Nitrogen deficiency increases the residence time of respiratory carbon in the respiratory substrate supply system of perennial ryegrass

Plant respiration draws on substrate pools of different functional/biochemical identity. Little is known about the effect of nitrogen deficiency on those pools' sizes, half-lives and relative contribution to respiration, and consequently, of carbon residence time in respiratory metabolism. Here we studied how nitrogen fertilization affects the respiratory carbon supply system of shoots and roots of Lolium perenne , a perennial grass. Plants grown at two nitrogen supply levels in continuous light were labelled with ¹³CO₂/¹²CO₂ for intervals ranging from 1 h to 1 month. The rate and isotopic composition of shoot, root and plant respiration were measured, and the time-courses of tracer incorporation into respired CO₂ were analysed by compartmental modelling. Nitrogen deficiency reduced specific respiration rate by 30%, but increased the size of the respiratory supply system by 30%. In consequence, mean residence time of respiratory carbon increased with nitrogen deficiency (4.6 d at high nitrogen and 9.2 d at low nitrogen supply). To a large extent, this was due to a greater involvement of stores with a long half-life in respiratory carbon metabolism of nitrogen-deficient plants. At both nitrogen supply levels, stores supplying root respiration were primarily located in the shoot, probably in the form of fructans.     

The utilization of recently assimilated carbon in graminaceous plants

Isotopic carbon and infra-red gas analysis techniques were used to measure the following growth attributes in maize, sorghum, winter wheat and perennial ryegrass: the rate of entry of carbon into each main shoot leaf; the rate of translocation of leaf assimilate to meristems; the fraction of leaf and total shoot assimilate respired in one diurnal period; and the distribution of residual assimilate to new leaf, stem, axillary shoots and root. The two tropical plants possessed higher leaf assimilation rates and larger leaves than the temperate species, but their efficiency of translocation was only marginally superior in the experimental conditions. In all species, c. 25% of the assimilate generated in the 8·4h photoperiod was respired in in the same diurnal period. Maize and sorghum partitioned a greater proportion of their total shoot assimilate to new leaf tissue at the main shoot apex and to root than wheat and ryegrass. On the other hand, wheat and ryegrass exported up to 30% of their assimilate to axillary shoots; in sorghum, little assimilate was translocated to axillary shoots, while in maize this activity was completely absent. Plant habit, as exemplified by the contrast between the annual, single-axis maize plant and the perennial, multi-tillering ryegrass plant, appears to be a reflexion of the pattern of assimilate distribution to areas of potential growth. With the exception of superior leaf assimilation rates in maize and sorghum, the four species showed no marked differences in respect of the production, transport and respiratory utilization of assimilates.     

Short-term dynamics of the carbon isotope composition of CO2 emitted from a wheat agroecosystem--physiological and environmental controls

Understanding environmental and physiological controls of the variations in δ(13) C of CO(2) respired (δ(13) C(R)) from different compartments of an ecosystem is important for separation of CO(2) fluxes and to assess coupling between assimilation and respiration. In a wheat field, over 3 days we characterised the temporal dynamics of δ(13) C(R) from shoots and roots, from the soil and from the whole agroecosystem. To evaluate the basis of potential variations in δ(13) C(R), we also measured δ(13) C in different organic matter pools, as well as meteorological and gas exchange parameters. We observed strong diel variations up to ca. 6% in shoot, root and soil δ(13) C(R), but not in δ(13) C of the putative organic substrates for respiration, which varied by not more than ca. 1% within 24 h. Whole ecosystem-respired CO(2) was least depleted in (13) C in the afternoon and most negative in the early morning. We assume that temporally variable respiratory carbon isotope fractionation and changes in fluxes through metabolic pathways, rather than photosynthetic carbon isotope fractionation, governs the δ(13) C of respired CO(2) at the diel scale, and thus provides insights into the metabolic processes related to respiration under field conditions.     

Arbuscular mycorrhizal colonization on carbon economy in perennial ryegrass: quantification by 13CO2/12CO2 steady-state labelling and gas exchange

Effects of the arbuscular mycorrhizal fungus (AMF) Glomus hoi on the carbon economy of perennial ryegrass (Lolium perenne) were investigated by comparing nonmycorrhizal and mycorrhizal plants of the same size, morphology and phosphorus status. Plants were grown in the presence of CO2 sources with different C isotope composition (delta13C -1 or -44). Relative respiration and gross photosynthesis rates, and belowground allocation of C assimilated during one light period ('new C'), as well as its contribution to respiration, were quantified by the concerted use of 13CO2/12CO2 steady-state labelling and 13CO2/12CO2 gas-exchange techniques. AMF (G. hoi) enhanced the relative respiration rate of the root + soil system by 16%, inducing an extra C flow amounting to 3% of daily gross photosynthesis. Total C flow into AMF growth and respiration was estimated at < 8% of daily gross photosynthesis. This was associated with a greater amount of new C allocated belowground and respired in mycorrhizal plants. AMF colonization affected the sources supplying belowground respiration, indicating a greater importance of plant C stores in supplying respiration and/or the participation of storage pools within fungal tissues. When ontogenetic and nutritional effects were accounted for, AMF increased belowground C costs, which were not compensated by increased photosynthesis rates. Therefore the instantaneous relative growth rate was lower in mycorrhizal plants.     

Partitioning and Utilization of Net Photosynthate in a Nodulated Annual Legume

The economy of carbon in nodulated white lupin (Lupinus albusL.) was studied in terms of consumption of net photosynthatein nitrogen fixation, in maintenance of respiration, and inthe production of dry matter and protein. Net photosynthesisrose to a maximum in early fruiting and then fell abruptly dueto shedding of leaves. Nodulated roots acquired translocateequivalent to 51% of the plant's net photosynthate, 78% of thecarbon of this translocate being respired, 10% entering drymatter, and 12% returning to the shoot attached to productsof nitrogen fixation. Nodules utilized 4?0–6?5 g C infixing 1 g nitrogen. Photosynthate was utilized most effectivelyfor nitrogen fixation in late vegetative growth. Fruits sequestered16% of the plant's net photosynthate, shoot night respiration17%, and dry matter formation in shoot vegetative parts 22%.Averaged over growth, 9?9 g net photosynthate was required toproduce 1 g seed dry matter and 31 g net photosynthate to produce1 g seed protein. Budgets for utilization of the carbon of netphotosynthate were constructed for 10 d intervals of the plant'sgrowth cycle. Feeding of shoots with ¹⁴CO₂ resulted in radiocarbonbecoming partitioned approximately as predicted by these budgets.The dependence of root respiration on recent photosynthate wasassessed by following the time course of release of ¹⁴CO₂ tothe rooting medium of the ¹⁴CO-labelled plants.     

Photoassimilate partitioning in nodulated soybean I. 11C methodology

An established method using ¹¹C for the in vivo measurement of photoassimilate partitioning within intact plants was applied to the characterization of partitioning of photoassimilate to soybean nodules. The method describes partitioning in terms of the magnitude and stability of partitioning flows, i.e. sink 'activity' and 'priority', and the transit time of tracer to a given sink. Leaflet labelling with ¹¹CO2 was recommended over whole shoot labelling to allow information on transport properties of the shoot to be acquired. The assumptions inherent in the method, that labelled and unlabelled photoassimilate in passage within the stem to the root system were well mixed and that tracer flow is unidirectional between source and sink (nodule), were validated. Tracer was re-exported from root to shoot, but this re-export process did not invalidate the assumption of unidirectional flow because the transit time of the re-export process was long relative to the half-life of the isotope. The transit time of tracer between entry to, and respiration from, the root system was also long (>60 min) relative to the half-life of the isotope. However, a significant fraction of tracer entering the root system was respired (c. 10% within 200 min), mainly by nodules (37% of tracer entering a nodule cluster was respired with 200 min). Therefore root-respired tracer was trapped and attributed to the nodule in partitioning calculations. A case study is presented using the method to assess changes in partitioning to nodules following treatment of the root system with nitrate, highlighting the limitation to this method of ontogenetic changes in the pattern of export from the load leaflet.     

Temporal dynamics of carbon partitioning and rhizodeposition in wheat

The temporal dynamics of partitioning and rhizodeposition of recent photosynthate in wheat (Triticum aestivum) roots were quantified in situ in solution culture. After a 30-min pulse of (14)CO(2) to a single intact leaf, (14)C activities of individual carbon fluxes in the root, including exudation, respiration, and root content, were measured continuously over the next 20 h concurrently with (14)C efflux from the leaf. Immediately after the end of the (14)CO(2) pulse, (14)C activity was detected in the root, the hydroponic solution, and in root respiration. The rate of (14)C exudation from the root was maximal after 2 to 3 h, and declined to one-third of maximum after a further 5 h. Completion of the rapid phase of (14)C efflux from the leaf coincided with peak (14)C exudation rate. Thus, exudation flux is much more rapidly and dynamically coupled to current photosynthesis than has been appreciated. Careful cross-calibration of (14)C counting methods allowed a dynamic (14)C budget to be constructed for the root. Cumulative (14)C exudation after 20 h was around 3% of (14)C fixed in photosynthesis. Partitioning of photosynthate between shoot and root was manipulated by partial defoliation before applying the (14)CO(2) pulse to the remaining intact leaf. Although the rate of photosynthesis was largely unaffected by partial defoliation, the proportion of new photosynthate subsequently partitioned to and exuded from the root was substantially reduced. This clearly indicates that exudation depends more on the rate of carbon import into the root than on the rate of photosynthesis.     

Carbohydrate supply and n(2) fixation in soybean : the effect of varied daylength and stem girdling

When arrival of shoot supplied carbohydrate to the nodulated root system of soybean was interrupted by stem girdling, stem chilling, or leaf removal, nodule carbohydrate pools were utilized, and a marked decline in the rates of CO₂ and H₂ evolution was observed within approximately 30 minutes of treatment. Nodule excision studies demonstrated that the decline in nodulated root respiration was associated with nodule rather than root metabolism, since within 3.5 hours of treatment, nodules respired at less than 10% of the initial rates. Apparently, a continuous supply of carbohydrate from the shoot is required to support nodule, but not root, function. Depletion of nodular carbohydrate pools was sufficient to account for the (diminishing) nodule respiration of girdled plants. Of starch and soluble sugar pools within the whole plant, only leaf starch exhibited a diurnal variation which was sufficient to account for the respiratory carbon loss of nodules over an 8 hour night. Under 16 hour nights, or in continuous dark, first the leaf starch pools were depleted, and then nodule starch reserves declined concomitant with a decrease in the rates of CO₂ and H₂ evolution from the nodules. Nodule soluble sugar levels were maintained in dark treated plants but declined in girdled plants. The depletion of starch in root nodules is an indicator of carbohydrate limitation of nodule function.     

A re-examination of phosphorus-lime interactions in perennial ryegrass

The results of a previous study had suggested that under conditions of limited P availability, Ca may be able to compensate for P in the shoot tissue of perennial ryegrass. To verify this preliminary finding, a factorial experiment was set up which simultaneously tested the effects of Ca and P fertilization on the yield and chemical composition of perennial ryegrass. Calcium was supplied as either lime or gypsum in order to differentiate between the effects of Ca and pH on the response of perennial ryegrass to P fertilization. In the final stage of the experiment a Zn treatment was included, to see whether altering the P/Zn ratios of plant shoots had any influence on the purported interaction between Ca and P. The results demonstrated that the P-sparing effect of lime occurs, at least partly, because Ca application improves the efficiency of absorbed P for DM production. However, it was reasonably clear that the site of the interaction between Ca and P was the soil-root interface, and not shoot tissue. It was suggested that under conditions of limited P supply, Ca stablizes root membranes and thereby minimizes both the efflux losses of nutrients from root tissue, and the compensatory flow of photosynthates from shoots to roots. No interaction was observed between P and Zn treatments in this study. Instead, a positive interaction was found between lime and Zn treatments, which suggests that the stabilizing action of Ca on root membranes requires Zn as a co-stabilizing factor. It is proposed that chemical analysis of shoot tissue alone may not be sufficient to accurately diagnose the P, Ca or Zn status of whole plants, since the critical levels of these elements in shoots appear to bear little relation to their requirements in the rhizosphere.     

Nitrogen and Carbon Flows Estimated by 15N and 13C Pulse-Chase Labeling during Regrowth of Alfalfa

The flow of 15N and 13C from storage compounds in organs remaining after defoliation (sources) to regrowing tissue (sinks), and 13C losses through root or shoot respiration were assessed by pulse-chase labeling during regrowth of alfalfa (Medicago sativa L.) following shoot removal. A total of 73% of labeled C and 34% of labeled N were mobilized in source organs within 30 d. Although all of the 15N from source organs was recovered in the regrowing tissue, much of the 13C was lost, mainly as CO2 respired from the root (61%) or shoot (8%), and was found to a lesser extent in sink tissue (5%). After 3, 10, or 30 d of regrowth, 87, 66, and 52% of shoot N, respectively, was derived from source tissue storage compounds; the rest resulted from translocation of fixed N2. Overall results suggest that most shoot C was linked to photosynthetic activity rather than being derived from mobilization of stored C in source organs. Furthermore, isotopic analysis of different chemical fractions of plant tissue suggests that between 14 and 58% of the shoot C derived from source tissues was linked to the mobilization of N compounds, not carbohydrates.     

Regrowth of western wheatgrass utilizing 14C-labeled assimilates stored in belowground parts

Summary Results of this study showed that carbohydrates stored in the roots of western wheatgrass are utilized for regrowth following clipping of the aboveground foliage. Shoots remained dependent on carbohydrates stored in roots until sufficient photosynthetic leaf surface was developed to supply carbon to the shoots. During early phenophases, the partitioning of carbohydrates between shoots and roots was identical, indicating equal metabolic demands for carbon from both the shoot and root systems. Subsequent fluctuations in root and shoot carbohydrates may be caused by selected pressure imposed on either the root or shoot systems by physiological changes in these organs.Respiratory losses of ¹⁴C were slower during the early phenophases which may indicate that either the rate of respiration was slower or that recently assimilated nonlabeled carbon sources were utilized for respiration instead of the endogenous sources assimilated earlier in the growth period. re]19760427     

C-isotope composition of CO2 respired by shoots and roots: fractionation during dark respiration?

The CO₂ respired by leaves is ¹³C-enriched relative to leaf biomass and putative respiratory substrates (Ghashghaie et al., Phytochemistry Reviews 2, 145–161, 2003), but how this relates to the ¹³C content of root, or whole plant respiratory CO₂ is unknown. The C isotope composition of respiratory CO₂ (δ_R) from shoots and roots of sunflower (Helianthus annuus L.), alfalfa (Medicago sativa L.), and perennial ryegrass (Lolium perenne L.) growing in a range of conditions was analysed. In all instances plants were grown in controlled environments with CO₂ of constant concentration and δ¹³C. Respiration of roots and shoots of individual plants was measured with an open CO₂ exchange system interfaced with a mass spectrometer. Respiratory CO₂ from shoots was always ¹³C-enriched relative to that of roots. Conversely, shoot biomass was always ¹³C-depleted relative to root biomass. The δ-difference between shoot and root respiratory CO₂ was variable, and negatively correlated with the δ-difference between shoot and root biomass (r² = 0.52, P = 0.023), suggesting isotope effects during biosynthesis. ¹³C discrimination in respiration (R) of shoots, roots and whole plants (e_Shoot, e_Root, e_Plant) was assessed as e = (δ_Substrate − δ_R)/(1 + δ_R/1000), where root and shoot substrate is defined as imported C, and plant substrate is total photosynthate. Estimates were obtained from C isotope balances of shoots, roots and whole plants of sunflower and alfalfa using growth and respiration data collected at intervals of 1 to 2 weeks. e_plant and e_Shoot differed significantly from zero. e_plant ranged between −0.4 and −0.9‰, whereas e_Shoot was much greater (−0.6 to −1.9‰). e_Root was not significantly different from zero. The present results help to resolve the apparent conflict between leaf- and ecosystem-level ¹³C discrimination in respiration.     

Contribution of new photosynthetic assimilates to respiration by perennial grasses and shrubs: residence times and allocation patterns

Quantification of the fate of carbon (C) used by plant metabolism is necessary to improve predictions of terrestrial ecosystem respiration and its sources. Here, a dual isotope ((13)C and (14)C) pulse-label was used to determine the allocation of new C to different respiratory pathways in the early and late growing seasons for two plant functional types, perennial grasses and shrubs, in the Owens Valley, CA, USA. Allocation differences between plant types exceeded seasonal allocation variation. Grasses respired 71 and 64% and shrubs respired 22 and 17% of the label below-ground in the early and late growing seasons, respectively. Across seasons and plant types, approximately 48-61% of the label recovered was respired in 24 h, approximately 68-84% in 6 d, and approximately 16-33% in 6-36 d after labeling. Three C pools were identified for plant metabolism: a fast pool with mean residence times (MRTs) of approximately 0.5 and approximately 1 d below- and above-ground, respectively; an intermediate pool with MRTs of 19.9 and 18.9 d; and a storage pool detected in new leaf early growing season respiration > 9 months after assimilation. Differences in allocation to fast vs intermediate C pools resulted in the mean age of C respired by shrubs being shorter (3.8-4.5 d) than that of the grasses (4.8-8.2 d).     

Soil temperature affects carbon allocation within arbuscular mycorrhizal networks and carbon transport from plant to fungus

How soil carbon balance will be affected by plant–mycorrhizal interactions under future climate scenarios remains a significant unknown in our ability to forecast ecosystem carbon storage and fluxes. We examined the effects of soil temperature (14, 20, 26 °C) on the structure and extent of a multispecies community of arbuscular mycorrhizal (AM) fungi associated with Plantago lanceolata. To isolate fungi from roots, we used a mesh‐divided pot system with separate hyphal compartments near and away from the plant. A ¹³C pulse label was then used to trace the flow of recently fixed photosynthate from plants into belowground pools and respiration. Temperature significantly altered the structure and allocation of the AM hyphal network, with a switch from more vesicles (storage) in cooled soils to more extensive extraradical hyphal networks (growth) in warmed soils. As soil temperature increased, we also observed an increase in the speed at which plant photosynthate was transferred to and respired by roots and AM fungi coupled with an increase in the amount of carbon respired per unit hyphal length. These differences were largely independent of plant size and rates of photosynthesis. In a warmer world, we would therefore expect more carbon losses to the atmosphere from AM fungal respiration, which are unlikely to be balanced by increased growth of AM fungal hyphae.     

Root turnover in pasture species: chicory,lucerne, perennial ryegrass and white clover

For pastures, root turnover can have an important influence on nutrient and carbon cycling, and plant performance. Turnover was calculated from mini‐rhizotron observations for chicory (Cichorium intybus), lucerne (Medicago sativa), perennial ryegrass (Lolium perenne) and white clover (Trifolium repens) grown in the Manawatu, New Zealand. The species were combined factorially with four earthworm species treatments and a no‐earthworm control. Split plots compared the effects of not cutting and cutting the shoots at intervals. Observations were made c. 18 days apart for 2.5 years. This article concentrates on differences between plant species in root turnover in the whole soil profile to 40 cm depth. At this scale, earthworm effects were generally small and short lived. For ryegrass and white clover, root length and mass were linearly related (R² = 0.82–0.99). For chicory and lucerne, the relationships were poorer (R² = 0.38–0.77), so for those species length turnover may be a poor indicator of mass turnover. Standing root length, total growth and death generally decreased in the sequence ryegrass > lucerne > chicory = white clover. In length terms, scaled turnover (growth divided by average standing root length) generally followed the sequence lucerne > white clover > perennial ryegrass = chicory. Across species the scaled turnover rate averaged 3.4 per year or 0.9% per day. Cutting shoots reduced standing root length, growth and death, but increased scaled turnover. These results indicate fast and prolonged root turnover. For ryegrass and white clover, at least there is need to reappraise how to measure and model shoot : root ratios, dry matter production and carbon cycling.     

Respiratory carbon metabolism following illumination in intact French bean leaves using (13)C/(12)C isotope labeling

The origin of the carbon atoms in the CO(2) respired by French bean (Phaseolus vulgaris) leaves in the dark has been studied using (13)C/(12)C isotopes as tracers. The stable isotope labeling was achieved through a technical device that uses an open gas-exchange system coupled online to an elemental analyzer and linked to an isotope ratio mass spectrometer. The isotopic analysis of the CO(2) respired in the dark after a light period revealed that the CO(2) was labeled, but the labeling level decreased progressively as the dark period increased. The pattern of disappearance depended on the amount of carbon fixed during the labeling and indicated that there were several pools of respiratory metabolites with distinct turnover rates. We demonstrate that the carbon recently assimilated during photosynthesis accounts for less than 50% of the carbon in the CO(2) lost by dark respiration and that the proportion is not influenced by leaf starvation in darkness before the labeling. Therefore, most of the carbon released by dark respiration after illumination does not come from new photosynthates.     

Compartmental Analysis of the Partitioning of Photo-assimilated Carbon in Nodulated Soybean Plants during the Light Period

Kouchi, H., Yoneyama, T. and Akao, S. 1986. Compartmental analysisof the partitioning of photo-assimilated carbon in nodulatedsoybean plants during the light period.—J. exp. Bot. 37:994–1005. Dynamics of the partitioning of photo-assimilated carbon invegetative nodulated soybean (Glycine max L.) plants in thelight period was investigated by compartmental analysis basedon data from steady-state ¹³CO₂ assimilation experiments. Themodel assumes a total of 18 compartments consisting of activeand temporary storage pools for soluble materials, starch andstructural materials in leaves, stems plus petioles, roots andnodules together with respired carbon from the roots and nodules.Carbon flow between compartments was described by 22 rate parameters.The rate parameters were evaluated by a non-linear least squaresearch method to optimize the fitness of the simulated resultswith the experimental tracer distribution. The compartment model was well applicable to interpret the carbonpartitioning in whole plants. The analysis showed that: (I)The largest carbon flux during the light period was to storagematerials (starch and temporary storage soluble pools) in theabove-ground parts. The total flux to storage pools was considerablylarger than the transporting flux to below-ground parts. (2)The main carbon flux to the nodules was via direct phloem pathwaysfrom the shoot and not via the compartment of root soluble materials.This flux was 72% of the total carbon flux from the shoot tothe nodulated root system. (3) A large amount of carbon wasreturned to the shoot from below-ground parts. The total returnof carbon flux to the shoot (85% from nodules) was equivalentto 54% of the total influx of carbon to below-ground parts.Direct carbon transfers between roots and nodules were relativelysmall. Key words: Compartmental analysis, carbon partitioning, root nodules, Glycine max L., ¹³CO₂, assimilation     

Carbon isotopes in terrestrial ecosystem pools and CO2 fluxes

Stable carbon isotopes are used extensively to examine physiological, ecological, and biogeochemical processes related to ecosystem, regional, and global carbon cycles and provide information at a variety of temporal and spatial scales. Much is known about the processes that regulate the carbon isotopic composition (delta(13)C) of leaf, plant, and ecosystem carbon pools and of photosynthetic and respiratory carbon dioxide (CO(2)) fluxes. In this review, systematic patterns and mechanisms underlying variation in delta(13)C of plant and ecosystem carbon pools and fluxes are described. We examine the hypothesis that the delta(13)C of leaf biomass can be used as a reference point for other carbon pools and fluxes, which differ from the leaf in delta(13)C in a systematic fashion. Plant organs are typically enriched in (13)C relative to leaves, and most ecosystem pools and respiratory fluxes are enriched relative to sun leaves of dominant plants, with the notable exception of root respiration. Analysis of the chemical and isotopic composition of leaves and leaf respiration suggests that growth respiration has the potential to contribute substantially to the observed offset between the delta(13)C values of ecosystem respiration and the bulk leaf. We discuss the implications of systematic variations in delta(13)C of ecosystem pools and CO(2) fluxes for studies of carbon cycling within ecosystems, as well as for studies that use the delta(13)C of atmospheric CO(2) to diagnose changes in the terrestrial biosphere over annual to millennial time scales.     

The effect of mineral nutrition on the growth and maintenance components of respiration during heterotrophic growth of barley seedlings

Spring barley seedling were grown in the dark for 21 d and respiration rates of the whole plant (including the seed), of the shoots, and of the roots were determined. A function describing the growth and maintenance components of respiration was interpolated through the experimental points and its parameters in plants under different mineral nutrition were compared. The plants grown in a complete nutrient solution showed the highest growth rate in the initial phase of development and thus reached the maximum respiration rate earlier than plants in the other variants. The highest proportion of substrate was respired in the shoot. Plants grown under deficiency of phosphorus and magnesium had a slower respiration rate than plants grown in the complete nutrient solution (NP), whereas the amount of respired substrate in plant parts was similar to that recorded in the NP plants. Plants grown in distilled water showed the lowest growth efficiency and respirated the highest proportion of substrate in the root.     

Temperature and Time-course of the Carbon Balance of Vegetative Tomato Plants During Prolonged Darkness: Examination of a Method of Estimating Maintenance Respiration

In order to examine the suitability of estimating maintenancerespiration in prolonged darkness, the variation of structuraldry matter (SDM) was calculated on vegetative tomato plantsduring 48 h of darkness. For that purpose, the time-coursesof respiration rate and carbohydrate content were recorded inshoots and roots at temperatures of 10, 15, 20, and 25 °C Two exponential declines of respiration rate, separated by ashort resumption, were observed in shoots and roots, differentcarbohydrate pools might be involved. Respiration rate was alwayshigher in roots than in shoots: the part played by energy costsof mineral absorption has to be investigated. After 14 h ofdarkness, a fall in respiration rate was associated with a progressiveexhaustion of sucrose and starch - which was quicker at highertemperatures - and a decrease in shoot to root carbon translccation.After 24 h of darkness, respiration stabilized at all temperatures.However, structural growth persisted throughout the dark periodat 10 °C, stopped after about 14 h darkness at. 15 and 20°C, and became negative beyond 24 h at 25 °C The hypothesis of maintenance of SDM after a period of darknesscan thus be invalidated. The simple observation of the time-courseof respiration rate does not allow complete inferences to bemade concerning biomass maintenance Lycopersicon esculentum Mill., tomato, respiration, maintenance respiration, carbohydrate reserves, translocation, structural dry matter, temperature