A method for determining tissue sulfate

A method for the determination of the inorganic sulfate present in rat liver homogenates has been developed. In order to determine sulfate, a protein-free extract is required. The classical protein precipitation methods of preparing protein-free extracts gave 2.5–40% recovery of added ³⁵SO₄^2?. Separation of the protein by ultrafiltration gave only 29% recovery when 0.15 m KCl was the homogenizing medium. A homogenization medium containing 0.154 m NH₄OH and 20 g EDTA per liter gave 102 ± 11% recovery of added ³⁵SO₄^2? when the protein was separated by ultrafiltration.     

Metabolism of inorganic sulphate in the isolated perfused rat liver. Effect of sulphate concentration on the rate of sulphation by phenol sulphotransferase

1. The metabolism of inorganic [³⁵S]sulphate (Na₂³⁵SO₄) was studied in the isolated perfused rat liver at three initial concentrations of inorganic sulphate in the perfusion medium (0, 0.65 and 1.30mm), in relation to sulphation and glucuronidation of a phenolic drug, harmol (7-hydroxy-1-methyl-9H-pyrido[3,4-b]indole). 2. [³⁵S]Sulphate rapidly equilibrated with endogenous sulphate in the liver. It was excreted in bile and reached, at the lowest concentration in the perfusion medium, concentrations in bile that were much higher than those in the perfusion medium; at the higher sulphate concentrations, these concentrations were equal. The physiological concentration of inorganic sulphate in the liver, available for sulphation of drugs, is similar to the plasma concentration. 3. At zero initial inorganic sulphate in the perfusion medium, the rate of sulphation was very low and harmol was mainly glucuronidated. At 0.65mm-sulphate glucuronidation was much decreased and considerable sulphation took place, indicating efficient competition of conjugation by sulphation. At 1.30mm-sulphate the sulphation increased still further. 4. The results suggest that an important factor in sulphation is the relatively high K_m of synthesis of adenosine 3′-phosphate 5′-sulphatophosphate (the co-substrate of sulphation) for inorganic sulphate, which is of the order of the plasma concentration of inorganic sulphate. The steady-state adenosine 3′-phosphate 5′-sulphatophosphate concentration may determine the rate of sulphate conjugation of drugs in the rat in vivo.     

Maroteaux-Lamy disease (mucopolysaccharidosis VI), subtype A: deficiency of a N-acetylgalactosamine-4-sulfatase

The non-reducing terminal moiety of ³⁵SO₄-dermatan sulfate accumulating in fibroblasts cultured from the skin of patients with one form of Maroteaux-Lamy disease was found to be N-acetylgalactosamine-4-sulfate. This end group accounted for about 3 % of the total radioactivity. Using both ³⁵SO₄- and ¹⁴C-N-acetylgalactosamine-labeled dermatan sulfates from the patients fibroblasts as substrates, it was found that homogenates of Maroteaux-Lamy fibroblasts, but not of normal, Hurler and Sandhoff fibroblasts fail to cleave inorganic sulfate from the non-reducing termini. We conclude, that deficiency of N-acetylgalactosamine-4-sulfatase is the biochemical basis for this form of Maroteaux-Lamy disease.     

Cycling of inorganic and organic sulfur in peat from Big Run Bog,West Virginia

Total S concentration in the top 35 cm of Big Run Bog peat averaged 9.7 mol·g — wet mass^–1 (123 mol·g dry mass^–1). Of that total, an average of 80.8% was carbon bonded S, 10.4% was ester sulfate S, 4.5% was FeS₂­S, 2.7% was FeS­S, 1.2% was elemental S, and 0.4% was SO₄ ^2–­S. In peat collected in March 1986, injected with³⁵S­SO₄ ^2– and incubated at 4 °C, mean rates of dissimilatory sulfate reduction (formation of H₂S + S⁰ + FeS + FeS₂), carbon bonded S formation, and ester sulfate S formation averaged 3.22, 0.53, and 0.36 nmol·g wet mass^–1·h^–1, respectively. Measured rates of sulfide oxidation were comparable to rates of sulfate reduction. Although dissolved SO₄ ^2– concentrations in Big Run Bog interstitial water (< 200 µM) are low enough to theoretically limit sulfate reducing bacteria, rates of sulfate reduction integrated throughout the top 30–35 cm of peat of 9 and 34 mmol·m^–2·d^–1 (at 4 °C are greater than or comparable to rates in coastal marine sediments. We suggest that sulfate reduction was supported by a rapid turnover of the dissolved SO₄ ^2– pool (average turnover time of 1.1 days). Although over 90% of the total S in Big Run Bog peat was organic S, cycling of S was dominated by fluxes through the inorganic S pools.     

The decreased synthesis of chondroitin sulfate-containing extracellular proteoglycans by SV40 transformed Balb/c 3T3 cells

Balb/c 3T3 cells synthesize 5–10 times more ³⁵SO₄^2?-labeled extracellular proteoglycan per cell than do Balb/c 3T3 cells transformed by SV40 (SV3T3). The extracellular ³⁵SO₄^2?-labeled proteoglycans of the Balb/c 3T3 and SV3T3 cells differ markedly in their acid mucopolysaccharide composition. Extracellular Balb/c 3T3 proteoglycans contain about 70–80% chondroitin sulfate, most of which is chondroitin 4-sulfate, and small amounts of heparan sulfate and/or heparin. On the other hand, extracellular SV3T3 proteoglycans contain 65–75% heparan sulfate and/or heparin and less than 15% chondroitin sulfate. Analysis of extracellular ³⁵SO₄^2?-labeled proteoglycan by sodium dodecyl sulfate-polyacrylamide gel electrophoresis reveals that Balb/c 3T3 alone synthesizes a class of proteoglycans capable of migrating in a 10% separating gel. This class of proteoglycans, designated as fraction C, accounts for up to 45% of the total extracellular Balb/c 3T3 ³⁵SO₄^2?-labeled proteoglycans and contains chondroitin sulfate exclusively. It is altogether absent in the extracellular SV3T3 proteoglycans. The absence of this and other classes of chondroitin sulfate-containing proteoglycans can account for the 5–10-fold decreased synthesis of ³⁵SO₄^2?-labeled proteoglycans by SV3T3 cells when compared to Balb/c 3T3 cells.     

Heparan sulfate at the surface of HeLa cells

Summary HeLa cells, labeled with Na₂ ³⁵SO₄, release into the culture medium³⁵SO₄ bound to plasma membrane vesicles next to³⁵SO₄-glycoproteins and free³⁵SO₄. Plasma membrane vesicles, experimentally produced by treatment with formaldehyde, contain³⁵SO₄ and their surface can be stained with high iron diamine. Scanning of chromatograms of the trypsinate from labeled cells demonstrates radioactivity on the spot of heparan sulfate. It is concluded that HeLa cells synthesize heparan sulfate, which is incorporated at the plasma membrane and released by shedding of small vesicles.Supported by a grant from the Algemene Spaar- en Lijfrentekas Cancer Fund, Brussels, Belgium.     

A simulation model of sulfur transformations in forested Spodosols

Transformations of organic and inorganic S in two forested Spodosols from the Hubbard Brook Experimental Forest, New Hampshire and the Huntington Forest in the Adirondack Mts. of New York were investigated using laboratory³⁵SO₄ ^2- incorporation experiments. Sulfur transformations were modeled as a set of three reversible, first-order reactions in which soluble SO ₄ ^2- is converted to adsorbed SO ₄ ^2- , ester sulfate and carbon-bonded S. Reaction rate contants for³⁵SO ₄ ^2- adsorption/desorption and immobilization reactions involving ester sulfate and carbon-bonded S were determined using a fifth order Runge-Kutta-Fehlberg integration routine combined with least squares fitting. Model simulations were able to account for over 93% of the variation in the distribution of³⁵S in S fractions. A hypothetical application of immobilization rate constants to field situations at the Hubbard Brook Experimental Forest suggests that large quantities of S cycle through organic forms in Northern Hardwood Forest Ecosystems.     

Reduction of Sulfur Compounds in the Sediments of a Eutrophic Lake Basin

Concentrations of various sulfur compounds (SO₄²⁻, H₂S, S⁰, acid-volatile sulfide, and total sulfur) were determined in the profundal sediments and overlying water column of a shallow eutrophic lake. Low concentrations of sulfate relative to those of acid-volatile sulfide and total sulfur and a decrease in total sulfur with sediment depth implied that the contribution of dissimilatory sulfur reduction to H₂S production was relatively minor. Addition of 1.0 mM Na₂³⁵SO₄ to upper sediments in laboratory experiments resulted in the production of H₂³⁵S with no apparent lag. Kinetic experiments with ³⁵S demonstrated an apparent K_m of 0.068 mmol of SO₄²⁻ reduced per liter of sediment per day, whereas tracer experiments with ³⁵S indicated an average turnover time of the sediment sulfate pool of 1.5 h. Total sulfate reduction in a sediment depth profile to 15 cm was 15.3 mmol of sulfate reduced per m² per day, which corresponds to a mineralization of 30% of the particulate organic matter entering the sediment. Reduction of ³⁵S⁰ occurred at a slower rate. These results demonstrated that high rates of sulfate reduction occur in these sediments despite low concentrations of oxidized inorganic compounds and that this reduction can be important in the anaerobic mineralization of organic carbon.     

Tissue distribution,metabolism, and elimination of perfluorooctanoic acid in male and female rats

The elimination, tissue distribution, and metabolism of [1-¹⁴C]perfluorooctanoic acid (PFOA) was examined in male and female rats for 28 days after a single ip dose (9.4 μmol/kg, 4 mg/kg). A sex difference in urinary elimination of PFOA-derived ¹⁴C was observed. Female rats eliminated PFOA-derived radioactivity rapidly in the urine with 91% of the dose being excreted in the first 24 hr. In the same period, male rats eliminated only 6% of the administered ¹⁴C in the urine. The sex-related difference in urinary elimination resulted in the observed difference in the whole-body elimination half-life (t_1/2) of PFOA in males (t_1/2 = 15 days) and females (t_1/2 < 1 day). Analysis of PFOA-derived ¹⁴C in tissues showed that the liver and plasma of male rats and the liver, plasma, and kidney of female rats were the primary tissues of distribution. The relatively high concentration of PFOA in the male liver was further examined using an in situ nonrecirculating liver perfusion technique. It was shown that 11% of the PFOA infused was extracted by the liver in a single pass. The ability of the liver to eliminate PFOA into bile was examined in rats whose renal pedicles were ligated to alleviate sex differences in the urinary excretion of PFOA. In a 6-hr period following IP administration of PFOA, there was no apparent difference in biliary excretion, where both males and females eliminated less than 1% of the PFOA dose via this route. We hypothesized that the sex difference in the persistence of PFOA was due to a more rapid formation of a PFOA-containing lipid (i.e., a PFOA-containing mono-, di-, or triacylglycerol, cholesteryl ester, methyl ester, or phospholipid) in the male rat. Also, the increased urinary elimination of PFOA in females may have been due to increased metabolism to a PFOA-glucuronide or sulfate ester. However, no evidence that PFOA is conjugated to form a persistent hybrid lipid was obtained, nor were polar metabolites of PFOA in urine or bile detected. In addition, daily urinary excretion of fluoride in male and female rats before or after PFOA treatment were similar, suggesting that the parent compound is not defluorinated. Thus, the more rapid elimination of PFOA from female rats is not due to formation of a PFOA metabolite.     

Sulfur dynamics in mineral horizons of two northern hardwood soils. A column study with 35S

Sulfur dynamics of two Spodosols were ascertained using soil columns constructed from homogenized mineral soil from nothern hardwood ecosystems at the Huntington Forest (HF) in the Adirondack Mountains of New York and Bear Brook Watershed in Maine (BBWM). Columns were leached for 20 weeks with a simulated throughfall solution with³⁵SO₄ ^2-. Sulfur constituents were similar to those of other Spodosols, with the organic S fractions (C-bonded S and ester sulfate) constituting over 90% of total S. HF soil columns had higher total S (14.9 mol S g^-1) than that for the BBWM soil columns (7.4 mol g^-1) primarily due to higher C-bonded S in the former.Initially, adsorbed SO₄ ^- accounted for 5 and 4% of total S for the BBWM and HF soil columns, respectively. After 20 weeks, adsorbed SO₄ ^2- decreased (81%) in BBWM and increased (33%) in HF soil columns. For both HF and BBWM soil columns, C-bonded S increased and ester sulfate decreased, but only for HF columns was there a net mineralization of organic S (5.6% of total S). The greatest decrease in ester sulfate occurred at the top of the columns.Leaching of³⁵S was less than 0.5% of the³⁵S added due to its retention in various S constituents. There was an exponential decrease in³⁵S with column depth and most of the radioisotope was found in C-bonded S (70–88 and 70–91% for BBWM and HF, respectively). The rapid turnover of adsorbed SO^2- ₄ was reflected in its high specific activity (834 and 26 kBq mol^-1 S for BBWM and HF, respectively). The lower specific activity of adsorbed SO₄ ^2- in HF was attributable to greater isotopic dilution by non-radioactive SO^2- ₄ derived from greater organic S mineralization in the HF versus the BBWM columns.Both soil columns initially had high levels of NO^- ₃ which resulted in the generation of H⁺ and net retention of SO₄ ^2- in the early phase of the experiment due to pH dependent sulfate adsorption; later NO₃ ^- decreased and SO₄ ^2- was desorbed. Leaching of NIO₃ ^- and SO₄ ^2- was correlated with losses of Mg²⁺ and Ca²⁺ of which the latter was the dominant cation.Analyses using both S mass balances and radioisotopes corroborate that for BBWM soil columns, SO^2- ₄ adsorption-desorption dominated the S biogeochemistry while in HF soil columns, organic S mineralization-immobilization processes were more important. It is suggested that similar techniques can be applied to soils in the field to ascertain the relative importances of SO₄ ^2- adsorption processes and organic S dynamics.     

Inactivation of Saccharomyces cerevisiae sulfate transporter Sul2p: use it and lose it

Saccharomyces cerevisiae SO₄⁼ transport is regulated over a wide dynamic range. Sulfur starvation causes ～10,000-fold increase in the ³⁵SO₄⁼ influx mediated by transporters Sul1p and Sul2p; >80% of the influx is via Sul2p. Adding methionine to S-starved cells causes a 50-fold decline (t_1/2 ～5 min) in SUL1 and SUL2 mRNA but a slower decline (t_1/2 ～1 h) in transport. In contrast, SO₄⁼ addition does not affect mRNA but causes a rapid (t_1/2 = 2–4 min) decrease in transport. In met3Δ cells (unable to metabolize SO₄⁼), addition of SO₄⁼ to S-starved cells causes inactivation of ³⁵SO₄⁼ influx over times in which cellular SO₄⁼ contents are nearly constant. The relationship between cellular SO₄⁼ and transport inactivation shows that cellular SO₄⁼ is not the signal for Sul2p inactivation. Instead, the transport inactivation rate has the same dependence on extracellular SO₄⁼ as ³⁵SO₄⁼ influx, indicating that Sul2p exhibits use-dependent inactivation; the transport process itself increases the probability of Sul2p inactivation and degradation. In addition, there is a transient efflux of SO₄⁼ shortly after adding >0.02 mM SO₄⁼ to S-starved met3Δ cells. This transient efflux provides further protection against excessive SO₄⁼ influx and may represent an alternate transport mode of Sul2p.     

Sulphate uptake and metabolism in the chrysomonad,Monochrysis lutheri

The intracellular concentration of inorganic ³⁵SO₄ in Monochrysis lutheri cells exposed to 0.513 mM Na₂ ³⁵SO₄ for up to 6-hr remained constant at about 0.038 mM. The exchange rate of this ³⁵SO₄ with the external unlabelled sulphate was negligible compared to the rate of influx across the plasmalemma (0.032 μmoles/g cells/hr). The flux of free ³⁵SO₄ to organic ³⁵S was 0.029 μmoles/g cells/hr. Assuming an internal electrical potential in the cells of-70 mV, this intracellular concentration of inorganic ³⁵SO₄ was well in excess of that obtainable by passive diffusion as calculated from the Nernst equation. These results indicate that sulphate is accumulated by an active mechanism rather than by facilitated diffusion. Sulphate uptake appears to occur via a carrier-mediated membrane transport system which conforms to Michaelis-Menten type saturation kinetics with a K _m of 3.2×10^-5 M and a V _max of 7.9×10^-5 μmoles sulphate/hr/10⁵ cells. Uptake was dependent on a source of energy since the metabolic inhibitor CCCP almost completely inhibited uptake under both light and dark conditions and DCMU caused a 50% decrease in uptake under light conditions. Under dark conditions, uptake remained at about 80% of that observed under light conditions and was little affected by DCMU, indicating that the energy for uptake could be supplied by either photosynthesis or respiration. A charge and size recognition site in the cell is implied by the finding that sulphate uptake was inhibited by chromate and selenate but not by tungstate, molybdate, nitrate or phosphate. Chromate did not inhibit photosynthesis. Cysteine and methionine added to the culture medium were apparently capable of exerting inhibition of sulphate uptake in both unstarved and sulphate-starved cells. Cycloheximide slightly inhibited sulphate uptake over an 8-hr period indicating, either a slow rate of entry of the inhibitor into the cells or a slow turnover of the proteins(s) associated with sulphate transport.     

Rapid depletion of dissolved organic sulphur (DOS) in freshwaters

Sulphur (S) is a key macronutrient for all organisms, with similar cellular requirements to that of phosphorus (P). Studies of S cycling have often focused on the inorganic fraction, however, there is strong evidence to suggest that freshwater microorganisms may also access dissolved organic S (DOS) compounds (e.g. S-containing amino acids). The aim of this study was to compare the relative concentration and depletion rates of organic ³⁵S-labelled amino acids (cysteine, methionine) with inorganic S (Na₂³⁵SO₄) in oligotrophic versus mesotrophic river waters draining from low nutrient input and moderate nutrient input land uses respectively. Our results showed that inorganic SO₄²⁻ was present in the water column at much higher concentrations than free amino acids. In contrast to SO₄²⁻, however, cysteine and methionine were both rapidly depleted from the mesotrophic and oligotrophic waters with a halving time < 1 h. Only a small proportion of the DOS removed from solution was mineralized and excreted as SO₄²⁻ (< 16% of the total taken up) suggesting that the DOS could be satisfying a demand for carbon (C) and S. In conclusion, even though inorganic S was abundant in freshwater, it appears that the aquatic communities retained the capacity to take up and assimilate DOS.

     

Effect of stress on sulfated glycol, metabolites of brain norepinephrine.

The present study examined the effect of footshock stress on the formation of the two major metabolites of rat brain norepinephrine (NE) - the sulfate conjugates of 3-methoxy-4-hydroxyphenylglycol (MOPEG-SO₄) and 3,4-dihydroxyphenylglycol (DOPEG-SO₄). Rats receiving intraventricular injections of either ³HNE or Na₂³⁵SO₄ prior to 0.5 hour of footshock showed significant and comparable increases in both sulfated glycols labeled with ³H or ³⁵SO₄. Elevations were greatest in the hypothalumus using Na₂³⁵SO₄. In pheniprazine pretreated rats footshock did not increase the production of MOPEG-³⁵SO₄ from intraventricular labeled sulfate given alone or in combination with various doses of exogenous MOPEG. The results indicate that neuronally released brain NE is metabolized to form both MOPEG-SO₄ and DOPEG-SO₄. The increase in these metabolites results from an increased glycol production and not from a stress-induced activation of brain sulfation mechanisms.     

The role of the Golgi complex in sulfate metabolism

This investigation was designed to determine if sulfate metabolism is the function of a particular cell organelle, or whether the site of sulfation varies, depending upon the type of cell and the class of sulfated compound. Rats and mice were injected intravenously with inorganic sulfate labeled with ³⁵S (H₂ ³⁵SO₄), and were then killed by vascular perfusion of fixative 5–30 min later. Several tissues were prepared for electron microscope autoradiography. 14 different types of specialized cells which incorporated the labeled sulfate were analyzed. In every case, the sulfate was initially detected in the smooth membranes and vesicles of the Golgi complex. Available evidence indicates that these cells were engaged in the synthesis of several different sulfated compounds, including mucopolysaccharides, glycoproteins, lipids, and steroids. These results lead to the generalization that the enzymes required for the transfer of inorganic sulfate to a variety of acceptor molecules are located in the Golgi complex.     

Effects of repeated (NH4)2SO4 application on sulfur pools in soil,soil microbial biomass,and ground vegetation of two watersheds in the Black Forest/Germany

The effect of repeated (NH₄)₂SO₄ applications (3 × 700 kg ha^–1 in 1988, 1991, and 1994, respectively) on S pools in soil, soil microbial biomass, and ground vegetation was studied at two Norway spruce (Picea abies L. [Karst.]) sites in the Black Forest/Germany. In both eco-systems, most of the total S pool was located in the soil. The soil also was the predominant compartment for retention of applied SO₄ ^2--S. The fractions of organic and inorganic S forms in the initial soil S content, and the retention of experimentally applied S was different for both sites. In the podzol Schluchsee, organic S accounted for 92% of total S. In the cambisol Villingen, the S pool consisted of 33% organic S and 67% inorganic S. The retention of applied S in various compartments of both ecosystems reflected these proportions. Only minor amounts of fertilized S (<1%) was retained in the spruce trees, ground vegetation, and soil microbial biomass. However, between 51% (Villingen) and 72% (Schluchsee) of the applied S was retained in the soil. In the Schluchsee podzol, 75% of retained fertilizer S was accumulated as ester sulfate, whereas SO₄ ^2-adsorption and precipitation of Al hydroxy sulfates were restricted by dissolved organic matter in the soil solution. In the Villingen cambisol, SO₄ ^2- adsorption was the dominant process of S retention, although 20% of the fertilized S again was retained as ester sulfate. The significant relevance of organic S forms in the retention of fertilizer S in both soils emphasizes the need for models which include the formation and re-mineralization of organic S compounds, especially of ester sulfates, for correctly simulating and predicting the retention and remobilization of S in acid forest soils subject to changing atmospheric N and S deposition.     

Localization of sulfate reduction in planted and unplanted rice field soil

Rates of in situ sulfate reduction (SRR) in planted and unplanted rice fieldsoil were measured by the ³⁵SO^2– ₄-radiotracermethod using soil microcosms. The concentration of ³⁵SO^2– ₄ decreased exponentially with time.However, time course experiments indicated that incubation times of10–30 min were appropriate for measurements of SRRusing a single time point in routine assays. Unplanted microcosmsshowed high SRR of 177 nmol cm^-3 d^-1 inthe uppermost centimeter where average sulfate concentrations were<33 µM. Fine scaled measurements (1 mmresolution) localized highest SRR (<100 nmol cm^-3d^-1) at the oxic/anoxic interface at 2–5 mmdepth. In planted rice field soil, SRR of <310 nmolcm^-3 d^-1 were observed at 0–2cm depth. Sulfate reduction rates were determined at a millimeter-scalewith distance to a two dimensional root compartment. The SRR was highestat 0–1.5 mm distance to the root layer with rates up to500 nmol cm^-3 d^-1, indicating a highstimulation potential of the rice roots. SRR seemed to be mainlydependent on the in situ sulfate porewater concentrations. At thesoil surface of unplanted microcosms sulfate concentration decreasedfrom <150 µM to <10 µM within the first 8 mm of depth. In planted microcosmssulfate concentration varied from 87–99 µMsulfate at the 0–3 mm distance to the root layer to48–62 µM sulfate at a root distance>4 mm from the roots.The depth distribution of inorganic sulfur compounds was determinedfor planted and unplanted rice field soil. Sulfate, acid volatilesulfide (AVS) and chromium reducible sulfide (CRS) were up to 20 foldhigher in planted than in unplanted microcosms. CRS was the majorinsoluble sulfur fraction with concentrations >1.7µmol cm^-3. Organic sulfur accounted for25–46% of the total sulfurpresent (269 µg/g dw) in an unplanted microcosm.The biogeochemical role of sulfate reduction forshort-term accumulation of inorganic sulfur compounds(FeS, FeS_{_2} and S°) in rice soil wasdetermined in a time course experiment with incubationperiods of 5, 10, 20, 30 and 60 min. The relativedistribution of CRS and AVS formation showedlittle depth dependence, whereas the formation of³⁵S° seemed to be the highest in themore oxidized upper soil layers and near the root surface.AV³⁵S was the first major product of sulfatereduction after 20–30 min, whereas CR³⁵Swas formed, as AV³⁵S and ³⁵S°decreased, at longer incubation periods of >30 min.     

The effect of chronic ethanol consumption on temperature-dependent physical properties of liver mitochondrial membranes

We have reported that the monovalent ionophore monensin causes undersulfated chondroitin sulfate biosynthesis in cultured chondrocytes. In order to clarify the mechanism of this diminished sulfation, we have measured the rate of incorporation of sulfate into chondrocytes and assayed the cellular ATP levels. We have also measured sulfatase activity, the incorporation of ³⁵SO₄ into 3′-phosphoadenosine 5′-phospho[³⁵S]sulfate and endogenous sulfotransferase activity in the cell-free extracts. We find that: (1) The incorporation of ³⁵SO₄ into the free sulfate pool in chondrocytes was not inhibited by monensin. (2) The ATP levels of monensin-treated chondrocytes were the same as control cells. (3) There was no sulfatase activity in both control and monensin-treated chondrocytes. (4) Enzymatic analyses revealed that ³⁵SO₄ incorporation into 3′-phosphoadenosine 5′-phospho[³⁵S]sulfate and subsequent sulfotransferase activity were not inhibited in the presence of monensin. At present the most tenable hypothesis to account for monensin causing undersulfated chondroitin sulfate synthesis is that the ionophore impairs the access of proteoglycans to the sulfotransferases in the luminal walls of the Golgi structures.     

Axonal transport of proteoglycans to the goldfish optic tectum

The study addressed the question of whether³⁵SO₄ labeled molecules that the have been delivered to the goldfish optic nerve terminals by rapid axonal transport include soluble proteoglycans. For analysis, tectal homogenates were subfractionated into a souluble fraction (soluble after centrifugation at 105,000g), a lysis fraction (soluble after treatment with hypotonic buffer followed by centrifugation at 105,000g) and a final 105,000g pellet fraction. The soluble fraction contained 25.7% of incorporated radioactivity and upon DEAE chromatographys was resolved into a fraction of sulfated glycoproteins eluting at 0–0.32 M NaCl and containing 39.5% of total soluble label and a fraction eluting at 0.32–0.60 M NaCl containing 53.9% of soluble label. This latter fraction was included on columns of Sepharose CL-6B with or without 4 M guanidine and after pronase digestion was found to have 51% of its radioactivity contained in the glycosaminoglycans (GAGs) heparan sulfate and chondroitin (4 or 6) sulfate in the ratio of 70% to 30%. Mobility of both intact proteoglycans and constituent GAGs on Sepharose CL-6B indicated a size distribution that is smaller than has been observed for proteoglycans and GAGs from cultured neuronal cell lines. Similar analysis of lysis fraction, containing 11.5% of incorporated³⁵SO₄, showed a mixture of heparan sulfate and chondroitin sulfate containing proteoglycans, apparent free heparan sulfate and few, if any, sulfated glycoproteins. Overall, the result support the hypothesis that soluble proteoglycans are among the molecules axonally transported in the visual system.     

Lysosomal sulfate efflux following glycosaminoglycan degradation: measurements in enzyme-supplemented Maroteaux-Lamy syndrome fibroblasts and isolated lysosomes

Studies using lysosomal membrane vesicles have suggested that efflux of the sulfate that results from lysosomal glycosaminoglycan degradation is carrier-mediated. In this study, glycosaminoglycan degradation and sulfate efflux were examined using cultured skin fibroblasts and lysosomes deficient in the lysosomal enzymeN-acetylgalactosamine-4-sulfatase. Such fibroblasts store dermatan sulfate lysosomally, which could be labelled biosynthetically with Na ₂ ³⁵ SO₄. The addition of recombinantN-acetylgalactosamine-4-sulfatase to the media of³⁵S labelled fibroblasts degraded up to 82% of the stored dermatan [³⁵S] sulfate over a subsequent 96 h chase and released inorganic [³⁵S] sulfate into the medium. In the presence of 4-acetamido-4-isothiocyanatostilbene-2,2-disulfonic acid (SITS), sulfate was reused to a minor extent in newly synthesized proteoglycan. Isolated granules from recombinant enzyme supplemented fibroblasts degraded stored dermatan [³⁵S]sulfate to sulfate which was rapidly released into the medium at a rate that was reduced by the extra-lysosomal presence of the lysosomal sulfate transport inhibitors SITS, Na₂SO₄ and Na₂MoO₄. SITS also inhibited dermatan sulfate turnover, although it had no effect on the action of purified recombinant enzymein vitro. These data imply that sulfate clearance occurred concomitantly with dermatan sulfate turnover in the lysosome even at high substrate loading, and that lysosome-derived sulfate, while available, is reutilized minimally in synthetic pathways.Abbreviations SITS 4-acetamido-4-isothiocyanatostilbene-2,-2-disulfonic acid - GAG glycosaminoglycan - 4S N-acetylgalactosamine-4-sulfatase - r4S recombinant humanN-acetylgalactosamine-4-sulfatase - PBS phosphate buffered saline - BME basal modified Eagle's medium - FBS fetal bovine serum - GalNAc4S-GlcA-GalitolNAc4S -(N-acetyl-d-galactosamine-4-sulfate)-(1–4)--d-glucuronic acid)-(1–3)-N-acetyl-d-[1-³H]galactosaminitol-4-sulfate - DS dermatan sulfate - MPS mucopolysaccharidosis