Uptake of [32P]orthophosphate by algae adn bacteria in Lake Kinneret

Differential filtration was used to apportion [³²p]orthophosphate(P₁) uptake to predominantly bacterial (<3 µm) or algal(>3 µm) components of Lake Kinneret microplankton.Bacteria generally showed preferential ³²P_i uptake in comparisonwith algae. Nevertheless, in most cases, the relative proportionof ³²P counts retained on 3 µm filters was greater thanthe proportion of ¹⁴C counts from heterotrophic bacterial incorporationof [¹⁴Clglucose, indicating that algae were competing for P_iwith bacteria with some measure of success. Most time courseexperiments did not show any consistent transfer of ³²P frombacteria to algae. The addition of a bacterial inhibitor (garamycin)caused a relative increase in the proportion of algal to bacterial³²P_i uptake. Added organic P substrates lowered the amount of³²P_i uptake and appeared to be preferentially utilized by bacteria.Apparent residence times for P_i in Lake Kinneret ranged from0.4 h (prior to overturn) to 17.4 h during bomothermy. Despitelow ambient P_i concentrations, P limitation in Lake Kinneretis not as extreme as in many other aquatic environments.     

Differential uptake of orthophosphate and organic phosphorus substrates by bacteria and algae in Lake Kinneret

The availability of six organic phosphorus substrates (OPS)to serve as sources of this nutrient for natural populationsof phytoplanktonic algae and bacteria was tested by measuringthe degree to which the organic substrates decreased uptakeof [³²P]orthophosphate (³²Pⁱ). When added to samples of LakeKinneret water, six organo-phosphorus compounds usually loweredthe amount of ³²P_i] taken up by microplankton retained on 0.2-µfilters.In contrast, OPS addition generally stimulated ³²P_i uptake intothe mainly algal fraction (>3 µm), indicating thatthe bacteria were mostly responsible for utilising OPS. Thesparing effect of OPS addition on ³²P₁ uptake was very fast,suggestingthat the micro-organisms possessed constitutive or rapidly inducedenzyme systems to exploit the OPS.The results of this studyindicate that a significant flux of phosphorus may pass viaDOP into microbiota, especially bacteria, in some aquatic systems.     

Ca2+ influx through alpha1S DHPR may play a role in regulating Ca2+ release from RyR1 in skeletal muscle

Skeletal muscle fiber types differ in their contents of total phosphate, which includes inorganic phosphate (P_i) and high-energy organic pools of ATP and phosphocreatine (PCr). At steady state, uptake of P_i into the cell must equal the rate of efflux, which is expected to be a function of intracellular P_i concentration. We measured ³²P-labeled P_i uptake rates in different muscle fiber types to determine whether they are proportional to cellular P_i content. P_i uptake rates in isolated, perfused rat hindlimb muscles were linear over time and highest in soleus (2.42 ± 0.17 µmol·g^–1·h^–1), lower in red gastrocnemius (1.31 ± 0.11 µmol·g^–1·h^–1), and lowest in white gastrocnemius (0.49 ± 0.06 µmol·g^–1·h^–1). Reasonably similar rates were obtained in vivo. P_i uptake rates at plasma P_i concentrations of 0.3–1.7 mM confirm that the P_i uptake process is nearly saturated at normal plasma P_i levels. P_i uptake rate correlated with cellular P_i content (r = 0.99) but varied inversely with total phosphate content. Sodium-phosphate cotransporter (PiT-1) protein expression in soleus and red gastrocnemius were similar to each other and seven- to eightfold greater than PiT-1 expression in white gastrocnemius. That the PiT-1 expression pattern did not match the pattern of P_i uptake across fiber types implies that other factors are involved in regulating P_i uptake in skeletal muscle. Furthermore, fractional turnover of the cellular P_i pool (0.67, 0.57, and 0.33 h^–1 in soleus, red gastrocnemius, and white gastrocnemius, respectively) varies among fiber types, indicating differential management of intracellular P_i, likely due to differences in resistance to P_i efflux from the fiber. inorganic phosphate; sodium-inorganic phosphate transporters; PiT-2; inorganic phosphate efflux     

Photosynthesis of Stands of Tomato, Cucumber and Sweet Pepper Measured in Greenhouses under Various CO2-concentrations

The rate of net photosynthesis (P) of whole plant stands oftomato (Lycopersicon esculentum Mill.), cucumber (Cucumis sativusL.) and sweet pepper (Capsicum annuum L.) was measured in sixlong-term experiments in large greenhouses under normal operatingconditions and CO₂-concentrations between 200 and 1200 µmolmol^-1. The objective was to quantify the responses to lightand carbon dioxide and to obtain data sets for testing simulationmodels. The method of measuring canopy photosynthesis involvedan accurate estimation of the greenhouse CO₂ balance, usingnitrous oxide (N₂O) as tracer gas to determine, on-line, theexchange rate between greenhouse and outside air. The estimatedrelative error in the observed P was about ± 10%, exceptthat higher relative errors could occur under particular conditions. A regression equation relating P to the photosynthetically activeradiation, the CO₂ concentration and the leaf area index explained83-91% of the variance. The main canopy photosynthesis characteristicscalculated with the fitted regression equations were: canopyP_max 5-9 g m^-2 h^-1 CO₂ uptake; ratio P_max/LAI 1·5-3 gm^-2 h^-1; light compensation point 32-86 µmol s^-1 m^-2;light use efficiency (quantum yield) at low light 0·06-0·10µmol µmol^-1 and CO₂ compensation point 18-54 µmolmol^-1. The results were related to the prevailing conditions.Copyright1994, 1999 Academic Press Canopy photosynthesis, Capsicum annuum L., carbon dioxide, CO₂, CO₂ balance, CO₂ use efficiency, cucumber, _{Cucumis sativus} L., glasshouse, greenhouse, light use efficiency, Lycopersicon esculentum Mill., sweet pepper, tomato, tracer gas     

Kinetic Characterization of Two Phosphate Uptake Systems with Different Affinities in Suspension-Cultured Catharanthus roseus Protoplasts

We studied the kinetics of inorganic phosphate (P₁) uptake from0.1–1,000 µM P₁ by protoplasts from suspension-culturedcells of Catharanthus roseus (L.) G. Don. Concentration dependenceof [³²P]P₁ uptake revealed two kinetically different uptakesystems, a high-affinity system and a low-affinity system, withK_m values of 3.0 and 47 µM, respectively. Protoplastsfrom cells grown in P_i-rich media had a medium level of thelow-affinity activity and a very low level of the high-affinityactivity. It appeared low-affinity system is expressed constitutively,while the high-affinity system is regulated by the availabilityof P_i. When cells grown in a P_i-rich media were transferredto P_i-depleted media, the high-affinity activity increased significantlyafter 2 d, but the low-affinity activity was barely changed.Upon addition of 10 mM P_i, the high level of the high-affinityactivity fell to almost undetectable level in 1d. Both uptakesystems exhibited maximum activity between pH 5 and 6. ¹ Present address: Tokyo Research Laboratories, Kyowa HakkoKogyo Co., Ltd., 3-6-6 Asahi-cho, Machida, Tokyo, 194 Japan.     

Nitrogen dynamics in lower Narragansett Bay, Rhode Island. I. Uptake by size-fractionated phytoplankton populations

The contribution of nanoplankton (< 10 µm fraction)to winter – spring (1977 – 78) and summer (1978,1979) phytoplankton nitrogen dynamics in lower NarragansettBay was estimated from ammonium, nitrate and urea uptake ratesmeasured by ¹⁵N tracer methods. During the winter – spring,an average of 80% of chlorophyll a and nitrogen uptake was associatedwith phytoplankton retained by a 10 µm screen. In contrast,means of 51 – 58% of the summer chlorophyll a standingcrops and 64 – 70% of nitrogen uptake were associatedwith cells passing a 10 µm screen. Specific uptake ratesof winter – spring nanoplankton populations were consistentlylower than those of the total population. Specific uptake ratesof fractionated and unfractionated summer populations were notsignificantly different. Ammonium uptake averaged between 50and 67% of the total nitrogen uptake for both the total populationand the < 10µm fraction. The total population and the10 µm fraction displayed similar preferences for individualnitrogen species. Though composed of smaller cells, flagellatedominated nanoplankton assemblages may not necessarily takeup nitrogen at faster rates than diatom dominated assemblagesof larger phytoplankters in natural populations. ¹Present address: Australian Institute of Marine Science, P.M.B.No. 3, Townsville M.S.O., Qld. 4810, Australia     

Carbon dynamics in the 'grazing food chain' of a subtropical lake

Studies were conducted over a 13 month period at four pelagicsites in eutrophic Lake Okeechobee, Florida (USA), in orderto quantify carbon (C) uptake rates by size-fractionated phytoplankton,and subsequent transfers of C to zooplankton. This was accomplishedusing laboratory ¹⁴C tracer methods and natural plankton assemblages.The annual biomass of picoplankton (<2 µm), nanoplankton(2–20 µm) and microplankton (<20 µm averaged60, 389 and 100 µg C 1^–1 respectively, while correspondingrates of C uptake averaged 7, 51 and 13 µg C1^–1h^–1. The biomass of microzooplankton (40–200 µm)and macrozooplankton (<200 µm averaged 18 and 60 µgC 1^–1, respectively, while C uptake rates by these herbivoregroups averaged 2 and 3 µg C 1^–1 h^–1. Therewere no strong seasonal patterns in any of the plankton metrics.The ratio of zooplankton to phytoplankton C uptake averaged7% over the course of the study. This low value is typical ofthat observed in eutrophic temperate lakes with small zooplanktonand large inedible phytoplankton, and indicates ineffectiveC transfer in the grazing food chain. On a single occasion,there was a high density (<40 1^–1) of Daphnia lumholrzii,a large-bodied exotic cladoceran. At that time, zooplanktoncommunity C uptake was <20 µg C 1^–1 h^–1and the ratio of zooplankton to phytoplankton C uptake was near30%. If D.lumholrzii proliferates in Lake Okeechobee and theother Florida lakes where it has recently been observed, itmay substantially alter planktonic C dynamics.     

Nitrate and ammonium uptake by plankton in an Amazon River floodplain lake

Uptake of ammonium and nitrate by plankton was measured in tropicalLake Calado, Brazil. Nitrate uptake was strongly influencedby light and was light saturated at {small tilde}340 µEm^–2 s^–1. In contrast, uptake of ammonium was lessinfluenced by light, and saturated at {small tilde}250 µEm^–2 s^–1. Uptake rates of both forms of nitrogenwere inhibited by up to 80% at light intensities higher thanthose required for saturation. Concentrations of ammonium andnitrate also had a strong influence on uptake rates. Half-saturationconstants (0.3–5 µM) were usually greater than ambientconcentrations (0.1–0.6 µM), indicating that uptakerates at ambient concentrations were less than one-half of thesaturated rates. Ammonium is the more important type of inorganicnitrogen for plankton of Lake Calado because nitrate concentrationsremain low to undetectable except during periodic inputs ofnitrate-rich water from the Amazon River. Using the observeddependence of uptake on concentration and light, maximum uptakerates per unit chlorophyll were computed to be in reasonableagreement with rates derived from P^B_m values for carbon uptake. ¹ Present address: Florida Department of Natural Resources,Marine Research Laboratory, St Petersburg, FL 33701, USA     

Dark uptake of inorganic14C in oligotrophic oceanic waters

Dark uptake of inorganic ¹⁴C by offshore plankton was measuredat two depths at 36 stations in the Atlantic Ocean from 52°Sto 26°N, mainly along 30°W. The samples were incubatedfor 2 h with and without inhibition of biological activity withHgCl₂. In addition, six time course experiments were performed.The mean dark uptake rate varied from 0.68 to 4.82 (µmolC m^–3 h^–1 over the transect and showed a significantpositive relationship with chlorophyll a. The dark uptake wasusually >5% of the maximum photosynthetic capacity (P^m),and higher values relative to P^m were associated with low valuesof P_m and not with high absolute dark values. A linear relationshipbetween dark uptake and P_m was found with a background value(y-axis intercept) of 0.51 (µmol C m^–3 h^–1and a slope of 0.77% of P^m. A major fraction of the dark signal,66–80% of the total signal, persisted in bottles treatedwith HgCl2, indicating that most of the dark signal was independentof biological activity. Time course experiments showed a lineardark uptake with time for the first hours, whereafter the uptakeceased. At stations with low concentrations of inorganic nitrogen[>1 (µmol (NH₄⁺+NO₃^–)], a second stage was observedafter 3–8 h, probably due to an increase in bacterialactivity. The results suggest three mechanisms for the darkvalue in short-term incubations in oligotrophic waters. A backgroundvalue independent of biomass and incubation time which was thedominant part of the dark signal in samples with very low phytoplanktonbiomass (>0.3 p-g Chi a 1"). Another important part was residualsof ¹⁴C associated with plankton, probably adsorbed to compoundsinside the cells. This fraction was dominant in short-term incubationsat chlorophyll concentrations >0.3 p.g Chi a H. Active uptakeby living cells (total minus ‘HgCl2 uptake‘) wasonly a minor part of the dark signal in short-term incubations,but dominated at longer incubation time (>3–9 h), probablydriven by an increase in bacterial activity. A significant enhancementof the non-photosynthetic uptake of ¹⁴C was observed in light,probably associated with a carbon-concentrating mechanism inphytoplankton or light stimulation of ß-carboxylationactivity. The results strongly suggest that dark values shouldbe subtracted from the light uptake. This correction is particularlyimportant when photosynthetic rates are low, e.g. at low lightor in short-term incubations where a time-zero background becomesa significant part of the total uptake in light. Present address: National Environmental Research Institute,Department of Marine Ecology and Microbiology, Frederiksborgvej399, PO Box 358, DK-4000 Roskilde, Denmark     

The Relationship between Metabolism and the 'Exchangeability' of Ions in Plant Tissues2

The uptake of the rubidium ion by well-washed disks of carrotparenchyma has been determined at 0·2° C and 25°C., in the presence and absence of 10^–4M. dinitrophenol,from solutions of rubidium chloride containing 0·5 and5·0 meq./l. Readily-exchangeable and non-exchangeablefractions were separately indentified. The lowering of temperature and application of DNP reduced themagnitude of both ion fractions at each of the two concentrationsof rubidium chloride. Despite the fact that the uptake of ionsinto an exchangeable form at 5·0 meq./l. was about 3times greater, the combined effect of low temperature and thepresence of DNP reduced this fraction by a relatively constantabsolute amount. Under the same conditions the uptake of ionsinto a non-exchangeable form from each concentration was reducedby approximately the same percentage. Over a 6-hour period the rate of uptake of rubidium into a non-exchangeableform at 25° C. was relatively constant, whereas at 0·2°C. there was an initial rapid uptake lasting for about 60 minutesfollowed by a slow steady uptake. The Q₁₀ of this latter processmeasured after 360 minutes was 2·3. It is concluded that an appreciable part of the capacity ofthe tissue to hold ions by exchange is dependent on concurrentmetabolism. The significance of measurements of exchangeability in the interpretationof mechanisms of ion uptake is discussed.     

Laboratory-measured grazing and ingestion rates of the salp, Thalia democratica Forskal, and the doliolid, Dolioletta gegenbauri Uljanin (Tunicata, Thaliacea)

Grazing and ingestion rates of laboratory-born Thalia democraticaaggregates and Dolioletta gegenbauri gonozooids, phorozooidsand oozooids were determined while fed Isochrysis galbana (4–5µm diameter) alone or in combination with Peridinium trochoideum(16–18 µm diameter) at concentrations of 0.15–0.70mm³ x 1^–1. Grazing rates (ml x zooid^–1 x 24 h ^–1)ranged from 10 to 355, and at zooid weights greater than 5 µgcarbon were in order oozooid > gonozooid > aggregate.Grazing rates increased exponentially with increasing zooidweight. Weight-specific grazing rates (ml x µgC^–1x 24 h^–1) were independent of the four-fold initial foodconcentration. Mean weight-specific grazing rates increasedlinearly with increasing zooid weight for the aggregates andoozooids, but gonozooid mean rates were independent of zooidweight. Aggregate and gonozooid ingestion rates (10⁶ µm³x zooid^–1 x 24 h^–1) ranged from 4 to 134 while oozooidrates ranged from 3 to 67. All ingestion rates were independentof the initial food concentration but increased linearly withincreasing zooid weight at similar rates. All mean weight-specificingestion rates (ml x µgC^–1 x 24 h^–1) wereindependent of zooid weight. The mean aggregate daily ration(µgC ingested x µg body C^–1) was 59% and themean doliolid ration was 132%. Field studies indicate that normalconcentrations of D. gegenbauri in the Georgia Bight clear theirresident water volume (1 m³) in about 4 months, but that highlyconcentrated, swarm populations which occur along thermohalinefronts clear their resident water volume in less than 1 day. ¹Current address: MacLaren Plansearch Ltd., P.O.Box 13250, sta.A.,St.John's, Nfld. A1B 4A5     

Estimation of thickness of airwaysurface liquid in ferret trachea in vitro

Duneclift, S., U. Wells, and J. Widdicombe. Estimationof thickness of airway surface liquid in ferret trachea in vitro. J. Appl. Physiol. 83(3): 761-767, 1997.The tracheae of ferrets and rabbits were mounted in vitro inorgan baths. While the tracheae were liquid filled, the permeabilitycoefficient ( P) was determined, and then while thetracheae were air filled, the percent clearance for^99mTc-labeleddiethylenetriaminepentaacetic acid (DTPA) was determined. The thicknessof airway surface liquid (ASL) was estimated by three methods.1) The initial concentration of^99mTc-DTPA and the total amount of^99mTc-DTPA (the sum of thatentering the outside medium, that draining from the trachea, and thatwashed out at the end of 40 min) gave the initial volume of ASL andthus its thickness. Mean values were 45.7 µm for the ferret and 41.9 µm for the rabbit. 2) Estimates ofASL thickness at the end of the 40-min period, based on the final^99mTc-DTPA concentration and theamount in the washout, were 42.9 µm for ferret and 45.4 µm forrabbit. 3) The ratio of Pto percent clearance gave mean ASL thickness values of 49.2 µm forthe ferret and 40.3 µm for the rabbit. Thus three separate methodsfor determining ASL thickness give very similar results, with means inthe range 40-49 µm. Administration of methacholine or atropineto ferret tracheae did not significantly change ASL thickness.

     

Dynamics of inorganic phosphorus in pelagic communities of the Sea of Okhotsk

Inorganic phosphorus uptake and regeneration in the OkhotskSea waters were investigated in July–August 1994 withthe use of radioisotopic techniques. The rates of PO₄-P uptakeby microplankton in the upper mixed layer were between 1.5 and6.6 µg P l^-1 day^-1 (average 2.75) in areas of diatom dominance,and between 0.68 and 1.68 µg P l^-1 day^-1 (average 1.16)in areas of intense warming and summer phytoplankton minimum.The residence time of PO₄-P standing stock in water at differentstations varied between 1.5 and 24 days (mean 9 days). The shareof bacterioplankton contributing to total PO₄-P uptake was 50%in areas of the summer phytoplankton minimum and 20–30%in areas of diatom dominance. The PO₄-P regeneration rate wasmeasured first time experimentally in the temperate sea. Itsrates varied from 0.30 to 1.65 µg P l^-1 day^-1. In areasof diatom dominance, it compensated with 30–60% of PO₄-Puptake. In zones of summer phytoplankton minimum and in thelayers of deep chlorophyll maxima at 10–25 m depths, thePO₄-P regeneration rate often exceeded its uptake. Primary phytoplanktonproduction correlated well with PO₄-P uptake values in the uppermixed layer, while no correlation was found between primaryproduction and the ambient PO₄-P content in water.     

Separate entry pathways for phosphate and oxalate in rat brain microsomes

ATP-dependent ⁴⁵Ca uptake in rat brainmicrosomes was measured in intracellular-like media containingdifferent concentrations of PO₄ and oxalate. In the absenceof divalent anions, there was a transient ⁴⁵Caaccumulation, lasting only a few minutes. Addition of PO₄did not change the initial accumulation but added a second stage that increased with PO₄ concentration. Accumulation during thesecond stage was inhibited by the following anion transport inhibitors: niflumic acid (50 µM),4,4'-dinitrostilbene-2,2'-disulfonic acid (DNDS; 250 µM),and DIDS (3-5 µM); accumulation during the initial stage wasunaffected. Higher concentrations of DIDS (100 µM), however,inhibited the initial stage as well. Uptake was unaffected by 20 mM Na,an activator, or 1 mM arsenate, an inhibitor of Na-PO₄ cotransport. An oxalate-supported ⁴⁵Ca uptake was larger,less sensitive to DIDS, and enhanced by the catalytic subunit ofprotein kinase A (40 U/ml). Combinations of PO₄ and oxalatehad activating and inhibitory effects that could be explained byPO₄ inhibition of an oxalate-dependent pathway, but notvice versa. These results support the existence of separate transportpathways for oxalate and PO₄ in brain endoplasmic reticulum.

     

A Comparison between the Uptake of Potassium by Plants from Solutions of Constant Potassium Concentration and during Depletion

A comparison was made between two methods of measuring the relationshipbetween the external [K⁺] and the flux of K⁺ into whole plantsof Lolium perenne and Raphanus sativus. The values of flux obtainedfrom solutions of 1.2 µM K⁺ held constant around the rootswere three and six times greater for Lolium and Raphanus respectivelythan the values obtained at the same concentration in a depletionexperiment in which the solutions, initially 100 µM K⁺,were depleted to below 1.2 µM K⁺ by plant uptake. In thedepletion experiment with Lolium, the flux was higher into plantsgrown at low [K⁺] than into plants grown at 100 µM eventhough [K⁺] within the plant was about the same for all groupsof plants. It is suggested that Lolium grown at low [K⁺] hasan efficient mechanism for K⁺ uptake which continues to operatefor some time after the plants have been transferred to a higherconcentration. With both species, K_m was 15–20 µMin the depletion experiment and below 1 µM when concentrationswere held constant.     

Intercellular Transport and Cytoplasmic Streaming in Chara hispida

The correlation between the velocities of cytoplasmic streamingand of translocation of ¹⁴C-photosynthate and ³²P-phosphateassociated radioactivity has been investigated in whole plantsof the green freshwater alga Chara hispida L. Tracer was suppliedto the plant's rhizoid system in a split-chamber. The velocityof cytoplasmic streaming of 52±3.3 µm s^–1compares with 57±10 µm s^–1 found for ¹⁴C-transportand 32±20 µm s^–1 found for ³²P-transport.There was no indication of intercellular translocation at avelocity faster than visible streaming. Cytochalasin B inhibitedthe translocation of ³²P and cytoplasmic streaming. CytochalasinB becomes fully effective in inhibiting streaming and transportafter an incubation time of at least 5 h. Key words: Chara hispida, Cytoplasmic streaming, Intercellular transport     

Characterization of transport mechanisms and determinants critical for Na+-dependent Pi symport of the PiT family paralogs human PiT1 and PiT2

The general phosphate need in mammalian cells is accommodated by members of the P_i transport (PiT) family (SLC20), which use either Na⁺ or H⁺ to mediate inorganic phosphate (P_i) symport. The mammalian PiT paralogs PiT1 and PiT2 are Na⁺-dependent P_i (NaP_i) transporters and are exploited by a group of retroviruses for cell entry. Human PiT1 and PiT2 were characterized by expression in Xenopus laevis oocytes with ³²P_i as a traceable P_i source. For PiT1, the Michaelis-Menten constant for P_i was determined as 322.5 ± 124.5 µM. PiT2 was analyzed for the first time and showed positive cooperativity in P_i uptake with a half-maximal activity constant for P_i of 163.5 ± 39.8 µM. PiT1- and PiT2-mediated Na⁺-dependent P_i uptake functions were not significantly affected by acidic and alkaline pH and displayed similar Na⁺ dependency patterns. However, only PiT2 was capable of Na⁺-independent P_i transport at acidic pH. Study of the impact of divalent cations Ca²⁺ and Mg²⁺ revealed that Ca²⁺ was important, but not critical, for NaP_i transport function of PiT proteins. To gain insight into the NaP_i cotransport function, we analyzed PiT2 and a PiT2 P_i transport knockout mutant using ²²Na⁺ as a traceable Na⁺ source. Na⁺ was transported by PiT2 even without P_i in the uptake medium and also when P_i transport function was knocked out. This is the first time decoupling of P_i from Na⁺ transport has been demonstrated for a PiT family member. Moreover, the results imply that putative transmembrane amino acids E⁵⁵ and E⁵⁷⁵ are responsible for linking P_i import to Na⁺ transport in PiT2. inorganic phosphate transport; retroviral receptor; SLC20     

Nitric oxide regulates oxygen uptake and hydrogen peroxide release by the isolated beating rat heart

Isolated rat heart perfused with 1.5-7.5µM NO solutions or bradykinin, which activates endothelial NOsynthase, showed a dose-dependent decrease in myocardial O₂uptake from 3.2 ± 0.3 to 1.6 ± 0.1 (7.5 µM NO, n = 18,P < 0.05) and to 1.2 ± 0.1 µM O₂ · min¹ · gtissue¹ (10 µM bradykinin, n = 10,P < 0.05). Perfused NO concentrations correlated with aninduced release of hydrogen peroxide (H₂O₂) inthe effluent (r = 0.99, P < 0.01). NO markedlydecreased the O₂ uptake of isolated rat heart mitochondria(50% inhibition at 0.4 µM NO, r = 0.99,P < 0.001). Cytochrome spectra in NO-treated submitochondrial particles showed a double inhibition of electron transfer at cytochrome oxidase and between cytochrome b andcytochrome c, which accounts for the effects in O₂uptake and H₂O₂ release. Most NO was bound tomyoglobin; this fact is consistent with NO steady-state concentrationsof 0.1-0.3 µM, which affect mitochondria. In the intact heart,finely adjusted NO concentrations regulate mitochondrial O₂uptake and superoxide anion production (reflected byH₂O₂), which in turn contributes to thephysiological clearance of NO through peroxynitrite formation.

     

The Water Permeability of Unplasmolysed Tissues2

1. The permeability of unplasmolysed cells of beetroot, v. ‘CrimsonGlobe’, was determined from the rate of water loss ofbeet slices on placing in sucrose solutions having O.P. greaterthan the suction pressure of the beet. The absolute values obtainedwere about 0?7µ³ water per µ² cell-surface per hourper atmosphere osmotic pressure difference, i.e. 0?7 µ/hr./atm.
2. The permeability of similar beet cells plasmolysed withintheircell walls was found to be about 13µ/hr./atm.
3. Thepermeability of beet cells which had been plasmolysed andallowedto recover was shown to be approximately the same asthat ofunplasmolysed cells.
4. The hypothesis is advanced that the increasein water permeabilityon plas-molysis is due to those partsof the plasma-membranewhich had formerly been pressed againstthe micelles of thecell wall becoming free and able to takepart in water transfer.
5. The energy requirement for the maintenanceof an excess hydrostaticpressure of five atmospheres withina cell by its vital activitywas shown to be about one-tenthof the total respiratory energyreleased in freshly cut beetslices.

     

Photoadaptation in Antarctic phytopfankton: variations in growth rate, chemical composition and P versus I curves

The response of phytoplankton to variations in the light regimewas studied during the VULCAN and ACDA cruises in the Antarctic.Unenriched batch cultures of 12–19 days' duration reachedchl concentrations of 10–50 µg^–1 and exhibitedexponential growth rates, with the maximal rate being 0.41 doubl,day^–1. Ice edge algae exhibited maximum growth rates atphoton flux densities (PFD) of 30–100 µE m^–2S^–1and the growth rate was reduced by about 30% at 500–1000µE m^–2S^–1 The chl/C ratio ranged between 0.004and 0.018, with the lowest ratios at PFDs above 500 µEm^–2S^–1 chl/C ratios were also below maximum at PFDsbelow 40–50 µE m^–2S^–1 The C:N:P ratioswere close to the Redfield ratios; the Si/C ratio averaged 0.16(atoms), and the ATP/C ratio averaged from 0.0024 to 0.0050in different culture senes. When thawed after having been frozenfor 10 days, shade-adapted cultures were in a much better conditionthan sun-adapted ones. P versus I data showed that the maximumassimilation number varied from 0.75 to 4.4 µg C (µgchl)^–1h^–1. It varied inversely with the chl/C ratio;therefore the maximum carbon turnover rate varied little betweensamples (0.024/0.035 h^–1). Low biomass communities exhibitedrelatively high values for (the initial slope of P versus Icurves), low values for 1_sat (160–330 µE m^–2S^–1),and they were susceptible to photoinhibition. In contrast, communitiesdominated by Odontella weissflogii exhibited low values for, a high value for I_sat (560 µE m^–2S^–1 andthey tolerated high PFDs. The photo-adaptational status of thephytoplankton in natural water samples is discussed relativeto the profile of water column stability and mixing processes.