and that may be involved in muscle pioneer and muscle attachment site formation. MAb F2A5 immunoreactivity appears in all muscle pioneers as soon as they extend processes, and continues in all muscle precursors. MAb 4H1 immunoreactivity is strongly expressed only after mesodermal cells have fused with the muscle pioneers; then it is concentrated at their growth-cone-like ends near developing attachment sites. During later embryonic development, MAb F2A5 and MAb 4H1 immunoreactivity become associated with the myofibrillar network. Biochemical experiments indicate that MAb 4H1 recognises a 47 kDa antigen, and MAb F2A5 recognises an 80 kDa antigen.     

Urease from Staphylococcus saprophyticus: purification,characterization and comparison to Staphylococcus xylosus urease

Urease from Staphylococcus saprophyticus was purified more than 800-fold by liquid chromatography reaching homogeneity, as shown by isoelectric focussing, at a maximum specific activity of 1979 U/mg. The molecular weight of the native enzyme was 420000; it consisted of subunits with molecular weights of 72400 (), 20400 (), and 13900 () in an estimated ()₄ stoichiometry. In native gradient polyacrylamide gel electrophoresis urease exhibited a multiple activity band pattern with molecular weights ranging from 420000 to 100000. In the native enzyme, 4.09 (±0.25) atoms of nickel per molecule were detected. The N-terminal amino acids of the urease subunits were identical to those from Staphylococcus xylosus, and amino acid analysis revealed high similarities in both enzymes; no cysteine was detected after acid hydrolysis of vinylpyridinylated urease. Electron micrographs of negatively stained urease specimens from both staphylococci showed identical size and structure.Abbreviation PAGE polyacrylamide gel electrophoresis     

Threonine is present instead of cysteine at the active site of urease from Staphylococcus xylosus

DNA sequence analysis of the stuctural urease genes from Staphylococcus xylosus revealed that three enzyme subunits are encoded in the order of 11000, 15400 and 61000 (mol. mass), which correspond to the single polypeptide chain of jack bean urease (90800). Comparing the deduced amino acid sequence of S. xylosus urease with the amino acid sequence of jack bean urease an overall portion of 56% identical residues was found. For S. xylosus urease a subunit structure of ()₄ was proposed, based on the comparison of the deduced amino acid content of the enzyme subunits with the total amino acid content of the purified enzyme. The staphylococcal enzyme contained no cysteine, as deduced from DNA sequence and confirmed by the determination of the total amino acid content in the purified enzyme. Instead of cysteine, known to be catalytically essential in the plant enzyme, and conserved among all bacterial ureases analyzed so far, threonine was found in S. xylosus. This amino acid-exchange was located within a highly conserved domain of 17 amino acids, supposed to be part of the active site. Sequence analysis of the respective region of Staphylococcus saprophyticus urease showed that it also contains threonine instead of cysteine. In contrast to jack bean urease S. xylosus urease was not affected by the SH-group inhibitor dipyridyl disulfide but was completely inhibited by the serine protease inhibitor phenylmethanesulfonyl fluoride. The presented results indicated that in these staphylococcal strains urea hydrolysis might function in a manner similar to the peptide bond cleavage by chymotrypsin.Abbreviations AA amino acid - ATZ anilino thiazolinone - DPDS dipyridyl disulfide - Kb kilobase pairs - PITC phenylisothiocyanate - PTH phenylthiohydantoin - PMSF phenylmethanesulfonyl fluoride     

Energy-dependent changes in the ATP/ADP ratio at the tight nucleotide binding site of chloroplast ATP synthase

Using DTT-modulated thylakoid membranes we studied tight nucleotide binding and ATP content in bound nucleotides and in the reaction mixture during [¹⁴C] ADP photophosphorylation. The increasing light intensity caused an increase in the rate of [¹⁴C] ADP incorporation and a decrease in the steady-state level of tightly bound nucleotides. Within the light intensity range from 11 to 710 w m^–2, ATP content in bound nucleotides was larger than that in nucleotides of the reaction mixture; the most prominent difference was observed at low degrees of ADP phosphorylation. The increasing light intensity was accompanied by a significant increase of the relative ATP content in tightly bound nucleotides. The ratio between substrates and products formed at the tight nucleotide binding site during photophosphorylation was suggested to depend on the light-induced proton gradient across the thylakoid membrane.Abbreviations AdN adenine nucleotide - Chl chlorophyll - DTT dithiothreitol - FCCP carbonylcianide p-trifluoromethoxyphenilhydrazone - P_i inorganic orthophosphate - PMS phenazine methosulfate - TLC thin-layer chromatography - Tricine N-[tris(hydroxymethyl)methyl] glycine     

The origin of Jurassic reefs: Current research developments and results

Summary In order to elucidate the control of local, regional and global factors on occurrence, distribution and character of Jurassic reefs, reefal settings of Mid and Late Jurassic age from southwestern Germany, Iberia and Romania were compared in terms of their sedimentological (including diagenetic), palaeoecological, architectural, stratigraphic and sequential aspects. Upper Jurassic reefs of southern Germany are dominated by siliceous sponge—microbial crust automicritic to allomicritic mounds. During the Oxfordian these form small to large buildups, whereas during the Kimmeridgian they more frequently are but marginal parts of large grain-dominated massive buildups. Diagenesis of sponge facies is largely governed by the original composition and fabric of sediments. The latest Kimmeridgian and Tithonian spongiolite development is locally accompanied by coral facies, forming large reefs on spongiolitic topographic elevations or, more frequently, small meadows and patch reefs within bioclastic to oolitic shoal and apron sediments. New biostratigraphic results indicate a narrower time gap between Swabian and Franconian coral development than previously thought. Palynostratigraphy and mineralostratigraphy partly allow good stratigraphic resolution also in spongiolitic buildups, and even in dolomitised massive limestones. Spongiolite development of the Bajocian and Oxfordian of eastern Spain shares many similarities. They are both dominated by extensive biostromal development which is related to hardground formation during flooding events. The Upper Jurassic siliceous sponge facies from Portugal is more localised, though more differentiated, comprising biostromal, mudmound and sponge-thrombolite as well as frequent mixed coral-sponge facies. The Iberian Upper Jurassic coral facies includes a great variety of coral reef and platform types, a pattern which together with the analysis of coral associations reflects the great variability of reefal environments. Microbial reefs ranging from coralrich to siliceous sponge-bearing to pure thrombolites frequently developed at different water depths. Reef corals even thrived within terrigeneous settings. In eastern Romania, small coral reefs of various types as well as larger siliceous sponge-microbial crust mounds grew contemporaneously during the Oxfordian, occupying different bathymetric positions on a homoclinal ramp. Application of sequence stratigraphic concepts demonstrates that onset or, in other cases, maximum development of reef growth is related to sea level rise (transgressions and early highstand) which caused a reduction in allochthonous sedimentation. The connection of reef development with low background sedimentation is corroborated by the richness of reefs in encrusting organisms, borers and microbial crusts. Microbial crusts and other automicrites can largely contribute to the formation of reef rock during allosedimentary hiatuses. However, many reefs could cope with variable, though reduced, rates of background sedimentation. This is reflected by differences in faunal diversities and the partial dominance of morphologically adapted forms. Besides corals, some sponges and associated brachiopods show distinct morphologies reflecting sedimentation rate and substrate consistency. Bathymetry is another important factor in the determination of reefal composition. Not only a generally deeper position of siliceous sponge facies relative to coral facies, but also further bathymetric differentiation within both facies groups is reflected by changes in the composition, diversity and, partly, morphology of sponges, corals, cementing bivalves and microencrusters. Criteria such as authigenic glauconite, dysaerobic epibentic bivalves,Chondrites burrows or framboidal pyrite in the surrounding sediments of many Upper Jurassic thrombolitic buildups suggest that oxygen depletion excluded higher reefal metazoans in many of these reefs. Their position within shallowing-upwards successions and associated fauna from aerated settings show that thrombolitic reefs occurred over a broad bathymetric area, from moderately shallow to deep water. Increases in the alkalinity of sea water possibly enhanced calcification. Reefs were much more common during the Late Jurassic than during the older parts of this period. Particularly the differences between the Mid and Late Jurassic frequencies of reefs can be largely explained by a wider availability of suitable reef habitats provided by the general sea level rise, rather than by an evolutionary radiation of reef biota. The scarcity of siliceous sponge reefs on the tectonically more active southern Tethyan margin as well as in the Lusitanian Basin of west-central Portugal reflects the scarcity of suitable mid to outer ramp niches. Coral reefs occurred in a larger variety of structural settings. Upper Jurassic coral reefs partly grew in high latitudinal areas suggesting an equilibrated climate. This appears to be an effect of the buffering capacity of high sea level. These feedback effects of high sea level also may have reduced oceanic circulation particularly during flooding events of third and higher order, which gave rise to the development of black shales and dysaerobic thrombolite reefs. Hence, the interplay of local, regional and global factors caused Jurassic reefs to be more differentiated than modern ones, including near-actualistic coral reefs as well as non-actualistic sponge and microbial reefs.     

Neutral Lipid Biosynthesis in Engineered Escherichia coli: Jojoba Oil-Like Wax Esters and Fatty Acid Butyl Esters

Wax esters are esters of long-chain fatty acids and long-chain fatty alcohols which are of considerable commercial importance and are produced on a scale of 3 million tons per year. The oil from the jojoba plant (Simmondsia chinensis) is the main biological source of wax esters. Although it has a multitude of potential applications, the use of jojoba oil is restricted, due to its high price. In this study, we describe the establishment of heterologous wax ester biosynthesis in a recombinant Escherichia coli strain by coexpression of a fatty alcohol-producing bifunctional acyl-coenzyme A reductase from the jojoba plant and a bacterial wax ester synthase from Acinetobacter baylyi strain ADP1, catalyzing the esterification of fatty alcohols and coenzyme A thioesters of fatty acids. In the presence of oleate, jojoba oil-like wax esters such as palmityl oleate, palmityl palmitoleate, and oleyl oleate were produced, amounting to up to ca. 1% of the cellular dry weight. In addition to wax esters, fatty acid butyl esters were unexpectedly observed in the presence of oleate. The latter could be attributed to solvent residues of 1-butanol present in the medium component, Bacto tryptone. Neutral lipids produced in recombinant E. coli were accumulated as intracytoplasmic inclusions, demonstrating that the formation and structural integrity of bacterial lipid bodies do not require specific structural proteins. This is the first report on substantial biosynthesis and accumulation of neutral lipids in E. coli, which might open new perspectives for the biotechnological production of cheap jojoba oil equivalents from inexpensive resources employing recombinant microorganisms.     

Über die Frühentwicklung von Triton alpestris bei Dunkelheit

Zusammenfassung 102 Keime von Triton alpestris wurden im Harrison-Stadium 1 in völlige Dunkelheit verbracht und nach 9–12 Tagen fixiert. Die Untersuchung unter der Lupe und in histologischen Serienschnitten ergab keine morphologisch faßbaren Abweichungen von der normalen Entwicklung. Es wird daraus geschlossen, daß auch für die speziell dem Licht zugeordneten Organe — wie Augen und Melanophoren — in diesen frühen Stadien das Licht keine formative Bedeutung hat.     

Über die Schwankungen der abiotischen Faktoren in der Elbmündung bei Cuxhaven

Zusammenfassung 1. Die Veränderungen der abiotischen Faktoren, die schon den frühen Untersuchern bekannt waren, werden besprochen.2. Langfristige Änderungen des Salzgehaltes werden durch die Abflußmenge der Elbe bedingt.3. Kurzfristige Änderungen der abiotischen Faktoren bringen die Gezeiten; ihr Ausmaß wird weitgehend von den Wetterbedingungen beeinflußt. Im Watt sind während der Ebbe je nach den Außenbedingungen starke Veränderungen im Chemismus festzustellen, deren Ursache z. T. auf die Photosynthese der Diatomeen zurückzuführen ist. Messungen selbst an nahe beieinander gelegenen Punkten bringen schon große Unterschiede der abiotischen Faktoren.4. In einem durch Molen abgegrenzten Gebiet an der Alten Liebe ist der Salzgehalt immer etwas höher als Folge seiner topographischen Besonderheit.5. Die Wirkungen der Veränderungen abiotischer Faktoren auf das biologische Geschehen werden an einigen Beispielen erläutert, z. B. das Erscheinen und Verschwinden bestimmter Arten in einzelnen Jahren in Abhängigkeit von der Abflußmenge der Elbe und im Zusammenhang damit von der Höhe des Salzgehaltes.

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On the fluctuations of abiotic factors in the Elbe estuary near Cuxhaven

The changes of abiotic factors, especially salinity, water temperature, O₂-content, pH and alcalinity in the Elbe river near Cuxhaven are documented. Long-term salinity fluctuations depend on the water outflow of the Elbe. Short-term salinity changes are caused by the tides. During the period from 1949 to 1953 and again in 1959, salinity was high (above 20% in summer). From 1954 to 1958, as well as in 1961, salinity was low, at times considerably below 15 At high tide with its increasing salinity, plankton samples contain more copepods and larvae of balanids and spionids since the maximum population density of these forms occurs in the polyhalinicum at the light-ship Elbe 3. If the conditions are favorable, the larvae can settle and start a new population. In a small locality near the Alte Liebe pier, marked off by two jetties, the salinity is always somewhat higher than it is in the river Elbe. In this higher salinity, populations ofCoryne sarsi as well as youngAsterias rubens were found in all years characterized by increased salinities (monthly average about 15 to 20%). In years with higher salinitiesTeredo navalis caused increased deterioration of timber work. Small water pools in the mud flat area showed profound changes in water temperature, salinity and pH. Their O₂ content is very high due to the photosynthesis of diatoms, reaching saturation values of 320%. These extremes disappear quickly as the water returns at high tide.