The influences of calcium and magnesium ions on the exchange of monovalent cations in Neurospora crassa

Low-K⁺, high-Na⁺ cells of strain RL21a of Neurospora crassa , in steady state with 25 m M Na⁺, were used to study K⁺/Na⁺ exchanges in the presence or absence of Ca²⁺ and Mg²⁺. In the presence of Ca²⁺ and Mg²⁺, a low concentration of K⁺ (0.3 m M ) triggered a rapid exchange, but in the absence of the divalents, a high K⁺ concentration (30 m M ) was required to initiate the exchange at a rapid rate. In the absence of Ca²⁺ and Mg²⁺, K⁺ uptake did not occur at low K⁺ concentration, internal K⁺ did not regulate Na⁺ influx in the presence of external K⁺, and the efflux of Na⁺ proceeded at maximum activity at very low-K⁺ contents.     

Renal excretion in channel catfish following injection of quinaldine sulphate or 3- trifluoromethyl-4-nitrophenol

Channel catfish, Ictalurus punctatus Rafinesque, injected intraperitoneally with 2-methyl-quinoline sulphate (QdSO₄) or 3-trifluoromethyl-4-nitrophenol (TFM) eliminate most of the dose of these compounds by extra-renal routes. Patterns of renal excretion of Na⁺, K⁺, Ca²⁺, Mg²⁺, and Cl⁻ (ρEq kg⁻¹ h⁻¹) appeared to be associated with the 'stress' of the urine collection technique rather than with the elimination of either compound. Concentrations of Na⁺, K⁺, Ca²⁺, Mg²⁺, and Cl⁻ (mEq/1) were determined in urine, plasma and gall bladder bile.     

Comparison of ion transportation before and after egg hatching in Amphinemura sp. (Plecoptera)

Abstract.  An increase in egg size with embryonic development in stoneflies is believed to result from the uptake of water by osmosis. The present study aims to investigate whether a selective ion transport through egg membranes exists before hatching, and whether ions are released after hatching. Viable and nonviable egg masses are incubated in Petri dishes filled with water, and the concentrations of the ions F⁻, Cl⁻, SO₄²⁻, NO₃⁻, Na⁺, K⁻, Mg²⁺ and Ca²⁺ in the water are determined. The ion transport of an egg mass before and after hatching and a nonviable egg mass is then calculated. Before hatching, Cl⁻, SO₄²⁻, NO₃⁻, Na⁺, Mg²⁺ and Ca²⁺ are taken up from the surrounding water into the inner egg. These ions are selectively taken into the egg. After hatching, Cl⁻, SO₄²⁻, Na⁺, Mg²⁺ and Ca²⁺ are released into the surrounding water. The amount of these ions released after hatching is lower than the amount taken up before hatching. Ions that are not released after hatching are considered to be used in embryonic development.     

The tonoplast H+-pyrophosphatase of radish seedlings: biochemical characteristics

The activity of the H⁺-pyrophosphatase (H⁺-PPase) was characterized in microsomes from 24-h-old radish ( Raphanus sativus L., ev. Tondo Rosso Quarantino) seedlings, which are virtually devoid of the tonoplast H⁺-ATPase. The H⁺-PPase was localized to membranes which roughly comigrated with the plasma membrane in a sucrose density gradient, but clearly separated from plasma membrane when microsomes were partitioned in an aqueous dextran-polyethylene glycol two-phase system. The H⁺-PPase activity was strictly dependent on Mg²⁺ and on the presence of a monovalent cation (K⁺=Rb⁺=NH₃⁺Cs⁺≫Na⁺Li⁺) and was insensitive to anions such as Cl−, Br−, NO₃− and SO₄^2-. It was inhibited by F−, imidodiphosphate and Ca²⁺. It had a pH optimum between pH 7.5 and 8.5 and was saturated by low concentrations of pyrophosphate (half saturation at 30 μ M pyrophosphate). All of these characteristics are identical to those reported for the tonoplast H⁺-PPase from various plant materials. The functional molecular weight of the H⁺-PPase, measured with the radiation-inactivation technique was 96 kDa.     

Changes in ion content and transport during development of embryonic rainbow trout

Wet mass and water content of four lots of whole eggs did not change throughout embryonic development of rainbow trout Oncorhynchus mykiss. Eggs in all four lots accumulated Na⁺. Eggs in lots 2 and 4 also accumulated Ca²⁺ and Cl^-, whereas eggs in lot 1 showed no significant change in Ca²⁺ or Cl^- and eggs in lot 3 showed no change in Cl^-and a small loss of Ca²⁺. Although the Na⁺ content of embryonic tissues increases in the later stages of development, the yolk sac content remained constant, indicating uptake of Na⁺ from the environment. Na+ uptake by whole eggs was non-saturable, consistent with diffusion of Na⁺ across the chorion into the perivitelline fluid. Na⁺ uptake in dechorionated embryos was saturable, as was Ca²⁺ uptake by both whole eggs and dechorionated embryos, consistent with active uptake or facilitated diffusion mechanisms at the surface of embryos. Very low Ca²⁺ uptake rates in dechorionated embryos suggest that the Ca²⁺ uptake mechanism is not fully developed until after hatching.     

Ionic regulation and Na+,K+-ATPase activity in gills and kidney of the Antarctic aglomerular cod icefish exposed to dilute sea water

When Notothenia neglecta was exposed to diluted, half strength, sea water for 6 h or 10 days, serum concentrations of Cl^-, Na⁺, K⁺ and Mg²⁺ did not differ from those of sea water controls. This indicates that the fish were capable of both short- and long-term regulation. Renal Na⁺,K⁺-ATPase activity decreased after a 6 h exposure to diluted sea water, but there were no differences between diluted sea water and controls after 10 days of exposure.     

Monovalent—divalent cation ratios and the occurrence of phytoplankton, with special reference to the desmids

SUMMARY. We have analysed data from ninety-nine Scottish freshwater lochs, to explore the relationship between water chemistry and phytoplankton assemblages. Our results confirm that there are strong correlations both between the phytoplankton quotient and divalent cation concentrations, particularly Ca⁺⁺, and also between the phytoplankton quotient and the (Na⁺+ K⁺)/(Ca⁺⁺+ Mg⁺⁺) ratio. However, the latter is evidently a spurious relationship, arising from the former association, together with an association between Ca⁺⁺ and the (Na⁺+K⁺)/ (Ca⁺⁺+ Mg⁺⁺) ratio. The observed correlation does not persist if account is taken of concomitant variations in the Ca⁺⁺concentration. This conclusion is suggested both by relatively informal analyses (median polish, partial correlation coefficients) and by more formal modelling and testing (stepwise regression, all-subsets regression).     

Effects of soil frost on nitrogen net mineralization, soil solution chemistry and seepage losses in a temperate forest soil

Freezing and thawing may alter element turnover and solute fluxes in soils by changing physical and biological soil properties. We simulated soil frost in replicated snow removal plots in a mountainous Norway spruce stand in the Fichtelgebirge area, Germany, and investigated N net mineralization, solute concentrations and fluxes of dissolved organic carbon (DOC) and of mineral ions (NH₄⁺, NO₃⁻, Na⁺, K⁺, Ca²⁺, Mg²⁺). At the snow removal plots the minimum soil temperature was −5 °C at 5 cm depth, while the control plots were covered by snow and experienced no soil frost. The soil frost lasted for about 3 months and penetrated the soil to about 15 cm depth. In the 3 months after thawing, the in situ N net mineralization in the forest floor and upper mineral soil was not affected by soil frost. In late summer, NO₃⁻ concentrations increased in forest floor percolates and soil solutions at 20 cm soil depth in the snow removal plots relative to the control. The increase lasted for about 2–4 months at a time of low seepage water fluxes. Soil frost did not affect DOC concentrations and radiocarbon signatures of DOC. No specific frost effect was observed for K⁺, Ca²⁺ and Mg²⁺ in soil solutions, however, the Na⁺ concentrations in the upper mineral soil increased. In the 12 months following snowmelt, the solute fluxes of N, DOC, and mineral ions were not influenced by the previous soil frost at any depth. Our experiment did not support the hypothesis that moderate soil frost triggers solute losses of N, DOC, and mineral ions from temperate forest soils.     

Changes in Ion Content in Heat-Treated Tetrahymena Cells

SYNOPSIS Changes in the amounts of Na⁺, K⁺, Mg²⁺ and Ca²⁺ were determined in the supernates of homogenized samples of Tetrahymena cells which were exposed to 7 heat shocks. The amounts of the same ions were also determined in the pH 4.5-soluble fractions after dialysis. During the last shock, i.e., 6.5 hr after the start of heat treatment, there was a change in the ion balance characterized by a gain in Na⁺, Ca²⁺ and non-dialyzable Mg²⁺ and a loss of K⁺. The change was not in phase with the synchronous cell division.     

Cationic and Anionic Requirements for the Binding of 2β-Carbomethoxy-3β-(4-Fluorophenyl)[3H]tropane to the Dopamine Uptake Carrier

Abstract: The present study reports the ion dependency of 2β-carbomethoxy-3β-(4-fluorophenyl)[³H]tropane ([³H]- CFT) binding to the dopamine transporter in the rat striaturn. The results indicate that [³H]CFT binding to synaptosomal P₂ membranes requires low concentrations of Na⁺ (peak binding between 20 and 50 m M Na⁺), is stimulated by phosphate anion or l^-, but is unaffected or only slightly affected by F^-, Cl^-, Br^-, NO₃^-, or SO₄^2-, Concentrations of Na⁺ of >50 m M become inhibitory except in the presence of l^-, which shifts peak binding levels toward higher Na⁺ concentrations and also elevates the peak binding level. K⁺ strongly decreased [³H]CFT binding with a shallow inhibition curve, and Na⁺ could not overcome this effect. Saturation analysis of [³H]CFT binding revealed a single binding site changing its affinity for CFT depending on the concentration of sodium phosphate buffer (6, 10, 30, 50, 130, or 200 m M ; 1 mM plus 49 mM NaCIversus 10 m M plus 40 m M NaCI; or 1 mM plus 129 m M Nal versus 10 m M plus 120 m M Nal). No differences were observed in the density of CFT binding sites between any of the conditions examined.     

Inhibition of Rat Brain Microsomal Na+,K+-ATPase by S-Adenosylmethionine

Abstract: Rat brain microsomes were preincubated with S -adenosylmethionine (SAM), MgCl₂, and CaCl₂, then re-isolated, and the activity of Na⁺,K⁺-ATPase determined. SAM inhibited the Na⁺,K⁺-ATPase activity compared with microsomes subjected to similar treatment in the absence of SAM. A biphasic inhibitory effect was observed with a 50% decrease at a SAM concentration range of 0.4 μ M -3.2 μ M and a 70% reduction at a concentration range above 100 μ M . Inclusion of either S- adenosylhomocysteine or 3-deazaadenosine in the preincubations prevented the SAM inhibition of Na⁺,K⁺-ATPase activity. The inhibition by SAM appeared to be Mg²⁺- or Ca²⁺-dependent.     

Regional Calcium Accumulation and Cation Shifts in Rat Brain by Kainate

Abstract: Following local application of kainic acid, changes in the contents of Na⁺, K⁺, Ca²⁺, and Mg²⁺ of the striatum, cerebellum, and hippocampus of the rat were observed at various times after surgery. Within 1 h the levels of K⁺ decreased 20% whereas the levels of Na⁺ and Ca²⁺ increased at least 50% and 20%, respectively. These changes persisted for more than 8 weeks. Ca²⁺ levels rose further, to more than 10-fold during 8 weeks. The Mg²⁺ levels were slightly and only transiently decreased. Unilateral injections of kainate into the striatum affected the contents of these cations not only in this area, but also in the overlying cerebral cortex, the olfactory tubercle, and the ipsilateral substantia nigra. The Ca²⁺ increases were less when rats were kept on a diet deficient in Ca²⁺ and vitamin D. ⁴⁵Ca²⁺, intravenously administered, accumulated significantly more in the kainate-lesioned striatum and substantia nigra than in the homotopic contralateral areas. Electron microscopic examination of the localization of Ca²⁺ with the oxalate-pyroantimonate technique showed the appearance of extracellularly located deposits and the accumulation of Ca²⁺ in (possibly degenerating) myelinated axons in kainate-lesioned striata. This study provides evidence that calcification of cerebral tissue is closely associated with neurodegenerative processes and shows that kainate may serve as a tool to elucidate the mechanism of brain calcification. The results are discussed in relation to idiopathic calcinosis (striopallidodentate calcinosis, Fahr's disease).     

Physiological effects of Na2SO4 and NaCl on callus cultures of Brassica campestris (Chinese cabbage)

Hypocotyl-derived callus cultures of Brassica campestris L. ssp. pekinensis cv. Kim-jung (Chinese cabbage) were grown on Murashige and Skoog medium containing no additional salt, NaCl or Na₂SO₄. Na₂SO₄ was more than twice as inhibitory in comparison to the same concentration of NaCl when growth and fresh:dry weight ratios of established callus were measured. Levels of protein, starch, sucrose and α-amino nitrogen were not significantly altered in salt-grown callus. Concentrations of reducing sugars and chlorophyll were 2–3 times greater in callus grown on either salt. Proline concentration increased 15–20 fold on the highest levels of salt. Final concentrations (reached in 20–24 days) were closely correlated to the initial Na⁺ concentration of the medium, regardless of salt type. The osmotic potential in callus transferred to NaCl or Na₂SO₄ reached a maximum negative value after 16 days. For both salts, subsequent increases were correlated to increases in fresh:dry weight and growth. On both salts, turgor remained relatively constant (0. 6–0.75 MPa). Changes in Na⁺, K⁺, Mg²⁺ and Ca²⁺ content were correlated to initial Na⁺ concentration in the medium, not salt type. Accumulation of Na⁺ was accompanied by loss of K⁺ and Mg²⁺. Six to seven times less sulfate was measured in callus grown on Na₂SO₄ than chloride in callus grown on similar concentrations of NaCl.     

Influence of exogenously supplied potassium and sodium salts on the abscisic acid-induced proline accumulation in barley leaf segments

A stimulation of the abscisic acid (ABA)-induced increase in proline was observed in leaf segments of barley ( Hordeum vulgare L. cv. Georgie) if K⁺ or Na⁺ were supplied in the external medium as salts of monovalent anions such as NO₃, Br, Cr and I, but not when sulphate or phosphate were used. To a lesser extent, the effect was evident also with RbCl, but it did not occur when chlorides of Li⁺. Cs⁺, NH₄⁺, Mg:⁺ and Ca²⁺ were used. Both KC1 and NaCl in the concentration range 2–100 m M influence the ABA-dependent proline accumulation to the same extent; the increase induced was about 100% at 10 m M , and reached a maximum between 60 and 100 m M. The effect is not due to the osmotic activity of the salts and does not seem to depend on changes in K⁺ and Na⁺ levels within the leaf tissue, but it is somehow linked to their external concentration. The existence of a specific interaction between ABA and K⁺ or Na⁺, possibly at the cell membrane level, is proposed.     

Salinity response of a freshwater charophyte, Chara vulgaris

Abstract. Chara vulgaris L. growing in an oligohaline lake was adapted to laboratory conditions and subjected to long-term salinity treatments ranging from 0 to 350 mol m ³ NaCl added to the lake water (40–680 mosmol kg ¹). Osmotic potential and concentration of the main osmotically active solutes (K⁺, Na⁺, Mg²⁺, Cl and sucrose) in the vacuolar sap of the central internodal cells were estimated. C. vulgaris did regulate turgor but incompletely. Turgor decreased from 335 mosmol kg ¹ under control conditions to 52–111 mosmol kg ¹ at 350 mol m ³ NaCl. The enhancement of πⁱ was achieved by increase in both ions and sucrose. Sterile and fertile plants differed in their response to osmotic stress. In sterile plants, the ions accounted for about 87% of the vacuolar osmotic potential. The increase of πⁱ under osmotic stress was exclusively due to an accumulation of Na⁺ and Cl^-. In fertile plants, sucrose accounted for about 35% of πⁱ and ions for about 51% Under osmotic stress, sucrose content increased together with the ionic content of Na⁺ and Cl^-.     

A LIGHT-SCATTERING TECHNIQUE FOR THE STUDY OF THE PERMEABILITY OF RAT BRAIN SYNAPTOSOMES IN VITRO

Abstract— (1) Swelling of synaptosomes was measured spectrophotometrically by recording changes in extinction at 520 nm.
(2) Synaptosomes behaved as osmometers in NaCl solutions. When the tonicity of the medium was changed, synaptosome volume changed in accordance with Boyle and van't Hoff's Law. These changes were reversed on restoring the tonicity of the medium.
(3) The rate at which a solute entered the synaptosome was determined from the rate of swelling in the presence of that solute. Permeability of synaptosomes to non-electrolytes was in the order glucose ≪ glycerol < thiourea = formamide < propylene glycol = dimethylsulphoxide.
(4) Synaptosomes were freely permeable to ammonium and acetate ions and impermeable to Ca²⁺, Mg²⁺, PO₄²⁻, SO₄²⁻ and oxalate ions.     

Uptake and distribution of calcium, magnesium and potassium in cucumber of different age

Uptake and distribution of Ca⁺, Mg²⁺ and K²⁺ were investigated in plants of cucumber ( Cucumis sativus L. var. Cila) which had been cultivated for 12, 19, 32, or 53 days in complete nutrient solution with 1.0 m M Ca²⁺, 2.0 m M Mg²⁺ and 2.0 m M K⁺. The ⁺ concentration was about the same in roots and shoots, while the Ca²⁺ and Mg²⁺ concentrations were low in roots compared to shoots. The K⁺ concentration decreased with increasing leaf age, while the Ca²⁺ and Mg²⁺ concentrations increased, except in older plants with flowers and fruits, where an increased concentration was found in the youngest leaves. This is discussed in connection with increased indoleacetic acid (IAA) synthesis in the shoot. Excision of leaves at different levels from 21-day-old plants, followed by uptake for 24 h from the nutrient solution on days 22 and 23, resulted in no immediate reduction in Ca²⁺ (⁴⁵Ca) uptake. Transport of Ca²⁺ increased to leaves above and below the excision point and total Ca²⁺ uptake remained at the same level as for the intact plant. It is suggested that regulation of Ca²⁺ uptake is primarily achieved in the root while the distribution in the shoot is regulated by the accessability of negative binding sites.     

Sucrose and ouabain effects on the kinetic properties of a membrane-bound (Na++ K++ Mg2+) ATPase in sugar beet roots

Kinetic studies of a microsomal (Na⁺+ K⁺+ Mg²⁺)ATPase from sugar beet roots ( Beta vulgaris L. cv. Monohill) show that sucrose influences the MgATPase in different ways depending on the presence of K⁺ and/or Na⁺ 1) In the presence of the substrate MgATP and Na⁺ the effect of sucrose follows simple Michaelis-Menten kinetics. 2) In the presence of substrate together with K⁺ or (K⁺+ Na⁺), sucrose has little effect on the ATPase activity. 3) In the presence of Na⁺, onabain acts as an uncompetitive inhibitor with respect to MgATP. 4) In the presence of K⁺ or (K⁺+ Na⁺), the inhibition by ouabain is somewhat depressed and shows non-linearity when 1/v is plotted versus 1/MgATP. 5) Sucrose and Na⁺ activate in a competitive way, so that a successive increase of the Na⁺ level decreases the activation by sucrose. Both K_m and V-values are thereby changed. 6) The sucrose activation in the presence of Na⁺ is also influenced by ouabain. It is, therefore, suggested that Na⁺ may regulate the interference between the Na⁺/K⁺ pump and a sucrose sensitive system.     

Roles for Potassium and Calcium Channels in the Initiation of Sperm Motility in Rainbow Trout.

It is well known that the motility of spermatozoa in rainbow trout is suppressed by K⁺. We showed here that although trout sperm are completely immotile in medium containing 5 mM K⁺, motility was initiated by the subsequent addition of several mM Ca²⁺, suggesting that both K⁺and Ca²⁺are related to the process of the initiation of sperm motility. It was further found that K⁺channel blockers tetraethylammonium, nonyltriethylammonium, Ba²⁺and Cs⁺, as well as the Ca²⁺channel blocker verapamil, inhibited the initiation of sperm motility at doses at which these reagents inhibit chnnel-related functions in other cells. However, Na⁺channel blocker, tetrodotoxin and anion channel blocker 4, 4-diisothiocyatatostilbene-2, 2'-disulfonic acid inhibited the motility only at extremely high doses. These results suggest that transport of K⁺and Ca²⁺through ion channels at the plasma membrane of spermatozoa is the first event that triggers the initiation of sperm motility in rainbow trout.     

Element concentrations in mosses and surface waters of western Canadian mires relative to precipitation chemistry and hydrology

Concentrations of N, P, S, Na, K, Mg, Ca, Mn, Fe, Cu, Cd, Zn, Pb, Al, and AIA (acid insoluble ash) m mosses (three Sphagnum species and Tomenthypnum nitens, all hummock species) from a variety of mires, both ombrotrophic and minerotrophic, in the coastal western and central parts of Canada are considered in relation to surface water pH and concentrations of Na⁺, K⁺, Mg²⁺, Ca²⁺, Cl⁻, and SO₄^2- Distinct west-east concentration gradients were present for most elements in both mosses and water, but there were correlations between surface water and moss concentrations only for Ca and Mg
On ombrotrophic sites and sites characterized by poor fen vegetation, wet deposition is the main source of elements in the surface water On rich fen sites, additional Ca and Mg from surrounding soils change the elemental proportions We conclude that hydrochemically the limit between poor and rich fen sites is more decisive than between bog and fen The increase in Ca may give brown mosses a competitive advantage over Sphagnum
Moss concentrations of Na and Mg are the only ones decreasing inland The constancy or inland increase of moss elemental concentrations may depend on either an increasing atmospheric supply (e g Pb), differences in moss growth rates (especially N, P, and K) or site conditions related to the water regime (e g Fe and Al)