Macroinvertebrate stream communities along regional and physico-chemical gradients in Western Greenland

1. Macroinvertebrates were collected and physico‐chemical variables measured at 16 stream sites in Western Greenland during July 1999. Eight sites were located on Disko Island in an arctic oceanic climate and eight sites in the Kangerlussuaq area close to the icecap where the climate is arctic continental. The streams had different water sources (glacial, groundwater, snowmelt and lake water). 2. The streams showed pronounced differences in water temperature (2.2–17.3 °C), concentrations of suspended solids (0–2400 mg L^?1), and conductivity (10–109 μS cm^?1). Principal component analysis (PCA) analysis of the physico‐chemical variables separated the Disko Island sites into a distinct group, whereas the sites in the Kangerlussuaq area were more dispersed. 3. A total of 56 macroinvertebrate species were found, including 31 species of Chironomidae, the most abundant of which was Orthocladius thienemanni. Diamesa sp. was only the sixth most abundant chironomid taxon. Species composition varied between sites, and abundance varied from about 20 individuals m^?2 in a glacier fed stream to more than 16 000 m^?2 in a lake outlet. 4. The macroinvertebrate communities of the 16 streams were separated into five TWINSPAN groups reflecting water source, irrespective of region. Lake outlets and ground‐water‐fed streams had the highest species richness and abundance, temperature and bed stability, while glacier‐fed streams were characterized by low species richness, abundance, temperature, bed stability and high concentrations of suspended solids. Macroinvertebrate species richness was positively correlated with water temperature and negatively with bed stability. Conductivity was positively correlated with invertebrate abundance. 5. The results of this study suggest that the source of stream water can be used to predict invertebrate community composition in Greenlandic streams and thus the effects of changes in water balance and flow regime, and to identify sites of special conservation interest.     

Characterization of PKC2, a gene encoding a second protein kinase C isotype of Saccharomyces cerevisiae

BACKGROUND: Protein kinase C (PKC) has attracted considerable attention over the past decade, primarily because of its presumed role in cellular growth control and tumourigenesis. Mammalian cells express at least 10 different isozymes of PKC; it is this complexity that has made elucidating the precise functions of PKC: so difficult. The identification of PKC homologues in organisms such as Drosophila, Xenopus, Dictyostelium, Aplysia and Caenorhabditis indicates that the enzyme is evolutionarily conserved, and this has stimulated our search for counterparts in the yeast Saccharomyces cerevisiae, in which powerful genetic analyses can be used. To date, only one PKC homologue, PKC1, has been identified in yeast and no biochemical activity has been definitively ascribed to the encoded protein. This, and the inability to identify other PKC homologues in yeast by DNA hybridization, has led to doubts about the existence of PKC isozymes in yeast. We have taken the approach of screening yeast expression libraries with anti-PKC antibodies in an attempt to identify further homologues. RESULTS: We have identified a novel PKC isozyme, Pkc2p, encoded by the gene PKC2. We report here the sequence of PKC2 and a comparison showing its similarity to other PKCs. Phylogenetic analysis suggests that all known PKC genes, including PKC2, originated from a common ancestor. Disruption of the PKC2 protein-coding region, deleting the entire catalytic domain of the encoded enzyme, is not lethal to yeast growing on rich media. However, the pkc2 mutant, unlike wild-type strains, fails to grow on minimal media containing limited concentrations of amino acids. This implicates Pkc2p in the response of yeast cells to amino-acid starvation. CONCLUSION: We have shown that yeast cells do express more than one PKC isozyme, by identifying and characterizing a novel PKC gene PKC2, the product of which may be involved in the cellular response to amino-acid starvation.     

Pleistophora oncoperae sp.n. (Protozoa: Microsporida) from Oncopera alboguttata (Lepidoptera: Hepialidae) in Australia

Pleistophora oncoperae sp.n. is described from adults and larvae of Oncopera alboguttata and O. rufobrunnea. The main site of infection was muscle, though fat body and connective tissue were also infected. Fresh pansporoblasts measured about 25 μm in diameter and contained 16 to 32 or more spores with a mean size of 5.9 × 3.1 μm. Macrospores measuring 7.7 × 4.4 μm were also seen. The mean polar filament length was 158 μm; ultrastructural studies showed that the filament is normally arranged in 14 coils (range, 13 to 20) at an angle of 53.5° to the axis of the spore. The species was found to be distinct from all previously described Pleistophora reported from Lepidoptera.     

Decline in Ecosystem <Emphasis Type="Italic">δ</Emphasis><Superscript>13</Superscript>C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence

Uncertainty about controls on long-term carbon (C) and nitrogen (N) balance, turnover, and isotopic composition currently limits our ability to predict ecosystem response to disturbance and landscape change. We used a two-century, postglacial chronosequence in Glacier Bay, Alaska, to explore the influence of C and N dynamics on soil and leaf stable isotopes. C dynamics were closely linked to soil hydrology, with increasing soil water retention during ecosystem development resulting in a linear decrease in foliar and soil δ¹³C, independent of shifts in vegetation cover and despite constant precipitation across sites. N dynamics responded to interactions among soil development, vegetation type, microbial activity, and topography. Contrary to the predictions of nutrient retention theory, potential nitrification and denitrification were high, relative to inorganic N stocks, from the beginning of the chronosequence, and gaseous and hydrological N losses were highest at mid-successional sites, 140–165 years since deglaciation. Though leaching of dissolved N is considered the predominant pathway of N loss at high latitudes, we found that gaseous N loss was more tightly correlated with δ¹⁵N enrichment. These results suggest that δ¹³C in leaves and soil can depend as much on soil development and associated water availability as on climate and that N availability and export depend on interactions between physical and biological state factors.     

Microglia are the major source of TNF-α and TGF-β1 in postnatal glial cultures; regulation by cytokines,lipopolysaccharide, and vitronectin

Damage to the central nervous system (CNS) leads to increased production of TNF-α and TGF-β1 cytokines that have pro- or anti-inflammatory actions, respectively. To define whether astrocytes or microglia express these cytokines, prior studies have used mixed glial cultures (MGC) to represent astrocytes, thought these results are inevitably complicated by the presence of contaminating microglia within MGC. To clarify the cellular source of these cytokines, here we employed a recently described method of preparing microglia-free astrocyte cultures, in which neural stem cells (NSC) are differentiated into astrocytes. Using ELISA to quantify cytokine production in three types of glial culture: MGC, pure microglia or pure astrocytes, this showed that microglia but not astrocytes, produce TNF-α, and that this expression is increased by LPS, IFN-γ, and to a lesser extent by vitronectin, but decreased by TGF-β1. In contrast, TGF-β1 was produced by microglia and astrocytes, though at 10-fold higher levels by microglia. TGF-β1 expression in microglia was increased by vitronectin and to a lesser extent by TNF-α and LPS, but astrocyte TGF-β1 expression was not regulated by any factor tested. In summary, our data reveal that microglia, not astrocytes are the major source of TNF-α and TGF-β1 in postnatal glial cultures, and that microglial production of these antagonistic cytokines is tightly regulated by cytokines, LPS, and vitronectin.     

Possible identity of a membrane-bound with a soluble cyclic AMP-independent erythrocyte protein kinase that phosphorylates spectrin

A soluble casein kinase isolated and purified to homogeneity from the human erythrocyte cytosol by phosphocellulose and Sephadex G-200 chromatographies is indistinguishable from the membrane-bound casein (spectrin) kinase according to physical and site-specificity criteria. The soluble enzyme shows an Mr of about 30000 by gel filtration and comigrates with the purified membrane spectrin kinase as a single polypeptide of 32000 Da on sodium dodecyl sulfate polyacrylamide gels. The soluble kinase phosphorylates spectrin in situ in spectrin kinase-depleted ghosts and catalyzes the in vitro phosphorylation of partially dephosphorylated spectrin with saturation kinetics identical to those displayed by the membrane spectrin kinase. When component 2 of spectrin that had been phosphorylated with [gamma-32P]ATP by either the soluble or the membrane kinases was subjected to limited proteolysis, the same 21500 Da papain-generated phosphopeptide was found to have been produced by the two enzymes. The same 21500 Da phosphopeptide was identified after papain digestion of spectrin isolated from intact cells that had been incubated with 32Pi. However, this particular peptide was not labeled in spectrin that had been phosphorylated in vitro by the catalytic subunit of cyclic AMP-dependent protein kinase. Identical phosphopeptide patterns were obtained by gel filtration and two-dimensional peptide maps of trypsin-cleaved component 2 of spectrin that had been labeled in situ, in intact ghosts or in spectrin kinase-depleted ghosts supplemented with the soluble kinase. These findings indicate a possible identity of the soluble with the membrane-bound casein (spectrin) kinase.