Interactions among oscillatory pathways in NF-kappa B signaling

Background  

Sustained stimulation with tumour necrosis factor alpha (TNF-alpha) induces substantial oscillations—observed at both the single cell and population levels—in the nuclear factor kappa B (NF-kappa B) system. Although the mechanism has not yet been elucidated fully, a core system has been identified consisting of a negative feedback loop involving NF-kappa B (RelA:p50 hetero-dimer) and its inhibitor I-kappa B-alpha. Many authors have suggested that this core oscillator should couple to other oscillatory pathways.     

Adsorption of ethylenediaminetetraacetic dianhydride modified oxalate decarboxylase on calcium oxalate

We used ethylenediaminetetraacetic acid dianhydride (EDTAD) to modify oxalate decarboxylase (OXDC) to improve its adsorption on calcium oxalate stones. The modified sites were identified by Ultra performance liquid chromatography-mass spectrometry (UPLC-MS) and the adsorption mechanism of the EDTAD-modified OXDC on calcium oxalate (CaOx) was investigated. We investigated adsorption time, initial enzyme concentration, temperature and solution pH on the adsorption process. Data were analyzed using kinetics, thermodynamics and isotherm adsorption models. UPLC-MS showed that EDTAD was attached to OXDC covalently and suggested that the chemical modification occurred at both the free amino of the side chain and the α-NH₂ of the peptide. The adsorption capacity of the EDTAD-OXDC on calcium oxalate was 53.37% greater than that of OXDC at the initial enzyme concentration of 5 mg/ml, pH = 7.0, at 37° C. The modified enzyme (EDTAD-OXDC) demonstrated improved oxalate degradation activity at pH 4.5?6.0. Kinetic data fitting analysis suggested a pseudo second order kinetic model. Estimates of the thermodynamic parameters including ΔG⁰, ΔH⁰ and ΔS⁰ of the adsorption process showed it to be feasible, spontaneous and endothermic. Isotherm data fitting analysis indicated that the adsorption process is reduced to monolayer adsorption at a low enzyme concentration and to multilayer adsorption at a high enzyme concentration. It may be possible to apply OXDC to degradation of calcium oxalate stones.     

Mitochondrial DNA structure and colony expansion dynamics of New Zealand fur seals (Arctocephalus forsteri) around Banks Peninsula

New Zealand fur seals are one of many pinniped species that survived the commercial sealing of the eighteenth and nineteenth centuries in dangerously low numbers. After the enforcement of a series of protection measures in the early twentieth century, New Zealand fur seals began to recover from the brink of extinction. We examined the New Zealand fur seal populations of Banks Peninsula, South Island, New Zealand using the mitochondrial DNA control region. We identified a panmictic population structure around Banks Peninsula. The most abundant haplotype in the area showed a slight significant aggregated structure. The Horseshoe Bay colony showed the least number of shared haplotypes with other colonies, suggesting a different origin of re-colonisation of this specific colony. The effective population size of the New Zealand fur seal population at Banks Peninsula was estimated at approximately 2500 individuals. The exponential population growth rate parameter for the area was 35, which corresponds to an expanding population. In general, samples from adjacent colonies shared 4.4 haplotypes while samples collected from colonies separated by between five and eight bays shared 1.9 haplotypes. The genetic data support the spill-over dynamics of colony expansion already suggested for this species. Approximate Bayesian computations analysis suggests re-colonisation of the area from two main clades identified across New Zealand with a most likely admixture coefficient of 0.41 to form the Banks Peninsula population. Approximate Bayesian computations analysis estimated a founder population size of approximately 372 breeding individuals for the area, which then rapidly increased in size with successive waves of external recruitment. The population of fur seals in the area is probably in the late phase of maturity in the colony expansion dynamic.     

Effect of hydrocarbon concentration of pasture production (<i>Brachiaria humidicola</i>) in Texistepec,Veracruz

In this study, the relationship between the concentration of extra-heavy crude petroleum in a clayey material and the toxicity, field capacity, temperature, and growth of a tropical forage grass (Brachiara humidicola) was determined empirically. For this type of petroleum the acute toxicity (Microtox^®) was slight (CE₅₀ = 63200 - 76400 mg/kg) even at high hydrocarbon concentrations (29279 mg/kg). Nonetheless, serious impacts were encountered in terms of an increase in soil temperature (+ 1.3 °C), reduction in field capacity (-10.7%) and reduction in aerial biomass (-97%). The relationship between hydrocarbon concentration and biomass resulted in a typical dose-response curve (r = 0.99), where a concentration of 2626 mg/kg of hydrocarbons corresponds to a maintenance of 90% biomass. Furthermore, during the duration of this study (one year) the biodegradation was proportional to the pasture biomass production (r = 0.997) indicating a synergistic relationship between the petroleum biodegrading microorganisms in the rhizosphere and the pasture.     

ARS replication during the yeast S phase

A 1.45 kb circular plasmid derived from yeast chromosome IV contains the autonomous replication element called ARS1. Isotope density transfer experiments show that each plasmid molecule replicates once each S phase, with initiation depending on two genetically defined steps required for nuclear DNA replication. A density transfer experiment with synchronized cells demonstrates that the ARS1 plasmid population replicates early in the S phase. The sequences adjacent to ARS1 on chromosome IV also initiate replication early, suggesting that the ARS1 plasmid contains information which determines its time of replication. The times of replication for two other yeast chromosome sequences, ARS2 and a sequence referred to as 1OZ, indicate that the temporal order of replication is ARS1 leads to ARS2 leads to 1OZ. These experiments show directly that specific chromosome regions replicate at specific times during the yeast S phase. If ARS elements are origins of chromosome replication, then the experiment reveals times of activation for two origins.     

Fertilization alters the spatial distribution and the density of voltage-dependent sodium current in the egg of the ascidian Boltenia villosa

The spatial distribution of voltage-dependent ionic currents was characterized in Boltenia villosa eggs before and after fertilization using two-microelectrode voltage clamp of paired animal-vegetal halves of eggs (merogones) made surgically. Major voltage-dependent conductances in the Boltenia egg are a transient inward Na current, a transient inward Ca current, and an inwardly rectifying K current. These currents were randomly distributed along the animal-vegetal axis in the unfertilized egg. When paired merogones (surgically prepared egg fragments) were made at the vegetal cap stage, 15-30 min after fertilization, Ca and K currents remained randomly distributed along the animal-vegetal axis. In contrast, the relative Na current density was found to be twofold lower in the vegetal vs the animal merogones made at the vegetal cap stage. By making pairs of merogones from unfertilized eggs and subsequently fertilizing one merogone of a pair, we showed that this change in current density ratio was due to a loss of absolute Na current density in the vegetal hemisphere shortly after fertilization. These results also show that this loss was intrinsic to the vegetal hemisphere, rather than being determined solely by the point of sperm entry. A second decrease in Na current was observed during the hour before first cleavage, 60-120 min after fertilization (M.L. Block and W.J. Moody, 1987, J. Physiol. 393, 619-634), both in fertilized eggs and in animal merogones fertilized after isolation. This second loss of Na current was not observed in vegetal merogones fertilized after isolation or in either animal or vegetal merogones made from fertilized eggs at the vegetal cap stage. Possible mechanisms for te rapid (complete by 40 min after fertilization) and the late (occurring from ca. 60 to 120 minutes after fertilization) Na current losses are discussed.