Carbon and nitrogen isotope ratios in different compartments of a healthy and a declining Picea abies forest in the Fichtelgebirge,NE Bavaria

Summary Natural carbon and nitrogen isotope ratios were measured in different compartments (needles and twigs of different ages and crown positions, litter, understorey vegetation, roots and soils of different horizons) on 5 plots of a healthy and on 8 plots of a declining Norway spruce (Picea abies (L.) Karst.) forest in the Fichtelgebirge (NE Bavaria, Germany), which has recently been described in detail (Oren et al. 1988a; Schulze et al. 1989). The ¹³C values of needles did not differ between sites or change consistently with needle age, but did decrease from the sun-to the shade-crown. This result confirms earlier conclusions from gas exchange measurements that gaseous air pollutants did no long-lasting damage in an area where such damage was expected. Twigs (¹³C between-25.3 and-27.8) were significantly less depleted in ¹³C than needles (¹³C between-27.3 and-29.1), and ¹³C in twigs increased consistently with age. The ¹⁵N values of needles ranged between-2.5 and-4.1 and varied according to stand and age. In young needles ¹⁵N decreased with needle age, but remained constant or increased in needles that were 2 or 3 years old. Needles from the healthy site were more depleted in ¹⁵N than those from the declining site. The difference between sites was greater in old needles than in young ones. This differentiation presumably reflects an earlier onset of nitrogen reallocation in needles of the declining stand. ¹⁵N values in twigs were more negative than in needles (-3.5 to-5.2) and showed age- and stand-dependent trends that were similar to the needles. ¹⁵N values of roots and soil samples increased at both stands with soil depth from-3.5 in the organic layer to +4 in the mineral soil. The ¹⁵N values of roots from the mineral soil were different from those of twigs and needles. Roots from the shallower organic layer had values similar to twigs and needles. Thus, the bulk of the assimilated nitrogen was presumably taken up by the roots from the organic layer. The problem of separation of ammonium or nitrate use by roots from different soil horizons is discussed.     

Evidence suggesting energy-dependent formaldehyde transport in an RuMP-type methylotroph (T15)

Formaldehyde accumulation ratios ([¹⁴CH₂O]_i/[¹⁴CH₂O]_o) as high as 12-fold were measured in anaerobic, CH₃OH-energized, whole cell suspensions of the ribulose monophosphate (RuMP)-type methylotrophic strain T15. Uptake kinetics were extremely rapid, enabling the attainment of equilibrium in only 10–30 s. Transport appears to be energy-dependent and associated with the protonmotive force (pmf). Anaerobic incubation with 5 M carbonyl p-(trifluoromethoxy)-phenylhydrazone (FCCP) led to 70%–90% reduction of the accumulation ratio. Though not as pronounced, diminished uptake was also observed in the presence of 140 M nigericin, 161 M valinomycin and 90 mM KSCN, commensurate with their effects on pmf. Accumulation of CH₂O as a function of external pH followed a trend more similar to that of pmf than either pH or . Preventing energization by incubation with 100 M N,N-dicyclohexylcarbodiimide (DCCD) led to nearly 80% inhibition of CH₂O transport. Over short time periods it was possible to chase accumulated ¹⁴CH₂O from previously loaded cells by collapsing pmf; however, this technique also indicated that significant ¹⁴CH₂O incorporation began to occur within 3 min.Abbreviations FCCP Carbonyl cyanide p-(trifluoromethyoxy)-phenylhydrazone - DCCD N,N-dicyclohexylcarbodiimide - RuMP ribulose monophosphate - TPP⁺ tetra[U-¹⁴C]phenylphosphonium - pmf protonmotive force     

Interpretation of sulfur cycling in two catchments in the Black Forest (Germany) using stable sulfur and oxygen isotope data

The isotopic composition of SO ₄ ^2- in bulk precipitation, canopy throughfall, seepage water at three different soil depths, stream water, and groundwater was monitored in two forested catchments in the Black Forest (Germany) between November 1989 and February 1992. Isotope measurements on aqueous sulfate were complemented by ³⁴S-analyses on SO₂ in the air, total sulfur and inorganic sulfate in the soil, and bedrock sulfur, in order to identify sources and biogeochemical processes affecting S cycling in catchments with base poor, siliceous bedrock. Stable S isotope data indicated that atmospheric deposition and not mineral weathering is the major source of S in both catchments since ³⁴S-values for sulfate in the soil, in seepage water, and in stream water were generally found to be similar to the mean ³⁴S-values of precipitation SO ₄ ^2- (+2.1. However, ¹⁸O-values of seepage water SO ₄ ^2- at 30 cm and especially at 80 cm depth were depleted by several per mil with respect to those of the atmospheric deposition (+7.5 to +13.5. This indicates that in both catchments a considerable proportion of the seepage water SO ₄ ^2- is derived from mineralization of carbon-bonded soil S and must therefore have cycled through the organic soil S pool. ³⁴S-values for different S compounds in the solid soil were found to differ markedly depending on S fraction and soil depth. Since atmospheric S deposition with rather constant ³⁴S-values was identified as the dominant S source in both catchments, this is interpreted as a result ofin situ isotope fractionation rather than admixture of isotopically different S. The differences between the ³⁴S-values of seepage water and soil sulfate and those of organic soil S compounds are consistent with a model in which SO ₄ ^2- uptake by vegetation and soil microorganisms favours³⁴SO ₄ ^2- slightly, whereas during mineralization of organic soil S to aqueous SOSO ₄ ^2- ,³²S reacts preferentially. However, the data provide evidence for negligible isotope fractionation during physico-chemical S transformations such as adsorption/desorption in aerated forest soils.     

Partitioning of water and nitrogen in co-occurring Mediterranean woody shrub species of different evolutionary history

We studied the interspecific and intraspecific variation in the development of water stress and in the use of different water and nitrogen sources during the spring (wet season) and summer (dry season) in a shrub community in NE Spain. We measured shoot water potentials, stable deuterium isotopic composition (D) of xylem sap, leaf mass per area, leaf N and C concentrations, gas exchange, leaf ¹³C, and leaf ¹⁵N of the dominant species (Quercus coccifera, Arbutus unedo, Pistacia lentiscus, Erica multiflora, Globularia alypum). The D, the ¹³C and the shoot water potential values showed diurnal, seasonal, intraspecific and interspecific variation in the source and use of water. There was also seasonal, intraspecific and interspecific variation in the foliar ¹⁵N and N concentrations. In summer, some species (A. unedo, P. lentiscus and E. multiflora) presented significantly different D values in morning and afternoon measurements likely indicating that they used different sources of water during the day, and a dual root system in these species. We conjecture that dew may be one of these water sources. Species predawn water potential was negatively correlated with species xylem water D. There was also a positive correlation between ¹³C and D in P. lentiscus, species for which we took additional samples from nearby sites. These results suggest that the access to water from greater depths allowed the maintenance of more favourable plant water supply. Multivariate principal component analysis based on the studied hydrological and isotope variables clearly separated the seasons (wet spring and dry summer) and the species. The species resulted separated according to their evolutionary history (Pre-Mediterranean and Mediterranean) and the associated root and functional traits. These results show water (and nitrogen) partitioning among coexisting species of the same functional type (Mediterranean woody shrubs). They also show the great intraspecific plasticity of responses to resource availability.     

Stable isotopic composition of otoliths from tagged Pacific halibut, Hippoglossus stenolepis

Data from tagging studies and stable isotope ratio analyses (¹⁸O and ¹³C) in otoliths of tagged Pacific halibut, Hippoglossus stenolepis, provided unique information about halibut distribution and area migration. The ¹⁸O values of otoliths of individual halibut tagged in the Bering Sea and the Gulf of Alaska ranged from –0.5 to +1.0 VPDB (Vienna Peedee belemnite) in the first few years, but gradually increased to 2.0–2.5 VPDB when these tagged fish were recaptured as adults in waters off British Columbia. Similar isotopic variations were found in ¹³C. Comparison of isotopic composition from the age-1 halibut (i.e., aragonite samples taken from the first annulus of otoliths) and the adult (ages 8) indicated that the ocean conditions between the Bering Sea and the northeast Pacific were markedly different over the tagging period, but the area boundaries between the Gulf of Alaska and British Columbia were not clear. We concluded that stable isotopic records in otoliths of tagged Pacific halibut were informative and particularly useful for details of subsequent movement of halibut between release and recovery.     

Carbon and nitrogen dynamics along the decay continuum: Plant litter to soil organic matter

Decay processes in an ecosystem can be thought of as a continuum beginning with the input of plant litter and leading to the formation of soil organic matter. As an example of this continuum, we review a 77-month study of the decay of red pine (Pinus resinosa Ait.) needle litter. We tracked the changes in C chemistry and the N pool in red pine (Pinus resinosa Ait.) needle litter during the 77-month period using standard chemical techniques and stable isotope, analyses of C and N.Mass loss is best described by a two-phase model: an initial phase of constant mass loss and a phase of very slow loss dominated by degradation of lignocellulose (acid soluble sugars plus acid insoluble C compounds). As the decaying litter enters the second phase, the ratio of lignin to lignin and cellulose (the lignocellulose index, LCI) approaches 0.7. Thereafter, the LCI increases only slightly throughout the decay continuum indicating that acid insoluble materials (lignin) dominate decay in the latter part of the continuum.Nitrogen dynamics are also best described by a two-phase model: a phase of N net immobilization followed by a phase of N net mineralization. Small changes in C and N isotopic composition were observed during litter decay. Larger changes were observed with depth in the soil profile.An understanding of factors that control lignin degradation is key to predicting the patterns of mass loss and N dynamics late in decay. The hypothesis that labile C is needed for lignin degradation must be evaluated and the sources of this C must be identified. Also, the hypothesis that the availability of inorganic N slows lignin decay must be evaluated in soil systems.     

Effect of organic and inorganic fertigation on yields, δ15N values, and δ13C values of tomato (Lycopersicon esculentum Mill. cv. Saturn)

We examined the effects of fertilizer application, especially the effects of fertigation and types of fertilizer (inorganic and organic) on yields and ¹⁵N and ¹³C values of tomato (Lycopersicon esculentum Mill. cv. Saturn). Fertigation is a method in which an appropriate diluted liquid fertilizer is applied to the plants each time they are drip-irrigated. We developed a method of organic fertigation using corn steep liquor (CSL) as the liquid fertilizer, because it is an industrial byproduct of cornstarch manufacture and can be used very effectively. We compared fruit yield, mineral content, ¹⁵N value, and ¹³C value of tomatoes grown under three different fertilizer treatments, basal dressing: basal dressing with granular chemical fertilizer; inorganic fertigation: fertigation with liquid chemical fertilizer; and organic fertigation: fertigaion with CSL. Mineral contents of tomatoes grown with basal dressing were generally lower than those grown under either fertigation treatment. These results indicated that yields and mineral contents were influenced more by the method of fertilizer application than by whether the fertilizers were inorganic or organic. There were, however, significant differences in the ¹⁵N values of tomato fruits grown under different types of fertilizer applications, especially between inorganic and organic fertilizers. The ¹⁵N value of the chemical fertilizer used for basal dressing was 0.81 ± 0.45{}, that of the chemical fertilizer for fertigation was 0.00 ± 0.04{}, and that of CSL was 8.50 ± 0.71{}. The ¹⁵N values of the soils reflected the ¹⁵N values of the fertilizers. Moreover, the ¹⁵N values of the fruits corresponded to the ¹⁵N values of the applied fertilizers. The ¹⁵N values were 3.18 ± 1.34{} in the fruits grown with a basal dressing of chemical fertilizer, 0.30 ± 0.61 in those grown under inorganic fertigation, and 7.09 ± 0.68 in those grown under organic fertigation. On the other hand, although the ¹³C values in the soil also reflected the ¹³C values of the applied fertilizers, there was no significant difference in the ¹³C values of fruits among the different treatments. In conclusion, because the ¹⁵N values of fertilizers correlated well with those of the fruits, it may be possible to use ¹⁵N values as an indicator of organic products.     

Polymerization of nucleotide analogues I: Reaction of nucleoside 5′-phosphorimidazolides with 2′-amino-2′-deoxyuridine

Summary 2-Amino-2-deoxyuridine reacts efficiently with nucleoside 5-phosphorimidazolides in aqueous solution. The dinucleoside monophosphate analogues were obtained in yields exceeding 80% under conditions in which little reaction occurs with the natural nucleosides.In a similar way, the 5-phosphorimidazolide of 2-amino-2-deoxyuridine undergoes self-condensation in aqueous solution to give a complex mixture of oligomers.The phosphoramidate bond in the dinucleoside monophosphate analogues is stable for several days at room temperature and pH 7. The mechanisms of their hydrolysis under acidic and alkaline conditions are described.Abbreviations A adenosine - C cytidine - G guanosine - U uridine - T thymidine - U_{N 3} 2-azido-2-deoxyuridine - U_{NH 2} 2-amino-2-deoxyuridine - ImpA adenosine 5-phosphorimidazolide - ImpU uridine 5-phosphorimidazolide - ImpU_{N 3} 2-azido-2-deoxyuridine 5-phosphorimidazolide - ImpU_{NH 2} 2-amino-2-deoxyuridine 5-phosphorimidazolide - pA adenosine 5-phosphate - pU uridine 5-phosphate - pU_{N 3} 2-azido-2-deoxyuridine 5-phosphate - pU_{NH 2} 2-amino-2-deoxyuridine 5-phosphate - UpA uridylyl-[35]-adenosine - UpU uridylyl-[35]-uridine - U_NpA adenylyl-[52]-2-amino-2-deoxy-uridine - U_NpU uridylyl-[52]-2-amino-2-deoxyuridine (pU_N)_n n=2,3,4 [25]-linked oligomers of pU_{NH 2} poly(A) polyadenylic acid - Im imidazole - MeIm l-methylimidazole     

Whole Leaf Thermoluminescence Emission in Pisum Sativum L.: Influence of Leaflet Age

The thermoluminescence signals from leaflets of the same pea plant varied gradually according to their developmental stage. The AG emission, due to a back flow of electrons towards photosystem 2 (PS2) along a cyclic/chlororespiratory pathway, was stronger in mature leaves than in the growing ones. These age-related variations could be explained by a higher capacity of cyclic electron flow in mature leaves.     

Variation in stable isotope signatures of seston and a zooplanktivorous fish in a eutrophic Chinese lake

Temporal and spatial changes in ¹³C and ¹⁵N of seston (mainly phytoplankton) and isotopic relationship between seston and the lake anchovy (Coilia ectenes) were studied in the large eutrophic freshwater Lake Chaohu in China. Much of the spatial and temporal variation in ¹³C of lake anchovies was explained by variation in seston, indicating a strong link between pelagic primary production and higher order consumers. Because the lake is shallow, there were no significant differences in ¹³C and ¹⁵N of seston between surface and overlying waters. Spatially, the relatively high ¹³C and ¹⁵N of seston in the western part of the lake might be due to high levels of anthropogenically derived N and C introduced from the surrounding cities through sewage drainage systems. The trophic position of the lake anchovy in the food web of Lake Chaohu was estimated to be 2.9–4.1 (3.5 ± 0.4), which agrees well with the previous stomach content analysis suggesting that the lake anchovy fed both on zooplankton and small planktivorous fishes.     

Conformationally constrained opioid peptide analogs with novel activity profiles

Novel conformationally constrained opioid peptide analogs with antagonist, mixed agonist/ antagonist or agonist properties were developed. TIP(P)-related antagonists showed unprecedented antagonist potency and receptor selectivity, and may have potential for use in analgesia in combination with agonists. A definitive model of their receptor-bound conformation was developed. Three prototype mixed agonist/ antagonists were discovered. They represent the only known compounds with this pharmacological profile and, as expected, one of them was shown to be a potent analgesic and to produce no dependence and less tolerance than morphine. Novel dipeptide derivatives turned out to be potent and selective agonists. Because of their low molecular weight and lipophilic character, these compounds may cross the blood-brain barrier and, thus, may have potential as centrally acting analgesics.     

Influence of temperature on energetics of hydrogen metabolism in homoacetogenic,methanogenic, and other anaerobic bacteria

Hydrogen consumption by various thermophilic, mesophilic and/or psychrotrophic homoacetogens and methanogens was measured at temperatures between 4 and 80°C. Within the tolerated temperature range H₂ was consumed until a final H₂ threshold partial pressure was reached. H₂ thresholds generally decreased with temperature, parallel to the values calculated from the thermodynamics prevailing under culture conditions, i.e. the Gibbs free energy (G) of H₂ oxidation corrected for temperature by both the free-energy form of the Nernst equation and the Van't Hoff equation. The difference between the observed and the calculated H₂ partial pressures gives the minimum energy required for H₂ utilization being about-5 to-6 kJ/mol H₂ for the homoacetogenes and-9 to-12 kJ/mol H₂ for methanogens. The temperature dependence of the standard Gibbs free energy (G⁰) as described by the Van't Hoff equation apparently became the more important for thermodynamics as well as H₂ thresholds the more the temperature deviated from standard conditions (i.e. 25°C). Correction factors for calculation of temperature-corrected G _infT ^sup0 are presented for various H₂-producing and H₂-consuming reactions.     

Unification of two methods for measuring the amount of nitrogen fixed by a legume crop

Summary Two methods for measuring nitrogen fixation, the so-called A value method and the so-called isotope dilution or substrate labelling method are shown to be both unifiable and yield independent.     

Seasonal Stable Isotope Records of Otoliths from Ocean-pen Reared and Wild Cod, Gadus morhua

Otoliths of ocean-pen reared cod, Gadus morhua, provide a unique opportunity to examine the lifetime history of the fish. Here we report 18 analyses of such otoliths on seasonal (winter and summer) stable oxygen and carbon isotope ratios. The calculated isotopic temperatures from otoliths of reared cod were essentially in agreement with the temperature record during rearing, suggesting that temperature is a dominant factor in the precipitation of otolith aragonite. Carbon isotope ratios increased with age and leveled off at 4 years old, presumed to correlate with sexual maturity of cod. As compared with otoliths of wild-caught cod, significant differences were found in isotope variation and the correlation between ¹³C and ¹⁸O. These differences were probably attributable to the different environmental constraints and food supply.     

Membranotropic effects of peptides from the V3 loop of HIV-1

The V3 loop from HIV-1 envelope glycoprotein gp120 is involved in viral entry and determines the cellular tropism and HIV-1-induced cell–cell fusion. Earlier we have shown that V3 loop peptides representing the sequences of syncytia-inducing HIV strains have high membranotropic activity. These peptides caused the lysis of liposomes of various lipid compositions, could fuse negatively charged liposomes and induced hemolysis of erythrocytes. In contrast, peptides mimicking the sequences of non-syncytia-inducing viruses showed no lytic or fusion activities at the same concentrations. Now we have found that the V3 loop synthetic peptides containing the conserved GPGR region, derived from T-lymphotropic strains (BRU and MN), as opposed to peptides containing the GPGQ region, are able to cause a pronounced membrane permeabilization (dissipation of the pH and the of human peripheral blood lymphocytes, erythrocytes and plasma membrane vesicles at micromolar concentrations with a dose-dependent kinetics. Analysis of the secondary structures of the peptides by circular dichroism revealed conformational changes in V3 loop peptides depending on solvent hydrophobicity: from random coil in water to an -helix/-sheet conformation in trifluoroethanol. Such structural changes of the V3 loop together with the membrane insertion of the gp41 N-terminal fusion peptide may promote the formation of the fusion pore during virus–cell fusion.     

Interferons up-regulate with different potency HLA class I antigen expression in M14 human melanoma cell line. Possible interaction with glucocorticoid hormones

The relative potency of interferon (IFN), interferon (IFN), and interferon (IFN) in inducing the expression of HLA class I antigens, as well as their capacity to counteract the inhibition induced by glucocorticoid hormones on HLA class I antigen expression, were analysed in the human melanoma cell line M14, both at membrane and at mRNA level. The data obtained indicate that (a) IFN enhance with different potency (IFN>IFN>IFN) the expression of HLA class I antigens in M14 cells, (b) prednisone inhibits HLA class I antigen expresion, (c) glucocorticoid hormones, when associated with IFN or IFN, inhibit the HLA class I enhancement induced by IFN alone, and ffinally, (c) the association between 1 M prednisone or 1 M deflazacort and IFN seems to potentiate the enhancing capacity of IFN on the expression of HLA class I molecules at the mRNA level. These findings, if confirmed, might indicate that IFN and glucocorticoid hormones are not mutually exclusive in the management of human melanoma.