Diurnal changes in allocation and partitioning of recently assimilated carbon in loblolly pine seedlings

We examined diurnal fluctuations in acquisition and partitioning of recently assimilated ¹⁴CO₂, and in subsequent allocation and partitioning to roots of loblolly pine (Pinus taeda L.) seedlings. Nonmycorrhizal seedlings were grown under optimal nutrient conditions in continuously flowin solution culture. Shoots of 15-week-old loblolly pine seedlings were labeled with ¹⁴CO₂ for 30 min at four separate labeling times: 1000, 1200, 1400 and 1600 h. Six whole plant harvests were conducted during a 48 h chase period, i.e. 0, 4, 8 12, 24 and 48 h after the end of the labeling and evacuation periods. Although assimilation of ¹⁴CO₂ was constant between 1000 and 1400 h, there were significant differences in partitioning of ¹⁴C-labeled assimilate in needles of all age classes. The highest percentage of recently assimilated ¹⁴CO₂ in the ethanol-soluble fraction of photosynthesizing tissue was observed near the beginning and end of the photoperiod. Partitioning of ¹⁴C in the ethanol-soluble fraction declined between the 1000 and 1400 h labeling eriods, and was accompanied by an increase in partitioning of recently assimilated ¹⁴CO₂ toward starch and a decrease in respiratory losses. These data suggest that most of the ¹⁴CO₂ assimilated at 1000 h was used to support shoot metabolic activities and possibly restore soluble sugar reserves. Peak starch accumulation in needles during the 1400 h labeling period, concomitant with minimal respiratory loss, indicated that photosynthate production exceeded demand and export out of source leaves. A possible feedback regulation of photosynthesis by starch and/or sugar accumulation may be responsible for the observed decline in assimilation of ¹⁴CO₂ during the 1600 h labeling period. Net accumulation of recently assimilated ¹⁴CO₂ in roots was correlated with assimilation rate of ¹⁴CO₂, but independent of partitioning of recently assimilated carbon in photosynthetic tissue. However, the percentage of total seedling ¹⁴C allocated to roots was essentially the same throughout the 48 h chase, regardless of time of labeling and assimilation rate. The data suggest a strong diurnal regulation of starch and soluble sugars synthesized from recently assimilated carbon in needles of loblolly pine seedlings that was independent of assimilation rate. Allocation and transport of recently assimilated carbon to roots of loblolly pine seedlings were not subject to short-term fluctuations in supply and demand.     

TRANSPORT OF CARBON AMONG CONNECTED RAMETS OF EICHHORNIA CRASSIPES (PONTEDERIACEAE) AT NORMAL AND HIGH LEVELS OF CO2

The floating, stoloniferous plant, Eichhornia crassipes, has high rates of productivity and rapidly invades new sites. Because the transport of carbon among connected ramets is known to increase the growth of clonal plants, we asked whether there is intraclonal carbon transport in E. crassipes. Because net photosynthesis of E. crassipes is significantly higher at high levels of atmospheric CO₂, we also asked if high CO₂ can change patterns of carbon transport in ways that might modify clonal growth. We exposed individual ramets within groups of connected ramets to ¹⁴CO₂ for 15–45 min and measured the distribution of ¹⁴C in the group after 4 days of growth at 350, 700, 1,400, or 2,800 μ1 1^−-1 CO₂. At 350 μ1 1^−-1 CO₂, a parent ramet exported approximately 10% of the ¹⁴C that it assimilated to its first rooted offspring ramet. The offspring exported a similar percentage of the ^l4C it assimilated toward the parent; two-thirds of this ¹⁴C was retained by the parent, and one-third moved into new offspring of the parent. In all ramets, imported carbon moved into leaves as well as roots. At the higher levels of CO₂, the percentage of assimilated carbon exported from a parent ramet to the leaf blades of its first offspring was lower by half. High CO₂ had little other effect on carbon transport. E. crassipes maintains bidirectional transport of carbon between ramets even under uniform and favorable environmental conditions and when external CO₂ levels are very high.     

INORGANIC CARBON AND ACETATE ASSIMILATION IN BOTRYOCOCCUS BRAUNII(CHLOROPHYTA)1

Assimilation of ¹⁴CO₂ or ¹⁴C-acetate by the hydrocarbon producing alga Botryococcus braunii Kützing was investigated to determine the allocation of incorporated ¹⁴C among early metabolites of photosynthesis and secondary metabolites. When the cells were exposed to NaH¹⁴CO₃ for 10 sec, over 90% of incorporated ¹⁴C was detected in phosphoglycerate, suggesting that this alga assimilates inorganic carbon by the C-3 pathway. The distribution pattern of ¹⁴C in the number of metabolites revealed that organic acids, neutral sugars and amino acids were first labelled with ¹⁴C, and, after lag periods of a few minutes, lipids including hydrocarbon were increasingly labelled. Addition of 5 mM acetate to the culture medium did not affect the growth of this alga but enhanced cellular respiration. The incorporation of ¹⁴CO₂ into the lipid fraction was stimulated, but net photosynthesis was inhibited by the addition of acetate. ¹⁴C-acetate was incorporated into lipids at a very low rate in comparison with the rate of ¹⁴CO₂ incorporation.     

Allocation of carbon to shoots,roots, soil and rhizosphere respiration by barrel medic (Medicago truncatula) before and after defoliation

The allocation of carbon to shoots, roots, soil and rhizosphere respiration in barrel medic (Medicago truncatulaGaertn.) before and after defoliation was determined by growing plants in pots in a labelled atmosphere in a growth cabinet. Plants were grown in a ¹⁴CO₂-labelled atmosphere for 30 days, defoliated and then grown in a ¹³CO₂-labelled atmosphere for 19 days. Allocation of ¹⁴C-labelled C to shoots, roots, soil and rhizosphere respiration was determined before defoliation and the allocation of ¹⁴C and ¹³C was determined for the period after defoliation. Before defoliation, 38.4% of assimilated C was allocated below ground, whereas after defoliation it was 19.9%. Over the entire length of the experiment, the proportion of net assimilated carbon allocated below ground was 30.3%. Of this, 46% was found in the roots, 22% in the soil and 32% was recovered as rhizosphere respiration. There was no net translocation of assimilate from roots to new shoot tissue after defoliation, indicating that all new shoot growth arose from above-ground stores and newly assimilated carbon. The rate of rhizosphere respiration decreased immediately after defoliation, but after 8 days, was at comparable levels to those before defoliation. It was not until 14 days after defoliation that the amount of respiration from newly assimilated C (¹³C) exceeded that of C assimilated before defoliation (¹⁴C). This revised version was published online in June 2006 with corrections to the Cover Date.     

Kohlenstoffassimilation von Chlamydobotrys (Volvocales)

Zusammenfassung Mit Hilfe C¹⁴-markierten Acetats und Bicarbonats wurde die Kohlenstoffassimilation aus Acetat und Kohlendioxyd von Chlamydobotrys unter verschiedenen Bedingungen untersucht. Der überwiegende Teil des aus Acetat in zelleigenes Material eingebauten Kohlenstoffs stammt aus der Methylgruppe, während entwickeltes Kohlendioxyd vorwiegend aus der Carboxylgruppe freigesetzt wird. Verglichen mit der Kohlenstofffixierung unter Anaerobiose steigern aerobe Bedingungen die Kohlenstoffassimilation aus Acetat im Licht um rund 25%. Im Dunkeln wird nur 10% des Kohlenstoffs aus Acetat in zelleigene Substanz eingebaut, das sind nur 3% des unter gleichen Bedingungen im Licht assimilierten.Zur Zeit optimaler Acetatassimilation findet nur eine sehr schwache Kohlendioxydfixierung statt, diese steigt mit dem Alter der Kultur. Die CO₂-Assimilation nimmt bei Acetatmangel zu; der aus CO₂ unter optimalen Bedingungen fixierte Kohlenstoff beträgt nur 5% des unter optimalen Verhältnissen aus Acetat assimilierten.

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Summary The carbon assimilation from radioactive labeled acetate and from NaH¹⁴CO₃ by Chlamydobotrys was studied under different conditions. Most of the carbon assimilated from acetate in the light comes from the methyl group, while the CO₂ produced was derived mainly from the carboxyl carbon. In light under aerobic conditions the carbon assimilation from acetate is higher by 25% than under anaerobic conditions. In the dark only 10% of the total acetate-carbon utilized are incorporated into cell material; that is only 3% of the total acetate carbon incorporated in light. During the period of high acetate assimilation the photosynthetic fixation of CO₂ is extremely weak. At acetate deficiency CO₂-fixation rises, but reaches only 5% of the carbon assimilated from acetate under optimum conditions.

     

Allocation and Turnover of Photosynthetically Assimilated CO(2) in Leaves of Glycine max L. Clark

The allocation and turnover of photosynthetically assimilated ¹⁴CO₂ in lipid and protein fractions of soybean (Glycine max L. Clark) leaves and stem materials was measured. In whole plant labeling experiments, allocation of photosynthate from a pulse of ¹⁴CO₂ into polymeric compounds was: 25% to proteins in 4 days, 20% to metabolically inert cell wall products in 1 to 2 days, 10% to lipids in 4 days, and 4% to starch in 1 day. The amount of ¹⁴C labeled photosynthate that an actively growing leaf (leaf 4) used for its own lipid synthesis immediately following pulse labeling was about 25%. The ¹⁴C of labeled proteins turned over with half-lives of 3.8, 3.3, and 4.1 days in leaves 1, 2, and 3, respectively; and turnover of ¹⁴C in total shoot protein proceeded with a half-life of 5.2 days. Three kinetic ¹⁴C turnover patterns were observed in lipids: a rapid turnover fraction (within a day), an intermediate fraction (half-life about 5 days), and a slow turnover fraction. These results are discussed in terms of previously published accounts of translocation, carbon budgets, carbon use, and turnover in starch, lipid, protein, and cell wall materials of various plants including soybeans.     

ALGAL EXCRETION OF 14C-LABELED COMPOUNDS AND MICROBIAL INTERACTIONS IN CYANIDIUM CALDARIUM MATS1

Acid spring effluents are often covered with mats of the eucaryotic phycocyanin-containing alga. Cyanidium caldarium. The primary bacterial component of such mats is an acidophilic strain of Bacillus coagulans, and the primary fungal component is Dactylaria gallopava. Because of the limited species diversity, C. caldarium mats appeared to be an excellent system for studying algal excretion and various microbial interactions in nature. From 2 to 6% of the NaH¹⁴CO₃ taken up by natural or laboratory populations of the alga was excreted as ¹⁴C-labeled materials. The maximum excretion occurred at temperature, light, and pH values optimum for NaH¹⁴CO₃ uptake. However, when excretion was expressed as a percentage of NaH14 CO₃ uptake, a higher percentage of the radioactivity was excreted at nonoptimal conditions for NaH¹⁴CO₃ uptake. Fungal biomass was directly proportional to algal density, but bacterial numbers varied widely and did not correlate with algal numbers. The bacterial and fungal components could be grown in mixed culture with either growing C. caldarium cultures or in an extract prepared, by healing algal cells.     

The effect of O2 and CO2 concentration on photosynthesis and glycolate accumulation in bean leaves treated with α-hydroxy-2-pyridinemethanesulfonic acid (α-HPMS), the glycolate oxidase inhibitor

¹⁴CO₂ assimilation, ¹⁴C incorporation into glycolate and glycolate accumulation in -HPMS treated bean leaves at various O₂ and CO₂ concentrations were studied. In 1% CO₂ oxygen concentration had no significant effect on glycolate accumulation and ¹⁴C incorporation into glycolate. In the CO₂ concentration range of 0.03% to 0.01%, increased oxygen concentration decreased not only ¹⁴CO₂ assimilation but also glycolate accumulation and ¹⁴C incorporation into glycolate. In 1% and 0.1% CO₂, no matter what O₂ concentration was supplied, and in 0.03% CO₂ with 2% and 21% O₂, all of the glycolate accumulated was formed from newly assimilated carbon. In 0.01% CO₂ and 2%, 21% and 100% O₂, and in 0.03% CO₂ with 100% O₂, a substantial portion of the glycolic acid that accumulated in leaves originated from endogenous unlabelled substrates. These findings are discussed in terms of possible changes in the ratio of RuBP carboxylation to RuBP oxygenation and of changes of RuBP pool size, induced by changing O₂ and CO₂ concentrations.This work was supported by the Polish Academy of Sciences, Contract No. 10.2.10.     

Differences in rhizosphere carbon-partitioning among plant species of different families

Interspecific variations in carbon (C) allocation and partitioning in the rhizosphere were investigated on 12 Mediterranean species belonging to different family groups (grasses, legumes, non-legume forbs) and having different life cycles. Plants grown individually in artificial soil, in a greenhouse and inoculated with rhizosphere microflora were labelled with ¹⁴CO₂ for 3 h at the vegetative stage. Rhizosphere respiration was measured during 6 days after which labelled C partitioning between shoots, roots, soil, root washing solution and respiration was estimated. The percentage of assimilated ¹⁴C allocated below ground differed significantly between species (41 – 76%) but no significant difference was found between grasses, legumes and non-legume forbs. When expressed as percentage of below-ground ¹⁴C, rhizosphere respiration was significantly smaller for non-legume forbs (42%) than for grasses (46%) and legumes (51%). Consequently more ¹⁴C was incorporated into root biomass in the former. Half-life of ¹⁴CO₂ evolution through respiration ranged from 23 h in legumes to 27 h for non-legume forbs and 37 h for grasses. This suggested differences in microbial activities due to quantities and quality of root exuded C. Rhizosphere respiration was positively correlated with the amount of ¹⁴C in the solution used to wash the roots on one hand, and root N concentration on the other hand. This led to a functional hierarchy between plant family groups of the overall rhizosphere activity. It went from non-legume forbs being the less active (except Crepis sancta)in terms of respiration and exudation, to grasses and then legumes, the most active but also the richest in nitrogen.     

Inorganic carbon fixation and metabolism in maize roots as affected by nitrate and ammonium nutrition

The effects of NO^?₃ and NH⁺₄ nutrition on the rates of dark incorporation of inorganic carbon by roots of hydroponically grown Zea mays L. cv. 712 and on the metabolic products of this incorporation, were determined in plants supplied with NaH¹⁴CO₃ in the nutrient solution. The shoots and roots of the plants supplied with NaH¹⁴CO₃ in the root medium for 30 min were extracted with 80%; (v/v) ethanol and fractionated into soluble and insoluble fractions. The soluble fraction was further separated into the neutral, organic acid, amino acid and non-polar fractions. The amino acid fraction was then analyzed to determine quantities and the ¹⁴C content of its individual components. The rates of dark incorporation of inorganic carbon calculated from H¹⁴CO^?₃ fixation and attributable to the activity of phosphoenolpyuvate carboxylase (EC 4.1.1.31), were 5-fold higher in ammonium-fed plants than in nitrate-fed plants after a 30-min pulse of ¹⁴C. This activity forms a small, but significant component of the carbon budget of the root. The proportion of ¹⁴C located in the shoots was also significantly higher in ammonium-fed plants than in nitrate-fed plants, indicating more rapid translocation of the products of dark fixation to the shoots in plants receiving NH⁺/sp₄ nutrition. Ammonium-fed plants favoured incorporation of ¹⁴C into amino acids, while nitrate-fed plants allocated relatively more ¹⁴C into organic acids. The amino acid composition was also dependent on the type of nitrogen supplied, and asparagine was found to accumulate in ammonium-fed plants. The ¹⁴C labelling of the amino acids was consistent with the diversion of ¹⁴C-oxaloacetate derived from carboxlyation of phosphoenolpyruvate into the formation of both asparatate and glutamate. The results support the conclusion that inorganic carbon fixation in the roots of maize plants provides an important anaplerotic source of carbon for NH⁺₄ assimilation.     

Photosynthesis of Lipids from CO(2) in Spinacia oleracea

Young expanding spinach leaves exposed to ¹⁴CO₂ under physiological conditions for up to 20 minutes assimilated CO₂ into lipids at a mean rate of 7.6 micromoles per milligram chlorophyll per hour following a lag period of 5 minutes. Label entered into all parts of the lipid molecule and only 28% of the ¹⁴C fixed into lipids was found in the fatty acid moieties, i.e. fatty acids were synthesized from CO₂in vivo at a mean rate of 2.1 micromoles per milligram chlorophyll per hour. Intact spinach chloroplasts isolated from these leaves incorporated H¹⁴CO₃ into fatty acids at a maximal rate of 0.6 micromole per milligram chlorophyll per hour, but were unable to synthesize either the polar moieties of their lipids or polyunsaturated fatty acids. Since isolated chloroplasts will only synthesize fatty acids at rates similar to the one obtained with intact leaves in vivo if acetate is used as a precursor, it is suggested that acetate derived from leaf mitochondria is the physiological fatty acid precursor.     

Rate of Belowground Carbon Allocation Differs with Successional Habit of Two Afromontane Trees

Background

Anthropogenic disturbance of old-growth tropical forests increases the abundance of early successional tree species at the cost of late successional ones. Quantifying differences in terms of carbon allocation and the proportion of recently fixed carbon in soil CO₂ efflux is crucial for addressing the carbon footprint of creeping degradation.

Methodology

We compared the carbon allocation pattern of the late successional gymnosperm Podocarpus falcatus (Thunb.) Mirb. and the early successional (gap filling) angiosperm Croton macrostachyus Hochst. es Del. in an Ethiopian Afromontane forest by whole tree ¹³CO₂ pulse labeling. Over a one-year period we monitored the temporal resolution of the label in the foliage, the phloem sap, the arbuscular mycorrhiza, and in soil-derived CO₂. Further, we quantified the overall losses of assimilated ¹³C with soil CO₂ efflux.

Principal Findings

¹³C in leaves of C. macrostachyus declined more rapidly with a larger size of a fast pool (64% vs. 50% of the assimilated carbon), having a shorter mean residence time (14 h vs. 55 h) as in leaves of P. falcatus. Phloem sap velocity was about 4 times higher for C. macrostachyus. Likewise, the label appeared earlier in the arbuscular mycorrhiza of C. macrostachyus and in the soil CO₂ efflux as in case of P. falcatus (24 h vs. 72 h). Within one year soil CO₂ efflux amounted to a loss of 32% of assimilated carbon for the gap filling tree and to 15% for the late successional one.

Conclusions

Our results showed clear differences in carbon allocation patterns between tree species, although we caution that this experiment was unreplicated. A shift in tree species composition of tropical montane forests (e.g., by degradation) accelerates carbon allocation belowground and increases respiratory carbon losses by the autotrophic community. If ongoing disturbance keeps early successional species in dominance, the larger allocation to fast cycling compartments may deplete soil organic carbon in the long run.     

14C UPTAKE BY THE MARINE ANGIOSPERM PHYLLOSPADIX SCOULERP

Rhizomes and attached leaves of Phyllospadix scouleri Hook, were collected in the intertidal zone along the central California coast and exposed to a solution of NaH¹⁴CO₃ in seawater under controlled laboratory conditions. Over a 90-min period roots and rhizomes absorbed very little ¹⁴C compared to leaves. Translocation during that time was minor. Plants pretreated with the photosynthetic inhibitor DCMU showed no ¹⁴C uptake, indicating that under normal circumstances the carbon which is absorbed by leaves is fixed and accumulates as photosynthate. The rate of gross photosynthesis was about 13 mg CO₂ g dry wt⁻¹ hr⁻¹. Gross photosynthesis of wet leaves exposed to ¹⁴CO₂ in air was significantly less than leaves exposed to NaH¹⁴CO₃. The effect of a leaf-grazing limpet (Notoacmea paleacea) on leaf anatomy and ¹⁴C uptake is discussed.     

A comparison of carbon flow from pre-labelled and pulse-labelled plants

Perennial rye-grass was subjected to two different¹⁴C labelling regimes to enable a partitioning of the carbon sources contributing to rhizosphere carbon-flow. Plant/soil microcosms were designed which enabled rye-grass plants to either receive a single pulse of¹⁴C?CO₂ or to be pre-labelled using a series of¹⁴C?CO₂ pulses, allowing the fate of newly photoassimilated carbon and carbon lost by root decomposition to be followed into the soil. For young rye-grass plants grown over a short period, rhizosphere carbon flow was found to be dominated by newly photoassimilated carbon. Evidence for this came from the observed percentage of the total¹⁴C budget (i.e. total¹⁴C?CO₂ fixed by the plants) lost from the root/soil system, which was 30 times greater for the pulse labelled compared to pre-labelled plants. Root decomposition was found to be less at 10°C compared to 20–25°C, though input of¹⁴C into the soil was the same at both temperatures.     

TRANSLOCATION IN THE NONPOLYTRICHACEOUS MOSS GRIMMIA LAEVIGATA

A superficially rhizomatous habit suggested that the moss Grimmia laevigata might function as a clonal, rhizomatous plant and translocate photoassimilates to belowground organs, even though the species is outside the order Polytrichales, which includes the only mosses known to possess sieve cells. Labelling with ¹⁴CO₂ indicated that at least 10% of newly assimilated carbon was translocated out of leafy shoot portions within 26 hr. Of this carbon, approximately 75% was apparently moved into leafless, basal shoot portions and 25% into belowground stems. Infrared gas analysis of net CO₂ flux was used to check that labelling gave a realistic measure of photosynthesis. Physiological integration and clonal spread may account for the unusual ability of this moss to colonize extremely xeric microsites.     

Aspartate Carbamyltransferase : Site of End-Product Inhibition of the Orotate Pathway in Intact Cells of Cucurbita pepo

Lovatt et al. (1979 Plant Physiol 64: 562-569) have previously demonstrated that end-product inhibition functions as a mechanism regulating the activity of the orotic acid pathway in intact cells of roots excised from 2-day-old squash plants (Cucurbita pepo L. cv Early Prolific Straightneck). Uridine (0.5 millimolar final concentration) or one of its metabolites inhibited the incorporation of NaH¹⁴CO₃, but not [¹⁴C]carbamylaspartate or [¹⁴C]orotic acid, into uridine nucleotides (ΣUMP). Thus, regulation of de novo pyrimidine biosynthesis was demonstrated to occur at one or both of the first two reactions of the orotic acid pathway, those catalyzed by carbamylphosphate synthetase (CPSase) and aspartate carbamyltransferase (ACTase). The results of the present study provide evidence that ACTase alone is the site of feedback control by added uridine or one of its metabolites. Evidence demonstrating regulation of the orotic acid pathway by end-product inhibition at ACTase, but not at CPSase, includes the following observations: (a) addition of uridine (0.5 millimolar final concentration) inhibited the incorporation of NaH¹⁴CO₃ into ΣUMP by 80% but did not inhibit the incorporation of NaH¹⁴CO₃ into arginine; (b) inhibition of the orotate pathway by added uridine was not reversed by supplying exogenous ornithine (5 millimolar final concentration), while the incorporation of NaH¹⁴CO₃ into arginine was stimulated more than 15-fold when both uridine and ornithine were added; (c) incorporation of NaH¹⁴CO₃ into arginine increased, with or without added ornithine when the de novo pyrimidine pathway was inhibited by added uridine; and (d) in assays employing cell-free extracts prepared from 2-day-old squash roots, the activity of ACTase, but not CPSase, was inhibited by added pyrimidine nucleotides.     

Carbon assimilation during larval development of the marine teleost Leiostomus xanthurus Lacépède

In larval spot, Leiostomus xanthurus Lacépède, ¹⁴C labeled food was rapidly digested and assimilated with up to 20% respired as ¹⁴CO₂ within 10 h from ingestion. Two indices of carbon assimilation, total carbon utilization (range 9.4 to 64.7%) and total carbon absorption (range 67.2 to 99.2%) were calculated from the amount of ¹⁴C ingested, retained, and defecated. Carbon utilization and absorption were not significantly (P > 0.10) related to development as measured by age (7 to 47 days from hatching), length (1.8 to 11.4 mm), or dry weight (0.022 to 4.425 mg).     

Carbon translocation to the rhizosphere of maize and wheat and influence on the turnover of native soil organic matter at different soil nitrogen levels

Wheat and maize were grown in a growth chamber with the atmospheric CO₂ continuously labelled with ¹⁴C to study the translocation of assimilated carbon to the rhizosphere. Two different N levels in soil were applied. In maize 26–34% of the net assimilated ¹⁴C was translocated below ground, while in wheat higher values (40–58%) were found. However, due to the much higher shoot production in maize the total amount of carbon translocated below ground was similar to that of wheat. At high N relatively more of the C that was translocated to the root, was released into the soil due to increased root respiration and/or root exudation and subsequent microbial utilization and respiration. The evolution rate of unlabelled CO₂ from the native soil organic matter decreased after about 25 days when wheat was grown at high N as compared to low N. This negative effect of high N in soil was not observed with maize.     

Distribution of assimilated carbon in plants and rhizosphere soil of basket willow (Salix viminalis L.)

Willow is often used in bio-energy plantations for its potential to function as a renewable energy source, but knowledge about its effect on soil carbon dynamics is limited. Therefore, we investigated the temporal variation in carbon dynamics in willow, focusing on below-ground allocation and sequestration to soil carbon pools. Basket willow plants (Salix viminalis L.) in their second year of growth were grown in pots in a greenhouse. At five times during the plants growth, namely 0, 1, 2, 3 and 4 months after breaking winter dormancy, a subset of the plants were continuously labelled with ¹⁴CO₂ in an ESPAS growth chamber for 28 days. After the labelling, the plants were harvested and separated into leaves, first and second year stems and roots. The soil was analysed for total C and ¹⁴C content as well as soil microbial biomass. Immediately after breaking dormancy, carbon stored in the first year stems was relocated to developing roots and leaves. Almost half the newly assimilated C was used for leaf development the first month of growth, dropping to below 15% in the older plants. Within the second month of growth, secondary growth of the stem became the largest carbon sink in the system, and remained so for the older age classes. Between 31 and 41% of the recovered ¹⁴C was allocated to below-ground pools. While the fraction of assimilated ¹⁴C in roots and root+soil respiration did not vary with plant age, the amount allocated to soil and soil microbial biomass increased in the older plants, indicating an increasing rhizodeposition. The total amount of soil microbial biomass was 30% larger in the oldest age class than in an unplanted control soil. The results demonstrate a close linkage between photosynthesis and below-ground carbon dynamics. Up to 13% of the microbial biomass consisted of carbon assimilated by the willows within the past 4 weeks, up to 11% of the recovered ¹⁴C was found as soil organic matter.     

Further studies on the photosynthesis of carrot tissue cultures

The influence of kinetin and sucrose on the photosynthetic activity of carrot (Daucus carota) tissue cultures in relation to growth was investigated. The results showed that light contributes heavily to the growth of tissue cultures measured in terms of fresh and dry weight and cell division activity. In light, the fresh weight, dry weight, and number of cells per explant were about or more than doubled. This indicated that after the development of chloroplasts, carrot tissue cultures can grow autotrophically at least as far as energy and carbon are concerned. Kinetin was shown to have an important role in developing the photosynthetic apparatus and photosynthetic activity of tissue cultures as manifested by the increase of chlorophyll content (60%), Hill activity (about 3-fold), and ¹⁴C-fixation from NaH¹⁴CO₃ (about 20%). On the other hand, the presence of sucrose in the medium reduced the chlorophyll content by about 30% and ¹⁴C-fixation from NaH¹⁴CO₃ in the soluble fraction by about 60%. A possible correlation between the influence of kinetin on sugar uptake and the effect of kinetin on ¹⁴C-fixation from NaH¹⁴CO₃ was discussed.