A circadian rhythm in the level of carbon dioxide compensation in Bryophyllum fedtschenkoi with zero values during the transient

Summary Detached shoots of Bryophyllum fedtschenkoi maintained in a closed system in the light exhibited an endogenous circadian rhythm in CO₂ compensation. The rhythm was sensitive to changes in light intensity and temperature. At 15° C it damped rapidly in light of 78 J m^-2 s^-1, but at 10° C a rhythm of considerable amplitude was evident at this same light intensity. During the transient (i.e. the temporary state of the rhythm before it acquired its steady state) low compensation values between 0 and 5 ppm CO₂ were achieved. When the plants were maintained at a higher light intensity prior to the measurements, the period of low compensation during the transient was extended, and zero values were obtained under some conditions.Studies of gas exchange at opposite phases of the rhythm revealed: (i) that the rate of uptake of ¹⁴CO₂ differed, both in light and darkness (the epidermis was removed during these observations to avoid interference from stomatal rhythms); (ii) photorespiration, estimated by extrapolation of the graph relating photosynthetic rate and CO₂ concentration, was highest during the peaks of the rhythm in CO₂ compensation; (iii) estimates of the capacity for photorespiration by the glycine-1-¹⁴C assay indicated highest values during the troughs of the rhythm. These findings are discussed in relation to the C₄-acid metabolism of this species. Low CO₂ compensation is probably due to the activity of phosphoenolpyruvate carboxylase and not to the absence of processes involving CO₂ evolution.     

Spatial and temporal variation in soil CO2 efflux in an old-growth neotropical rain forest, La Selva, Costa Rica

Our objectives were to quantify and compare soil CO₂ efflux of two dominant soil types in an old-growth neotropical rain forest in the Atlantic zone of Costa Rica, and to evaluate the control of environmental factors on CO₂ release. We measured soil CO₂ efflux from eight permanent soil chambers on six Oxisol sites. Three sites were developed on old river terraces (old alluvium) and the other three were developed on old lava flows (residual). At the same time we measured soil CO₂ concentrations, soil water content and soil temperature at various depths in 6 soil shafts (3 m deep). Between old alluvium sites, the two-year average CO₂ flux rates ranged from 117.3 to 128.9 mg C m^–2 h^–1. Significantly higher soil CO₂ flux occurred on the residual sites (141.1 to 184.2 mg C m^–2 h^–1). Spatial differences in CO₂ efflux were related to fine root biomass, soil carbon and phosphorus concentration but also to soil water content. Spatial variability in CO₂ storage was high and the amount of CO₂ stored in the upper and lower soil profile was different between old alluvial and residual sites. The major factor identified for explaining temporal variations in soil CO₂ efflux was soil water content. During periods of high soil water content CO₂ emission decreased, probably due to lower diffusion and CO₂ production rates. During the 2-year study period inter-annual variation in soil CO₂ efflux was not detected.     

Uptake of organic matter by the roots of sweet potato: Analysis of the δ14C value of plants

Summary To determine whether sweet potato (Ipomoea batatas (L.) Poir.) takes up organic matter through the roots from the medium, the concentrations of natural¹⁴C (¹⁴C) in plant organic matter, atmospheric CO₂ and compost applied to media were examined under soil and sand culture conditions. In these experiments, three kinds of composts of different ¹⁴C were used. CO₂ derived from the mineralization of compost was continuously pumped out from the pots and its direct uptake by the leaves was prevented.¹⁴C of plant parts harvested after the 43 days experimental period were affected by the ¹⁴C of the compost in the treatments where the compost of rice straw was applied, and which suggested that a significant amount of plant carbon was derived from the compost.     

Observations on carbon dioxide fixation in the Nant-y-moch reservoir,Ceredigion, Wales

High rates of carbon dioxide fixation, both in the light and the dark have been observed in Nant-y-Moch Mountain reservoir; these are surprising because of the sparse algal population. The values of CO₂-carbon fixed in the light per milligramme of Chlorophyll a per hour, ranged from 0.1167 mgC/ mg Chl a/hr. to infinity and are much higher than any recorded previously. The uptake of ¹⁴C-sucrose and ¹⁴C glucose was also determined. Factors which might possibly account for these observations, either alone or in combination are discussed. Possible CO₂ fixing agencies include detritus, flagellates and other organisms capable of obtaining energy by dark reactions (chemotrophs).     

Elevated CO2 effects on carbon and nitrogen cycling in grass/clover turves of a Psammaquent soil

Effects of elevated CO₂ (525 and 700 L L^–1), and a control (350 L L^–1 CO₂), on biochemical properties of a Mollic Psammaquent soil in a well-established pasture of C3 and C4 grasses and clover were investigated with continuously moist turves in growth chambers over four consecutive seasonal temperature regimes from spring to winter inclusive. After a further spring period, half of the turves under 350 and 700 L L^–1 were subjected to summer drying and were then re-wetted before a further autumn period; the remaining turves were kept continuously moist throughout these additional three consecutive seasons. The continuously moist turves were then pulse-labelled with ¹⁴C-CO₂ to follow C pathways in the plant/soil system during 35 days.Growth rates of herbage during the first four seasons averaged 4.6 g m^–2 day^–1 under 700 L L^–1 CO₂ and were about 10% higher than under the other two treatments. Below-ground net productivity at the end of these seasons averaged 465, 800 and 824 g m^–2 in the control, 525 and 700 L L^–1 treatments, respectively.in continuously moist soil, elevated CO₂ had no overall effects on total, extractable or microbial C and N, or invertase activity, but resulted in increased CO₂-C production from soil, and from added herbage during the initial stages of decomposition over 21 days; rates of root decomposition were unaffected. CO₂ produced h^–1 mg^–1 microbial C was about 10% higher in the 700 L L^–1 CO₂ treatment than in the other two treatments. Elevated CO₂ had no clearly defined effects on N availability, or on the net N mineralization of added herbage.In the labelling experiment, relatively more ¹⁴C in the plant/soil system occurred below ground under elevated CO₂, with enhanced turnover of ¹⁴C also being suggested.Drying increased levels of extractable C and organic-N, but decreased mineral-N concentrations; it had no effect on microbial C, but resulted in lowered microbial N in the control only. In soil that had been previously summer-dried, CO₂ production was again higher, but net N mineralization was lower, under elevated CO₂ than in the control after autumn pasture growth.Over the trial period of 422 days, elevated CO₂ generally appears to have had a greater effect on soil C turnover than on soil C pools in this pasture ecosystem.     

Biodegradation of pentachorophenol by tropical basidiomycetes in soils contaminated with industrial residues

Summary The ability of tropical Brazilian basidiomycetes to degrade pentachlorophenol (PCP) in soils from areas contaminated with organochlorine industrial residues was studied. Thirty-six basidiomycetes isolated from different tropical ecosystems were tested for tolerance to high PCP concentrations in soil. Peniophoracinereaand Psilocybecastanella, two strains of Trametes villosa,Agrocybe perfecta, Trichaptum bisogenumand Lentinus villosuswere able to colonize soil columns containing up to 4600 mg pentachlorophenol kg⁻¹soil. The first four species were inoculated into soil containing 1278 mg pentachlorophenol kg⁻¹ soil supplemented with gypsum and sugar cane bagasse. P. cinerea,P.castanella, T. villosaCCB176 and CCB213 and Agrocybe perfectareduced the PCP present in the contaminated soil by 78, 64, 58, 36 and 43%, respectively, after 90 days of incubation. All fungi mineralized [¹⁴C] pentachlorophenol, mainlyP. cinereaandT. villosawith the production of 7.11 and 8.15% ¹⁴CO₂, respectively, during 120 days of incubation. All fungi produced chloride ions during growth on soil containing PCP, indicating dehalogenation of the molecule. Conversion of PCP to pentachloroanisole was observed only after 90 days of incubation in soils inoculated with A. perfecta, P.cinereaand one of T. villosastrain. The present study shows the potential of Brazilian fungi for the biodegradation of toxic and persistent pollutants and it is the first to report fungal growth and PCP depletion in soils with high pentachlorophenol concentrations.     

Evolution of the single copyαA-crystallin gene: differently sized mRNAs of mammals and birds show homology in their 3′ non-coding regions

A-Crystallin, a major structural polypeptide of the vertebrate eye lens, is evolutionarily highly conserved. We have analyzed the corresponding nucleic acid sequences in both genomic DNA digests as well as in lens cytoplasmic RNA preparations from a wide variety of vertebrates by blot hybridization with cloned rat A₂-crystallin cDNA probes. The probes are not able to hybridize under any conditions to RNA and DNA derived from fishes and amphibia, but do show substantial homology with the sequences of mammals, birds and reptiles. The A-crystallin gene, which has been isolated from a hamster gene library occurs only once in the haploid genome. Coding and 3-untranslated regions of A₂-crystallin mRNA are conserved among all mammals and birds examined. However, the regions comprising the conserved sequences are differently represented in the ultimate mRNA. The A₂-mRNA 3-non-coding regions of reptiles and birds are 300–550 bases longer than those of mammals. Some rodents produce next to the A₂-mRNA another messenger that encodes the A^lns-polypeptide possessing an insertion of 22/23 amino acid residues between positions 63 and 64 of the A₂-polypeptide chain. A₂ and A^lns-mRNA are generated from a single gene as major and minor species, respectively, in a proportion which is similar to the ratio of the polypeptides foundin vivo andin vitro. The size heterogeneity of the A₂-mRNA from most mammals examined is due to the variable size of the poly(A) tail.     

Nitrogen and phosphorus requirements for raising mycorrhizal seedlings of Leucaena leucocephala in containers

A greenhouse study was undertaken to determine the nitrogen and phosphorus fertilization requirements for raising mycorrhizal seedlings in soil in containers. Seedlings of Leucaena leucocephala were grown for 40 days in dibble tubes containing fumigated or nonfumigated soil uninoculated or inoculated with Glomus aggregatum. The soil was fertilized with NH₄NO₃ solution to obtain 25–200 mg N kg^-1 soil, and with a KH₂PO₄ solution to establish target soil solution P concentrations of 0.015–0.08 mg P l^-1. At the end of 40 days, seedlings were transplanted into pots containing 5-kg portions of fumigated soil. Posttransplant vesicular arbuscular mycorrhizal fungal (VAMF) effectiveness, measured as pinnule P content, plant height, shoot dry weight and tissue N and P concentrations, was significantly increased by pretransplant VAMF colonization in both soils. The best posttransplant mycorrhizal colonization and mycorrhizal growth responses were observed if the nonfumigated pretransplant soil was amended with 50 mg N kg^-1 soil and 0.04 mg P l^-1 or if the fumigated pretransplant soil was amended with 100 mg N kg^-1 soil and 0.04 mg P 1^-1. There was no relationship between NP ratios of nutrients added to the pretransplant soil medium and shoot NP ratios observed after transplanting. Shoot NP ratio was also not correlated with root colonization level.Contribution from the Hawaii Institute of Tropical Agriculture and Human Resources Journal Series No. 4025     

Incorporation of 14CO2 into C4 acids by leaves of C3-C4 intermediate and C3 species of Moricandia and Panicum at the CO2 compensation concentration

Comparative ¹⁴CO₂ pulse-¹²CO₂ chase studies performed at CO₂ compensation ()-versus air-concentrations of CO₂ demonstrated a four-to eightfold increase in assimilation of ¹⁴CO₂ into the C₄ acids malate and aspartate by leaves of the C₃-C₄ intermediate species Panicum milioides Nees ex Trin., P. decipiens Nees ex Trin., Moricandia arvensis (L.) DC., and M. spinosa Pomel at . Specifically, the distribution of ¹⁴C in malate and aspartate following a 10-s pulse with ¹⁴CO₂ increases from 2% to 17% (P. milioides) and 4% to 16% (M. arvensis) when leaves are illuminated at the CO₂ compensation concentration (20 l CO₂/l, 21% O₂) versus air (340 l CO₂/l, 21% O₂). Chasing recently incorporated ¹⁴C for up to 5 min with ¹²CO₂ failed to show any substantial turnover of label in the C₄ acids or in carbon-4 of malate. The C₄-acid labeling patterns of leaves of the closely related C₃ species, P. laxum Sw. and M. moricandioides (Boiss.) Heywood, were found to be relatively unresponsive to changes in pCO₂ from air to . These data demonstrate that the C₃-C₄ intermediate species of Panicum and Moricandia possess an inherently greater capacity for CO₂ assimilation via phosphoenolpyruvate (PEP) carboxylase (EC 4.1.1.31) at the CO₂ compensation concentration than closely related C₃ species. However, even at , CO₂ fixation by PEP carboxylase is minor compared to that via ribulosebisphosphate carboxylase (EC 4.1.1.39) and the C₃ cycle, and it is, therefore, unlikely to contribute in a major way to the mechanism(s) facilitating reduced photorespiration in the C₃-C₄ intermediate species of Panicum and Moricandia.Abbreviations Rubisco ribulose-1,5-bisphosphate carboxylase/oxygenase - PEP phosphoenolpyruvate - CO₂ compensation concentration - 3PGA 3-phosphoglycerate - SuP sugar monophosphates - SuP₂ sugar bisphosphates Published as Paper No. 8249, Journal Series, Nebraska Agricultural Research Division     

CO2 fixation in halobacteria

Seven strains of extremely halophilic bacteria (Halobacterium spp., Halococcus spp., and Haloarcula sp.) fixed CO₂ under light and dark conditions. Light enhanced CO₂ fixation in Halobacterium halobium but inhibited it in Halobacterium volcanii and Haloarcula strain GN-1. Propionate stimulated ¹⁴CO₂ incorporation in some strains, but inhibited it in others. Semi-starvation in basal salts plus glycerol induced enhanced CO₂ fixation rates. ¹⁴CO₂ fixation in semi-starved cells was stimulated by NH ₄ ⁺ or pyruvate and inhibited by succinate and acetate in most strains. No possible reductant was found. In cell-free extracts of H. halobium, NH ₄ ⁺ but not propionate stimulated ¹⁴CO₂ fixation. No RuBP carboxylase activity was detected. The main ¹⁴C-labeled -keto acid detected after a 2-min incubation with ¹⁴CO₂ and pyruvate was pyruvate. Little or no -ketobutyrate was detected among the early products of propionate-stimulated CO₂ fixation. Glycine was the major amino acid synthesized during a 2-min incubation with NH ₄ ⁺ , propionate, and ¹⁴CO₂. Propionate-stimulated CO₂ fixation was sensitive to trimethoprim and insensitive to avidin. A novel pathway for non-reductive CO₂ fixation involving a glycine synthase reaction with CO₂, NH ₄ ⁺ , and a methyl carbon derived from the -carbon cleavage of propionate is tentatively proposed.Abbreviations used BBS buffered basal salts - HEPES N-2-hydroxyethylpiperazine-N-2-ethanesulfonic acid - MOPS 3-(N-morpholino)propanesulfonic acid - DNPH 2,4-dinitrophenylhydrazine - DNP dinitrophenyl - TLC thin-layer chromatography - FH₄ tetrahydrofolate This work was supported by National Science Foundation grant PCM-8116330 and Petroleum Research Fund grant PRF 13704-AC2