Refuge availability and sequence of predators determine the seasonal succession of crustacean zooplankton in a clay-turbid lake

The contribution of predators and abiotic factors to the regulation of the biomass and seasonal succession of crustacean zooplankton was studied in Lake Rehtijärvi (southern Finland). Field data in combination with bioenergetics modeling indicated that invertebrate planktivory by Chaoborus depressed cladoceran populations during early summer. In particular, bosminids that generally form the spring biomass peak of cladocerans in stratified temperate lakes did not appear in the samples until July. In July, predation pressure by chaoborids was relaxed due to their emergence period and cladoceran population growth appeared to be limited by predation by planktivorous fish. The effect of fish predation was amplified by reduced refuge availability for cladocerans. The concentration of dissolved oxygen below the epilimnion was depleted, forcing cladocerans to move upward to less turbid and thus more dangerous water layers. The effect of size selective predation by fish resulted in reduced mean size of cladocerans during the period when refuge thickness (thickness of the water layer with oxygen concentration <1 mg l^?1 and water turbidity >30 NTU) was lowest. The results confirmed that in clay-turbid lakes, invertebrate predators could be the main regulators of herbivorous zooplankton even when cyprinid fish are abundant.     

Methyl-β-cyclodextrin Suppresses Hyaluronan Synthesis by Down-regulation of Hyaluronan Synthase 2 through Inhibition of Akt

Hyaluronan synthases (HAS1–3) are integral plasma membrane proteins that synthesize hyaluronan, a cell surface and extracellular matrix polysaccharide necessary for many biological processes. It has been shown that HAS is partly localized in cholesterol-rich lipid rafts of MCF-7 cells, and cholesterol depletion with methyl-β-cyclodextrin (MβCD) suppresses hyaluronan secretion in smooth muscle cells. However, the mechanism by which cholesterol depletion inhibits hyaluronan production has remained unknown. We found that cholesterol depletion from MCF-7 cells by MβCD inhibits synthesis but does not decrease the molecular mass of hyaluronan, suggesting no major influence on HAS stability in the membrane. The inhibition of hyaluronan synthesis was not due to the availability of HAS substrates UDP-GlcUA and UDP-GlcNAc. Instead, MβCD specifically down-regulated the expression of HAS2 but not HAS1 or HAS3. Screening of signaling proteins after MβCD treatment revealed that phosphorylation of Akt and its downstream target p70S6 kinase, both members of phosphoinositide 3-kinase-Akt pathway, were inhibited. Inhibitors of this pathway suppressed hyaluronan synthesis and HAS2 expression in MCF-7 cells, suggesting that the reduced hyaluronan synthesis by MβCD is due to down-regulation of HAS2, mediated by the phosphoinositide 3-kinase-Akt-mTOR-p70S6K pathway.     

Fluxes of nitrous oxide from boreal peatlands as affected by peatland type,water table level and nitrification capacity

Peat soils with high nitrogen content are potential sources of nitrous oxide (N₂O). Fluxes of nitrous oxide were measuredin situ on nine virgin and ten drained peatlands of different hydrology and nutrient status. Numbers of nitrifying bacteria were estimated in different layers of the peat profiles with a most-probable-number technique. Nitrification potentials were determined in soil slurries of pH 4 and 6 from the profiles of six peat soils. Many virgin peatlands showed low N₂O uptake. Lowering of the water table generally increased the average fluxes of N₂O from the soils, although more in minerotrophic (nutrient rich) than in ombrotrophic (nutrient poor) sites. Ammonium oxidizing bacteria were found on only two sites but nitrite oxidizers were detected in almost all peat profiles. More nitrite oxidizers were found in drained than in virgin peat profiles. Nitrification was enhanced after lowering of the water table in minerotrophic peat but not in ombrotrophic peat. The N₂O fluxes correlated positively with the numbers of nitrite oxidizers, nitrification potential, N, P and Ca content and pH of the soil and negatively with the level of water table (expressed as negative values) and K content of the soil.     

Demethylation of 3-methylthymine in DNA by bacterial and human DNA dioxygenases

Rare DNA lesions that are chemically stable and refractory to repair may add disproportionately to the accumulation of mutations in long lived cells. 3-Methylthymine is a minor lesion that is induced by DNA-methylating agents and for which no repair process has been described previously. Here we demonstrate that this lesion can be directly demethylated in vitro by bacterial and human DNA dioxygenases. The Escherichia coli AlkB and human ABH3 proteins repaired 3-methylthymine in both single-stranded and double-stranded polydeoxynucleotides, whereas the human ABH2 protein preferred a duplex substrate. Thus, the known substrates of these enzymes now include 3-methylthymine in DNA, as well as 1-methyladenine and 3-methylcytosine, which all have structurally similar sites of alkylation. Repair of 3-methylthymine by AlkB and ABH3 was optimal at pH 6, but inefficient. At physiological pH, 3-methylthymine, which is a minor methylated lesion, was more slowly repaired than the major lesion generated in single-stranded DNA, 3-methylcytosine. Our data suggest that 3-methylthymine residues in DNA will be repaired inefficiently in vivo and therefore may occur at a low steady-state level, but the residues should not gradually accumulate to high levels in long lived cells.     

Caspase multiplexing: simultaneous homogeneous time-resolved quenching assay (TruPoint) for caspases 1, 3, and 6

Caspases are a group of cysteine proteases involved in apoptosis and inflammation. A multiparametric homogeneous assay capable of measuring activity of three different caspases in a single well of a microtiter plate is described. Different fluorescent europium, samarium, terbium, and dysprosium chelates were coupled to a caspase substrate peptide, their luminescence properties, were analyzed, and their function in a time-resolved fluorescence quenching-based caspase 3 assay was studied. Substrates for caspases 1, 2, 3, 6, and 8 and granzyme B were also synthesized and their specificities for different caspases were determined. By selecting suitable lanthanide chelates and substrates we developed a multiparametric homogeneous time-resolved fluorescence quenching-based assay for caspases 1, 3, and 6. The assay was capable of measuring the activity of both single caspases and a mixture of three caspases mixed in the same well.     

Functional properties of Pfr(Tic)amide and BIBP3226 at human neuropeptide FF2 receptors

The functional characteristics of two putative neuropeptide FF (NPFF) antagonists, BIBP3226 and PFR(Tic)amide, on the human neuropeptide FF receptor subtype 2 (hNPFF2) were investigated. Surprisingly, PFR(Tic)amide was shown to exhibit agonist properties in the [³⁵S]guanosine-5′-O-(3-thio)triphosphate ([³⁵S]GTPγS) binding assay. The efficacy of PFR(Tic)amide was significantly greater than that of (1DMe)Y8Fa, a stable analog of NPFF, and PFR(Tic)amide can therefore be classified as a ‘super-agonist’. BIBP3226 did act as a reversible competitive antagonist on the hNPFF2 receptor. However, high concentrations of BIBP3226 also non-specifically increased [³⁵S]GTPγS binding. The usefulness of BIBP3226 as an antagonist tool on the NPFF receptor is thus limited.     

Minimal methylated substrate and extended substrate range of Escherichia coli AlkB protein,a 1-methyladenine-DNA dioxygenase

The Escherichia coli AlkB protein, and two human homologs ABH2 and ABH3, directly demethylate 1-methyladenine and 3-methylcytosine in DNA. They couple Fe(II)-dependent oxidative demethylation of these damaged bases to decarboxylation of alpha-ketoglutarate. Here, we have determined the kinetic parameters for AlkB oxidation of 1-methyladenine in poly(dA), short oligodeoxyribonucleotides, nucleotides, and nucleoside triphosphates. Methylated poly(dA) was the preferred AlkB substrate of those tested. The oligonucleotide trimer d(Tp1meApT) and even 5'-phosphorylated 1-me-dAMP were relatively efficiently demethylated, and competed with methylated poly(dA) for AlkB activity. A polynucleotide structure was clearly not essential for AlkB to repair 1-methyladenine effectively, but a nucleotide 5' phosphate group was required. Consequently, 1-me-dAMP(5') was identified as the minimal effective AlkB substrate. The nucleoside triphosphate, 1-me-dATP, was inefficiently but actively demethylated by AlkB; a reaction with 1-me-ATP was even slower. E. coli DNA polymerase I Klenow fragment could employ 1-me-dATP as a precursor for DNA synthesis in vitro, suggesting that demethylation of alkylated deoxynucleoside triphosphates by AlkB could have biological significance. Although the human enzymes, ABH2 and ABH3, demethylated 1-methyladenine residues in poly(dA), they were inefficient with shorter substrates. Thus, ABH3 had very low activity on the trimer, d(Tp1meApT), whereas no activity was detected with ABH2. AlkB is known to repair methyl and ethyl adducts in DNA; to extend this substrate range, AlkB was shown to reduce the toxic effects of DNA damaging agents that generate hydroxyethyl, propyl, and hydroxypropyl adducts.     

Short-term effects of changing water table on N2O fluxes from peat monoliths from natural and drained boreal peatlands

The effect of the water table on nitrous oxide (N₂O) fluxes from peat profiles representing boreal peatlands of differing nutrient status was studied in the laboratory. Lowering of the water table in peat monoliths taken from two natural waterlogged peatlands for 14 weeks in a greenhouse at 20 °C increased the fluxes of N₂O, an effect that was enhanced further by incubation in the dark. Raising of the water table in monoliths from two drained and forested peatlands caused cessation of the N₂O fluxes from the drained peats, which had previously been sources of N₂O. It is known that N₂O fluxes have increased in peatlands drained several decades ago. The results suggest that it is not necessary for the water table to be lowered for several years to change a boreal peatland from a N₂O sink to a source of the gas. In addition to the draining of peatlands, climate change can be expected to lower ground water levels during the summertime in the boreal zone, and this could cause marked changes in N₂O fluxes from boreal peatlands by enhancing the microbial processes involved in nitrogen transformations.