Seasonal allocation of photoassimilated carbon in douglas fir seedlings

The uptake of CO₂ by Douglas fir (Pseudotsuga menziesii [Mirb.] Franco) seedlings and the allocation of photoassimilated carbon among five vegetative tissues were closely related to seedling phenology. In May, newly flushing needles required 5.2% day⁻¹ of photoassimilated carbon relative to needle tissue carbon. As these needles matured, this carbon requirement declined to 1.95% day⁻¹ in August, to 0.94% day⁻¹ in November, and to 0.76% day⁻¹ in January. Other tissues of Douglas fir seedlings required different amounts of photoassimilated carbon for growth and metabolism. These data provide a strong link between daily CO₂ uptake and the regulation of carbon allocation by seasonal phenology.     

Control of Adventitious Root Production and Hypocotyl Hypertrophy of Sunflower (Helianthus annuus) in Response to Flooding

Needles of 20-year-old Scots pine trees (Pinus silvestris L.) were permitted to photoassimilate ¹⁴CO₂ for 1 h on different dates during the growing season. The loss of radioactivity from current, 1-year-old, and 2-year-old needles was followed, and the translocation of photoassimilated ¹⁴CO₂ from older needle age-classes to the elongating new needles studied. The effects of good mineral and water supply on translocation were also considered. In the spring, 1-year-old and 2-year-old needles accumulated ¹⁴C. These reserves, together with current photosynthate, were utilized when the trees started growing. The 1-year-old needles exported ¹⁴C to the current needles during the first weeks of elongation of the later, while no such translocation occurred from the 2-year-old needles. Removal of the 1-year-old needles resulted in translocation of assimilates from the 2-year-old needles to the current needles. The general pattern of translocation observed in the control trees was not changed when the trees were fertilized and irrigated. The new needles started to export assimilates in the middle of July when the photosynthetic rate per needle was comparable with that of the older age-classes. This occurred about 4 weeks after positive net photosynthesis was first measured for the current shoot. The current needles of trees with good nutrient and water supply seemed to become self-sufficient in photoassimilates earlier than the current needles of the control trees.     

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.     

Carbon uptake and respiration in above-ground parts of a Larix decidua × leptolepis tree

Summary Shade needles of hybrid larch (Larix decidua × leptolepis) had the same rates of photosynthesis as sun needles per dry weight and nitrogen, and a similar leaf conductance under conditions of light saturation at ambient CO₂ (A_max). However, on an area basis, A_max and specific leaf weight were lower in shade than in sun needles. Stomata of sun needles limited CO₂ uptake at light saturation by about 20%, but under natural conditions of light in the shade crown, shade needles operated in a range of saturating internal CO₂ without stomatal limitation of CO₂ uptake. In both needle types, stomata responded similarly to changes in light, but shade needles were more sensitive to changes in vapor pressure deficit than sun needles. Despite a high photosynthetic capacity, the ambient light conditions reduced the mean daily (in summer) and annual carbon gain of shade needles to less than 50% of that in sun needles. In sun needles, the transpiration per carbon gain was about 220 mol mol^–1 on an annual basis. The carbon budget of branches was determined from the photosynthetic rate, the needle biomass and respiration, the latter of which was (per growth and on a carbon basis) 1.6 mol mol^–1 year^–1 in branch and stem wood. In shade branches carbon gains exceeded carbon costs (growth + respiration) by only a factor of 1.6 compared with 3.5 in sun branches. The carbon balance of sun branches was 5 times higher per needle biomass of a branch or 9 times higher on a branch length basis than shade branches. The shade foliage (including the shaded near-stem sun foliage) only contributed approximately 23% to the total annual carbon gain of the tree.     

Isotope Labeling and Microautoradiography of Active Heterotrophic Bacteria on the Basis of Assimilation of 14CO2

Most heterotrophic bacteria assimilate CO₂ in various carboxylation reactions during biosynthesis. In this study, assimilation of ¹⁴CO₂ by heterotrophic bacteria was used for isotope labeling of active microorganisms in pure cultures and environmental samples. Labeled cells were visualized by microautoradiography (MAR) combined with fluorescence in situ hybridization (FISH) to obtain simultaneous information about activity and identity. Cultures of Escherichia coli and Pseudomonas putida assimilated sufficient ¹⁴CO₂ during growth on various organic substrates to obtain positive MAR signals. The MAR signals were comparable with the traditional MAR approach based on uptake of ¹⁴C-labeled organic substrates. Experiments with E. coli showed that ¹⁴CO₂ was assimilated during both fermentation and aerobic and anaerobic respiration. The new MAR approach, HetCO₂-MAR, was evaluated by targeting metabolic active filamentous bacteria, including “Candidatus Microthrix parvicella” in activated sludge. “Ca. Microthrix parvicella” was able to take up oleic acid under anaerobic conditions, as shown by the traditional MAR approach with [¹⁴C]oleic acid. However, the new HetCO₂-MAR approach indicated that “Ca. Microthrix parvicella,” did not significantly grow on oleic acid under anaerobic conditions with or without addition of NO₂⁻, whereas the addition of O₂ or NO₃⁻ initiated growth, as indicated by detectable ¹⁴CO₂ assimilation. This is a metabolic feature that has not been described previously for filamentous bacteria. Such information could not have been derived by using the traditional MAR procedure, whereas the new HetCO₂-MAR approach differentiates better between substrate uptake and substrate metabolism that result in growth. The HetCO₂-MAR results were supported by stable isotope analysis of ¹³C-labeled phospholipid fatty acids from activated sludge incubated under aerobic and anaerobic conditions in the presence of ¹³CO₂. In conclusion, the novel HetCO₂-MAR approach expands the possibility for studies of the ecophysiology of uncultivated microorganisms.     

Use of anin situ labeling technique for the determination of seasonal14C distribution in Ponderosa pine

A¹⁴C labeling apparatus was developed to permit the labeling of four-year-old Ponderosa pine with¹⁴CO₂ in the field. The labeling system is a completely closed canopy system with¹⁴CO₂ monitored by a GM tube ratemeter apparatus. The level of¹⁴CO₂ corresponding to ambient levels is monitored by a microloggercomputer which controls a¹⁴CO₂ generating system. The generated¹⁴CO₂ is mixed in the canopy by circulating the atmosphere with 12V diaphram pumps. The portable system requires little operator attention. At approximately monthly intervals over a one-year period two four-year-old Ponderosa pine trees were labeled for three to five days using this labeling apparatus. After an assimilate distribution period, one tree was excavated and analyzed for¹⁴C distribution. During late spring and early summer most of the carbon assimilated (>60%) was found in the active growing tips and new needles, with little being allocated to the roots (<10%) or woody material (<20%). During mid to late fall there was an increase in root labeling along with an increase in carbon going to woody material. Over the winter period, most of the fixed carbon (65%) resided in the older leaves. The early spring labeling period showed another pulse of root labeling along with some labeling of woody tissues.     

Forms of Dissolved Carbon Dioxide Required for Photosystem II Activity in Chloroplast Membranes

High concentrations of both bicarbonate and formate inhibit photosynthetic O₂ evolution at pH 8.0. At this pH, only 2.4% of the total dissolved carbon dioxide exists as CO₂. At pH 7.3, where 11% of the total dissolved carbon dioxide exists as CO₂, HCO₃⁻ no longer inhibits. While formate still inhibits O₂ evolution at pH 7.3, its effect can be partially overcome if CO₂ is also present. The rate of binding of added ¹⁴C-labeled inorganic carbon is nearly 10-fold more rapid when the internal pH of thylakoid membranes is at 6.0 than when it is at 7.8. These observations suggest that CO₂, not HCO₃⁻, is initially bound to the photosystem II reaction center and that the location of the binding site is on the inside thylakoid surface. However, additional data presented here suggest that, after binding, CO₂ is hydrated to HCO₃⁻ + H⁺ in a pH-dependent reaction. Two possible explanations of the “bicarbonate effect” are presented.     

Utilization of Exogenous Inorganic Carbon Species in Photosynthesis by Chlorella pyrenoidosa

The nature of the inorganic carbon utilized during photosynthesis by Chlorella pyrenoidosa was investigated using three experimental techniques (open gas analysis system with “artificial leaf” or “aqueous” chambers and O₂ electrode system) to measure carbon assimilation. Photosynthesis was studied as a function of pH and CO₂ concentration. The CO₂ concentration was inadequate to meet the requirements of photosynthesis only when HCO₃⁻ was added at high pH. Under all other conditions, the low and constant K_m (CO₂), in contrast to the highly variable K_m (HCO₃⁻), suggested that CO₂ was the major species utilized.     

The Rate of Photorespiration during Photosynthesis and the Relationship of the Substrate of Light Respiration to the Products of Photosynthesis in Sunflower Leaves

Single attached leaves of sunflower (Helianthus annus L. “Mennonite”) were supplied ¹⁴CO₂ of constant specific radioactivity in gas mixtures containing various CO₂ and O₂ concentrations. The ¹⁴CO₂ and CO₂ fluxes were measured concurrently in an open system using an ionization chamber and infrared gas analyzer.     

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.     

Characterization and Partial Purification of Aldose-6-phosphate Reductase (Alditol-6-Phosphate:NADP 1-Oxidoreductase) from Apple Leaves

The Pereskia are morphologically primitive, leafed members of the Cactaceae. Gas exchange characteristics using a dual isotope porometer to monitor ¹⁴CO₂ and tritiated water uptake, diurnal malic acid fluctuations, phosphoenolpyruvate carboxylase, and malate dehydrogenase activities were examined in two species of the genus Pereskia, Pereskia grandifolia and Pereskia aculeata. Investigations were done on well watered (control) and water-stressed plants. Nonstressed plants showed a CO₂ uptake pattern indicating C₃ carbon metabolism. However, diurnal fluctuations in titratable acidity were observed similar to Crassulacean acid metabolism. Plants exposed to 10 days of water stress exhibited stomatal opening only during an early morning period. Titratable acidity, phosphoenolpyruvate carboxylase activity, and malate dehydrogenase activity fluctuations were magnified in the stressed plants, but showed the same diurnal pattern as controls. Water stress causes these cacti to shift to an internal CO₂ recycling (“idling”) that has all attributes of Crassulacean acid metabolism except nocturnal stomata opening and CO₂ uptake. The consequences of this shift, which has been observed in other succulents, are unknown, and some possibilities are suggested.     

Effects of Chronic Internal beta-Radiation from Photoassimilated CO(2) on the Retention and Distribution of C in Young White Pine Plants

Eastern white pines (Pinus strobus L.) in their 3rd year of growth photoassimilated 35, 110, 220, or 400 microcuries of ¹⁴CO₂ on a single occasion in the spring when needle expansion was occurring. Once assimilated into organic products and translocated to various sinks, the retained ¹⁴C represented an internal chronic source of ionizing radiation to the plant. About 2.5 months later, the pines were harvested, and the distribution of ¹⁴C activity was determined. In addition, new needle lengths, fresh weights, and rates of processes involving CO₂ exchange were measured.     

Further studies on a new pathway of photosynthetic carbon dioxide fixation in sugar-cane and its occurrence in other plant species

1. The pathway of photosynthesis in sugar-cane, which gives most of the radio-activity fixed during short periods in ¹⁴CO₂ in C-4 of oxaloacetate, malate and aspartate, was examined under varied conditions. 2. The pattern of labelling was essentially the same with leaves of different ages and with leaves equilibrated at carbon dioxide concentrations in the range 0–3·8% (v/v) and light-intensities in the range 1400–9000ft.-candles before adding ¹⁴CO₂. 3. Radioactive products were examined after exposing leaves of 33 different plant species to ¹⁴CO₂ for 4sec. under standard conditions. 4. A labelling pattern typical of sugar-cane was found in several species of Gramineae but not in others. Of 16 species from other Families only a species of Cyperaceae contained a large proportion of the fixed radioactivity in oxaloacetate, malate and aspartate.     

Role of Carbon Dioxide in Catabolism of Propane by “Nocardia paraffinicum” (Rhodococcus rhodochrous)

The catabolism of propane by “Nocardia paraffinicum” (Rhodococcus rhodochrous) has been shown to involve CO₂ fixation after its oxidation to propionic acid. “N. paraffinicum” failed to grow on either propane or 1-propanol in the absence of CO₂. The rate of propane utilization was directly related to the initial CO₂ concentration, and Warburg respirometry suggested that CO₂ was required for the catabolism of 1-propanol, propionaldehyde, and propionate but not for 2-propanol. These data also suggested that the predominant pathway for the utilization of propane by “N. paraffinicum” was through 1-propanol. The use of [2-¹⁴C]propane and ¹⁴CO₂ confirmed the catabolism of propane and the fixation of CO₂. Through the use of these isotopes and the pyruvate carboxylase inhibitor sodium arsenite, the labeled 2,4-dinitrophenylhydrazine derivative of pyruvate was trapped and isolated via thin-layer chromatography. The trapping of [¹⁴C]pyruvate in this manner was considered to be indicative of the presence of the methylmalonyl coenzyme A pathway for CO₂ fixation.     

Effects of climate change on labile and structural carbon in Douglas-fir needles as estimated by δ13C and Carea measurements

Models of photosynthesis, respiration, and export predict that foliar labile carbon (C) should increase with elevated CO₂ but decrease with elevated temperature. Sugars, starch, and protein can be compared between treatments, but these compounds make up only a fraction of the total labile pool. Moreover, it is difficult to assess the turnover of labile carbon between years for evergreen foliage. Here, we combined changes in foliar C_area (C concentration on an areal basis) as needles aged with changes in foliar isotopic composition (δ¹³C) caused by inputs of ¹³C‐depleted CO₂ to estimate labile and structural C in needles of different ages in a four‐year, closed‐chamber mesocosm experiment in which Douglas‐fir (Pseudotsuga menziesii (Mirb.) Franco) seedlings were exposed to elevated temperature (ambient + 3.5 °C) and CO₂ (ambient + 179 ppm). Declines in δ ¹³C of needle cohorts as they aged indicated incorporation of newly fixed labile or structural carbon. The δ ¹³C calculations showed that new C was 41 ± 2% and 28 ± 3% of total needle carbon in second‐ and third‐year needles, respectively, with higher proportions of new C in elevated than ambient CO₂ chambers (e.g. 42 ± 2% vs. 37 ± 6%, respectively, for second‐year needles). Relative to ambient CO₂, elevated CO₂ increased labile C in both first‐ and second‐year needles. Relative to ambient temperature, elevated temperature diminished labile C in second‐year needles but not in first‐year needles, perhaps because of differences in sink strength between the two needle age classes. We hypothesize that plant‐soil feedbacks on nitrogen supply contributed to higher photosynthetic rates under elevated temperatures that partly compensated for higher turnover rates of labile C. Strong positive correlations between labile C and sugar concentrations suggested that labile C was primarily determined by carbohydrates. Labile C was negatively correlated with concentrations of cellulose and protein. Elevated temperature increased foliar %C, possibly due to a shift of labile constituents from low %C carbohydrates to relatively high %C protein. Decreased sugar concentrations and increased nitrogen concentrations with elevated temperature were consistent with this explanation. Because foliar constituents that vary in isotopic signature also vary in concentrations with leaf age or environmental conditions, inferences of c_i/c_a values from δ ¹³C of bulk leaf tissue should be done cautiously. Tracing of ¹³C through foliar carbon pools may provide new insight into foliar C constituents and turnover.     

Solid-state fermentation,lignin degradation and resulting digestibility of wheat straw fermented by selected white-rot fungi

Summary Lignin biodegradation, carbon loss and in vitro dry matter digestibility (IVDMD) have been investigated during the solid state fermentation of wheat straw by eight previously selected strains of white-rot fungi. A mathematical model of the degradation kinetics is presented. [The time period required to reach maximum rates of ¹⁴CO₂ and unlabeled CO₂ release from (¹⁴C)-lignin-labelled wheat straw and from whole wheat straw, respectively, was generally short (6–10 days).] High rates of ¹⁴C-lignin degradation were achieved by Pycnoporus cinnabarinus (2.9% ¹⁴CO₂ evolved/day), an unidentified strain Nancon (3.0%/day), Sporotrichum pulverulentum Nov. (3.4%/day), Bjerkandera adusta (2.4%/day), and Dichomitus squalens (2.3%). However, only the latter two strains degraded whole wheat straw slowly and Bjerkandera adusta was not able to degrade more than 23% of the ¹⁴C-lignin. Cyathus stercoreus and Dichomitus squalens facilitated the highest improvement in IVDMD (68% against 38% for the sound straw) after 20 and 15 days of cultivation respectively, with low dry matter losses (15–20%). A study of the fate of ¹⁴C-lignin during fermentation using these two fungal strains showed that maximal levels of (¹⁴C)-water-soluble compounds are reached before peak levels of ¹⁴CO₂ evolution suggesting that these compounds are intermediates in lignin degradation. A possible relationship between water-soluble lignins and IVDMD improvement is discussed.     

Characterization and In Situ Carbon Metabolism of Phototrophic Consortia

A dense population of the phototrophic consortium “Pelochromatium roseum” was investigated in the chemocline of a temperate holomictic lake (Lake Dagow, Brandenburg, Germany). Fluorescence in situ hybridization revealed that the brown epibionts of “P. roseum” constituted up to 37% of the total bacterial cell number and up to 88% of all green sulfur bacteria present in the chemocline. Specific amplification of 16S rRNA gene fragments of green sulfur bacteria and denaturing gradient gel electrophoresis fingerprinting yielded a maximum of four different DNA bands depending on the year of study, indicating that the diversity of green sulfur bacteria was low. The 465-bp 16S rRNA gene sequence of the epibiont of “P. roseum” was obtained after sorting of individual consortia by micromanipulation, followed by a highly sensitive PCR. The sequence obtained represents a new phylotype within the radiation of green sulfur bacteria. Maximum light-dependent H¹⁴CO₃⁻ fixation in the chemocline in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea suggested that there was anaerobic autotrophic growth of the green sulfur bacteria. The metabolism of the epibionts was further studied by determining stable carbon isotope ratios (δ¹³C) of their specific biomarkers. Analysis of photosynthetic pigments by high-performance liquid chromatography revealed the presence of high concentrations of bacteriochlorophyll (BChl) e and smaller amounts of BChl a and d and chlorophyll a in the chemocline. Unexpectedly, isorenieratene and β-isorenieratene, carotenoids typical of other brown members of the green sulfur bacteria, were absent. Instead, four different esterifying alcohols of BChl e were isolated as biomarkers of green sulfur bacterial epibionts, and their δ¹³C values were determined. Farnesol, tetradecanol, hexadecanol, and hexadecenol all were significantly enriched in ¹³C compared to bulk dissolved and particulate organic carbon and compared to the biomarkers of purple sulfur bacteria. The difference between the δ¹³C values of farnesol, the major esterifying alcohol of BChl e, and CO₂ was −7.1%, which provides clear evidence that the mode of growth of the green sulfur bacterial epibionts of “P. roseum” in situ is photoautotrophic.     

Carbon assimilation by the autotrophic thermophilic archaebacterium Thermoproteus neutrophilus

Growth of Thermoproteus neutrophilus at 85°C was studied using an improved mineral medium with CO₂, CO₂ plus acetate, CO₂ plus propionate, or CO₂ plus succinate as carbon sources; sulfur reduction with H₂ to H₂S was the sole source of energy. None of the carbon compounds added was oxidized to CO₂. The organism grew autotrophically with a generation time of 9–14 h, up to a cell density of 0.5 g dry weight per liter (2×10⁹ cells/ml). Propionate did not stimulate, succinate slightly stimulated the growth rate. Acetate, even at low concentrations (0.5 mM), stimulated the growth rate, the generation time being shortened to 3–4 h. Acetate provided 70% of the cell carbon, which shows that Thermoproteus neutrophilus is a facultative autotroph. The path of these carbon precursors into cell compounds was studied by ¹⁴C long-term labelling and investigation of enzyme activities. Propionate could not be used as a major carbon source and was incorporated only into isoleucine, probably via the citramalate pathway. Acetate was a preferred carbon source which suppressed autotrophic CO₂ fixation: acetate grown cells exhibited an incomplete citric acid cycle in which 2-oxoglutarate dehydrogenase was present, but fumarate reductase was repressed. The succinate incorporation pattern and enzyme pattern indicated that autotrophic CO₂ fixation proceeded via a yet to be defined reductive citric acid cycle.     

Effect of Fall Turnover on Terminal Carbon Metabolism in Lake Mendota Sediments

The carbon and electron flow pathways and the bacterial populations responsible for the transformation of H₂-CO₂, formate, methanol, methylamine, acetate, ethanol, and lactate were examined in eutrophic sediments collected during summer stratification and fall turnover. The rate of methane formation averaged 1,130 μmol of CH₄ per liter of sediment per day during late-summer stratification versus 433 μmol of CH₄ per liter of sediment per day during the early portion of fall turnover, whereas the rate of sulfate reduction was 280 μmol of sulfate per liter of sediment per day versus 1,840 μmol of sulfate per liter of sediment per day during the same time periods, respectively. The sulfate-reducing population remained constant while the methanogenic population decreased by one to two orders of magnitude during turnover. The acetate concentration increased from 32 to 81 μmol per liter of sediment while the acetate transformation rate constant decreased from 3.22 to 0.70 per h, respectively, during stratification versus turnover. Acetate accounted for nearly 100% of total sedimentary methanogenesis during turnover versus 70% during stratification. The fraction of ¹⁴CO₂ produced from all ¹⁴C-labeled substrates examined was 10 to 40% higher during fall turnover than during stratification. The addition of sulfate, thiosulfate, or sulfur to stratified sediments mimicked fall turnover in that more CO₂ and CH₄ were produced. The addition of Desulfovibrio vulgaris to sulfate-amended sediments greatly enhanced the amount of CO₂ produced from either [¹⁴C]methanol or [2-¹⁴C]acetate, suggesting that H₂ consumption by sulfate reducers can alter methanol or acetate transformation by sedimentary methanogens. These data imply that turnover dynamically altered carbon transformation in eutrophic sediments such that sulfate reduction dominated over methanogenesis principally as a consequence of altering hydrogen metabolism.     

Seasonal Shifts of Photosynthesis in Portulacaria afra (L.) Jacq

Portulacaria afra (L.) Jacq., a perennial facultative Crassulacean acid metabolism (CAM) species, was studied under natural photoperiods and temperatures in San Diego, California. The plants were irrigated every fourth day throughout the study period. Measurements of ¹⁴CO₂ uptake, stomatal resistance, and titratable acidity were made periodically from July 1981 through May 1982. P. afra maintained C₃ photosynthesis during the winter and the spring. Diurnal acid fluctuations were low and maximal ¹⁴CO₂ uptake occurred during the day. The day/night ratio of carbon uptake varied from 5 to 10 and indicated little nocturnal CO₂ uptake. CAM photosynthesis occurred during the summer and a mixture of both C₃ and CAM during the fall. Large acid fluctuations of 100 to 200 microequivalents per gram fresh weight were observed and maximal ¹⁴CO₂ uptake shifted to the late night and early morning hours. Daytime stomatal closure was evident. A reduction in the day/night ratio of carbon uptake to 2 indicated a significant contribution of nocturnal CO₂ uptake to the overall carbon gain of the plant. The seasonal shift from C₃ to CAM was facilitated by increasing daytime temperature and accompanied by reduced daytime CO₂ uptake despite irrigation.