The balance between photosynthesis and grazing in Antarctic mixotrophic cryptophytes during summer

SUMMARY 1. Grazing and photosynthetic contributions to the carbon balance of planktonic, mixotrophic cryptophytes in Lakes Fryxell and Hoare in the Taylor Valley, Antarctica were measured during November and December 2000.
2. The cryptophytes never became entirely photosynthetic, although carbon derived from grazing decreased in December. Individual grazing rates ranged between 5.28 and 10.08 bacteria cell⁻¹ day⁻¹ in Lake Fryxell and 0.36–11.76 bacteria cell⁻¹ day⁻¹ in Lake Hoare. Grazing rates varied temporally and with depth in the water column. In Lake Fryxell, which is a meromictic lake, highest grazing occurred just above the chemocline. Individual photosynthetic rates ranged from 0.23 to 1.35 pg C cell⁻¹ h⁻¹ in Lake Fryxell and 0.074 to 1.08 pg C cell⁻¹ h⁻¹ in Lake Hoare.
3. Carbon acquisition by the cryptophyte community gained through grazing ranged between 8 and 31% during November in Lake Fryxell, dropping to between 2 and 24% in December. In Lake Hoare grazing contributed 12–21% of the community carbon budget in November and 1–28% in December. Around 4% of the carbon acquired from grazing and photosynthesis was remineralised through respiration.
4. Mixotrophy is probably a major survival strategy for cryptophytes in the extreme lakes of the Dry Valleys, because perennial ice-cover severely limits light penetration to the water column, whereas these phytoflagellates are not normally mixotrophic in lower latitude lakes. The evidence suggests that mixotrophy may be a mechanism for supplementing the carbon budget, as well as a means of acquiring nutrients for growth.     

Bacterivory by starved marine heterotrophic nanoflagellates of two species which feed differently, estimated by uptake of dual radioactive-labelled bacteria

Abstract: The rates of ingestion of bacteria and of accumulation of bacterial biomass by hungry Pteridomonas danica and Paraphysomonas imperforata were measured using dual radioactive-labelled bacteria in experiments lasting 4–8 h. Pteridomonas continuously consumed 4–5 bacteria h⁻¹ throughout experiments lasting 8 h, irrespective of bacterial concentration above a threshold of about 5 × 10⁵ bacteria ml⁻¹, and continued to catch bacteria even below this density. The clearance rate of about 1 nl cell⁻¹ h⁻¹ at higher bacterial concentrations increased three or four times as bacterial numbers fell. Paraphysomonas cells, with only half the biomass of Pteridomonas , ingested up to 10 bacteria h⁻¹ at high bacterial concentrations, and gradually reduced the feeding rate, effectively ceasing to feed at 10⁶ bacteria ml⁻¹; their initial clearance rate of 1–2.5 nl cell⁻¹ h⁻¹ subsequently fell as low as 0.1 nl cell⁻¹ h⁻¹. Estimation of feeding rate by extrapolation from short-term experiments on such flagellates requires extreme caution. These flagellates, starved to levels typical of the natural environment, accumulated ingested bacterial biomass at an efficiency of between 16 and 21%, indicating that in nature they would recycle 80% or more of the nutrients contained in their food.     

A RE-EVALUATION OF CORALLINE RED ALGAL TAXONOMY USING ULTRA-STRUCTURAL INFORMATION

The marine dinoflagellate, Gymnodinium breve (Davis), produces several neurotoxins that cause neurotoxic shellfish poisoning (nsp), massive fish kills and respiratory irritation in marine mammals and humans. The common method for discerning toxic levels of G. breve for public health advisories is enumeration of live cells in a given water mass. In this study, laboratory cultures, as well as natural blooms, were added to a stirred ultra-filtration cell concentrator to separate viable cells containing intra-cell toxins from ambient water containing extra-cell toxins. Methods were validated using various mixtures of lysed and whole G. breve laboratory culture. Extractions and recovery of brevetoxins were done using a C-18 bonded-phase glass fiber extraction disc eluted with methanol. Total PbTx toxin concentrations were quantified by HPLC/UV using a C-18 column and an 85:15 methanol:water (1 ml min⁻¹) isocratic elution at 215 nm. This method of separation and extraction was subsequently applied to water samples collected during natural blooms along two different areas of the Florida Gulf coast. The results indicated that early stages of G. breve blooms contained primarily intra-cell toxins with extra-cell toxins increasing as the bloom progressed, even though very few viable G. breve cells were present. This suggests that enumeration of cells alone may be insufficient and additional toxin quantitation is necessary.     

Detection and quantification of Desulforhabdus amnigenus in anaerobic granular sludge by dot blot hybridization and PCR amplification

A species-specific 16S rRNA oligonucleotide probe (ASRB1) was developed for the detection of Desulforhabdus amnigenus in anaerobic granular sludge. The presence of nucleic acids from cells of D. amnigenus in granular sludge was determined using ASRB1 as a specific primer for polymerase chain reaction (PCR) amplification or as a probe for dot blot hybridizations. The detection threshold and the reproducibility of these two methods were determined with sludge amended with 10⁴–10¹⁰ D. amnigenus cells per gram of volatile suspended solids (VSS). For D. amnigenus cells with a ribosomal RNA content of 15 fg cell⁻¹, the lowest number of target cells detected by hybridization was 1 × 10⁸ cells g⁻¹ VSS. With the PCR amplification method the lowest number of target cells which could be detected was 1 × 10⁷ g⁻¹ VSS. This corresponds to a threshold level for hybridization of 0·1–0·001‰ of the total bacterial sludge population, while the threshold level obtained with the PCR approach amounted to 0·01–0·0001‰. The rRNA content of D. amnigenus was found to be affected by the growth rate and the growth phase, and it ranged from 19 fg cell⁻¹ in slow-growing cultures to 90 fg cell⁻¹ in fast-growing cultures. Therefore, the detection threshold of the dot blot hybridization method for fast-growing cells is lower than for slow-growing cells.     

Mixotrophic cryptophytes and their predators in the Dry Valley lakes of Antarctica

1. The ingestion rates of planktonic, mixotrophic cryptophytes in two perennially ice-covered Antarctic lakes in the McMurdo Dry Valleys, were investigated during the summer of 1997–1998.
2. In Lake Fryxell, which is meromictic, ingestion rates increased with depth in November and were highest in a cryptophyte maximum close to the chemocline. In Lake Hoare, which is unstratified and freshwater, there was no significant difference in ingestion rates with depth. In both lakes, the highest ingestion rates occurred in early summer, decreasing in December and January. Ingestion rates varied between 0.2 bacteria cell⁻¹ h⁻¹ and 3.6 bacteria cell⁻¹ h⁻¹.
3. During November, mixotrophic cryptophytes removed up to 13% of bacterial biomass day⁻¹ and had a greater grazing impact than heterotrophic nanoflagellates (HNAN). As summer progressed, the grazing impact of cryptophytes and HNAN became similar.
4. The maximum depth of cryptophytes in Lake Fryxell was predated by a population of the ciliate Plagiocampa. Plagiocampa had an ingestion rate of 0.13–0.19 cryptophytes cell⁻¹ h⁻¹. The grazing impact on the cryptophyte community was insignificant. However, the ciliate appeared to be indulging in temporary mixotrophy, sequestering the cryptophytes for a number of weeks before digesting them.
5. It is suggested that mixotrophy is an important survival strategy in the extreme lake ecosystems of the McMurdo Dry Valleys.     

Effect of acetate on growth and ammonium uptake in the microalga Scenedesmus obliquus

The effect of acetate on growth and rate of ammonium uptake in Scenedesmus obliquus (UTEX 78) was investigated under light-limiting conditions. Addition of acetate to autotrophic cells with a growth constant of 0.71 day⁻¹ resulted in an increase in the growth rate (mixotrophy, k = 1.3 day⁻¹), and in the presence of acetate, growth occurred in the dark (heterophy, k = 0.44 day⁻¹). The rate of ammonium uptake in autotrophy (17.8 amol cell⁻¹ min⁻¹) was similar to that in heterotrophy (17.4 amol cell⁻¹ min⁻¹) but was 3.7 times lower than that in mixotrophy (65.9 amol cell⁻¹ min⁻¹). In general, mixotrophic cells showed optimum ammonium uptake at the acetate concentration at which they were grown. In autotrophy, uptake of ammonium leveled off at about 12.5 μ M while no saturation was observed in mixotrophic cells. An increase in the rate of uptake of ammonium was observed in autotrophic cells within 1 h after the addition of acetate. The activity of isocitrate lyase (EC 4.1.3.1), a key enzyme for the regulation of the glyoxylate cycle responsible for acetate catabolism, showed a 3.9-fold increase in activity after 24 h in the dark in the presence of acetate. The level of isocitrate lyase activity in cells grown for 24 h in the dark in the presence of 0–20 m M acetate also increased as a function of acetate concentration.     

Inhibition of Maitotoxin-Induced Ca2+ Influx in Rat Glioma C6 Cells by Brevetoxins and Synthetic Fragments of Maitotoxin

Abstract: ⁴⁵Ca²⁺ influx in rat glioma C6 cells induced by 0.3 n M maitotoxin (MTX) was markedly inhibited by brevetoxin A (PbTx1) and brevetoxin B (PbTx2), with EC₅₀ values of 16 and 13 µ M , respectively. This inhibition was observed immediately after addition of MTX when monitored with fura-2, which suggests that PbTx2 directly blocks the action of MTX. This blockade by PbTx2 was not affected by tetrodotoxin, which excludes the involvement of voltage-sensitive sodium channels. The depolarizing effects of these brevetoxins were also not a likely cause of this inhibition, because melittin, a channel-forming peptide, did not significantly block MTX-induced ⁴⁵Ca²⁺ influx. Instead, this inhibition was thought to be mediated by blockade of an MTX-binding site by the brevetoxins, based on the fact that these toxins, particularly PbTx2, closely mimic the partial structure of MTX. Synthetic fragments of MTX corresponding to the hydrophilic EF-GH rings (200 µ M ) and LM-NO rings (500 µ M ) of MTX significantly reduced MTX-elicited Ca²⁺ influx. The observation that the effects of MTX were inhibited by structural mimics of both its hydrophobic and hydrophilic portions implies that both portions of the MTX molecule recognize its target.     

Availability, uptake and turnover of glycerol in hypersaline environments

Abstract A sensitive assay for glycerol and other polyols was developed, based on periodate oxidation to formaldehyde, followed by a colorimetric assay with 3-methyl-2-benzothiazolone hydrazone. Apparent glycerol concentrations thus measured in saltern crystallizer ponds were around 20–36 μM, while in the Dead Sea, during a Dunaliella bloom, values were up to 27 μM. However, these values probably overestimate the glycerol concentrations present, as shown by labeled glycerol uptake experiments. Values of [K + S_n] (natural concentration + affinity constant) in saltern ponds were as low as 0.76–1.4 μM, with V_max values of 193–303 nmol 1⁻¹h⁻¹, and turnover times between 2.6–7.2 h at 35°C. Similar measurements in the Dead Sea were: [K + S_n] 0.07–1.41 μM, V_max values 160–426 nmol 1⁻¹h⁻¹, and turnover times in the range of 0.45–3.3 h.     

Winter Ciliates in a British Columbian Fjord: Six New Species and an Analysis of Ciliate Putative Prey

ABSTRACT. This work provides the first study of North Pacific planktonic ciliates by quantitative protargol staining. Triplicate water bottle samples were collected at a depth of 2 m (above the shallow pycnocline) at six stations in Indian Arm, British Columbia, on February 15, 1990, and February 26, 1991. Thirty-six ciliate species were observed. Six new species are described from protargolstained specimens: Strombidium lynni n. sp., Strombidium taylori n. sp., Strombidium basimorphum n. sp., Slrombidiurn ventropinnum n. sp., Strobilidium undinum n. sp., and Urotricha cyrtonucleata n. sp.
Ciliate abundance varied significantly (ANOVA, α= 0.05) between sampling sites, ranging from 550 to 6,800 cells/liter in 1990 and from 1,800 to 7,900 cells/liter in 1991. Biomass also varied significantly (ANOVA, α= 0.05) ranging from 3.7 × 10⁵ to 3.3 × 10⁶ pg carbon/liter in 1990 and 3.04 × 10⁶− 6.97 × 10⁶ pg carbon/liter in 1991. Putative prey were enumerated in three size fractions (1.5–5 μm, 5–10 μm and 10–25 μm). The source of variation in ciliate abundance and biomass was not identified. Parameters of salinity, temperature, putative prey, chlorophyll a and pycnocline depth did not significantly correlate with ciliate biomass or abundance (α= 0.05).     

Stability and conjugal transfer kinetics of a TOL plasmid in Pseudomonas aeruginosa PAO 1162

Abstract Batch mating experiments were employed to study the kinetics of the conjugal transfer of a TOL plasmid, using the transconjugant strain Pseudomonas aeruginosa PAO 1162 (TOL) as the plasmid donor and Pseudomonas putida PB 2442 and Pseudomonas aeruginosa PAO 1162N as the plasmid recipients. Transfer rates from PAO 1162 (TOL) to PAO 1162N and PB 2442 measured for exponentially grown PAO 1162 (TOL) were 1.81 × 10⁻¹⁴ (standard error (S.E.) 1.25 × 10⁻¹⁵) ml·cell⁻¹min⁻¹ and 3.32 × 10⁻¹³ (S.E. 4.42 × 10⁻¹⁴) ml·cell⁻¹min⁻¹, respectively. The instability of the TOL plasmid in PAO 1162 (TOL) was evaluated under conditions that were non-selective for maintenance of the TOL catabolic functions. The measured rates of instability were 6.7 10⁻⁶ to 8.3 10⁻⁶ min⁻¹, and the loss of the catabolic functions was mainly caused by structural instability of the plasmid.     

Ferric iron-reducing Shewanella putrefaciens and N2-fixing Bradyrhizobium japonicum with uptake hydrogenase are unable to oxidize atmospheric H2

Abstract Bradyrhizobium japonicum and Shewanella putrefaciens were unable to oxidize hydrogen at atmospheric concentrations (0.55 ppmv), neither in suspension nor when added to sterile soil. The K _m-value of S. putrefaciens for H₂ (39 ppmv in gas phase, 0.22 μM in aqueous phase), using Fe(III) as electron acceptor, showed a 4–5-fold higher affinity for H₂ than that of B. japonicum (1200 ppmv; 0.84 μM) or other hydrogen-oxidizing bacteria. However, the V _max (4.54 fmol H₂ h⁻¹ cell ⁻¹) and threshold (> 0.5 ppmv; 0.35 nM) of S. putrefaciens and the V _max (7.19 fmol H₂ h⁻¹ cell⁻¹) and threshold (> 0.5 ppmv; 0.35 nM) of B. japonicum were in the same order of magnitude as data for Knallgas bacteria from relevant literature. To enable hydrogen oxidation in soil the soil-samples with S. putrefaciens even had to be supplemented with Fe(III). Fresh soil, on the other hand, oxidized hydrogen very efficiently below atmospheric mixing ratios, demonstrating that there must be other oxidation activities in soil.     

8 Grazing by heterotrophic nanoflagellates on virus- and bacteria-sized particles in two lakes of different trophy

Although viruses are now widely recognized to infect aquatic bacteria as well as prokaryotic and eukaryotic phytoplankton, our understanding of how they fit into aquatic foodwebs remains still deficient. The present study examined the potential nutritional food source that viral particles represent for natural assemblages of heterotrophic nanoflagellates (HNF). We determined the seasonal and depth-related variability in the grazing activity of HNF on virus- and bacteria-sized particles in the oligomesotrophic Lake Pavin and the eutrophic Lake Aydat. Ingestion rates were determined using 50 and 500 nm diameter fluorescent microspheres. Estimated ingestion rates ranged from 0.01 to 1.7 viruses cell⁻¹·h⁻¹ (Aydat) and from 0.01 to 2 viruses cell⁻¹·h⁻¹ (Pavin). Derived clearance rates for viruses represented 3–5% (Aydat) and 10–12% (Pavin) of those for bacteria. In general, HNF grazing on both viruses and bacteria showed a similar pattern characterized by an apparent decrease in summer followed by autumnal peaks, with lowest values always being recorded in the hypolimnion. Viral production, estimated from the frequency of visibly infected cells (using transmission electronic microscopy), was consumed by HNF at rates averaging 2% (Aydat) and 10% (Pavin). This study suggests that, viruses, which are assumed to correspond to 1×10⁻⁷ ng C/particle, are likely to be of low nutritive value for HNF in both lakes. However, these results imply that HNF grazing may contribute significantly to the removal of viruses in freshwaters, especially in low productive systems.     

Induction of nitrate reductase in needles of Scots pine seedlings by NOX and NO3−

The possibility to induce nitrate reductase (NR; EC 1.6.6.2) in needles of Scots pine ( Pinus sylvestris L.) seedlings was studied. The NR activity was measured by an in vivo assay. Although increased NR activities were found in the roots after application of NO₃⁻, no such increase could be detected in the needles. Detached seedlings placed in NO₃⁻ solution showed increasing NR activities with increasing NO₃⁻ concentrations. Exposure of seedlings to NO_x (70–80 ppb NO₂ and 8–12ppb NO) resulted in an increase of the NR activity from 10–20 nmol NO₂⁻ (g fresh weight)⁻¹ h⁻¹ to about 400 nmol NO₂⁻ (g fresh weight)⁻¹ h⁻¹. This level was reached after 2–4 days of exposure, thereafter the NR activity decreased to about 200 nmol NO₂⁻ (g fresh weight)⁻¹ h⁻¹. Analyses of free amino acids showed low concentrations of arginine and glutamine in NO_x-fumigated seedlings compared to corresponding controls.     

Thermoregulation and metabolism in the Cape golden mole (Insectivora: Chrysochloris asiatica)

The Cape golden mole, Chrysochloris asiatica is an insectivore which excavates superficial foraging burrows as it searches for its food. It has a mean (±S.D.) resting metabolic rate (RMR) when newly captured of 1–17±0.17 cm³ O₂g^-1 h^-1 ( n = 14), within the thermoneutral zone (TNZ) of 30–32°C.
The body temperature (Tb) of the mole in the TNZ is low 32.9 ± 0.36 ( n = 14) and remains stable at ambient temperatures (Tas) from 28–32°C. Above 32°C (range 34–37°C), Tb increases albeit slightly to 36 ± 1.75°C ( n = 14). The conductance is high 0.27 ± 006cm³ O₂g^-1 h^-l°C^-1 ( n = 46) at the lower limit of thermoneutrality. The mean RMR at 9°C (the lowest Ta tested) was 4.82±11 cm³ O₂g^-1h^-1, which is 4.1 times that of the RMR in the TNZ.
At an ambient temperature of 9°C, three of the golden moles entered a state of torpor where the RMR was reduced from 5.9±0.56 to 10 1.0 ± 0.69cm³O₂g^-1h^-1.     

The occurrence and ecological importance of dissolved ATP in fresh water

SUMMARY. Dissolved ATP, defined as ATP which passes through 0.2 μm filters, was found in fresh water. During the spring diatom bloom in two eutrophic Danish lakes, concentrations of dissolved ATP varied between 0.1 and 3.8 μgl⁻¹, constituting 14–76% of the total ATP (particulate plus dissolved ATP). The kinetics of the light emission obtained from mixing firefly enzyme with dissolved ATP demonstrated that the major proportion of the dissolved ATP was in fact ATP. Despite some variations, the seasonal changes in dissolved ATP paralleled the changes in the increasing phytoplankton population during the rise of the diatom blooms. The dissolved ATP increased after the diatom peak, indicating that release of ATP from the phytoplankton due to mortality may be a major source of dissolved ATP.
Consumption of dissolved ATP was evaluated in uptake experiments using ³H-ATP. Rates of uptake of ³H-ATP by micro-organisms (diameter 0.2–0.6 μm) proved to be close to the rates for ³H-D-glucose uptake. The variations in ³H-ATP uptake during the diatom blooms showed non-systematic changes and ranged between 1.0 and 15.8% h⁻¹ (mean = 4.9% h⁻¹) of the quantity added. Turnover rates for dissolved ATP varied between 12 and 730 ng l⁻¹ h⁻¹ (mean = 175 ng l⁻¹). These rather high rates of turnover suggest that dissolved ATP is an important compound in the metabolism of freshwater bacteria.     

Comparison of epilithic and epixylic biofilm development in a boreal river

SUMMARY. 1. We assessed substratum effects on lotic biofilm development by placing glass and white pine sampling units in a fourth-order boreal river, and analysing, at 6-week intervals, upper-surface biofilms for ATP, chlorophyll, ergosterol, and the activities of nine exoenzymes.
2. All parameters, except chlorophyll standing stock (range 80–320 μg dm⁻²) and β-xylosidase activity (range 0.4–4.8 μmol h⁻¹ dm⁻²), were significantly greater for epixylic biofilms than for epilithic ones, but the magnitude of the increases varied from 2 to 5 fold, showing that, even under similar hydrodynamic conditions, epilithic and epixylic biofilms are structurally and functionally distinct. For example, ergosterol concentrations ranged from undetectable to 0.93 μg dm⁻² for epilithon and from 11–49 μg dm⁻² for epixylon; corresponding ranges for ATP were 1.6–3.7 (epilithon) and 4.2–7.7 μg dm⁻² (epixylon), for acid phosphatase activity: 2.3–4.9 and 20–41 μmolh⁻¹dm⁻², and for alkaline phosphatase activity: 1.9–8.1 and 29–150 μmol h⁻¹dm⁻², respectively.
3. The more extensive epixylic development was attributed to utilization of the wood substratum as a supplemental carbon source and to a higher density of microbial attachment sites.     

Characterization of two virulent Lactobacillus fermentum bacteriophages isolated from sour dough

Two different bacteriophages, FE5-B1 and Z63-B1, active against strains of Lactobacillus fermentum were isolated from a sample of sour dough of a regional wheat bread. They showed different host specificities when tested against 58 strains of obligately heterofermentative lactic acid bacteria, as well as differences in adsorption and one-step growth kinetics. The burst size of FE5-B1 was about 100 pfu cell⁻¹. This phage belonged to the A₁ morphotype of Myoviridae family, having an icosahedral head (83 nm diam.) and a sheathed contractile tail (170 nm in length). The phage consisted of five major structural proteins and had a genome of 86 kbp. Z63-B1 showed a burst size of 10 pfu cell⁻¹ and belonged to the B₁ morphotype or Siphoviridae family. Z63-B1 had an isometric head (60 nm diam.) and a non-contractile tail (160 nm in length), with eight major different structural proteins and a genome of 32 kbp.     

Activity of methanotrophic bacteria in Green Bay sediments

Abstract Sediment pore water samples obtained from a 19 m station in Green Bay in Lake Michigan were examined for levels of ambient dissolved methane and copper, and for the potential for in situ methane oxidation by methanotrophs found within surface sediments. The in situ methane concentration in the upper oxic sediment layer ranged from 20–150 μmol · 1⁻¹ at this station. The activity of methanotrophs and the kinetics of methane oxidation in these sediments were demonstrated by the uptake of radiolabeled methane. K_s values varied between 4.1–9.6 nmol · cm³ of sediment slurry. High V_max values (12.7–35.2 nmol · cm⁻³ · h⁻¹) suggest a large population of methanotrophs in the sediments. An average methane flux to the oxic sediments of 0.24 mol · m⁻² · year⁻¹ was calculated from the pore water methane gradients. Pore water concentrations of copper in the upper sediment layer ranged from 10–120 nmol · 1⁻¹. Based upon the copper concentration, other measured parameters, and equilibrium conditions defined by WATEQF4, an estimate for dissolved free Cu²⁺ concentration of 5–38 nmol · 1⁻¹ pore water was obtained. Several factors control the rate of methane oxidation, including oxygen, methane, and the bioavailability of free Cu²⁺.     

Growth and physiological changes during metamorphosis of Senegal sole reared in the laboratory

The metamorphosis of Solea senegalensis was studied in larvae reared at 20° C and fed four different feeding regimes. A, Artemia (4 nauplii ml⁻¹); B, Artemia (2 nauplii ml⁻¹); C, mixed diet (2 nauplii ml⁻¹ and 3 mg ml⁻¹ microencapsulated diet); and D, microencapsulated diet (3·7 mg ml⁻¹). Rotifers were also supplied in all cases during the first days of feeding. These feeding regimes supported different growth rates during the pre-metamorphosis period (regime A, G=0·376 day⁻¹; regime B, G=0·253 day⁻¹; regime C, G=0·254 day⁻¹; regime D, G=0·162 day⁻¹). Larvae started metamorphosis 9 days after hatching (DAH) when fed the regime A, 13 DAH with regime B, 11 DAH with regime C and 15 DAH with regime D. A minimum 5·6–5·9 mm L_T was required under all feeding regimes to initiate the metamorphosis. Eye translocation was completed when the larvae reached 8·6–8·7 mm L_T (regimes A, B and C), but only 7·3 mm L_T with regime D. 4·4–6·2 days were required to complete eye migration under the regimes A, B and C, and 18·3 days under the regime D. This transformation is concomitant with changes in body reserves, and with the pattern of some digestive enzymes.     

Rubidium Uptake and Accumulation in Peripheral Myelinated Internodal Axons and Schwann Cells

Abstract: To study mechanisms of K⁺ transport in peripheral nerve, uptake of rubidium (Rb⁺), a K⁺ tracer, was characterized in rat tibial nerve myelinated axons and glia. Isolated nerve segments were perfused with zero-K⁺ Ringer's solutions containing Rb⁺ (1–20 m M ) and x-ray microanalysis was used to measure water content and concentrations of Rb, Na, K, and Cl in internodal axoplasm, mitochondria, and Schwann cell cytoplasm and myelin. Both axons and Schwann cells were capable of removing extracellular Rb⁺ (Rb⁺_o) and exchanging it for internal K⁺. Uptake into axoplasm, Schwann cytoplasm, and myelin was a saturable process over the 1–10 m M Rb⁺_o concentration range, although corresponding axoplasmic uptake rates were higher than respective glial velocities. Mitochondrial accumulation was a linear function of axoplasmic Rb⁺ concentrations, which suggests involvement of a nonenzymatic process. At 20 m M Rb⁺_o, a differential stimulatory response was observed; i.e., axoplasmic Rb⁺ uptake velocities increased more than fivefold relative to the 10 m M rate, and glial cytoplasmic uptake rose almost threefold. Finally, Rb⁺_o uptake rate into axons and glia was completely inhibited by ouabain (2–4 m M ) exposure or incubation at 4°C. These results suggest that Rb⁺ uptake into peripheral nerve internodal axons and Schwann cells is mediated by Na⁺,K⁺-ATPase activity and implicate the presence of axonal- and glial-specific Na⁺ pump isozymes.