Measured and Calculated Transpiration in Trifolium repens under Different Water Potentials

The relationship between transpiration measured gravimetrically,a generalized transpiration equation, and the ratio VPD/r_leafwas investigated in Trifolium repens plants subjected to varyingwater potentials. Dawn leaf water potential was measured witha pressure chamber, leaf diffusion resistance with a diffusionporometer, leaf temperatures with a thermistor, and relativehumidity with an aspirated psychrometer. During drought transpirationrates determined by both methods were quite similar particularlyat the lowest water potentials. After rewatering calculatedrates were somewhat higher than measured ones. It is concludedthat transpiration calculated by the indirect method is a usefuland reasonable estimate of transpiration for single plants undervarying water potentials.     

The Regulation of the Water Potential Gradient in the Host and Parasite Relationship betweenSorghum bicolorandStriga hermonthica

A glasshouse experiment was carried out to investigate the factorscontrolling the abstraction of xylem fluid from its host bythe parasiteStriga hermonthica(Scrophulariaceae).Strigahad amean daily transpiration rate far exceeding that of its hostsorghum (Sorghum bicolor), with infestation byStrigaalso shownto lower the transpiration rate of the host. Stopping the host'stranspiration was shown to decrease the transpiration rate ofthe parasite. Stopping the parasite's transpiration only gavean initial increase in the host's transpiration rate which wasnot sustained. The parasite had a lower water potential thanits host, values being -0.42 MPa and -0.23 MPa, respectively,and an accompanying higher osmotic pressure of 0.68 MPa against0.51 MPa for sorghum. Modifying the water potential gradientby bagging both partners together showed that the differentialin osmotic pressure and water potential was largely maintainedby the parasite's higher rate of transpiration. A favourablewater potential gradient towards the parasite still existedfollowing the cessation of transpiration, this being generatedby the haustorial resistance to hydraulic conductivity whichwas found to be some 1.5–4.5 times greater than that offeredby the parasite shoot. Both the high rate of transpiration andthe increased resistance across the haustoria would appear tobe necessary means to facilitate the diversion of host resourcesto the parasite.Copyright 1997 Annals of Botany Company Striga hermonthica; sorghum; water relations; haustorium; root parasite     

Transition from Water to Land in Isopod Crustaceans

The fossil record of land isopods is of little help in tracingthe evolution of their terrestrial adaptations; however, wecan usefully correlate the traits of various extant specieswith their various environments. Loss of cuticular water variesgreatly between species, generally in relation to habitat, althoughthe mechanism restricting loss is unclear. Both endocuticularand epicuticular barriers have been reported, the latter inVenizillo arizonicus. Pseudotracheae are advantageous for respirationin dry air, but again the mechanism is not clear. Excess nitrogenis excreted mainly as ammonia gas. Wide osmotic variation inthe hemolymph resulting from dehydration is tolerated. Lethaltemperatures vary in general according to habitat, and are affectedby size, humidity, permeability of the cuticle, and previoustemperature history. Evaporative cooling is sometimes of survivalvalue for short periods. Metabolic rate is affected by season,and both long photoperiod and high temperatures are necessaryfor gonadal development and breeding. Responses to light, temperature,and humidity are more labile than previously thought. A peripheralhygro-receptor has tentatively been identified. The mechanismof bunching is largely thigmotactic, but olfaction may playa part, as it does in shelter-seeking. More information is nowavailable about the micro-climates of habitats. In Porcellioscaber, nightly activity on trees in some situations permitselimination of excess water by transpiration. In Armadillidiumvulgare nightly activity is greater in moister air, and drowningis a density-dependent mechanism for population control duringheavy rains. Isopods are successful as land animals. Furtherstudy of population and distribution limits by combined ecologicaland physiological methods would be fruitful.     

Photosynthesis and Transpiration in Leaves and Ears of Wheat and Barley Varieties

Carbon exchange rate (CER) and transpiration were measured inflag leaves, whole ears, glumes (referring to the total areaof glumes and lemmas) and awns, in six hexaploid spring wheats(Triticum aestivum L.), three cultivated tetraploid spring wheats(T. turgidum L.), four wild tetraploid wheats (T. dicoccoides),eight six-rowed barleys (Hordeum vulgare L.) and five two-rowedbarleys (H. vulgare L.). Differences between varieties and between species in total earCER and transpiration were associated largely with differencesin ear surface area rather than with rates per unit area. Ratesof CER and transpiration per unit area of ears were 40–80%of those of flag leaves, depending on the species. However, since ear surface area was greater than flag leaf areaby a factor of 1.1, 3.9, 5.5 and 4.4, in hexaploid wheat, tetraploidwheat, six-rowed barley, and two-rowed barley, respectively,total ear CER reached up to 90% of that of the flag leaf. The contribution of awns to total ear CER depended largely ontotal awn surface area per ear, rather than on CER per unitawn area. Awns contributed about 40–80% of total spikeCER, depending on the species, but only 10–20% of spiketranspiration. The disproportionately small contribution ofawns to ear transpiration was caused by the very low rate oftranspiration per unit area of awns. Thus, while transpirationratio (CER/transpiration) was about the same in flag leavesand glumes, it was higher by several orders of magnitude inthe awns. A large amount of awns in the ear is therefore a drought adaptiveattribute in these cereals, for which tetraploid wheat exceededhexaploid wheat and six-rowed barley exceeded two-rowed barley. Key words: Carbon exchange rate, Transpiration, Barley, Wheat     

Transpiration and water uptake of Senecio medley-woodii and Aloe jucunda under changing environmental conditions: measurements with a potometric water-budget-meter

Transpiration, water uptake by the roots and CO₂ exchange oftwo leaf succulents, Senecio medleywoodii (Asteraceae) and Aloejucunda (Asphodeliaceae), were monitored simultaneously andcontinuously with a gas exchange cuvette combined with an apparatusto quantify water uptake (= waterbudget- meter). Measurements,which are primarily valid for plants with a sufficient watersupply, were made with the same plant for up to 29 consecutivedays. Ambient air temperature varied between 17 and 35 C witha constant dewpoint temperature of 13C of the ambient air anda 12 h photoperiod at 400–500mol m^–2s^–1 photonirradiance. The net water flux (J_w(net)=water uptake–transpiration)and the water balance (J_w(net) integrated for a timespan) werecalculated. Various tests were made to determine the accuracyof the measurements made with this rather complex equipment.In most cases the errors for transpiration and uptake rateswere much lower than 8% determined under the conditions of drastically(about 10 K per 30 min) increased or decreased ambient air temperatures.The experimental set-up proved to be a most valuable tool todetermine and analyse interactions between transpiration andwater uptake, changes in plant water status and the bufferingof negative J_wnet). Increasing the temperature of ambient air resulted, for bothspecies investigated, in a quick and considerably enhanced transpiration,but there was only a minor impact on water uptake. Water lossexceeding uptake was buffered by internal water reserves whichwere refilled within about 1 d after the plant was relievedof heat and drought stress caused by a period of high ambientair temperatures and high water vapour saturation deficits ofthe air. Repeated simulation of such stress periods showed thatthe absolute values of transpiration and the water uptake for24 h can vary, but the diurnal course of the values showed thesame pattern if the environmental conditions were identical.Such standardized diurnal transpiration and water uptake curvescould be very useful for the validation of mathematical modelsused to describe plant water relations. Key words: Plant water relations, water budget, drought stress, transpiration, water uptake     

Root Water Uptake, Leaf Water Storage and Gas Exchange of a Desert Succulent: Implications for Root System Redundancy

A technique used for hydroponics was adapted to measure instantaneousroot water uptake from the soil for a leaf succulent CAM species,Agave deserti. Comparisons were made to previously modelledwater fluxes for A. deserti and to Encelia farinosa, a non-succulentC₃species. Net CO₂uptake and transpiration forA. deserti underwell-watered conditions occurred primarily at night whereasroot water uptake was relatively constant over 24 h. Leaf thicknessdecreased when transpiration commenced and then increased whenrecharge from the stem and soil occurred, consistent with previousmodels. A drought of 90 d eliminated net CO₂uptake and transpirationand reduced the water content of leaves by 62%. Rewetting theentire root system for 7 d led to a full recovery of leaf waterstorage but only 56% of maximal net CO₂uptake. Root water uptakewas maximal immediately after rewetting, which replenished rootwater content, and decreased to a steady rate by 14 d. Whenonly the distal 50% of the root system was rewetted, the timefor net CO₂uptake and leaf water storage to recover increased,but by 30 d gas exchange and leaf water storage were similarto 100% rewetting. Rewetting 10 or 20% of the root system resultedin much less water uptake; these plants did not recover leafwater storage or gas exchange by 30 d after rewetting. A redundancyin the root system of A. deserti apparently exists for dailywater uptake requirements under wet conditions but the entireroot system is required for rapid recovery from drought.Copyright1999 Annals of Botany Company Agave deserti Engelm., desert, drought, gas exchange, rewetting, roots, succulent, water uptake.     

Microsporogenesis in Taxus baccata L.: The Development of the archaesporium

An ultrastructural and cytochemical investigation of the developmentof the mierosporangium of Taxus baccata reveals many resemblancesto comparable events in other land plants, but also severaldistinctive features. During early development the archaesporiumcontains groups of degenerate cells which ultimately disappear,presumably by resorption. Scattered elsewhere in the cells ofthe archaesporium are highly ordered bodies, possibly crystal-likeformations of tubulin. The tapetum differentiates from the outerlayer of the archaesporium. Mitoses coincidentally cease tobe detectable within the sporangium and the sporogenous cellsbecome recognizable about three weeks before their nuclei entermeiosis. Although, as in other gymnosperms investigated, theearly development of the archaesporial cells is not synchronized,there is a tendency for synchrony to be acquired by the sporogenouscells and diad formation takes place more or less simultaneouslythroughout the sporangium. Measurements by microfluorometry of RNA levels during developmentof the archaesporium show a progressive rise in the RNA contentof the cells up to the beginning of meiosis. Microsporogenesis, Taxus baccata, archesporium     

Water Movement Into and Through Tradescantia virginiana (L.) Leaves: III. UPTAKE DURING CONDITIONS OF DYNAMIC CHANGE

Water uptake into the ventral epidermis and the other tissuesof T. virginiana leaves was recorded when the uptake rate wassuddenly increased. Results indicated that there was considerableevaporation, or stomatal transpiration, from the epidermal tissues,and that the water relationships of the epidermis are more affected,at least in the short term, by changes in factors which affectthe transpiration rate than are the water relationships of theother leaf tissues.     

Influence of phytoplankton composition and stratification degree on gut pigment content of Ceriodaphnia sp. at dawn

Very short-term feeding activity of the cladoceran Ceriodaphniasp. was investigated in situ in a eutrophic reservoir in thesouth of Spain, using fluorimetric analysis of the gut pigmentcontent in periods when the water column was relatively mixedor strongly stratified. The results obtained in the mixed watercolumn showed a clear increase in gut pigment content at dawn,a period sampled with high frequency. The accumulation of thecladoceran at the depth of maximum concentration of phytoplankton,and the high gut pigment concentration in cladocerans at thatdepth just after dawn, suggested active feeding of Ceriodaphniaon phytoplankton at that time. During stratification, the abundanceof Ceriodaphnia was higher, but the gut pigment contents werevery low and they did not reflect any clear feeding patterns,with either time or depth. Changes in phytoplankton concentrationand composition between the relatively mixed and the stratifiedwater column suggest a shift in feeding activity from herbivorousto.     

Photosynthesizing Leaves and Nodulated Roots as Donors of Carbon to Protein of the Shoot of the Field Pea (Pisum arvense L.)

In Pisum arvense, the amides and amino-acids normally suppliedto the shoot in the transpiration stream transfer carbon toprotein largely throught the amino-acids, aspartic acid (+asparagine),glutarnic acid (+glutamine), threonine, lysine, arginine, andproline. Carbon from carbon dioxide enters the protein of photosynthesizingtissues through an essentially complementary set of amino-acidsincluding glycine, alanine, serine, valine, and the aromaticamino-acids tyrosine, phenylalnine, and histidine. Young tissuesof the shoot synthesize certain amino-acids de novo by metabolismof sugars supplied from photosynthesizing leaves. Each mature leaf on a shoot contributes carbon to current synthesisof protein at the shoot apex. Sucrose accounts for more than90 per cent of the labelled carbon leaving any age of leaf whichhas been fed with ¹⁴CO₂. Upper leaves supply labelled assimilatesdirectly to the shoot apex, and the radiocarbon from these assimilatesis subsequently incorporated into a wide range of amino-acidunits of protein. The majority of the labelled assimilates exportedfrom a lower leaf move downwards to the root and nodules and,in consequence, the amino-acids and amides associated with rootmetabolism are strongly represented among the compounds eventuallylabelled in the apical region of the shoot.     

Studies on Foliar Penetration: I. FACTORS CONTROLLING THE ENTRY OF 2, 4 - DICHLOROPHENOXYACETIC ACID

A technique, using leaf disks, has been developed to study thepenetration of isotopically labelled compounds into leaves underconditions where there is no appreciable change in the concentrationof the external solution and no subsequent translocation. Inthis preliminary survey, the leaves of Phaseolus vulgaris andColeus Blumei were employed to investigate the entry of 2,4-dichlorophenoxyaceticacid (2,4-D), labelled in the carboxyl group with ¹⁴C. Over3 days there is no loss of ¹⁴C to the atmosphere from treatedleaves of Phaseolus. The rate of penetration is enhanced when(a) the leaves are young, (b) the water status is lowered, (c)the temperature is raised (Q₁₀=2.3–2.8), and (d) a surface-activeagent is added to the external solution. Penetration is alsofavoured by a decrease in the pH, the relation indicating thatboth ions and molecules enter. Penetration is greater in thelight and prior illumination of the tissues positively affectsthe subsequent rate in the light, but not in the dark. In boththe light and the dark considerably more 2,4-D penetrates theabaxial surface of Phaseolus leaves. For Coleus an even greaterdifference between surfaces is found in the light but not inthe dark. For both species in the light the rates of entry intoboth surfaces are proportional to their respective stomataldensities. The simultaneous addition of indoleacetic acid tothe external solution caused more 2,4-D to enter Phaseolus leaves,but the addition of triiodobenzoic acid restricts entry. Therate of penetration remains constant over 24 hours and between0.1 and 200 mg./l. the rate is linearly related to concentration.Subsequent to entry, the 2,4-D is in a form which does not diffusefrom the tissue into buffer or exchange with unlabelled 2,4-D.Moreover, no outward movement takes place from treated tissuewhich has been frozen and thawed. These findings are discussedin relation to previous work on foliar penetration. It is concludedthat at least with Phaseolus penetration largely takes placethrough the guard cells and/or accessory cells.     

Water Movement into and through Tradescantia virginiana (L.) Leaves: I. UPTAKE DURING CONDITIONS OF DYNAMIC EQUILIBRIUM

Water uptake into the ventral epidermis and the other tissuesof excised T. virginiana leaves was measured separately andsimultaneously when the uptake rates were steady. It was foundthat uptake into the ventral epidermis was proportionately greater,compared with uptake into the remainder of a leaf, than wouldbe expected from the ratio of conductances of the two pathways.This result led to the conclusion that not only is the epidermisa pathway for water transport in the transpiration stream butthat it is an important site of evaporation for stomatal transpiration.     

Experimental Studies of the Factors Controlling Transpiration: III. THE INTERRELATIONS BETWEEN TRANSPIRATION RATE, STOMATAL MOVEMENT, AND LEAF-WATER CONTENT

Transpiration rates of single leaves of Pelargonium and wheatwere measured under constant conditions of light, temperature,and air flow. Concurrently, stomatal movement was followed withthe resistance porometer during cycles of changing water contentof the leaf and changes induced by light and darkness. Stomatalmovement was found to exert a large controlling influence onthe transpiration rate, whereas water content had an extremelysmall or negligible effect. An approximately inverse linearrelation between transpiration rate and logarithm of resistanceto viscous flow through the leaf is believed to be the resultantof an inverse curvilinear relationship between the diffusiveconductance of the stomata and log. leaf resistance and thedecreasing difference of vapour pressure arising from the highertranspiration rates with increasing stomatal conductances. Nevertheless,the relation demonstrates that the transpiration rate is influencedby the degree of stomatal opening throughout its entire range. There was some evidence of lower transpiration rates duringand after recovery from wilting than before wilting. This isattributed to a decrease in a cell-wall conductance, the evaporatingsurface being located within the cell wall. During wilting partiallyirreversible contraction of the cell wall occurs. There wasalso evidence of slow changes in cell volume at full turgidityattributable to plastic flow. These occurred when the leaf wastransferred from environments of a high to low potential forevaporation. Extensive movement of the stomata followed changes in leaf water,passive opening resulting from decrease and closure from increaseof leaf water. It is suggested that the direction and extentof stomatal changes induced by water deficits is a consequenceof the rate of change of leaf water content and not of the absolutevalues. The stomata also showed an enhanced tendency to closein dry moving air following a period of wilting even after theleaf had regained turgidity.     

The Foregut of Gecarcinus lateralis as an Organ of Salt and Water Balance

The permeability of the foregut of the land crab, Gecarcinuslateralis, to tritiated water (THO), Na²², and Cl³⁶ was studiedin vitro during the intermolt period and after ecdysis. In crabswith eyestalks, the foregut is permeable to water and ions inthe direction hemolymph-to-lumen and lumen-to-hemolymph, bothduring the intermolt period and after ecdysis. However, theforegut of animals without eyestalks is impermeable after ecdysis. The movement of THO always follows the movement of Na²² acrossthe wall of the foregut, while the movement of Cl³⁶ may or maynot be correlated with the movement of Na²² and THO. Comparisonof the ratio of water to ions in the hemolymph with the ratiocalculated from radioisotope flux indicates that Na⁺ and waterare probably moving isosmotically, although not necessarilyaccompanied by Cl^– When an extract of the thoracic ganglionic mass of G. lateralisis added to the "hemolymph side" of the foregut in vitro, thereis immediately a large increase in permeability to water andsalts. This occurs in the foregut of crabs with eyestalks duringintermolt and also in eyestalkless crabs after ecdysis. Thus, not only is the foregut of Gecarcinus lateralis permeableto water and salts in both directions, but also the extent ofits permeability is under neuroendocrine control. As a consequence,the animal may be able to move water and salts into the foregutor out of it into the hemolymph as needed. This may be an importantadaptation for a terrestrial crab that must conserve water,especially at the critical time of ecdysis.     

Effects of Waterlogging on Water Relations of Actively-growing and Dormant Sitka Spruce Seedlings

Two-year-old Sitka spruce [Picea sitchensis (Bong.) Carr.] seedlings,either actively growing or dormant, were waterlogged in a growthroom at 15 °C. Shoot and root growth, transpiration andleaf water potential were observed. In actively-growing plants shoot extension continued after waterlogging,though at a reduced rate, and shoots of dormant plants brokebud and extended during the waterlogging period. Root growthwas suppressed by waterlogging in both types of plant. The 22day waterlogging treatment eventually killed the actively-growingplants but plants which were dormant at the time of waterloggingwere more tolerant. Changes in plant water relations after waterloggingwere entirely different depending on the condition of the plantswhen the soil was flooded. Dormant plants showed a gradual reductionin transpiration and increased water stress over the waterloggingperiod; after the soil was drained leaf water potential increasedto equal the value of control plants which had been maintainedin a freely drained condition, but transpiration did not increaseuntil root growth began. Actively-growing plants exhibited amore complex behaviour, characterized by a very rapid reductionin transpiration after waterlogging, accompanied by a briefperiod of water stress, followed by a period of increasing transpirationrate in the absence of water stress. Finally a second reductionin transpiration occurred and water stress increased as theseedlings died. The importance of the stage of activity of theroot system to the response of plants to waterlogging is discussed. Picea sitchensis (Bong.) Carr., Sitka spruce, waterlogging, water relations, dormancy, transpiration, water potential     

TRANSPORT OF UNCONTAMINATED AND MOLLUSCICIDE-CONTAINING FOOD IN THE DIGESTIVE TRACT OF THE SLUG DEROCERAS RETICULATUM (MULLER)

By X-ray analysis of food transport in the alimentary tractof Deroceras reticulatum it was shown that even ten hours afteringestion of a thorium sulfate-containing bait, this materialcan be detected in the crop. After 2.5 h, some parts of labelledfood passes down from the anterior to the posterior part ofthe gut. After 13 h, thorium sulfate-containing material canbe observed only in the gut. After 19 h, no more labelled materialis present in the alimentary tract of the animals. After addition of Cloethocarb, the animals feed on only smallamounts of food. The labelled material only enters the anteriorpart of the gut. After ten hours, the food does not move anymore and does not leave the crop even 19 h after feeding. After molluscicide application, the crop epithelium is moreinfolded than in control animals and the cells are elongated.After 30 h, cells protrude into the lumen of the digestive tract. (Received 11 May 1992; accepted 26 June 1992)     

In situ diel variation in gut pigment contents of Ceriodaphnia sp. in stratification and destratification periods

The short-term, in situ diel grazing of Ceriodaphnia sp. duringperiods of stratification and mixing was investigated usingthe technique of fluorimetric analysis of the gut pigments.There were considerable seasonal differences in feeding behaviourIn mixing, when the concentration of chlorophyll a in the watercolumn was high and Ceriodaphnia abundance was low, gut pigmentcontents showed clear diel variation patterns, probably dueto diel variations of the high values of feeding activity observedin the 24 hour cycle The maximum values were found at dawn.On the other hand, no diel variations in gut pigment were observedduring periods of stratification and while the amounts of pigmentsin the water and in the gut were very low, species abundancewas high. Taking into account the ambient conditions, the authorsdiscuss the possibility that the change of feeding of the Ceriodaphniasp. observed when the environment changed from a mixing periodto one of stratification represents a change from herbivorousto detritivorous behavior.     

Transpiration of <Emphasis Type="Italic">Cyclobalanopsis glauca</Emphasis> (syn. <Emphasis Type="Italic">Quercus glauca</Emphasis>) stand measured by sap-flow method in a karst rocky terrain during dry season

Seasonal drought may have a high impact on the karst ecosystem. The transpiration from Cyclobalanopsis glauca (syn. Quercus glauca) stand on a rocky hilly slope in South China was measured during the dry period of 2006 by using the Granier’s sap-flow method. During the experimental period, maximum sap flux density (J _s) ranged from 20 to 40 g H₂O m⁻² s⁻¹ according to diameter of breast height (DBH) of individual trees. On sunny days, daily transpiration varied between 3.4 and 1.8 mm day⁻¹. Transpiration of C. glauca was closely correlated to the radiation, air temperature, and vapor pressure deficit (VPD). Soil moisture was a very important factor influencing transpiration. The very low soil water content might result in low stand transpiration even when VPD is high, but high soil water content might also result in low transpiration if it was low VPD. However, VPD rather than soil moisture, affected largely the stand transpiration under high soil water content. The amount of transpiration was much more than that of the total soil moisture loss during the continuous sunny days, indicating that the dry shallow soils were probably not the only source for root-uptake water. C. glauca grows deep roots through the rock fissures of epikarst, indicating that epikarst might be another main source for sustaining transpiration in response to dry demand in autumn. Therefore, a large amount of deep roots of karst species would be a very important hydraulic connecting from the epikarst to above ground by transpiration, which would promote the biogeochemical process in a karst system.     

Feeding, excretion and egg production by individuals and populations of the marine, planktonic copepods, Acartia spp. and Centropages furcatus

Diel variations in vertical distribution, gut pigment content,ammonium excretion and egg production were investigated foradult females of Acartia erythraea and A.pacifica in the verticallymixed Inland Sea of Japan and Centropages furcatus in the stratified,neritic Gulf of Mexico. Gut pigment content and egg productionrate were maximal at night and ammonium excretion was maximalduring the daytime. Neither A.erythraea nor A.pacifica adultfemales showed an apparent diel migration, but the former werehighly concentrated in the surface layer during the afternoon.In contrast, C.furcatus adult females showed a clear diel migration,residing immediately above the bottom during the daytime andbeing concentrated between 10 and 25 m depth during the nighttime.Individual-based data on gut content and excretion and egg productionrates were combined with vertical-distribution data to calculatepopulation values. In the Inland Sea of Japan, the resultantpattern for Acartia spp. reflected the diel variation in physiologicalrates and even distribution of adult females, except for theafternoon, surface aggregation of A.erythraea. In the Gulf ofMexico, the pattern for C.furcatus reflected largely the dielvariation in each rate process and the heterogeneous distributionof adult females in the water column. Elevated nocturnal feedingactivity of these copepods may be due to an endogenous rhythm.The daytime maximum in ammonium excretion and night-time maximumin egg production rate indicated approximate half-day and daytime lags, respectively, after the intake of food until itsconversion into dissolved excreta and released eggs.     

The Use of 14C-Ethane Diol as a Quantitative Tracer for the Transpirational Volume Flow of Water and an Investigation of the Effects of Salinity upon Transpiration, Net Sodium Accumulation and Endogenous ABA in Individual Leaves of Oryza sativa L.

Yeo, A. R., Yeo, M. E., Caporn, S. J. M., Lachno, D. R. andFlowers, T. J. 1985. The use of ¹⁴C-ethane diol as a quantitativetracer for the transpirational volume flow of water and an investigationof the effects of salinity upon transpiration, net sodium accumulationand endogenous ABA in individual leaves of Oryza sativa L.—J.exp. Bot. 36: 1099–1109. Oryza sativa L. (rice) seedlings growing in saline conditionsexhibit pronounced gradients in leaf sodium concentration whichis always higher in the older leaves than the younger ones.Individual leaf transpiration rates have been investigated todiscover whether movement of sodium in the transpiration streamis able to explain these profiles from leaf to leaf. The useof ¹⁴C labelled ethane diol to estimate transpiration was evaluatedby direct comparison with values obtained by gas exchange measurements.Ethane diol uptake was linearly related to the transpirationalvolume flow and accurately predicted leaf to leaf gradientsin transpiration rate in saline and non-saline conditions. ¹⁴C-ethanediol and ²²NaCl were used to compare the fluxes of water andsodium into different leaves. The youngest leaf showed the highesttranspiration rate but the lowest Na accumulation in salineconditions; conversely, the older leaves showed the lower transpirationrates but the greater accumulation of Na. The apparent concentrationof Na in the xylem stream was 44 times lower into the youngerleaf 4 than into the older leaf 1. Exposure to NaCl (50 molm^–3) for 24 h elicited an increase in endogenous ABA inthe oldest leaf only, but no significant changes occurred inthe younger leaves. Key words: —Salinity, rice, Oryza sativa L., transpiration, volume flow, abscisic acid