Intracellular Ca indicator Quin-2 inhibits Ca2+ inflow via Na/Ca exchange in squid axon

Until recently, intracellular free calcium has been amenable to measurement and investigation only in cells large enough to permit either microinjection of a suitable Ca sensor such as a aequorin or arsenazo III or insertion of a Ca-sensitive microelectrode. This constraint on cell size was removed by the development of the fluorescent Ca2+ -sensitive dye Quin-2 and its acetoxymethyl ester, which can be introduced into a wide range of cell types. A major requirement of any intracellular Ca2+ indicator is that it should not disturb intracellular Ca2+ homeostasis and Quin-2 is generally considered to be satisfactory in this respect. We now report that injection of Quin-2 into squid (Loligo forbesi) axons can almost completely abolish one component of Ca2+ entry--intracellular Na+ (Nai)-dependent Ca2+ inflow, which occurs via Na/Ca exchange. Mixtures of Ca and Quin-2 that buffer an ionized Ca2+ at close to physiological concentrations also block Nai-dependent Ca2+ influx but these same mixtures fail to block the extracellular Na+ (Na0)-dependent extrusion of Ca2+, showing that Quin-2 acts specifically on Ca2+ inflow.     

Genetic basis of BCG-induced suppression of delayed hypersensitivity

BCG can either act as an adjuvant to potentiate immunological responses or, in some cases, can induce suppression. The reasons for these differential activities are not clear but may include routes and doses of administration, as well as variable host reactivity to the agent. In this study, we have used killed BCG administered intravenously to produce chronic granulomatous inflammation (CGI) in the lungs and spleen of inbred mice. We report that strains which develop CGI were usually anergic, as evaluated by the development of delayed hypersensitivity (DH) to sheep erythrocytes (SRBC). Studies on the genetics of BCG-induced anergy indicated that it was unigenic, recessive and linked (approximately 28 recombination units) to the immunoglobulin heavy-chain allotype (Igh). There was no influence by genes linked to the major histocompatibility complex. The study indicates that anergy associated with CGI is under genetic control, which may explain the variability of anergy in patients with granulomatous diseases. The implication of linkage to the Igh complex is not clear, but it may be associated with VH receptors on T lymphocytes, which in turn act on macrophages to mediate suppression.     

Changes in intracellular pH and cell volume during the early phase of DMSO-induced differentiation of Friend erythroleukemia cells

Changes in intracellular pH and water volume were measured after treatment of Friend erythroleukemia cells with 1.5% DMSO. It was found that a continuous decrease in pHi occurred, beginning 1 h after induction and a decline in pHi of 0.18 was measured after 9 h. In addition a decline in cellular water volume, of 12% only 15 min after induction, and 23% after 9 h, was observed.     

Capacity of purified Lyt-2+ T cells to mount primary proliferative and cytotoxic responses to Ia- tumour cells

Allogeneic gene products of the major histocompatibility complex, the HLA complex in man and the H-2 complex in mice, induce T lymphocytes to exert powerful mixed lymphocyte reactions (MLR) and cell-mediated lympholysis (CML). In mice, the subset of T cells carrying the L3T4 surface antigen but lacking the Lyt-2 antigen responds predominantly to H-2 class II (Ia) differences whereas the L3T4- Lyt-2+ subset reacts to class I (K/D) differences. For primary responses the stimulus for MLR and CML appears to be controlled by Ia+ cells of the macrophage/dendritic cell lineages, for both L3T4+ and Lyt-2+ cells. The finding that Ia+ cells are required for responses involving Lyt-2+ cells has been taken to imply that triggering of these cells is controlled by Ia-restricted L3T4+ cells. Lyt-2+ cells have thus come to be regarded as crippled cells which are heavily dependent on 'help' from other T cells. This well-entrenched view is challenged by evidence presented here that purified Lyt-2+ cells can give high primary responses to certain Ia- tumour cells in vitro.     

Scaling metabolism from organisms to ecosystems

Understanding energy and material fluxes through ecosystems is central to many questions in global change biology and ecology. Ecosystem respiration is a critical component of the carbon cycle and might be important in regulating biosphere response to global climate change. Here we derive a general model of ecosystem respiration based on the kinetics of metabolic reactions and the scaling of resource use by individual organisms. The model predicts that fluxes of CO2 and energy are invariant of ecosystem biomass, but are strongly influenced by temperature, variation in cellular metabolism and rates of supply of limiting resources (water and/or nutrients). Variation in ecosystem respiration within sites, as calculated from a network of CO2 flux towers, provides robust support for the model's predictions. However, data indicate that variation in annual flux between sites is not strongly dependent on average site temperature or latitude. This presents an interesting paradox with regard to the expected temperature dependence. Nevertheless, our model provides a basis for quantitatively understanding energy and material flux between the atmosphere and biosphere.     

Development of anisotropic structure in the Earth's lower mantle by solid-state convection

Seismological observations reveal highly anisotropic patches at the bottom of the Earth's lower mantle, whereas the bulk of the mantle has been observed to be largely isotropic. These patches have been interpreted to correspond to areas where subduction has taken place in the past or to areas where mantle plumes are upwelling, but the underlying cause for the anisotropy is unknown-both shape-preferred orientation of elastically heterogeneous materials and lattice-preferred orientation of a homogeneous material have been proposed. Both of these mechanisms imply that large-strain deformation occurs within the anisotropic regions, but the geodynamic implications of the mechanisms differ. Shape-preferred orientation would imply the presence of large elastic (and hence chemical) heterogeneity whereas lattice-preferred orientation requires deformation at high stresses. Here we show, on the basis of numerical modelling incorporating mineral physics of elasticity and development of lattice-preferred orientation, that slab deformation in the deep lower mantle can account for the presence of strong anisotropy in the circum-Pacific region. In this model-where development of the mineral fabric (the alignment of mineral grains) is caused solely by solid-state deformation of chemically homogeneous mantle material-anisotropy is caused by large-strain deformation at high stresses, due to the collision of subducted slabs with the core-mantle boundary.     

A 20-km-diameter multi-ringed impact structure in the North Sea

Most craters found on Earth are highly eroded, poorly preserved and only exposed on land. Here we describe a multi-ringed impact structure discovered in the North Sea from the analysis of three-dimensional seismic reflection data. The structure is 20 km in diameter, and has at least ten distinctive concentric rings located between 2 and 10 km from the crater centre. The structure affects Cretaceous chalk and Jurassic shales, and is well preserved below several hundred metres of post-impact Tertiary strata, which constrains its age to be 60-65 Myr old. The formation of concentric ringed impact structures at this relatively small scale had not previously been thought possible, especially on the terrestrial planets. We have mapped the ring structures at a resolution of tens of metres both laterally and in depth, and show that the rings are fault-bounded graben structures, similar to fault arrays formed in low-strain-rate detachment tectonic settings. Strata deeper than 500 m palaeodepth appear unfaulted, and we infer that the concentric ring structures may have accommodated post-impact extension towards the excavated crater, through detachment on weak layers within the chalk.     

Involvement of DARPP-32 phosphorylation in the stimulant action of caffeine

Caffeine has been imbibed since ancient times in tea and coffee, and more recently in colas. Caffeine owes its psychostimulant action to a blockade of adenosine A(2A) receptors, but little is known about its intracellular mechanism of action. Here we show that the stimulatory effect of caffeine on motor activity in mice was greatly reduced following genetic deletion of DARPP-32 (dopamine- and cyclic AMP-regulated phosphoprotein of relative molecular mass 32,000). Results virtually identical to those seen with caffeine were obtained with the selective A(2A) antagonist SCH 58261. The depressant effect of the A(2A) receptor agonist, CGS 21680, on motor activity was also greatly attenuated in DARPP-32 knockout mice. In support of a role for DARPP-32 in the action of caffeine, we found that, in striata of intact mice, caffeine increased the state of phosphorylation of DARPP-32 at Thr 75. Caffeine increased Thr 75 phosphorylation through inhibition of PP-2A-catalysed dephosphorylation, rather than through stimulation of cyclin-dependent kinase 5 (Cdk5)-catalysed phosphorylation, of this residue. Together, these studies demonstrate the involvement of DARPP-32 and its phosphorylation/dephosphorylation in the stimulant action of caffeine.