A new experimental setup for studying the formation of phosphate binding iron oxides in marine sediments. Preliminary results

A new laboratory method is introduced to study theformation of phosphate binding iron(III) oxides at theredox boundary in marine sediments. A sediment core isgiven a very well-defined oxic-anoxic interface byplacing a 0.45 µm filter between the sediment andthe overlying water. After a period of 1 months thefilter is covered with a layer of fresh iron oxides,formed by the oxidation of upward diffusing Fe²⁺from the sediment pore water. The formed iron oxidesare investigated by electron probe X-ray microanalysis(EXPMA). With a sediment core from the brackish BalticSea the average molar composition of 788 formedparticles is Fe_1.00±0.13P_0.55±0.06Ca_0.37±0.04 plus unknown amounts of O, H andC. The results show that the particles have a uniformcomposition, and that calcium plays an important rolein the phosphate binding. The laboratory method is auseful supplement to in situ sampling forstudies of iron oxides.     

The Actin-Related Protein2/3 Complex Regulates Mitochondrial-Associated Calcium Signaling during Salt Stress in Arabidopsis

Microfilament and Ca²⁺ dynamics play important roles in stress signaling in plants. Through genetic screening of Arabidopsis thaliana mutants that are defective in stress-induced increases in cytosolic Ca²⁺ ([Ca2+]_cyt), we identified Actin-Related Protein2 (Arp2) as a regulator of [Ca2+]_cyt in response to salt stress. Plants lacking Arp2 or other proteins in the Arp2/3 complex exhibited enhanced salt-induced increases in [Ca2+]_cyt, decreased mitochondria movement, and hypersensitivity to salt. In addition, mitochondria aggregated, the mitochondrial permeability transition pore opened, and mitochondrial membrane potential Ψm was impaired in the arp2 mutant, and these changes were associated with salt-induced cell death. When opening of the enhanced mitochondrial permeability transition pore was blocked or increases in [Ca2+]_cyt were prevented, the salt-sensitive phenotype of the arp2 mutant was partially rescued. These results indicate that the Arp2/3 complex regulates mitochondrial-dependent Ca²⁺ signaling in response to salt stress.     

The role of the ironhydroxide-phosphate-sulphide system in the phosphate exchange between sediments and overlying water

The accumulation of inorganic phosphate in lake sediments and a possible following release is due to the adsorption of phosphate onto Fe(OOH) and, especially in hard waters, to the precipitation of apatite. Attempts are made to quantify both processes.For the quantification of the P adsorbed, P_ads, onto Fe(OOH) the Freundlich adsorption isotherm, P_ads=A(o-P)^B, gave good results. The constants A and B could be quantified. Constant A appeared to depend on the pH and the Ca²⁺ and Mg²⁺ concentrations in the water. Constant B appeared to approach 0.333. The full equation becomes then: % MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGak0dh9WrFfpC0xh9vqqj-hEeeu0xXdbba9frFj0-OqFf% ea0dXdd9vqaq-JfrVkFHe9pgea0dXdar-Jb9hs0dXdbPYxe9vr0-vr% 0-vqpWqaaeaabaGaciaacaqabeaadaqaaqaaaOqaaiaadcfadaWgaa% WcbaGaamyyaiaadsgacaWGZbaabeaakiabg2da9iaaikdacaaIZaGa% aGOnaiaaicdacaaIWaGaaiOlaiaacIcacaaIXaGaaGimamaaCaaale% qabaGaaGimaiaac6cacaaI0aacbiGaa8hCaiaa-HeaaaGccaGGPaGa% aiikaiaaikdacaGGUaGaaG4naiaaiEdacqGHsislcaaIXaGaaiOlai% aaiEdacaaI3aGaai4oaiaadwgadaahaaWcbeqaaiabgkHiTiaa-nea% caWFHbaaaOGaaiykamaakeaabaGaam4BaiabgkHiTiaadcfaaSqaai% aaiodaaaaaaa!57AF!\[P_{ads} = 23600.(10^{0.4pH} )(2.77 - 1.77;e^{ - Ca} )\sqrt[3]{{o - P}}\]. with the Ca concentration in mmol l^–1 and the o-P and P_ads concentrations in mg l^–1.For the quantification of the solubility of calcium-bound phosphate the solubility product of apatite being 10^–50, as found in the two hard water rivers Rhine and Rhone, was used. With this solubility product the solubility of o-P can be calculated as function of the Ca²⁺ concentration and the pH. The two equations, for adsorption and precipitation, are put together in a so-called solubility diagramme, which describes the o-P concentration as function of the Fe(OOH) concentration in the sediments, and the pH and the Ca²⁺ concentration in the overlying water.The release of phosphate from the Fe(OOH)P complex under anoxic conditions after adding H₂S in inorganic suspensions was shown to be limited. Only when a large excess of H₂S was added there was some release, but if less than 75% of the Fe(OOH) was converted into FeS, there was no release. The possibility of organic phosphate as the source of phosphate release under anoxic conditions is discussed. For a full understanding of this possibility, fractionation of sediment bound phosphate must be carried out in such a way, that these organic phosphates are not hydrolysed.This article is dedicated to the memory of Dr Kees de Groot, who died on 21 September 1994. He was a young enthusiastic, promising scientist who will be missed by all who have known him.     

Effects of aluminum,iron, oxygen and nitrate additions on phosphorus release from the sediment of a Danish softwater lake

The effects of oxygen, aluminum, iron and nitrate additions on phosphate release from the sediment were evaluated in the softwater Lake Vedsted, Denmark, by a 34-day experiment with undisturbed sediment cores. Six treatments were applied: (1) Control - O₂ (0–20% saturation), (2) O₂ (100% saturation) (3) Al³⁺ – O₂, (4) Fe³⁺ + O₂, (5) Fe³⁺ – O₂, and (6) NO₃ ^– – O₂. Al₂(SO₄)₃*18 H₂O and FeCl₃*4H₂O were added in amounts that theoretically should immobilize the exchangeable P-pool in the top 5 cm of the sediment, while sodium nitrate concentrations were increased to 5 mg N l^–1. The four treatments with metals or NO₃ ^– reduced the P efflux from the sediment significantly as compared to the suboxic control treatment. Mean accumulated P-release rates for suboxic treatments with Al³⁺, Fe³⁺, and NO₃ ^– were: –0.27 mmol m^–2 (st. dev = 0.02 mmol m^–2, N = 5), 0.58 mmol m^–2 (st. dev = 0.30 mmol m^–2, N = 5) and 1.40 mmol m^–2 (st. dev = 0.14 mmol m^–2, N = 5), respectively. The oxic treatment with Fe³⁺ had a P efflux of 0.36 mmol m^–2 (st. dev = 0.08 mmol m^–2, N = 5). The two highest P-release rates were observed in the control treatment and the treatment with O₂ (14.50 mmol m^–2 (st. dev = 3.90 mmol m^–2, N = 5) and 2.31 mmol m^–2 (st. dev = 0.80 mmol m^–2, N = 5), respectively). In order to identify changes in the P and Fe binding sites in the sediment as caused by the treatments, a sequential P extraction procedure was applied on the sediment before and after the efflux experiment. Addition of O₂, Fe³⁺ and NO₃ ^– to the sediment increased the amounts of oxidized Fe³⁺ and P_BD. Al³⁺ addition resulted in a lower fraction of P_BD but a correspondingly higher fraction of Al-bound P. Addition of Al³⁺ decreased the Fe-efflux from the suboxic sediment as well as the amount of oxidized Fe³⁺ in the sediment. This questions the use of Al compounds that contain sulfate because of the possible formation of FeS, which will restrict upward migration of Fe²⁺ and the formation of new Fe-oxides in the surface sediment. Instead, we suggest the use of AlCl₃ for lake restoration purposes.     

The uptake of calcium by isolated chromaffin granules of the adrenal medulla

Bovine chromaffin secretory granules were purified by isopycnic Metrizamide gradient centrifugation and their Ca²⁺ sequestration pathways were characterized. The rate of Ca²⁺ sequestration at 37°C was first order, with a maximal uptake of 26.9 ±0.46 (mean ± S.D., n = 3) nmol Ca²⁺/mg protein and a first order rate constant (k) of 0.046 ± 0.002 min^–1. At 4°C the rate of uptake was substantially attenuated, with only 2.47 ± 0.2 (mean ± S.D, n = 3) nmol Ca²⁺/mg protein sequestered in 60 min. Ca²⁺ sequestration was 93% inhibited by 180 mM NaCl [I_50% of 78.7 ± 9.3 mM NaCl (mean ± S.D., n = 11)] but only slightly inhibited by KCl or MgCl₂. Ca ²⁺ sequestration was not stimulated by incubation with MgATP but was inhibited by 57% after incubation with 30 M monensin. Ca ²⁺ sequestration was dependent on extravesicular Ca ²⁺ with half-maximal sequestration at pCa²⁺ 6.81 ± 0.028 (mean ± S.D., n = 3). Sequestered Ca²⁺ could be exchanged with external ⁴⁵Ca²⁺, the exchange rate was first order (k of 0.042 ± 0.004: mean ± S.D., n = 3) and saturated at 27.7 ± 1.1 nmol Ca²⁺/mg (mean ± S.D., n = 3). The Ca²⁺/Ca²⁺ exchange system was totally inhibited by NaCl or KCl but only slightly by MgCl₂. About 75% of sequestered ⁴⁵Ca²⁺ could be released by incubation with NaCl, but only 8% was released by incubation with KCI. Half-maximal release of sequestered ⁴⁵Ca²⁺ required 69.3 ± 12.2 mM NaCl (mean ± S.D., n = 3). The Na⁺-induced release of sequestered ⁴⁵Ca²⁺ was rapid, t_0.5 of 2.80 ± 0.63 min (mean ± S.D., n = 3) and inhibited at 4°C. The concurrent incubation of chromaffin granules with ⁴⁵Ca²⁺ and either annexin proteins V or VI resulted in attenuated uptake of ⁴⁵Ca²⁺. These results suggest that Ca²⁺ uptake in adrenal chromaffin granules is regulated by Na⁺ and Ca²⁺ gradients and also possibly by annexins V and VI.Abbreviations EGTA ethylene glycol bis (-aminoethyl ether)-N,-N,N,N-tetraacetic acid - SDS Sodium dodecyl sulphate - PAGE Polyacrylamide gel electrophoresis - BSA bovine serum albumin - AI Annexin I - AIIt Annexin II tetramer - AIII Annexin III - AIV Annexin IV - AV Annexin V - AVI Annexin VI - k first order rate constant - AT total extent of Ca²⁺ uptake (nmol) - BufferA 300 mM sucrose, 10 mM potassium phosphate (pH 7.0), 5 mM EGTA - Buffer B 300 mM sucrose, 10 mM potassium phosphate (pH 7.0) and 1 mM EGTA - Buffer C 300 mM sucrose, 10 mM potassium phosphate (pH 7.0) - Buffer D 300 mM sucrose, 10 mM potassium phosphate (pH 7.0), 0.5 mM EGTA and 0.65 MM CaCl₂ - Buffer E 300 mM sucrose, 10 mM potassium phosphate (pH 7.0), 0.25 mM EGTA and 0.325 mM CaCl₂     

Intracellular Ca2+ in pancreatic acinar cells: Regulation and role in stimulation of enzyme secretion

Evidence for a primary role for intracellular Ca²⁺ in the stimulation of pancreatic enzyme secretion is reviewed. Measurements of cytoplasmic free Ca²⁺ concentration have allowed direct demonstration of its importance in triggering enzyme secretion and defined the concentration range over which membrane Ca²⁺ pumps must work to regulate intracellular Ca²⁺. Current evidence suggests a key role for the Ca²⁺ Mg-ATPase of rough endoplasmic reticulum in regulating intracellular Ca²⁺ and accumulating a Ca²⁺ store which is released by the action of inositol-l,4,5 trisphosphate following stimulation of secretion.Abbreviations Used EGTA (ethylene dioxy) diethylene-dinitrilotetraacetic acid - BAPTA 1,2-bis (2-aminophenoxy) ethane NNN,N-tetracetic acid - InsP₃ inositol trisphosphate - Ins-1,4,5P₃ and Ins-1,3,4P₃ isomers of inositol trisphosphate with the position of phosphate groups assigned - Ins-1,3,4,5P₄ inositol tetrakisphosphate     

Binding of phosphate in sediment accumulation areas of the eastern Gulf of Finland,Baltic Sea

The relationships between P and components binding P were studied by analysing the concentrations of N, P, Fe, Mn, Ca and Al in sediments and pore water along the estuarine transect of the River Neva in August 1995. The high sediment organic matter concentration resulted in low surface redox potential and high pore-water o-P concentration, whereas the abundance of amphipods resulted in high surface redox potentials and low pore-water o-P concentration. However, despite the variation in sediment organic matter and the abundance of amphipods, very reduced conditions and slightly variable concentrations of Tot-P (0.7–1.1 mg g^–1 DW) were observed in the 10–15 cm sediment depth along the estuarine gradient, indicating that the pools of mobile P were largely depleted within the depth of 0–15 cm. Multiple regression analysis demonstrated that organic matter and Tot-Fe concentration of the sediment were closely related to the variation in Tot-P concentration of the sediments (r ² = 0.817, n=32). In addition, the high total Fe:P ratio suggested that there is enough Fe to bind P in sediments along the estuarine gradient. However, low Fe_diss concentrations in the pore water of reduced sediment (redox-potential <–50 mV) indicated efficient precipitation of FeS (FeS and FeS₂), incapable to efficiently bind P. Consequently, the low Fe_diss:o-P ratio (< 1) recorded in pore water in late summer implied that Fe³⁺ oxides formed by diffusing Fe_diss in the oxic zone of the sediments were insufficient to bind the diffusing o-P completely. The measured high o-P concentrations in the near-bottom water are consistent with this conclusion. However, there was enough Fe_diss in pore water to form Fe³⁺ oxides to bind upwards diffusing P in the oxic sediment layer of the innermost Neva estuary and the areas bioturbated by abundant amphipods.     

Peat and solution chemistry responses to CaCO3 application in wetlands next to Woods Lake,New York

We studied the effect of a calcite (CaCO₃) treatment on peat and pore water chemistry in poor fen and conifer swamp wetlands next to Woods Lake and its tributaries to evaluate the role of wetlands in an Experimental Watershed Liming Study (EWLS). Peat was characteristically organic rich and nutrient poor, with exchangeable Ca concentrations of < 13 cmol_ckg^–1. We estimated that between 0.4 to 4 Mg (CaCO₃) ha^–1 fell directly on three study sites; however, one year after the treatment the increase in Ca concentration (0–8 cm depth) was equivalent to a (CaCO₃) dosage of 3 Mg ha^–1 with an additional 2–4 Mg ha^–1 of undissolved (CaCO₃) still present, suggesting the peat retained Ca supplied from uplands. Most aspects of peat chemistry including microbial respiration and SO₄ reduction did not respond to the treatment.Peat pore water (5 and 20 cm depths) had a mean pH of 4.82 before treatment with high concentrations of dissolved organic carbon (DOC mean of 790 mol C/l) and low Ca²⁺ concentration (mean of 32 mol/l). The (CaCO₃) treatment increased concentrations of Ca²⁺ to a mean of 87 mol/l and dissolved inorganic carbon (DIC) from 205 to a mean of 411 mol/l, whereas it decreased monomeric Al concentration from 19 to 10 mol/l. Otherwise, pore water chemistry showed little response to the treatment, at least within natural spatial and temporal variation of solute concentrations. The results suggest that liming watersheds with the relatively low (CaCO₃) dosage applied in this study can benefit acidic waters downstream by exporting more Ca and DIC and less monomeric Al, with otherwise little effect on the peat itself.     

On the red blood cell Ca2+-pump: An estimate of stoichiometry

Summary Efflux of Ca²⁺ from reversibly hemolyzed human red blood cell ghosts was determined by a Ca²⁺ selective electrode, by atomic absorption spectroscopy, and by the use of⁴⁵Ca. Hydrolysis of ATP was determined by measurement of inorganic phosphate (P_i). At 25°C, ghosts loaded with CaCl₂, MgCl₂, Na₂ATP, and Tris buffer (pH 7.4) extruded Ca²⁺, with mean rates ranging from 58.8±3.5 (sd) to 74.7±8.2 (sd) moles·liter ghosts^–1·min^– depending on the method of Ca²⁺ determination. The ratio of Ca²⁺ transported to P_i released in the presence of ouabain without correction for background ATP splitting was 0.83, 0.83, and 0.80, respectively, for the three methods of Ca²⁺ determination. Correction for the ATPase activity not associated with Ca²⁺ transport resulted in a ratio of 0.91:1. In other experiments, the use of La³⁺ to inhibit the Ca²⁺-pump allowed an estimate of the ATPase activity associated with Ca²⁺ extrusion. In the presence of various concentrations of La³⁺, the ratio of Ca²⁺ pumped to P_i liberated was 0.86 or 1.02, depending on the method of Ca²⁺ determination. It is concluded that the stoichiometry of the Ca²⁺-pump of the RBC plasma membrane is one Ca²⁺ pumped per ATP hydrolyzed.     

Flux of reduced chemical constituents (Fe2+, Mn2+, NH inf4 sup+ and CH4) and sediment oxygen demand in Lake Erie

Sediment pore water concentrations of Fe²⁺, Mn²⁺, NH _inf4 ^sup+ and CH₄ were analyzed from both diver-collected cores and anin situ equilibration device (peeper) in Lake Erie's central basin. Sediment oxygen demand (SOD) was measured at the same station with a hemispheric chamber (including DO probe and recorder) subtending a known area of sediments. The average SOD was 9.4 mM m⁻² day⁻¹ (0.3 g m⁻² day⁻¹). From pore water gradients within the near-surface zone, the chemical flux across the interface was calculated indirectly using Fick's first law modified for sediments. These calculations, using core and peeper gradients, always showed sediment loss to overlying waters, and variations between the two techniques differed by less than an order of magnitude for Fe²⁺ and CH₄. The transport of these reduced constituents can represent a sizeable oxygen demand, ranging from less than 1% for Fe²⁺ and Mn²⁺ to as high as 26% for NH _inf4 ^sup+ , and 30% for CH₄. The average flux of these constituents could account for about a third of the SOD at the sediment-water interface of this station.     

Controlling phosphate release from phosphate-enriched sediments by adding various iron compounds

In a laboratory experiment, different ironsalts (FeCl₂, FeCl₃, FeSO₄) andFe₂O₃ were added to a phosphateenriched silty loam sediment in order to studytheir effect on phosphate mobilisation.Phosphate concentrations in sediment pore waterwere not reduced by the addition ofFe₂O₃. Addition of both ironchlorides, however, resulted in a strongdecrease of phosphate levels in sediment porewater. A similar but less pronounced effect wascaused by the addition of iron as iron(II)sulphate. Sulphate appears to counteract theimmobilisation of phosphate brought about byiron(II). Phosphate release from the sedimentappeared to be determined by the iron/phosphateratio in the sediment pore water. The additionof Fe₂O₃ barely affected thephosphate release from the sediment whereas theaddition of iron salts was effective inpreventing phosphate release. Increased amountsof iron added to the sediment resulted in adecreased phosphate release.     

Intramitochondrial and extramitochondrial free calcium ion concentrations of suspensions of heart mitochondria with very low,plausibly physiological,contents of total calcium

The 2-oxoglutarate dehydrogenase of intact rat heart mitochondria is activated by Ca²⁺, with 50% activation at approximately 0.5 nmol of total Ca/mg of mitochondrial protein, in the presence of P_i and Mg²⁺. Mitochondrial Ca contents in excess of 2 nmol/mg of protein result in 100% activation of the enzyme. Investigation of Ca²⁺ release from the mitochondria using the metallochromic indicator Arsenazo III defines aS _0.5 of 5.4±0.4 nmol of Ca/mg of protein, when the endogenous Ca content of the mitochondria is progressively depleted with EGTA, prior to the initiation of the release process being studied. The subsequent determination of matrix free Ca²⁺ concentration by the null-point technique has allowed expression of these results in terms of free concentration rather than Ca content, with an activity coefficient of approximately 0.001 for matrix Ca²⁺. From the above, Ca²⁺ efflux from heart mitochondria is not saturated at the mitochondrial Ca contents or Ca²⁺ concentrations which give effective regulation of dehydrogenase activity. A consequence is that heart mitochondria do not buffer the pCa of the extramitochondrial medium at these Ca contents (<2 nmol/mg of protein), and this is shown in direct measurements of extramitochondrial pCa. This is taken to question the physiological significance of mitochondrial buffering of cytosolic free Ca²⁺ in normal heart.     

Nutrient release rates from the sediments of Saginaw Bay,Lake Huron

Direct measurements of net production rates and pore water profiles of solutes in the fine-grained sediments of Saginaw Bay, imply corresponding steady-state fluxes to the overlying water of 1.1–1.3 (I), 450–1010 (NH₄ ⁺), 1250–2650 (Si(OH)₄), 3000–3400 (Ca²⁺), 440–1330 (Mg²⁺), 1.5–728 (Fe²⁺), and 179–281 (Mn²⁺) moles/m²/day and 11.0–11.8 (alkalinity) meq/m²/day at 17.5 °C. Silica production rates in sediments apparently follow first order kinetics with a rate coefficient of 0.09/day and a steady-state silica concentration of 1.2 mM at 23.5°C. The remaining solutes follow kinetics approximately independent of solute concentration over the range of concentrations observed. Measured solute production rates are consistent with observed solute profiles only if lateral diffusion gradients are maintained in the sediments by the burrowing and irrigation activity of benthic organisms such asChironomous, the dominant burrower in Saginaw Bay. Assuming that solute fluxes from Saginaw Bay are representative of all of the post-glacial sediments of Lake Huron, the iodine flux from sediments is comparable to the total fluvial input of iodine. The extrapolated silica fluxes from Lake Huron sediments balance the estimated biogenic silica flux to the sediments.     

Mitochondria in Ca2+ Signaling and Apoptosis

Cellular Ca²⁺ signals are crucial in the control of most physiological processes, cell injuryand programmed cell death; mitochondria play a pivotal role in the regulation of such cytosolicCa²⁺ ([Ca²⁺]_c) signals. Mitochondria are endowed with multiple Ca²⁺ transport mechanismsby which they take up and release Ca²⁺ across their inner membrane. These transport processesfunction to regulate local and global [Ca²⁺]_c, thereby regulating a number of Ca²⁺-sensitivecellular mechanisms. The permeability transition pore (PTP) forms the major Ca²⁺ effluxpathway from mitochondria. In addition, Ca²⁺ efflux from the mitochondrial matrix occursby the reversal of the uniporter and through the inner membrane Na⁺/Ca²⁺ exchanger. Duringcellular Ca²⁺ overload, mitochondria take up [Ca²⁺]_c, which, in turn, induces opening of PTP,disruption of mitochondrial membrane potential (_m) and cell death. In apoptosis signaling,collapse of ;_m and cytochrome c release from mitochondria occur followed by activationof caspases, DNA fragmentation, and cell death. Translocation of Bax, an apoptotic signalingprotein from the cytosol to the mitochondrial membrane, is another step during thisapoptosis-signaling pathway. The role of permeability transition in the context of cell death in relationto Bcl-2 family of proteins is discussed.     

Distribution of iron in Lake Banyoles in relation to the ecology of purple and green sulfur bacteria

The distribution of iron both in suspended sediment and in the water column has been studied during summer stratification in Lake Banyoles. In this lake, near bottom springs, a very fine material suspended sediment remains in suspension. Dissolved Fe²⁺ in interstitial water of this suspended sediment, is related to redox potential and to the bottom water inflow. In the water column, soluble iron is present in the hypolimnion of the six different basins forming Lake Banyoles. Under those conditions Fe²⁺ is partially removed by sulfide produced in the anoxic sediment. In addition, a peak of Fe²⁺ found at the density gradient level in basins C-III, C-IV and C-VI. A three compartment model on the dynamics of the processes involving iron in Lake Banyoles is proposed. The bottom springs supply oxygen to the anoxic hypolimnion affecting chemical processes of the iron cycle. The presence of phototrophic sulfur bacteria in the anoxic monimolimnion of basins C-III and C-IV can be related to the kinetics of Fe²⁺ and sulfide. In C-III sulfide concentration exceeds Fe²⁺ concentration whereas in C-IV sulfide is not detectable and iron reached values up to 60 mM. The presence of phototrophic sulfur bacteria in iron-containing environments with no detectable sulfide is explained by the ability of such microorganisms to use FeS as electron donor instead of H₂S.     

Natural and man-caused factors affecting the abundance and cycling of dissolved organic substances in precambrian shield lakes

A study on nutrient regeneration processes and a measure of their fluxes at the sediment-water interface was carried out in two different stations of a shallow lagoon of the Po delta river (Italy). A few parameters on the solid fraction (grain-size, porosity, C, N) and pore water profiles of o-P, NH₃, NO _inf3 ^sup– , SiO₂, Tot-CO₂, SO _inf4 ^sup2– , Fe, Mn, Ca, Mg, pH, Eh were determined. At both stations the results were typical for fine sediments rich in organic matter. The ratio of variations of sulphate (SO _inf4 ^sup2– ) to total carbonate demonstrates the main role sulphate reduction plays on the organic matter decay. The use of the ratios of variations of sulphate (SO _inf4 ^sup2– ) to ammonia (NH₃) and of sulphate (SO _inf4 ^sup2– ) to phosphate (o-P) in pore waters enabled us to calculate the C/N/P of the decomposing organic matter. Obtained C/N/P indicated an enrichment of N and P with regard to C/N/P ratios of the solid fraction, due to the selective stripping of N and P during organic matter mineralization. This phenomenon decreases with depth, where organic matter becomes more refractory. Calculations on saturation degrees have shown the possibility of authigenic calcite, apatite and rhodochrosite precipitation in sediments. Nutrient fluxes were estimated for SiO₂, NH₃ and o-P by means of benthic chambers and modelling the pore water profiles. The model used for the calculation of fluxes allowed us to account for the bioturbation-irrigation influence near the interface, by means of a cumulative diffusion coefficient. Directly measured fluxes proved to be always significantly greater than the theoretical ones. These differences seem to be due to surface processes which do not affect pore water concentrations (degradation of fresh materials at the interface; micro-bioturbation by small gasteropoda such as Hydrobia ventrosa) and/or to the different concept of the two methods in time and space. Number, size and biomass of macrobenthic species living in the sediment underneath the benthic chambers were determined. The comparison between data on macrobenthic populations and flux values showed a good relationship between the number of organisms and benthic fluxes within each station. However, flux variations between stations are to be attributed mainly to the different arrangement of the tubes of the polychaetes Polydora ciliata in the sediment.     

Microphytobenthos and chironomid larvae attenuate nutrient recycling in shallow‐water sediments

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Asymmetric effects of divalent cations and protons on active Ca2+ efflux and Ca2+-ATPase in intact red blood cells

Summary The influence of the asymmetric addition of various divalent cations and protons on the properties of active Ca²⁺ transport have been examined in intact human red blood cells. Active Ca²⁺ efflux was determined from the initial rate of⁴⁵Ca²⁺ loss after CoCl₂ was added to block Ca²⁺ loading via the ionophore A23187. Ca²⁺-ATPase activity was measured as phosphate production over 5 min in cells equilibrated with EGTA-buffered free Ca²⁺ in the presence of A23187. The apparent Ca affinity of active Ca²⁺ efflux (K _0.5=30–40 mol/liter cells) was significantly lower than that measured by the Ca²⁺-ATPase assay (K _0.5=0.4 m). Possible reasons for this apparent difference are considered. Both active Ca²⁺ efflux and Ca²⁺-ATPase activity were reduced to less than 5% of maximal levels (20 mmol/liter cells · hr) in Mg²⁺-depleted cells, and completely restored by reintroduction of intracellular Mg²⁺. Active Ca²⁺ efflux was inhibited almost completely by raising external CaCl₂ (but not MgCl₂) to 20mm, probably by interaction of Ca²⁺ at the externally oriented E₂P conformation of the pump. Cd²⁺ was more potent than Ca²⁺ in this inhibition, while Mn²⁺ was less potent and 10mm Ba²⁺ was without effect. A Ca²⁺: proton exchange mechanism for active Ca²⁺ efflux was supported by the results, as external protons (pH 6–6.5) stimulated active Ca²⁺ efflux at least twofold above the efflux rate at pH 7.8 Ca²⁺ transport was not affected by decreasing the membrane potential across the red cell.     

Modulation of Ca2+ mobilization by protein kinase C in the submandibular duct cell line A253

The expression of protein kinase C (PKC) isoforms and the modulation of Ca²⁺ mobilization by PKC were investigated in the human submandibular duct cell line A253. Three new PKC (nPKC) isoforms (, , and ) and one atypical PKC (aPKC) isoform () are expressed in this cell line. No classical PKC (cPKC) isoforms were present. The effects of the PKC activator phorbol 12-myristate-13-acetate (PMA) and of the PKC inhibitors calphostin C (CC) and bisindolymaleimide I (BSM) on inositol 1,4,5-trisphosphate (IP₃) and Ca²⁺ responses to ATP and to thapsigargin (TG) were investigated. Pre-exposure to PMA inhibited IP₃ formation, Ca²⁺ release and Ca²⁺ influx in response to ATP. Pre-exposure to CC or BSM slightly enhanced IP₃ formation but inhibited the Ca²⁺ release and the Ca²⁺ influx induced by ATP. In contrast, pre-exposure to PMA did not modify the Ca²⁺ release induced by TG, but reduced the influx of Ca²⁺ seen in the presence of this Ca²⁺-ATPase inhibitor. These results suggest that PKC modulates elements of the IP₃/Ca²⁺ signal transduction pathway in A253 cells by (1) inhibiting phosphatidylinositol turnover and altering the sensitivity of the Ca²⁺ channels to IP₃, (2) altering the activity, the sensitivity to inhibitors, or the distribution of the TG-sensitive Ca²⁺ ATPase, and (3) modulating Ca²⁺ entry pathways.     

Aluminium impacts elements of the phosphoinositide signalling pathway in neuroblastoma cells

Inositol phosphate formation was examined in aluminium-treated murine neuroblastoma cells labelled with [³H]-myoinositol. Employing fluoride-stimulated intact cells, aluminium (0.2M to 1 mM) reduced inositol phosphate formation in a dose-dependent manner. In digitonin-permeabilized cells, stimulated with nonhydrolyzable GTP[S], inositol phosphate formation was also inhibited by increasing aluminium doses; the IC₅₀ value was about 20M aluminium, while the inositol phosphate level was reduced 2.5 to 3 fold by 50M aluminium. The inhibitory effect of aluminium (50M) could not be reversed by increasing GTP[S] concentrations up to 500M. Prechelation of aluminium to citrate or EGTA completely abolished the aluminium-triggered inhibition of fluoride-stimulated inositol phosphate formation in intact cells, but had little effect on the inhibition of permeabilized cells stimulated with GTP[S]. In neuroblastoma cells phosphoinositide hydrolysis could be evoked either through a pathway involving the Mg²⁺/guanine nucleotide binding (G_p) protein, or via a pathway operative in the presence of high intracellular Ca²⁺ concentrations. In the Mg²⁺/G_p protein-mediated pathway, formation of inositol triphosphate, IP₃, inositol diphosphate, IP₂, and inositol monophosphate, IP, was apparently inhibited by aluminium in an interdependent manner. As to the Ca²⁺-mediated pathway, aluminium application mainly diminished the release of IP₃. Following interiorization, aluminium thus acts upon elements critical for phosphoinositide-associated signal transduction. An aluminium target apparently resides on the G_p protein. Phosphatidylinositol-4,5-diphosphate-specific phospholipase C probably harbours a second aluminium target.