A novel role for interleukin 2 in antibody responses: down-regulation of T helper cell activation

This report provides new insights into the role of the T cell growth factor interleukin 2 (IL 2) for the regulation of antibody responses. Evidence is presented that IL 2 down-regulates T helper cell (Thc) activation but not Thc effector function, i.e., Thc-B cooperation. Thus, reagents which block the IL 2 pathway, e.g., cyclosporin A (CsA) or IL 2 receptor monoclonal antibodies (IL 2R Mab) enhanced Thc activation although T cell proliferation was blocked. In contrast, CsA or IL 2R Mab blocked Thc-B cooperation, suggesting that IL 2 is required for this step. The regulatory role of IL 2 was reconfirmed by the addition of exogenous IL 2 into the cultures which reversed the enhancing or blocking effect of CsA.     

SOS Chromotest study concerning some appreciation criteria of humic substances' genotoxic potency

The genotoxicity of 5 compounds: 2 fulvic acids, a trade humic acid, a synthetic humic material (SHM), and 2,5-dihydroxybenzoic acid, was assessed after chlorination, by means of the SOS Chromotest for tester strain E. coli PQ 37 without metabolic activation. Chlorination was carried out for humic material concentration of 0.5 mg total organic carbon per liter, and chlorine concentrations in the range of 0.1-2.0 chlorine equivalents per mole of carbon. Among all the considered criteria that can account for potent toxicity: chemical degradation determined by the UV absorption decrease, chlorine consumption, average molecular weight, only the polymerization index (O.D. 665 nm/O.D. 465 nm) can be related to the genotoxicity of humic samples. This latter criterion appears a possible predictor of genotoxic potency, revealed subsequent to the aqueous chlorination of humic materials. Looking at the various genotoxic activities of the tested compounds, SHM can be considered a better model of natural humic materials than the trade humic acid.     

Duration of retained fetal membranes and subsequent fertility in dairy cows

Lactations from 1,111 heifers and 2,493 cows were evaluated for the effects of the duration of retained fetal membranes on subsequent fertility. Cows or heifers with metritis, ovarian cyst, both metritis and cyst, or neither were evaluated in separate strata in order to control for the effects of parity, metritis, and cyst on fertility. Duration of retention had no effect on fertility if an animal had metritis or cyst. There was a suggestion that retained fetal membranes in heifers free of metritis and cyst decreased conception rate at first service. In multiparous cows free of metritis and cyst there was a significant decrease in conception rate at first service when retention exceeded 5 days, and delays of +18 days to 1st service and +57 days to conception when retention exceeded 7 days.     

Stages of tubulin assembly and disassembly studied by time-resolved synchrotron X-ray scattering

The structural transitions occurring during the assembly and disassembly of pig brain microtubule protein were investigated by time-resolved X-ray scattering using synchrotron radiation. The reactions were introduced by a slow temperature scan (2 deg.C/min) from 0 °C to 37 °C and back. Several structurally distinct states could be resolved during one cycle of assembly/disassembly. During the temperature rise, one observes four main phases: prenucleation events, microtubule nucleation, growth, and postassembly events.Heating from 0 °C to 22 °C results in a biphasic breakdown of rings and other aggregates, while the apparent mean diameter increases from 38 to 41 nm. Parallel time-resolved electron microscopic observations suggest that the initial solution contains several types of aggregates, mostly double concentric and single rings, but also rod-like particles, clusters of rings and other aggregates. All of these tend to break down with increasing temperature. Double concentric rings seem to dissociate into large and small single rings before both types of rings break down into protofilament fragments and tubulin subunits. From the breakdown products, associations of several protofilament fragments are formed, which are important for initiating microtubule nucleation. Assembly of nuclei begins around 22 °C. Microtubule elongation takes place between 25 and 30 °C. They grow mainly by addition of tubulin subunits but not via rings.During the reverse temperature scan, microtubules shorten by the release of subunits and/or small protofilament fragments from their ends. The degree of disassembly is strongly increased below 22 °C. Below about 10 °C rings are reformed, probably from the fragments, but their final number is much less than initially.Conditions that prevent microtubule nucleation such as GDP or Ca²⁺ also stabilize rings, even at 37 °C. Thus, rings are viewed as storage aggregates of tubulin and microtubule associated proteins, whose breakdown is a prerequisite for microtubule formation, and whose reformation is independent of microtubule breakdown.The midpoints of microtubule growth and breakdown differ by about 12 deg.C so that the system shows hysteresis-like behavior. It is dependent on microtubule formation and is not seen when the temperature is cycled below that required for nucleation. Thus, even during a slow temperature scan, microtubule assembly is kinetically limited by nucleation. By contrast, depolymerization proceeds close to equilibrium.The radius of gyration of the tubulin heterodimers is 3.1 nm. The weight average diameter of rings in cold solutions is 38 nm, that of microtubules is 24.5 nm.At radiation dose rates of about 100 rad/s. radiation damage is of minor importance, as judged by the criterion of polymerizability. Total doses of up to 500,000 rad can be applied.Some concepts of analyzing time-resolved X-ray scattering data are presented. They make use of the fact that the scattering intensities vary continuously both with scattering angle and time. Cross-correlation of different regions of the pattern, and comparison of their temperature derivatives, reveals structural transitions not seen by other techniques.     

Evaluation of Ia+ tumor cell lines and peritoneal exudate macrophages as accessory cells: differential requirements for the activation of certain T cell functions

Several Ia+ (BC3A, TA3, D1B) or Ia-inducible (WEHI-3, P388D1) tumor lines were tested for accessory cell function for the activation of antigen-specific T cell proliferation and for the induction of T helper cells that help B cells in antibody production. All lines were able to induce antigen-specific T cell proliferation in an MHC-restricted way, but none activated T helper cells to soluble antigens under all conditions tested. In comparison, starch-induced peritoneal exudate macrophages induced T cell proliferation as well as T cell help. Some of the lines tested induced nonspecific suppressor cells that were Ly-2-positive and partially or completely inhibited antibody responses. The induction of suppressor cells, however, is not the reason for the failure of the tumor lines to activate T helper cells. These data indicate that antigen-specific T cell proliferation and helper activity do not necessarily correlate.     

Assay of free-radical toxicity and antioxidant effect on the Hep 3B cell line: a test survey using lindane

The content of reduced glutathione and of glutathione disulfide as well as the activities of glutathione reductase, glutathione peroxidase, glutathione S-transferases, catalase and superoxide dismutases were determined in human hepatoma Hep 3B cells in relation to free-radical toxicity in order to appreciate the defense capacities of these cells compared to data on normal hepatocytes. When Hep 3B cells were exposed to lindane, a known inducer of free-radical production, superoxide dismutase activity appeared as the best-adapted cellular parameter for early detection of the resulting free-radical toxicity.Abbreviations AAS atomic absorption spectrometry - CDNB 1-chloro-2,4-dinitrobenzene - DMEM Dulbecco's modified Eagle medium - GPx glutathione peroxidase - G.Red glutathione reductase - GSH reduced glutathione - GSSG glutathione disulfide - GST glutathione S-transferases - Prot proteins - SOD superoxide dismutase     

Human appropriation of net primary production as driver of change in landscape-scale vertebrate richness

Aim

Land use is the most pervasive driver of biodiversity loss. Predicting its impact on species richness (SR) is often based on indicators of habitat loss. However, the degradation of habitats, especially through land-use intensification, also affects species. Here, we evaluate whether an integrative metric of land-use intensity, the human appropriation of net primary production, is correlated with the decline of SR in used landscapes across the globe.

Location

Global.

Time period

Present.

Major taxa studied

Birds, mammals and amphibians.

Methods

Based on species range maps (spatial resolution: 20 km × 20 km) and an area-of-habitat approach, we calibrated a “species–energy model” by correlating the SR of three groups of vertebrates with net primary production and biogeographical covariables in “wilderness” areas (i.e., those where available energy is assumed to be still at pristine levels). We used this model to project the difference between pristine SR and the SR corresponding to the energy remaining in used landscapes (i.e., SR loss expected owing to human energy extraction outside wilderness areas). We validated the projected species loss by comparison with the realized and impending loss reconstructed from habitat conversion and documented by national Red Lists.

Results

Species–energy models largely explained landscape-scale variation of mapped SR in wilderness areas (adjusted R²-values: 0.79–0.93). Model-based projections of SR loss were lower, on average, than reconstructed and documented ones, but the spatial patterns were correlated significantly, with stronger correlation in mammals (Pearson's r = 0.68) than in amphibians (r = 0.60) and birds (r = 0.57).

Main conclusions

Our results suggest that the human appropriation of net primary production is a useful indicator of heterotrophic species loss in used landscapes, hence we recommend its inclusion in models based on species–area relationships to improve predictions of land-use-driven biodiversity loss.     

Phyto- and protozooplankton biomass during austral summer in surface waters of the Weddell Sea and vicinity

Summary Phyto- and protozooplankton were sampled in the upper 10 m of the water column in austral summer during a cruise of RV Polarstern from January 6 to February 20 1985 in the eastern Bransfield Strait vicinity and in the northern, southeastern (off Vestkapp, twice: I and II) and southern Weddell Sea (Vahsel Bay across the Filchner Depression to Gould Bay). The plankton assemblages are discussed in relation to physical, chemical and biological factors in the different geographical areas in summer. Phytoplankton biomass (Phytoplankton carbon, PPC) ranged from 4–194 g carbon/l and consisted on average of 65% diatoms and 35% autotrophic flagellates. Whereas in the northwest phytoplankton assemblages were dominated by small nanoflagellates (78% of PPC), higher biomass of diatoms (54–94% of PPC) occurred at the other sampling sites. In general autotrophic flagellates and small pennate diatoms dominated at oceanic stations; in neritic areas large centric diatoms prevailed. Chlorophyll a concentrations ranged from 0.25–3.14/g chl a/l with a mean of 1.13/gmg chlorophyll a/l and an average phytoplankton carbon/chlorophyll a ratio of 39. Protozooplankton biomass (Protozooplankton carbon, PZC) ranged from 0–67 g carbon/l and consisted of 49% ciliates, 49% heterotrophic dinoflagellates and 2% tintinnids. Heterotrophic dinoflagellates were more important in the northern investigation areas (58%–84% of PZC). Ciliates dominated the protozooplankton in the southeast and south (56%–65% of PZC); higher abundances of tintinnids were observed only in the south (11% of PZC). The most remarkable feature of the surface waters was the high protozooplankton biomass: protozooplankton amounted to 25% on an average of the combined biomass of PPC plus PZC for the entire investigation period. Protozoan biomass in the southeastern and southern Weddell Sea occasionally exceeded phytoplankton biomass. Temperature, salinity, and inorganic nutrients were generally lower in the southern regions; at most of these stations a meltwater layer occurred in the upper meters of the water column. We suggest that this physical regime allows a well developed summer system with a high proportion of heterotrophic microplankton. In the eastern Bransfield Strait, in the northern Weddell Sea and close to the coast off Vestkapp (I), however, early summer conditions occurred with less protozooplankton contribution.Contribution no. 427 from the Alfred-Wegener-Institute for Polar and Marine Research