Effect of bacterial density and substrate concentration on yield coefficients.

Measurements were made of the yield coefficient during the aerobic metabolism of glucose by a heterogeneous bacterial mixture. Expressed in terms of carbon, the coefficient was approximately 0.48. The value did not vary with initial bacterial densities ranging from 0.4 pg to 40 micrograms of cell carbon per ml and with glucose concentrations ranging from 43 pg to 100 micrograms of carbon per ml. Under all these circumstances, about 44% of the glucose carbon was converted to CO2, and 7.4% was excreted as organic products. The significance of uncharacterized organic substrates contaminating the medium to the coefficients calculated for low glucose concentrations is discussed.     

Kinetics of mineralization of phenols in lake water.

The kinetics of mineralization of phenol and p-nitrophenol in lake water was determined at concentrations from 200 pg/ml to 5 micrograms/ml. The mineralization data were fit by nonlinear regression to equations for 14 kinetic models that describe patterns of biodegradation by nongrowing cells or by microorganisms growing on either the test chemical or other organic substrates. The kinetics od mineralization of phenol in water samples collected in July was best described by first-order models for 0.5 ng of phenol per ml; by Monod-without-growth, logistic, and logarithmic models for 1.0 and 2.0 ng/ml and 5.0 ng/ml to 1.0 micrograms/ml, respectively, if it is assumed that the mineralizing population uses phenol as the sole carbon source for growth; by models (for phenol at concentrations of 2.0 ng/ml to 1.0 micrograms/ml) that assume that the phenol-mineralizing populations do not grow or grow logarithmically or logistically on uncharacterized carbon compounds but metabolize the phenol when present at levels below and above Km, respectively, for that compound; and by a logarithmic model at 5.0 micrograms/ml. Under the test conditions, usually less than 10% of the phenol C that was metabolized was incorporated into microbial cells or retained by other particulate material in the water at substrate concentrations of 10 ng/ml or less, and the percentage increased at higher substrate concentrations.(ABSTRACT TRUNCATED AT 250 WORDS)     

Kinetics of mineralization of phenols in lake water

The kinetics of mineralization of phenol and p-nitrophenol in lake water was determined at concentrations from 200 pg/ml to 5 micrograms/ml. The mineralization data were fit by nonlinear regression to equations for 14 kinetic models that describe patterns of biodegradation by nongrowing cells or by microorganisms growing on either the test chemical or other organic substrates. The kinetics od mineralization of phenol in water samples collected in July was best described by first-order models for 0.5 ng of phenol per ml; by Monod-without-growth, logistic, and logarithmic models for 1.0 and 2.0 ng/ml and 5.0 ng/ml to 1.0 micrograms/ml, respectively, if it is assumed that the mineralizing population uses phenol as the sole carbon source for growth; by models (for phenol at concentrations of 2.0 ng/ml to 1.0 micrograms/ml) that assume that the phenol-mineralizing populations do not grow or grow logarithmically or logistically on uncharacterized carbon compounds but metabolize the phenol when present at levels below and above Km, respectively, for that compound; and by a logarithmic model at 5.0 micrograms/ml. Under the test conditions, usually less than 10% of the phenol C that was metabolized was incorporated into microbial cells or retained by other particulate material in the water at substrate concentrations of 10 ng/ml or less, and the percentage increased at higher substrate concentrations.(ABSTRACT TRUNCATED AT 250 WORDS)     

Rates of Mineralization of Trace Concentrations of Aromatic Compounds in Lake Water and Sewage Samples

The rates of mineralization of phenol, benzoate, benzylamine, p-nitrophenol, and di(2-ethylhexyl) phthalate added to lake water at concentrations ranging from a few picograms to nanograms per milliliter were directly proportional to chemical concentration. The rates were still linear at levels of <1 pg of phenol or p-nitrophenol per ml, but it was less than the predicted value at 1.53 pg of 2,4-dichlorophenoxyacetate per ml. Mineralization of 2,4-dichlorophenoxyacetate was not detected in samples of lake water containing 200 ng of the chemical per ml. The slope of a plot of the rate of phenol mineralization in samples of three lakes as a function of its initial concentration was lower at levels of 1 to 100 μg/ml than at higher concentrations. In lake water and sewage supplemented with <60 ng of ¹⁴C-labeled benzoate or phenylacetate per ml, 95 to 99% of the radioactivity disappeared from solution, indicating that the microflora assimilated little or none of the carbon. The extent of mineralization of some compounds in samples of two lakes and sewage was least in the water with the lowest nutrient levels. No mineralization of 2,4-dichlorophenoxyacetate and the phthalate ester was observed in samples of an oligotrophic lake. These data suggest that mineralization of some chemicals at concentrations of <1 μg/ml is the result of activities of organisms different from those functioning at higher concentrations or of organisms that metabolize the chemicals at low concentrations but assimilate little or none of the substrate carbon.     

Anomalies in mineralization of low concentrations of organic compounds in lake water and sewage

The rates of mineralization of nitrilotriacetic acid (NTA), 2,4-dichlorophenoxyacetic acid (2,4-D), p-nitrophenol, aniline, and isopropyl N-phenylcarbamate (IPC) at one or more concentrations ranging from 100 pg/ml to 1.0 microgram/ml were proportional to chemical concentrations in samples of three lakes. The rates at 100 pg of NTA, 2,4-D, p-nitrophenol, and aniline per ml in samples of one or more lakes were less than predicted, assuming the rates were linearly related to the concentration. Neither NTA nor 2,4-dichlorophenol at 2.0 ng/ml was mineralized in some lake waters, but higher levels of the two chemicals were converted to CO2 in samples of the same waters. In samples from two lakes, little or no mineralization of IPC or 2,4-D occurred at 1.0 microgram/ml, but 10 ng/ml or lower levels of the herbicides were mineralized. The mineralization in sewage of 1.0 microgram of NTA per ml was biphasic; about 20% of the substrate was mineralized in 20 h, and mineralization was only reinitiated after a period of 130 h. The biphasic transformation was not a result of the accumulation of organic products, and it was still evident if protozoan activity was inhibited. NTA also underwent a biphasic mineralization in lake waters, and the biphasic pattern was not altered by additions of growth factors and inorganic nutrients. From 40 to 60% of the carbon of aniline added to lake water at levels of 100 pg/ml to 1.0 microgram/ml was mineralized, but more than 90% of the carbon of NTA, 2,4-D, or p-nitrophenol added to lake water at 10 ng/ml or 1.0 microgram/ml was mineralized.(ABSTRACT TRUNCATED AT 250 WORDS)     

Anomalies in mineralization of low concentrations of organic compounds in lake water and sewage.

The rates of mineralization of nitrilotriacetic acid (NTA), 2,4-dichlorophenoxyacetic acid (2,4-D), p-nitrophenol, aniline, and isopropyl N-phenylcarbamate (IPC) at one or more concentrations ranging from 100 pg/ml to 1.0 microgram/ml were proportional to chemical concentrations in samples of three lakes. The rates at 100 pg of NTA, 2,4-D, p-nitrophenol, and aniline per ml in samples of one or more lakes were less than predicted, assuming the rates were linearly related to the concentration. Neither NTA nor 2,4-dichlorophenol at 2.0 ng/ml was mineralized in some lake waters, but higher levels of the two chemicals were converted to CO2 in samples of the same waters. In samples from two lakes, little or no mineralization of IPC or 2,4-D occurred at 1.0 microgram/ml, but 10 ng/ml or lower levels of the herbicides were mineralized. The mineralization in sewage of 1.0 microgram of NTA per ml was biphasic; about 20% of the substrate was mineralized in 20 h, and mineralization was only reinitiated after a period of 130 h. The biphasic transformation was not a result of the accumulation of organic products, and it was still evident if protozoan activity was inhibited. NTA also underwent a biphasic mineralization in lake waters, and the biphasic pattern was not altered by additions of growth factors and inorganic nutrients. From 40 to 60% of the carbon of aniline added to lake water at levels of 100 pg/ml to 1.0 microgram/ml was mineralized, but more than 90% of the carbon of NTA, 2,4-D, or p-nitrophenol added to lake water at 10 ng/ml or 1.0 microgram/ml was mineralized.(ABSTRACT TRUNCATED AT 250 WORDS)     

Growth of phenol-mineralizing microorganisms in fresh water.

A method was developed to enumerate the procaryotic and eucaryotic phenol-mineralizing microorganisms present in samples of fresh water. Sixty-five percent or greater mineralization of [U-14C]phenol was considered a positive tube (contained phenol-mineralizing microorganisms) in the most-probable-number technique. Replicate most-probable-number tubes contained no microbial inhibitors, streptomycin and tetracycline, or cyclohexamide and nystatin plus 200 pg to 100 micrograms of phenol per ml. Phenol mineralization rates were obtained by measuring the amount of exogenous phenol that disappeared from solution over time in the presence or absence of the microbial inhibitors. Initially, less than 100 phenol-mineralizing bacteria per ml and 1 phenol-mineralizing fungus per ml were present at both 200 pg and 100 micrograms of phenol per ml. Phenol mineralization rates were 6.3 times greater for the mineralizing bacteria than for the fungi at 200 pg of phenol per ml. Phenol concentrations above 10 micrograms/ml were inhibitory to the microorganisms capable of mineralizing phenol. The phenol mineralizers grew in the water samples in the absence of phenol, indicating that there were sufficient indigenous nutrients in the lake water to support growth. There was no difference in the growth rate of these microorganisms in the presence or absence of 1 ng of phenol per ml, whereas the growth rate was more rapid at 1 microgram of phenol per ml than in its absence. There was a correlation between microbial growth and the amount of phenol mineralized at 1 microgram but not at 1 ng of phenol per ml.(ABSTRACT TRUNCATED AT 250 WORDS)     

Growth of phenol-mineralizing microorganisms in fresh water

A method was developed to enumerate the procaryotic and eucaryotic phenol-mineralizing microorganisms present in samples of fresh water. Sixty-five percent or greater mineralization of [U-14C]phenol was considered a positive tube (contained phenol-mineralizing microorganisms) in the most-probable-number technique. Replicate most-probable-number tubes contained no microbial inhibitors, streptomycin and tetracycline, or cyclohexamide and nystatin plus 200 pg to 100 micrograms of phenol per ml. Phenol mineralization rates were obtained by measuring the amount of exogenous phenol that disappeared from solution over time in the presence or absence of the microbial inhibitors. Initially, less than 100 phenol-mineralizing bacteria per ml and 1 phenol-mineralizing fungus per ml were present at both 200 pg and 100 micrograms of phenol per ml. Phenol mineralization rates were 6.3 times greater for the mineralizing bacteria than for the fungi at 200 pg of phenol per ml. Phenol concentrations above 10 micrograms/ml were inhibitory to the microorganisms capable of mineralizing phenol. The phenol mineralizers grew in the water samples in the absence of phenol, indicating that there were sufficient indigenous nutrients in the lake water to support growth. There was no difference in the growth rate of these microorganisms in the presence or absence of 1 ng of phenol per ml, whereas the growth rate was more rapid at 1 microgram of phenol per ml than in its absence. There was a correlation between microbial growth and the amount of phenol mineralized at 1 microgram but not at 1 ng of phenol per ml.(ABSTRACT TRUNCATED AT 250 WORDS)     

Evidence for suppression of serum LH without elevation in serum estradiol or prolactin with a brain-enhanced redox delivery system for estradiol

We developed a redox system for brain-enhanced delivery of estradiol based on an interconvertible dihydropyridine in equilibrium pyridinium salt carrier. Estradiol (E2), when combined with the lipoidal carrier, readily crosses the blood-brain barrier. The carrier, when oxidized, reduces the rate of exit of the estradiol-carrier complex from the brain. Subsequent hydrolysis of the carrier provides sustained production of estradiol in the brain. The aim of the study was to evaluate the effects of single vs. multiple injections of the estradiol-chemical delivery system (E2-CDS) on both central and peripheral estrogen-responsive tissues. Ovariectomized Sprague-Dawley rats received an intravenous injection of E2-CDS at 10, 33, 100 or 333 micrograms/kg BW or the drug vehicle, dimethyl sulfoxide (DMSO; 0.5 ml/kg) every 2 days for 7 injections (2 weeks) or a single injection only at 2 days before sacrifice. With a single injection, E2-CDS did not affect serum luteinizing hormone (LH) levels at the 10 micrograms/kg dose but caused a dose-dependent reduction in serum LH of 39-52% at the dose range of 33 to 333 micrograms/kg. By contrast, multiple injections of E2-CDS caused a 32 to 76% reduction in serum LH levels at doses ranging from 10 micrograms/kg to 333 micrograms/kg. Additionally, multiple doses of E2-CDs caused a dose-dependent reduction in body weight at the 10 and 33 micrograms/kg doses with the higher doses causing no further weight reduction. For both single and multiple dosage groups, serum E2 levels remained unchanged after doses of E2-CDS of 10 and 33 micrograms/kg, then increased to 21 pg/ml for the single dosage group and to 23 pg/ml for the multiple dosage group at the 100 micrograms/kg dose, and to 59 pg/ml for singly-injected rats and 60 pg/ml for multiply-injected rats at the 333 micrograms/kg dose. Serum prolactin concentrations were closely correlated with serum E2 levels for both the single and multiple dose groups. These data reveal that a single or multiple doses of E2-CDS can reduce serum LH levels without elevating serum E2 or prolactin concentrations, supporting the concept of brain-enhanced delivery of estradiol with an estradiol chemical delivery system.     

Effect of estradiol and relaxin on growth of fibroblastic cells isolated from guinea pig mammary glands

Fibroblasts were isolated from the mammary glands of guinea pigs and grown in 96-well culture plates. They were treated with a factorial arrangement of porcine relaxin (0.0, 0.5, 1.0 or 1.5 micrograms/ml) and estradiol-17 beta (0, 200, 400 or 600 pg/ml). Tritiated thymidine or uridine was added to a final activity of 25 nCi per well and the cells incubated at 37 degrees C for 48 h. Cells were then harvested onto filter paper and counted for tritium. Controls (0.0 micrograms/ml relaxin and 0 pg/ml estradiol) incorporated 3.7 nCi of tritiated thymidine and 4.8 nCi tritiated uridine. Both relaxin and estradiol altered the incorporation of thymidine and uridine. There was also an interaction between the two hormones. Thymidine incorporation with no estradiol and 1.5 micrograms/ml relaxin was 129% of controls. The optimum incorporation of thymidine occurred with 0.5 micrograms/ml relaxin and 400 pg/ml estradiol. This combination of hormones gave a response of 145% of controls. Uridine incorporation followed a different pattern. Relaxin alone at a concentration of 1.5 micrograms/ml gave a near-optimum response of 141% of control. The optimum combination of relaxin and estradiol for uridine incorporation was 1.5 micrograms/ml relaxin and 400 pg/ml estradiol, which gave a response of 156% of controls. These data indicated that relaxin and estradiol alter DNA and RNA synthesis in mammary fibroblasts and thus may be important in controlling the growth of the mammary gland stroma.     

Kinetics and Extent of Mineralization of Organic Chemicals at Trace Levels in Freshwater and Sewage

A sensitive and rapid method was developed to measure the mineralization of ¹⁴C-labeled organic compounds at picogram-per-milliliter or lower levels in samples of natural waters and sewage. Mineralization was considered to be equivalent to the loss of radioactivity from solutions. From 93 to 98% of benzoate, benzylamine, aniline, phenol, and 2,4-dichlorophenoxyacetate at one or more concentrations below 300 ng/ml was mineralized in samples of lake waters and sewage, indicating little or no incorporation of carbon into microbial cells. Assimilation of ¹⁴C by the cells mineralizing benzylamine in lake water was not detected. Mineralization in lake waters was linear with time for aniline at 5.7 pg to 500 ng/ml, benzylamine at 310 ng/ml, phenol at 102 fg to 10 mg/ml, 2,4-dichlorophenoxyacetate at 1.5 pg/ml, and di-(2-ethylhexyl) phthalate at 21 pg to 200 ng/ml, but it was exponential at several p-nitrophenol concentrations. The rate of mineralization of 50 and 500 ng of aniline per ml and 200 pg and 2.0 ng of the phthalate per ml increased with time in lake waters. The phthalate and 2,4-dichlorophenoxyacetate were mineralized in samples from a eutrophic but not an oligotrophic lake. Addition to eutrophic lake water of a benzoate-utilizing bacterium did not increase the rate of benzoate mineralization at 34 and 350 pg/ml but did so at 5 and 50 ng/ml. Glucose and phenol reduced the percentage of p-nitrophenol mineralized at p-nitrophenol concentrations of 200 ng/ml but not at 22.6 pg/ml and inhibited the rates of mineralization at both concentrations. These results show that the kinetics of mineralization, the capacity of the aquatic community to assimilate carbon from the substrate or the extent of assimilation, and the sensitivity of the mineralizing populations to organic compounds are different at trace levels than at higher concentrations of organic compounds.     

Effect of glucose concentration on peritoneal inflammatory cytokines in continuous ambulatory peritoneal dialysis patients

OBJECTIVE: It is known that glucose concentrations of peritoneal dialysis solutions are detrimental to the peritoneal membrane. In order to determine the effect of glucose concentration on cytokine levels of peritoneal fluid of continuous ambulatory peritoneal dialysis (CAPD) patients, a cross-sectional study was performed. METHODS: Nine non-diabetic CAPD patients participated in two 8-h dwell sessions of overnight exchanges in consecutive days, with 1.36% and 3.86% glucose containing peritoneal dialysis solutions (Baxter-Eczacibas). Peritoneal dialysis fluid tumor necrosis factor (TNF)-alpha and interleukin (IL)-6 levels were measured. RESULTS: TNF-alpha levels after 1.36% and 3.86% glucose used dwells were 23+/-14 pg/ml and 28+/-4 pg/ml, respectively (p=0.78). The IL-6 levels were 106+/-57 pg/ml and 115+/-63 pg/ml (p=0.81), respectively. CONCLUSION: In our in vivo study we found that the glucose concentration of the conventional lactate-based CAPD solution has no effect on basal IL-6 and TNF-alpha levels of peritoneal fluid. Further in vivo studies with non-lactate-based CAPD solutions are needed in order to determine the effect of glucose concentration per se on cytokine release.     

Pyroglutamyl apelin-13 identified as the major apelin isoform in human plasma

Apelin is emerging as an important hormone regulator of cardiovascular homoeostasis and an important biomarker for heart failure. Apelin concentrations have historically been measured by immunoassays; however, reported apelin concentrations measured in healthy volunteers show a large disparity from a few picograms per milliliter (pg/ml) to several nanograms per milliliter (ng/ml). Apelin exists in several isoforms ranging in size from 12 to 36 residues, and immunoassays generally cannot distinguish the specific forms present. In this study, an optimized method for enriching apelin peptides with cation-exchange beads followed with mass spectrometry analysis is presented. Apelin peptides are labile in plasma at physiological conditions; however, by lowering the plasma pH to 4.5, the recovery of apelin peptides can be increased significantly. Through optimizing the cation-exchange extraction process, we improved the lower limit of detection for most of the apelin peptides monitored to a few pg/ml. Using the improved method, we detected pyroglutamyl apelin-13 [(pyr)apelin-13] as the major apelin isoform present in plasma from several healthy volunteers at concentrations ranging from 7.7 to 23.3 pg/ml.     

Action of citrinin on bacterial chromosomal and plasmid DNA in vivo and in vitro.

Citrinin, a mycotoxin of Penicillium citrinum and other species of the genera Penicillium and Aspergillus, caused the following effects at different concentrations in Escherichia coli. In vivo at 100 micrograms/ml single-strand breaks were caused in the chromosomal DNA. In the presence of 100 micrograms/ml, UV (254 nm)-induced DNA damage was repaired in the bacterial cells without need for a complete growth medium. At 300 micrograms/ml lambda ts prophage was induced in a lysogenic E. coli strain. In an E. coli strain carrying a F' lac plasmid, 4.7% of the cells displayed the Lac- phenotype after treatment with 200 micrograms of citrinin per ml, suggesting elimination of the F' factor. In vitro, DNA repair synthesis was observed at 5 micrograms of citrinin per ml in permeabilized cells, and replicative DNA synthesis was inhibited at 200 micrograms/ml. In these systems synthesis of stable RNAs was slightly diminished at 300 micrograms/ml, and protein synthesis was not affected at concentrations up to 450 micrograms/ml. Lambda and ColE1 plasmid DNA were cleaved in vitro when small amounts of copper ions were present. This DNA-attacking activity was prevented by NADPH, catalase, and superoxide dismutase and by higher concentrations of hydroxyl radical scavengers, suggesting the involvement of free radicals in the mechanism of action of citrinin on DNA.     

Action of citrinin on bacterial chromosomal and plasmid DNA in vivo and in vitro

Citrinin, a mycotoxin of Penicillium citrinum and other species of the genera Penicillium and Aspergillus, caused the following effects at different concentrations in Escherichia coli. In vivo at 100 micrograms/ml single-strand breaks were caused in the chromosomal DNA. In the presence of 100 micrograms/ml, UV (254 nm)-induced DNA damage was repaired in the bacterial cells without need for a complete growth medium. At 300 micrograms/ml lambda ts prophage was induced in a lysogenic E. coli strain. In an E. coli strain carrying a F' lac plasmid, 4.7% of the cells displayed the Lac- phenotype after treatment with 200 micrograms of citrinin per ml, suggesting elimination of the F' factor. In vitro, DNA repair synthesis was observed at 5 micrograms of citrinin per ml in permeabilized cells, and replicative DNA synthesis was inhibited at 200 micrograms/ml. In these systems synthesis of stable RNAs was slightly diminished at 300 micrograms/ml, and protein synthesis was not affected at concentrations up to 450 micrograms/ml. Lambda and ColE1 plasmid DNA were cleaved in vitro when small amounts of copper ions were present. This DNA-attacking activity was prevented by NADPH, catalase, and superoxide dismutase and by higher concentrations of hydroxyl radical scavengers, suggesting the involvement of free radicals in the mechanism of action of citrinin on DNA.     

Effects of dissolved organic carbon and second substrates on the biodegradation of organic compounds at low concentrations

Pseudomonas acidovorans and Pseudomonas sp. strain ANL but not Salmonella typhimurium grew in an inorganic salts solution. The growth of P. acidovorans in this solution was not enhanced by the addition of 2.0 micrograms of phenol per liter, but the phenol was mineralized. Mineralization of 2.0 micrograms of phenol per liter by P. acidovorans was delayed 16 h by 70 micrograms of acetate per liter, and the delay was lengthened by increasing acetate concentrations, whereas phenol and acetate were utilized simultaneously at concentrations of 2.0 and 13 micrograms/liter, respectively. Growth of Pseudomonas sp. in the inorganic salts solution was not affected by the addition of 3.0 micrograms each of glucose and aniline per liter, nor was mineralization of the two compounds detected during the initial period of growth. However, mineralization of both substrates by this organism occurred simultaneously during the latter phases of growth and after growth had ended at the expense of the uncharacterized dissolved organic compounds in the salts solution. In contrast, when Pseudomonas sp. was grown in the salts solution supplemented with 300 micrograms each of glucose and aniline, the sugar was mineralized first, and aniline was mineralized only after much of the glucose carbon was converted to CO2. S. typhimurium failed to multiply in the salts solution with 1.0 micrograms of glucose per liter. It grew slightly but mineralized little of the sugar at 5.0 micrograms/liter, but its population density rose at 10 micrograms of glucose per liter or higher. The hexose could be mineralized at 0.5 micrograms/liter, however, if the solution contained 5.0 mg of arabinose per liter.(ABSTRACT TRUNCATED AT 250 WORDS)     

Effect of dimethyl sulphoxide and some antibiotics on cultured human T-lymphoma cells as measured by microcalorimetry

The influence of dimethyl sulphoxide (I), penicillin/streptomycin (II), gentamicin (III), and amphotericin B (IV) on growing human T-lymphoma cells was measured by microcalorimetry. There was a dose-dependent decrease in the heat production rate of the cells after 24 h of incubation with I in concentrations ranging from 0-2% (v/v). At 3.6%, about half of the cells died. II and III had no effect on the cells after incubation for 6 days, at concentrations from 1 to 10 times that of the normal (50-500 IU/ml; 50-500 micrograms/ml). IV was used in combination with II (50 IU/ml; 50 micrograms/ml) and III (50 micrograms/ml), respectively, at concentrations between 0.25 and 7.5 micrograms/ml. After 6 days of incubation, the results were similar to those obtained with II and III separately.     

Oral contraceptives containing 20 or 30 micrograms ethinylestradiol and 150 micrograms desogestrel: pharmacokinetics and pharmacodynamic parameters

The serum concentrations of ethinylestradiol (EE) and 3-keto-desogestrel (KDG) were compared during treatment with a combination of 20 micrograms EE + 150 micrograms DG (20EE/DG) or of 30 micrograms EE + 150 micrograms DG (30EE/DG). During intake of both preparations, the peak levels and the areas under the curve (AUC) of EE increased significantly by approximately 100% between days 1 and 10. In the steady state, the maximal EE levels were 75 +/- 34 pg/ml (20EE/DG) and 136 +/- 55 pg/ml (30EE/DG), and the AUC were 464 +/- 236 pg.h/ml and 840 +/- 492 pg.h/ml. The KDG levels, which were identical with both preparations, increased between days 1 and 21 by approximately 300% up to values of 4.5 +/- 1.6 ng/ml. There were large interindividual variations in the AUC of EE and KDG and no correlation between the levels of EE and KDG. On day 21 of intake of 30EE/DG, the serum concentrations of sex-hormone- and corticosteroid-binding globulin were higher by 16% and 12%, respectively than with 20EE/DG. Although the morning peak levels of cortisol did not differ, the decrease which occurred thereafter, according to the circadian rhythm, was slower with 30EE/DG. There was no relationship between the serum concentrations of EE and/or KDG and the occurrence of irregular bleedings, which was similar during treatment with both preparations. As most of the women who bled had bleedings both with 20EE/DG and 30EE/DG, an influence of predisposition can be assumed.(ABSTRACT TRUNCATED AT 250 WORDS)     

Effects of dissolved organic carbon and second substrates on the biodegradation of organic compounds at low concentrations.

Pseudomonas acidovorans and Pseudomonas sp. strain ANL but not Salmonella typhimurium grew in an inorganic salts solution. The growth of P. acidovorans in this solution was not enhanced by the addition of 2.0 micrograms of phenol per liter, but the phenol was mineralized. Mineralization of 2.0 micrograms of phenol per liter by P. acidovorans was delayed 16 h by 70 micrograms of acetate per liter, and the delay was lengthened by increasing acetate concentrations, whereas phenol and acetate were utilized simultaneously at concentrations of 2.0 and 13 micrograms/liter, respectively. Growth of Pseudomonas sp. in the inorganic salts solution was not affected by the addition of 3.0 micrograms each of glucose and aniline per liter, nor was mineralization of the two compounds detected during the initial period of growth. However, mineralization of both substrates by this organism occurred simultaneously during the latter phases of growth and after growth had ended at the expense of the uncharacterized dissolved organic compounds in the salts solution. In contrast, when Pseudomonas sp. was grown in the salts solution supplemented with 300 micrograms each of glucose and aniline, the sugar was mineralized first, and aniline was mineralized only after much of the glucose carbon was converted to CO2. S. typhimurium failed to multiply in the salts solution with 1.0 micrograms of glucose per liter. It grew slightly but mineralized little of the sugar at 5.0 micrograms/liter, but its population density rose at 10 micrograms of glucose per liter or higher. The hexose could be mineralized at 0.5 micrograms/liter, however, if the solution contained 5.0 mg of arabinose per liter.(ABSTRACT TRUNCATED AT 250 WORDS)     

Heterotrophic microbial activity and organic matter degradation in coastal lagoons of Colombia

In this study we measured the community respiration and the bacterial respiration as part of the overall degradation process of organic material. Additionally, the turnover rates of the pools of dissolved free glucose and acetate as representatives of the fraction of easily degradable low molecular organic solutes were determined. The study was performed in several coastal lagoons of the "Outer Delta of the Río Magdalena" in northern Colombia. The lagoons can be separated into two groups: The first group contains highly productive brackish lagoons with chl a concentrations ranging from 62-130 micrograms/l. The second group consists of less productive freshwater lagoons with chl a between 5.5-19 micrograms/l. Turnover rates of glucose and acetate were very fast in the highly productive lagoons resulting in turnover times of less than 20 min for both compounds. In the less productive systems the cycling of glucose and acetate was much slower. Here the mean values of the turnover times were 2 hr for glucose and 1.5 hr for acetate. The rates of bacterial DNA-formation measured as thymidine incorporation differed significantly between both groups of lagoons, being very high (1.86-2.76 nmol/l/hr) in the highly productive and relatively low (0.073-0.55 nmol/l/hr) in the less productive group. Water column community respiration ranged between 122 and 16 micrograms C/l/hr with means of 88 micrograms C/l/hr in the highly and 19 micrograms C/l/hr in the less productive group. In the first group the mean values of the bacterial contribution to community respiration amounted to 37% and in the second group to 18%. The bacterial respiration was determined in an indirect way via bacterial biomass production and assuming a growth efficiency of 50%. It is discussed whether this relatively high growth efficiency allows reasonable results in both groups of lagoons.