Ionic Currents across the Plasmalemma of Chara inflata Cells: III. WATER-RELATIONS PARAMETERS AND THEIR CORRELATION WITH MEMBRANE ELECTRICAL PROPERTIES

The water-relations parameters of Chara inflata cells were determineddirectly using the micro pressure probe technique. The turgorpressure of cells in artificial pond water (₀ = 0.06 MPa) wasabout 0.65 MPa and the half-time (T_1/2) for water exchange wasabout 6.5 s. The calculated values of the hydraulic conductivity(L_P) were in the range 1–2 ? 10^–6m s^–1 (MPa)^–1.The volumetric elastic modulus () was 32.8 MPa for turgor rangingfrom 0.77 to 0.82 MPa. Large changes in the water-relations parameters and the electricalproperties of the membrane occurred when the turgor was decreasedto low values. These changes included: (i) a decrease in theT_1/2 for water exchange, (ii) an increase in L_P and (iii) depolarizationof the membrane potential difference (V_m). The micro pressure probe, which enabled the turgor pressureof the cell to be altered, was used in combination with thevoltage-clamp technique to determine the relationship betweenK⁺ and Cl^– conductances of the plasmalemma and the cellturgor. The K⁺ conductance increased reversibly as the turgorwas reduced in the range 0 to 0.6 MPa and the Cl^– -conductanceincreased as the turgor was reduced in the range 0.1 to 0.5MPa. It is suggested that these pressure-dependent K⁺ and Cl^–conductances may have a dual role in electrical events and thenon-electrical responses such as changes in the cell volume. Key words: Chara inflata, membrane conductances, ion channels, water-relations parameters     

Ionic Currents across the Plasmalemma of Chara inflata Cells: II. EFFECTS OF EXTERNAL Na+, Ca2+ AND Cl- ON K+ AND Cl CURRENTS

The electrical conductance of the plasmalemma of cells of Charainflata, due to the diffusion of ions, consists predominantlyof K⁺, Cl^– and leak components. When the membrane electricalpotential difference is stepped in a negative direction witha voltage-clamp, the resulting inward current has componentsI_K, I_Cl and I_L (leak). During such voltage-clamp steps I_K isinactivated, and Ic activated with voltage-dependent half-times.Increases in the external NaCl concentration reduce the magnitudeof I_K and increase the magnitude of I_c, but reduce the half-timeof inactivation or activation. The NaCl-induced changes in I_kand I_Cl and their kinetics were more pronounced at pH₀ =6.5than at pH₀ =9.5. When the concentration of external CaCl₂ wasincreased, I_k, I_Cl and the half-time of inactivation, (T_1/2),of I_k were all reduced. The half-time of activation of I_Cl wasincreased. The NaCI-induced changes could result from increases in bothexternal ion concentration and osmotic pressure. Previous experimentshave shown that an increase in external osmotic pressure alonealters the properties of the conductances. In this paper weattempt to separate the purely ionic effects from the osmoticones. Key words: Chara inflata, ionic effects, K⁺ and Cl^– currents     

Past and present distribution, densities and movements of blue whales Balaenoptera musculus in the Southern Hemisphere and northern Indian Ocean

• 1 Blue whale locations in the Southern Hemisphere and northern Indian Ocean were obtained from catches (303 239), sightings (4383 records of ≥8058 whales), strandings (103), Discovery marks (2191) and recoveries (95), and acoustic recordings.
• 2 Sighting surveys included 7 480 450 km of effort plus 14 676 days with unmeasured effort. Groups usually consisted of solitary whales (65.2%) or pairs (24.6%); larger feeding aggregations of unassociated individuals were only rarely observed. Sighting rates (groups per 1000 km from many platform types) varied by four orders of magnitude and were lowest in the waters of Brazil, South Africa, the eastern tropical Pacific, Antarctica and South Georgia; higher in the Subantarctic and Peru; and highest around Indonesia, Sri Lanka, Chile, southern Australia and south of Madagascar.
• 3 Blue whales avoid the oligotrophic central gyres of the Indian, Pacific and Atlantic Oceans, but are more common where phytoplankton densities are high, and where there are dynamic oceanographic processes like upwelling and frontal meandering.
• 4 Compared with historical catches, the Antarctic (‘true’) subspecies is exceedingly rare and usually concentrated closer to the summer pack ice. In summer they are found throughout the Antarctic; in winter they migrate to southern Africa (although recent sightings there are rare) and to other northerly locations (based on acoustics), although some overwinter in the Antarctic.
• 5 Pygmy blue whales are found around the Indian Ocean and from southern Australia to New Zealand. At least four groupings are evident: northern Indian Ocean, from Madagascar to the Subantarctic, Indonesia to western and southern Australia, and from New Zealand northwards to the equator. Sighting rates are typically much higher than for Antarctic blue whales.
• 6 South‐east Pacific blue whales have a discrete distribution and high sighting rates compared with the Antarctic. Further work is needed to clarify their subspecific status given their distinctive genetics, acoustics and length frequencies.
• 7 Antarctic blue whales numbered 1700 (95% Bayesian interval 860–2900) in 1996 (less than 1% of original levels), but are increasing at 7.3% per annum (95% Bayesian interval 1.4–11.6%). The status of other populations in the Southern Hemisphere and northern Indian Ocean is unknown because few abundance estimates are available, but higher recent sighting rates suggest that they are less depleted than Antarctic blue whales.

     

A SIMPLE METHOD FOR TESTING THE TOXICITY OF VOLATILE ANTISEPTICS TO WOOD-ROTTING FUNGI

Methods used for determining toxicity of volatile compounds to fungi are reviewed and a simple laboratory method for carrying out such tests is described.
Results from this type of test may be applicable in practice where the mycelium of the fungus is freely exposed to the action of the vapour, but if it is desired to sterilize infected wood of any appreciable thickness, information about the penetration of the vapour across the grain of the wood and of its sorption by the wood must be obtained before any treating schedule can be drawn up.     

Microbial growth and detritus transformations during decomposition of leaf litter in a stream

SUMMARY. 1. Despite the widely accepted importance of bacteria and fungi in degrading detritus in aquatic ecosystems there is still very little quantitative information on the abundance and dynamics of these microorganisms. Using epifluorescent microscopy, we measured the biomass of bacteria and fungi during decomposition of three types of leaf detritus. Bacterial production was determined from the rate of incorporation of ³H-thymidine into DNA.
2. The transformation of leaf carbon into dissolved organic carbon and fine particulate organic carbon was followed in order to compare the amounts of leaf material that were converted into these 'end-products' of decomposition versus the amount converted into microbial biomass.
3. The amount of microbial carbon in the leaf-detritus complex never exceeded 5.2% of the total carbon, and fungal biomass was always much greater than bacterial biomass. Despite the greater standing stock of fungi, the rapid turnover of bacteria (doubling about once per day) implies that their role in degrading leaf litter or as a food source for detritivores might be as great as for fungi.
4. Removal of microbial biomass from leaf litter may occur as release of fungal spores and consumption or shedding of bacterial biomass. Fungal spores can be a significant part of the fine particulate organic carbon released from leaf detritus and potentially represent an important food resource for filter-feeding organisms.     

Exoenzyme activities as indicators of dissolved organic matter composition in the hyporheic zone of a floodplain river

1. We measured the hyporheic microbial exoenzyme activities in a floodplain river to determine whether dissolved organic matter (DOM) bioavailability varied with overlying riparian vegetation patch structure or position along flowpaths. 2. Particulate organic matter (POM), dissolved organic carbon (DOC), dissolved oxygen (DO), electrical conductivity and temperature were sampled from wells in a riparian terrace on the Queets River, Washington, U.S.A. on 25 March, 15 May, 20 July and 09 October 1999. Dissolved nitrate, ammonium and soluble reactive phosphorus were also collected on 20 July and 09 October 1999. Wells were characterised by their associated overlying vegetation: bare cobble/young alder, mid‐aged alder (8–20 years) and old alder/old‐growth conifer (25 to >100 years). POM was analysed for the ash‐free dry mass and the activities of eight exoenzymes (α‐glucosidase, β‐glucosidase, β ‐N‐acetylglucosaminidase, xylosidase, phosphatase, leucine aminopeptidase, esterase and endopeptidase) using fluorogenic substrates. 3. Exoenzyme activities in the Queets River hyporheic zone indicated the presence of an active microbial community metabolising a diverse array of organic molecules. Individual exoenzyme activity (mean ± standard error) ranged from 0.507 ± 0.1547 to 22.8 ± 5.69 μmol MUF (g AFDM)^?1 h^?1, was highly variable among wells and varied seasonally, with the lowest rates occurring in March. Exoenzyme activities were weakly correlated with DO, DOC and inorganic nutrient concentrations. 4. Ratios of leucine aminopeptidase : β‐glucosidase were low in March, May and October and high in July, potentially indicating a switch from polysaccharides to proteins as the dominant component of microbial metabolism. 5. Principal components analysis indicated that there were patch effects and that these effects were strongest in the summer. 6. DOM degradation patterns did not change systematically along hyporheic flowpaths but varied with overlying forest patch type in the Queets River hyporheic zone, suggesting that additional carbon inputs exist. We hypothesise that the most likely input is the downward movement of DOM from overlying riparian soils. Understanding this movement of DOM from soils to subsurface water is essential for understanding both the hyporheic metabolism and the carbon budget of streams and rivers.