Diel changes of uptake of inorganic carbon and nitrogen by phytoplankton, and the relationship between inorganic carbon and nitrogen uptake in Lake Nakanuma, Japan

Diel changes of uptake of inorganic carbon and nitrogen wereexamined in a small freshwater lake, Lake Nakanuma, Japan, bythe ¹³C and ¹⁵N method. Experiments were earned out in spring,summer and autumn in 1984. Carbon and nitrogen uptake in thelight incubation showed maxima around noon at the three seasons.Carbon uptake ceased at night, but ammonium uptake was fairlylarge at night. In the dark incubation carbon uptake did notoccur. Ammonium uptake showed a maximum at dusk in the darkexperiments. Diel changes of nitrate uptake were less clearthan those of ammonium uptake. These results indicate that nitrogenuptake partly depended on the carbon uptake. Then, we triedto explain the diel changes of nitrogen uptake, assuming thatthe nitrogen uptake partly depends on stored carbohydrate. Thediel changes may be elucidated by the sum of three terms: oneis the term of decay of stored carbohydrate, the second is theterm which indicates cumulative increase of stored carbohydrateand the third is the term which directly depends on light.     

ULTRAVIOLET-B RADIATION EFFECTS ON INORGANIC NITROGEN UPTAKE BY NATURAL ASSEMBLAGES OF OCEANIC PLANKTON1

Ultraviolet-B radiation (UVBR: 290-320 nm) inhibited ammonium uptake (p_NH4) and nitrate uptake (p_NO3) in natural plankton assemblages collected during a transect from 37° N to 55° N in the Pacific Ocean. Comparison of responses in p_NH4 to ambient solar- and lamp-enhanced UVBR spectra allowed calculation of an action spectrum for p_NH4 inhibition. The slope of the action spectrum for Pnh₄ is half as steep as action spectra for UVBR inhibition of photosynthetic carbon uptake. Consequently, WBR-induced photoinhibition of p_NH4 extends to greater depths than inhibition of carbon fixation due to the greater relative effect of longer UVBR wavelengths. Inhibition of p_NH4 was dependent upon UVBR dose when doses were weighted by the p_NH4 action spectrum. Dependence of WBR inhibition of p_NH4 on dose rate was not apparent. We found that near-surface p_NH4 and p_NO3 can be overestimated in excess of 50% when measured using standard incubation vessels made of UVBR-absorbing materials such as polycarbonate.     

Diel variability in nitrogenous nutrient uptake by phytoplankton in the Chesapeake Bay plume

Diel patterns in the uptake of nitrogenous nutrients were observedin the coastal plume of the Chesapeake Bay system, but the specificpatterns varied with season. During the winter months, ratesof NH₄⁺ and urea uptake were significantly higher at night thanduring the day, and rates of NO₃^– uptake were higher duringthe day. During the summer, rates of NH₄⁺ and urea uptake weresignificantly higher at night only during half the studies conducted;during the remaining studies, there was either no significantdifference or rates of uptake of NH₄⁺ were higher during theday. Rates of NO₃^– uptake during the summer months werealso higher during the day than at night. Seasonal differenceswere also apparent in the time of day at which maximum observeduptake rates of each nitrogen nutrient occurred. During thewinter-spring months, maximum observed rates of NO₃^– uptakeoccurred between first light and noon, whereas during the summermonths, maximum observed uptake rates of NO₃^– occurredboth morning and afternoon, and consistently 9–16 h afterthe maximum observed peak in the uptake of reduced nitrogen.We interpret these findings in terms of seasonal shifts in nitrogennutritional status of the assemblages, as well as species-specificdifferences in the effect of a given stimulus (e.g. a nitrogenpulse at the mouth of the Bay) to entrain an uptake response,and we suggest that the extent of this variability must be understoodbefore generalizations about the use of f-ratios as characteristicsof specific populations or water masses can be drawn.     

Influence of solar ultraviolet radiation on photosynthesis and motility of marine phytoplankton

Abstract: The effects of solar ultraviolet radiation (UV) on carbon uptake, oxygen evolution and motility of marine phytoplankton were investigated in coastal waters at Kristineberg Marine Research Station on the west coast of Sweden (58° 30'N, 11° 30'E). The mean irradiances at noon above the water surface during the investigation period were: photosynthetic active radiation (PAR, 400–700 nm) 1670 μmol m⁻² s⁻¹; ultraviolet-A radiation (UV-A, 320–400 nm) 35.9 W m⁻² and ultraviolet-B radiation (UV-B, 280–320 nm) 1.7 W m⁻². UV-B radiation was much more attenuated with depth in the water column than were PAR and UV-A radiation. UV-B radiation could not be detected at depths greater than 100–150 cm. Inhibition of carbon uptake by UV-A and UV-B in natural phytoplankton populations was greatest at 50 cm depth and the effects of UV-B were greater than those of UV-A. At depths greater than 50 cm there was almost no effect of ultraviolet radiation on carbon uptake. PAR, UV-A and UV-B decreased oxygen evolution by the dinoflagellate Prorocentrum minimum . Inhibition of oxygen evolution was greater after 4 h than 2 h but it was not possible to distinguish the negative effects of the different light regimes. The motility of P. minimum was not affected by PAR, UV-A and UV-B. The importance of exposure of phytoplankton to different light regimes before being exposed to natural solar radiation is discussed.     

On the compatibility of carbon uptake rates calculated from stable and radioactive isotope data: implications for the design of experimental protocols in aquatic primary productivity

Basic differences between the ¹³C and the ¹⁴C techniques ofmeasuring carbon uptake by phytoplankton exist at the levelof the isotopic analysis. With the first method, a ratio ofisotopic abundances is measured on the sample, whereas an absoluteamount of isotope is estimated with the second method. If acarbon source other than the labeled one is utilized by thephytoplankton during incubation, the stable isotope method maybe biased. Specific uptake values will be underestimated bythis effect. It is, however, possible to obtain unbiased estimatesof the ¹³C-labeled carbon uptake by using an equation containinga term describing the final particulate carbon concentration.Only under this condition will carbon uptake rates derived from¹³C isotope data be always compatible with the ¹³C method ofmeasuring primary production ^*This paper is the result of a study made at the Group for AquaticPrimary Productivity (GAP), Second International Workshop heldat the National Oceanographic Institute, Haifa, Israel in April–May1984.     

Occurrence of mycosporine-like amino acids in the red-tide dinoflagellate Alexandrium excavatum: UV-photoprotective compounds?

Water extracts of the red-tide dinoflagellate Alexandrium excavatumgrown at ‘high’ light intensity (200 µE m^–2s^–1) show a broad absorbance maximum in the UV regionof the spectrum (310–360 nm). Using TLC and reverse-phaseHPLC a series of mycosporine-like amino acids have been characterized:mycosporine-glycine (_max = 310 nm), palythine (_max = 320 nm),asterina-330 (_max = 330 nm), shinorine (_max = 334 nm), porphyra-334(_max= 334 nm), palythenic acid (_max = 337 nm) and the isomericmixture of usujirene and palythene (_max = 359 nm). From theobserved spectral changes during transference from ‘low’(20 µE m^–2 s^–1) to ‘high’ (200µE m^–2 s^–1) light intensities and vice versa,the series of compounds are supposed to be biogenically relatedto one another. The presence of these compounds in A.excavatumis discussed in relation to their possible role in the photoprotectionto deleterious UV radiation.     

CO<Subscript>2</Subscript> exchange in a temperate Japanese cypress forest compared with that in a cool-temperate deciduous broad-leaved forest

To examine the characteristics of carbon exchange in coniferous forests, we analysed the seasonal and diurnal patterns of CO₂ exchange, as measured using the eddy covariance method, in a Japanese cypress forest in the Kiryu Experimental Watershed (KEW) in central Japan. The net CO₂ exchange data during periods of low-friction velocity conditions and during periods of missing data were interpolated. The daily CO₂ uptake was observed throughout the year, with maximum values occurring in early summer. Periods of low carbon uptake were seen in late summer owing to high respiratory CO₂ efflux. The diurnal and seasonal patterns of daytime CO₂ exchange at KEW were compared with those in a cool-temperate deciduous forest of the Tomakomai Experimental Forest (TOEF) in Japan. The environmental differences between evergreen and deciduous forests affected the seasonal patterns of carbon uptake. Although there were great differences in the mean monthly air temperatures between the sites, the mean monthly daytime carbon uptake was almost equal at both sites during the peak growing period. The carbon-uptake values at the same PAR level were greater before noon than after noon, especially at TOEF, suggesting the stomatal regulation of carbon uptake.     

极端干旱条件下锡林河流域羊草草原净生态系统碳交换特征

采用涡度相关法对2005年生长季内蒙古锡林河流域羊草(Leymus chinensis)草原净生态系统交换(Net ecosystem exchange, NEE)进行了观测。观测结果表明:作为生长季降雨量仅有126 mm的干旱年,锡林河流域羊草草原生态系统受到强烈的干旱胁迫,其净生态系统碳交换的日动态表现为具有两个吸收高峰,净吸收峰值出现在8∶00和18∶00左右。最大的CO₂吸收率为-0.38 mg CO₂·m^-2·s^-1,出现在6月底,与丰水年相比生态系统最大CO₂吸收率下降了1倍。就整个生长季而言,不管是白天还是晚上2005年都表现为净CO₂排放,整个生长季CO₂净排放量为372.56 g CO₂·m^-2,是一个明显的CO₂源。土壤含水量和土壤温度控制着生态系统CO₂通量的大小,尤其是在白天,CO₂通量和土壤含水量的变化呈现出显著的负相关关系,和土壤温度表现为正相关关系。     

Response of Wheat Seedlings to Low O2 Concentrations in Nutrient Solution: I. GROWTH, O2 UPTAKE AND SYNTHESIS OF FERMENTATIVE END-PRODUCTS BY ROOT SEGMENTS

Root growth of 7-d-old wheat (Triticum aestivum cv. Gamenya)seedlings was impaired at dissolved O₂ concentrations of 0.01and 0.055 mol m^–3 O₂, while growth at 0.115 mol m^–3O₂ was the same as that in continuously aerated controls (0.26mol m^–3 O2). Oxygen uptake by apical (0–2 mm), expanding (2–4mm) and expanded (10–12 mm) tissues of the roots decreasedbelow 0.16, 0.09 and 0.05 mol m^–3 O₂, respectively. Thishierarchy is consistent with the metabolic rates of these tissues.There was a small (c. 9%) inhibition of O₂ uptake and some netsynthesis of ethanol and alanine in root apices at 0.115 molm^–3 O₂. Significant amounts of anaerobic end-productsaccumulated at 0.055 mol m^–3 O₂ and even more so at 0.01mol m^–3 O₂, indicating that oxidative phosphorylationwas strongly inhibited. Net alanine synthesis increased in fully expanded (10–16mm) tissues exposed to <0.003–0.01 mol m^–3 O₂,and this increase was accompanied either by a proportionallysmaller increase in the concentration of other free amino acidsor by a net decrease in free amino acid levels excluding alanine.This suggests that alanine was synthesized as an end-productof anaerobic catabolism and did not accumulate simply becauseof decreased net protein synthesis. Comparing the carbon flow to CO₂, ethanol, lactate and alaninein roots at 0.01 mol m^–3 O₂ with carbon loss as CO₂ inaerated roots suggests that carbon flow to products of metabolismwas not greatly enhanced due to O₂ deficiency. This infers,but does not prove that, in wheat, generation of energy duringperiods of O₂ deficiency is not enhanced due to a Pasteur effect. Key words: Anaerobic, fermentation, oxygen, wheat     

An Endogenous Circadian Rhythm in the Rate of Carbon Dioxide Output of Bryophyllum: VI. ACTION SPECTRUM FOR THE INDUCTION OF PHASE SHIFTS BY VISIBLE RADIATION

A comparison has been made of the effectiveness of a 4-h exposureto equal quantum-flux densities of radiation in different zonesof the visible spectrum in shifting the phase of the endogenouscircadian rhythm of carbon dioxide metabolism in leaves of Bryoyihyllumfedtschenkoi. At an incident quantum-flux density of 8.9 ? 10^–13einsteins cm^–2 8^–1, only radiation between 600 and700 nm induced a phase shift, maximum activity being found at(560 nm. At a higher incident quantum-flux density of 1.9 ?10^–11 einsteins cm^–2 8^{– 1}, the peak of activitywas broader and extended from 560 to 700 nm. At both flux densitiesa sharp cut-off occurred at 700 nm. The action spectra are somewhat similar to the absorption spectrumof phytochrome except that they show no minor peak in the bluezone. No evidence has yet been obtained that the inductive effectof red light can be reversed by exposure to far-red radiationas in the case of a typical phytochrome-mediated response. Ultra-violet radiation at 237 nm had no effect upon the phaseof the rhythm.     

Response of Wheat Seedlings to Low O2 Concentrations in Nutrient Solution: II. K +/Na+ SELECTIVITY OF ROOT TISSUES9

This paper reports the effects of low O₂ concentration (0–01,0–055, and 0.115mol m^–3) in nutrient solutions onK⁺/Na⁺ selectivity of growing and mature root tissues of 6-to 8-d-old, intact, wheat (Triticum aestivum cv. Gamenya) seedlings. Increases in anaerobic catabolism and decreases in O₂ uptake,K⁺ uptake and K⁺/Na⁺ selectivity were all more pronounced and/oroccurred at higher external O₂ concentrations in the apex (0–2mm) than in the expanding tissues (2–4 mm); these growingtissues were, in turn, more affected than the expanded tissuesof the roots (4–12 mm). Selectivity for K⁺ over Na⁺ in roots and shoots was particularlysensitive to O₂ deficiency. For example, in apical tissues (0–2mm) K ⁺ /Na⁺ selectivity was already reduced at 0.115 mol m^–3O₂, yet at this O₂ concentration there was no effect on eithergrowth or (K⁺/Na⁺) uptake. Upon transfer from 0.01 to 0.26 mol m^–3 O₂, a detailedstudy of the 12 mm root tips showed that 70% of these tips regainedhigh (K⁺ + Na⁺) concentrations and K⁺/^Na+ ratios. In contrast,there was no recovery in the remaining 30% of the 12 mm roottips. Net K⁺ transport to the shoots during the period afterre-aeration was negative for the population as a whole. Theseverity of these effects supports the view that the root tipsand the stele were more susceptible to O2 deficiency than wasthe cortex of the fully-developed root tissues. Key words: Hypoxia, K⁺/Na⁺ selectivity, expanded and expanding tissues     

Coupling Ratios H+/e=3 versus H+/e=2 in Chloroplasts and Quantum Requirements of Net Oxygen Exchange during the Reduction of Nitrite, Ferricyanide or Methylviologen

Using intact and osmotically ruptured chloroplasts, ratios ofcoupling between deposition of protons in the intrathylakoidspace and light-dependent transport of electrons from waterto an external acceptor were determined. The data indicate couplingbetween proton and electron transport at a ratio of H⁺/e=3 withmethylviologen as electron acceptor in thylakoids and with nitriteas electron acceptor in intact chloroplasts. With ferricyanideas electron acceptor in thylakoids, values close to H⁺/e=2 wereobserved. Evidence is discussed that H⁺/e=3 is a fixed valuein intact chloroplasts at levels of thylakoid energization sufficientfor supporting effective carbon assimilation. In the presence of methylviologen and ascorbate, the minimumquantum requirement of oxygen uptake by thylakoids was about2.7 quanta of 675 nm light per O₂ indicating an e/O₂ ratio of1.33. In the absence of ascorbate, and with KCN present in additionto methylviologen, e/O₂ ratios up to 4 were observed. The minimumquantum requirement of oxygen evolution by thylakoids in thepresence of ferricyanide and by intact chloroplasts in the presenceof nitrite was about 8 quanta/O₂. (Received May 1, 1995; Accepted October 2, 1995)     

Characteristics of light-induced 515-nm absorbance change in spinach chloroplasts at lower temperatures II. Relationship between 515-nm absorbance change and rapid H+ uptake in chloroplasts after a short flash illumination

The absorbance change at 515 nm induced by a short (7.6 µsec)light flash in spinach chloroplasts was studied at sub-roomtemperatures in relation to rapid H⁺ uptake into chloroplasts. Lowering of temperature caused a marked decrease in the rateof recovery of 515-nm absorbance change after a flash illumination.Initial rate of rapid H⁺ uptake, measured with absorbance changeof bromcresol purple (BCP), was also reduced at lower temperatures,in a parallel fashion. Half-recovery time of the absorbancechange at 515 nm and rise-time of the pH-indicating absorbanceincrease of BCP coincided well at each temperature studied.Values of the calculated activation energy for these two processeswere almost the same. The parallelism between the 515-nm absorbance change and therapid H⁺ uptake after a single flash illumination was also observedwhen the electric field decay and/or H⁺ translocation were acceleratedby ionophorous antibiotics, carbonylcyanide m-chlorophenylhydrazoneor phenazine methosulfate. From these results, it is suggestedthat the rapid H⁺ uptake into chloroplast is chemically coupledto electron transfer and at the same time diffusion- (or transport-)controlled. Membrane potential, reflected in the 515-nm absorbancechange is dissipated with the rapid H⁺ influx. A model for theelectron-transfer-coupled H⁺ translocation involving a plastosemiquinoneloop is presented. Dissipation of the illumination-formed inside-positivemembrane potential by the influx of H⁺ is explained by the model. (Received September 17, 1976; )     

Stop-flow studies of solute uptake in rat lungs

Stop-flow studies were used to characterize solute uptake inisolated rat lungs. These lungs were perfused at 8 or 34 ml/min for10-28 s with solutions containing¹²⁵I-albumin and two or more ofthe following diffusible indicators: [³H]mannitol,[¹⁴C]urea,³HOH,²⁰¹Tl⁺,or⁸⁶Rb⁺.After this loading period, flow was stopped for 10-300 s and thenresumed to flush out the perfusate that remained in the pulmonary vasculature during the stop interval. Concentrations of²⁰¹Tl⁺and⁸⁶Rb⁺in the venous outflow decreased after the stop interval, indicating uptake from exchange vessels during the stop interval. The amount ofthese K⁺ analogs lost from thecirculation during the stop interval was greater when the intervalswere longer. However, losses of²⁰¹Tl⁺at 90 s approached those at 300 s. Because extraction continued afterthe vasculature had been flushed, vascular levels had presumably fallento negligible levels during the stop interval. By 90 s of stop flow thevascular volume that was cleared of²⁰¹Tl⁺averaged 0.657 ± 0.034 (SE) ml in the experiments perfused at 8 ml/min and 0.629 ± 0.108 ml in those perfused at 34 ml/min. Increases in perfusate K⁺decreased the cleared volumes of²⁰¹Tl⁺and⁸⁶Rb⁺.Uptake of[³H]mannitol,[¹⁴C]urea, and³HOH during the stop intervals wasobserved only when the lungs were loaded at high flow for shortintervals. Decreases in²⁰¹Tl⁺and⁸⁶Rb⁺concentrations in the pulmonary outflow can be used to identify thefraction of the collected samples that were within exchange vessels ofthe lung during the stop interval and may help determine thedistribution of solute and water exchange along the pulmonary vasculature.

     

Effects of solar radiation on the endemic Mediterranean red alga Rissoella verruculosa: photosynthetic performance, pigment content and the activities of enzymes related to nutrient uptake

The effects of full-spectrum solar radiation and of solar radiation deprived of total u.v. radiation (λ<395 nm) on the endemic Mediterranean red alga Rissoella verruculosa (Bertoloni) J. Agardh were studied in situ in early summer, from sunrise to sunset. Photosynthetic performance, pigment content and the activities of enzymes related to nutrient uptake, were monitored under both radiation conditions throughout a daylight period.
The doses of solar radiation, measured on the day during which the experiments were carried out (24 June 1997), were 9228·25, 1109·70 and 13·03 kJ m⁻² for PAR (λ=400–700 nm), u.v.-A (λ=315–400 nm) and u.v.-B (λ=280–315 nm), respectively. Under these conditions, a clear daily variation in photosynthetic performance was found. However, no significant differences were detected between the two radiation conditions. At noon, strong sunlight impaired O₂ evolution by 75%, but complete recovery occurred during the afternoon, reaching similar values to those measured in the early morning. By contrast, photoinhibition of optimal quantum yield ( F _v/ F _m), and the relative electron transport rate was followed by only a slight recovery during the afternoon. The rate of photosynthesis in air (simulating emersion conditions), estimated by CO₂ exchange, showed a negative balance at noon, which was accentuated in plants exposed to the full-solar spectrum.
Significant changes in the activities of nitrate reductase and carbonic anhydrase were found throughout the day under both radiation conditions. In thalli receiving solar radiation deprived of u.v., total CA activity decreased throughout the day. However, in thalli exposed to full-spectrum solar radiation, the activity of the enzyme tended to increase in the afternoon, correlating with an increase in NR activity.     

Action spectrum of phototaxis in a cryptomonad alga, Cryptomonas sp.

The action spectrum of the positive topo-phototaxis in Cryptomonaswas determined by photometry in the region of 400 to 680 nmat a stimulus intensity of 8.3 ? 10^–11 Einsteins cm^–2sec^–1. The action spectrum had a main peak at about 560nm unlike peaks for most other flagellated algae. Blue lightwas not very effective and red light above 640 nm had not effect. Swimming rates of individual organisms were measured by darkfield photomicrography. We concluded that the photokinetic effectwas negligible. Among the component pigments of this alga, phycoerythrin hadan absorption spectrum whose main peak appeared to coincidewith that of the phototactic action spectrum. (Received October 31, 1973; )     

Diurnal variations in the contributions of autotrophic picoalgae and heterotrophic bacteria to planktonic production in an upland lake

An investigation of the diurnal variation in contributions toproduction of the autotrophic and heterotrophic components ofthe picoplankton community was carried out during August andSeptember in Llyn Padarn, a mesotrophic upland lake in NorthWales. The picoplankton was separated using 1 µm pore-sizedfilters into the smaller cell sized fraction (<1 µm),the majority of the bacteria and the larger cell sized picoalgae(<3>1 µm), together with some bacteria. The distributionof bacterial heterotrophic activity between these two fractionsof picoplankton was assessed by uptake of [¹⁴C]glucose and differentialfiltration. Thus, the absolute autotrophic production by picoalgaeand the heterotrophic contribution by bacteria to picoplanktoncommunity production via uptake of extracellular organic carbon(EOC) were determined. Rates of picoplankton community productionexhibited diurnal variation with maximum rates of 19.1 mg Cm^–3 h^–1 recorded at 18.00 h at 4 m depth in September.The bacterial contribution to picoplankton community productionincreased markedly between 15.00 and 18.00 h. Rates of absoluteautotrophic production varied less over 24 h than rates of accumulationin bacteria of ¹⁴C-labelled EOC released from the entire phytoplanktoncommunity. Bacteria contributed up to 86–98% of the neworganic carbon within the picoplankton community at the endof the day. The maximum rate of absolute autotrophic productionin the picoplankton was 1.6 mg C m^–3 h^–1 at 18.00h at 1 m in August, and the maximum rate of bacterial accumulationof new organic carbon was 18.5 mg C m^–3 h^–1 at 18.00h in September at 4 m depth. The diurnal pattern of picoplanktoncommunity production involved increasing rates during the daywith a maximum at 18.00 h. Autotrophic processes were dominantin the first 3–6 h of the light cycle and heterotrophicuptake of ¹⁴C-labelled EOC was the major component from 15.00h onwards. Bacterial uptake of newly released EOC by phytoplanktonwas rapid, comprised the majority of picoplankton production,particularly later in the day, and contributed a maximum of60% of the total pariculate primary production in plankton between15.00 and 18.00 h at 4 m in September with a mean contributionof between 6 and 26% over 24 h in these investigations. Theimportance of autotrophic processes in picoplankton communityproduction has been overestimated in previous investigations.Bacteria play a major role in transferring newly produced EOCrapidly from phytoplankton to the picoplankton community. Atthe end of the day, the majority of newly produced organic carbonis in bacterial cells and this production is significant inthe dynamics of carbon production within the entire planktoniccommunity.     

Influence of UV-B radiation on bacterial activity in coastal waters

The impact of UV-B radiation (290–315 nm) on bacterialactivity and abundance in coastal water was studied in mesocosmexperiments in May 1994 and May 1995 at Kristineberg MarineResearch Station, Sweden. Mesocosms (6 m³) containing naturalpelagic communities were exposed either to ambient irradiation(AMB), ambient irradiation with enhanced UV-B (+UV) (0.7 W m^–24 h every day around noon), or ambient irradiation screenedfor UV-B (–UV). Bacterial activity in the mesocosms wasmeasured by means of thymidine incorporation in short-term testsduring incubations at ambient irradiation, at ambient irradiationwith enhanced UV-B, and at ambient irradiation screened forUV-B. In +UV mesocosms, bacterial activity was significantlystimulated when incubated at ambient radiation. The stimulatingeffect was suggested to be due to an increase in carbon or nutrientsupply through a photodegradation of recalcitrant dissolvedorganic material (DOM). Low attenuation coefficients for UV-Band PAR (400–700 nm) in the +UV mesocosms supported thishypothesis. The bacterial activity in +UV mesocosms, however,was inhibited when incubations were made at enhanced UV-B irradiation,implying that the bacteria had become more sensitive to UV-Bradiation. The increased sensitivity to UV-B exposure in bacterialassemblages that already had been exposed and stressed by UV-Bradiation is suggested to be due to an overburdening of theenergy-consuming DNA repair mechanism. The data suggest thatincreased UV-B radiation, which might occur with ozone depletion,may both stimulate and suppress bacterial activity in coastalwaters, implying that the net outcome of enhanced UV-B radiationcould be an unchanged bacterial activity.     

Microclimate, Photosynthesis and Growth of Lucerne (Medicago sativa L.). I. Microclimate and Photosynthesis

Measurements of microclimate and photosynthesis of lucerne var.Europe were made in the field during the spring of 1976. Themaximum rate of canopy gross photosynthesis (14.3 g CO₂ m^–2h^–1, I = ) was 2.5 times greater than that of S 24 perennialryegrass at the same LAI. This difference was due to differencesin individual leaf photosynthesis. The photosynthetic rate ofthe youngest fully expanded leaf of lucerne remained constantthroughout the experimental period at 3.6 g CO₂ m^–2 h^–1(300 W m^–2). Measurements of soil water potential profiles indicated thatlucerne extracted water from the soil to a depth of at least800 mm, with a region of maximum uptake between 400 and 600mm. This capability, with a moderate mean leaf resistance of460 s m^–1, conferred a high assimilation efficiency onlucerne, with a mean water use efficiency of 34 g H₂O lost pergram of carbohydrate assimilated, compared with 200 g H₂O pergram of carbohydrate for S 24. Medicago sativa L, lucerne, photosynthesis, assimilation efficiency     

Comparison of radioactive and stable isotope tracer techniques for measuring photosynthesis: 13C and 14C uptake by marine phytoplankton

The stable carbon isotope ¹³C has been used in the open oceanto estimate the inorganic carbon uptake by phytoplankton andthis technique has been compared with the ¹³C tracer method.An overall correlation coefficient of 0.806 and a regressionslope of 1.29 were calculated from 50 sample pairs gatheredduring three cruises in widely different oceanic areas rangingin production rates from 0.01 to 6 mgC m^–3 h^–1.However, significant differences between the two methods wereapparent for cruises located in nutrient-depleted areas. Possibleexplanations lie either in a volume effect, the high silicatecontent of the ¹⁴C solution which could stimulate the ¹⁴C uptakeor in errors associated with the particulate carbon measurementswhich are necessary to convert specific uptake rates to absoluteuptake rates and to yield compatible units for the comparison,in laboratory cultures the ¹⁴C technique overestimated the netparticulate carbon increase by — 16%. ⁺Present address: Laboratoire marin CNRS-IFREMER, L'Houmeau,17137 Nieul-sur-Mer, France. ^*This paper is the result of a study made at the Group for AquaticPrimary Productivity (GAP) First International Workshop heldat the Limnological Institute, University of Konstanz, in April1982.