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.     

Strain-specific incorporation of methanotrophic biomass into eukaryotic grazers in a rice field soil revealed by PLFA-SIP

In wetland ecosystems, methane is actively utilized by methanotrophs. The immobilized methane carbon is then passed on to other organisms such as grazers. Here, we traced the incorporation of methanotrophic biomass into eukaryotes in a rice field soil using phospholipid fatty acid stable-isotope probing (PLFA-SIP). Addition of (13)C-labeled cells of five methanotrophs to soil (5 × 10(7) cells g(-1) soil) did not affect the CO(2) release rate, but significantly increased the carbon isotopic ratio within 24 h. In 48 h, 2-7% of the added bacterial biomass carbon was detected as (13)CO(2) . The soil with Methylobacter luteus released the highest amount of (13)CO(2) , comparable to that with Escherichia coli. The amount of polyunsaturated PLFAs (C18:3ω6c and C20:4ω6c) was not affected by the addition of bacterial cells to soil, but their carbon isotopic ratio increased significantly within 24-48 h. The extent of (13)C-enrichment in PLFAs differed between the added methanotrophs, with the highest labeling upon addition of M. luteus. The relative abundance of (13) C-labeled C18:3ω6c to C20:4ω6C also differed between the strains. The results indicated that the eukaryotes in soil, probably protozoa, preferentially graze on specific methanotrophs and immediately incorporate their biomass.     

Soil microbial community structure and activity in a 100-year-old fertilization and crop rotation experiment

Aims Nitrogen (N) fertilization and lime addition may affect soil microbial and nematode communities and ecosystem functions through changing environmental conditions, such as soil pH and soil organic carbon. The objectives of this experiment were to examine the impact of N input and liming on soil microbial and nematode communities and to identify the key environmental determinant of community composition in a century-old fertilization and crop rotation experiment.Methods The field experiment consisting of a 3-year crop rotation regime was established in 1911 in southeastern USA. Four treatments, (i) no-input control, (ii) NPK with winter legume, (iii) PK with legume and lime and (iv) NPK with legume and lime, were included in this study. Soil samples collected at the 0–5cm depth were used to determine the bacterial growth rate by the 3 H-thymidine incorporation technique. Incorporation of 13 C into neutral lipids, glycolipids and phospholipid fatty acids (PLFAs) was measured after incubation of soil with 13 C-labeled acetate for 24h. Free-living nematodes in fresh soil were extracted using a density sucrose centrifugal flotation method and identified to trophic group level.Important findings Liming resulted in a 10-fold increase in bacterial growth rates compared with the no-input control, whereas N fertilization had no significant effect. Multivariate analysis of PLFA profiles showed that soil microbial community composition was different among the four treatments; the difference was primarily driven by soil pH. PLFAs indicative of Gram-negative bacteria covaried with soil pH, but not those of fungi and actinobacteria. Liming enhanced 13 C incorporation into neutral lipids, glycolipids and phospholipids by 2–15 times. In addition, 13 C incorporation into 16:0, 16:1ω9, 18:1ω9, 18:1ω7 and 18:2ω6 were greater than other PLFAs, suggesting that Gram-negative bacteria and fungi were more active and sensitive to simple C input. Bacterivorous nematodes were the dominant trophic group in the soil, but no significant differences in nematode communities were found among the treatments. Our results suggest that soil pH had a greater impact than N fertilization on soil microbial community composition and activity in a crop rotation system including legumes.     

The diel imprint of leaf metabolism on the δ13 C signal of soil respiration under control and drought conditions

Recent (13) CO(2) canopy pulse chase labeling studies revealed that photosynthesis influences the carbon isotopic composition of soil respired CO(2) (δ(13) C(SR)) even on a diel timescale. However, the driving mechanisms underlying these short-term responses remain unclear, in particular under drought conditions. The gas exchange of CO(2) isotopes of canopy and soil was monitored in drought/nondrought-stressed beech (Fagus sylvatica) saplings after (13) CO(2) canopy pulse labeling. A combined canopy/soil chamber system with gas-tight separated soil and canopy compartments was coupled to a laser spectrometer measuring mixing ratios and isotopic composition of CO(2) in air at high temporal resolution. The measured δ(13) C(SR) signal was then explained and substantiated by a mechanistic carbon allocation model. Leaf metabolism had a strong imprint on diel cycles in control plants, as a result of an alternating substrate supply switching between sugar and transient starch. By contrast, diel cycles in drought-stressed plants were determined by the relative contributions of autotrophic and heterotrophic respiration throughout the day. Drought reduced the speed of the link between photosynthesis and soil respiration by a factor of c. 2.5, depending on the photosynthetic rate. Drought slows the coupling between photosynthesis and soil respiration and alters the underlying mechanism causing diel variations of δ(13) C(SR).     

Does ear C sink strength contribute to overcoming photosynthetic acclimation of wheat plants exposed to elevated CO2?

Wheat plants (Triticum durum Desf., cv. Regallo) were grown in the field to study the effects of contrasting [CO(2)] conditions (700 versus 370 μmol mol(-1)) on growth, photosynthetic performance, and C management during the post-anthesis period. The aim was to test whether a restricted capacity of sink organs to utilize photosynthates drives a loss of photosynthetic capacity in elevated CO(2). The ambient (13)C/(12)C isotopic composition (δ(13)C) of air CO(2) was changed from -10.2‰ in ambient [CO(2)] to -23.6‰ under elevated [CO(2)] between the 7th and the 14th days after anthesis in order to study C assimilation and partitioning between leaves and ears. Elevated [CO(2)] had no significant effect on biomass production and grain filling, and caused an accumulation of C compounds in leaves. This was accompanied by up-regulation of phosphoglycerate mutase and ATP synthase protein content, together with down-regulation of adenosine diphosphate glucose pyrophosphatase protein. Growth in elevated [CO(2)] negatively affected Rubisco and Rubisco activase protein content and induced photosynthetic down-regulation. CO(2) enrichment caused a specific decrease in Rubisco content, together with decreases in the amino acid and total N content of leaves. The C labelling revealed that in flag leaves, part of the C fixed during grain filling was stored as starch and structural C compounds whereas the rest of the labelled C (mainly in the form of soluble sugars) was completely respired 48 h after the end of labelling. Although labelled C was not detected in the δ(13)C of ear total organic matter and respired CO(2), soluble sugar δ(13)C revealed that a small amount of labelled C reached the ear. The (12)CO(2) labelling suggests that during the beginning of post-anthesis the ear did not contribute towards overcoming flag leaf carbohydrate accumulation, and this had a consequent effect on protein expression and photosynthetic acclimation.     

Temporal variation in δ<Superscript>13</Superscript>C of ecosystem respiration in the Pacific Northwest: links to moisture stress

We measured seasonal and interannual variations in delta(13)C values within the carbon reservoirs (leaves and soil) and CO(2) fluxes (soil and ecosystem respired CO(2)) of an old growth coniferous forest in the Pacific Northwest USA with relation to local meteorological conditions. There were significant intra-annual and interannual differences in the carbon isotope ratios of CO(2) respired at both the ecosystem (delta(13)C(R)) and the soil levels (delta(13)C(R-soil)), but only limited variations in the carbon isotope ratios of carbon stocks. The delta(13)C(R) values varied by as much as 4.4 per thousand over a growing season, while delta(13)C(R-soil )values changed as much as 6.2 per thousand. The delta(13)C of soil organic carbon (delta(13)C(SOC)) and needle organic carbon (delta(13)C(P)) exhibited little or no significant changes over the course of this study. Carbon isotope discrimination within leaves (Delta(p)) showed systematic decreases with increased canopy height, but remained fairly constant throughout the year (Delta(p)=17.9 per thousand -19.2 per thousand at the top of the canopy, Delta(p)=19.6 per thousand -20.9 per thousand at mid-canopy, Delta(p)=23.3 per thousand -25.1 per thousand at the canopy base). The temporal variation in the delta(13)C of soil and ecosystem respired CO(2) was correlated ( r=0.93, P<0.001) with soil moisture levels, with dry summer months having the most (13)C-enriched values. The dynamic seasonal changes in delta(13)C of respired CO(2) are hypothesized to be the result of fast cycling of recently fixed carbon back to the atmosphere. One scaling consequence of the seasonal and interannual variations in delta(13)C(R) is that inversion-based carbon-cycle models dependent on observed atmospheric CO(2) concentration and isotope values may be improved by incorporating dynamic delta(13)C(R) values to interpret regional carbon sink strength.     

Effects of open-top chambers and substrate type on biogeochemical processes at disturbed boreal forest sites in northwestern Quebec

In the context of land use change, the dynamics of the water extractable organic carbon (WEOC) pool and CO₂ production were studied in soil from a native oak-beech forest and a Douglas fir plantation during a 98-day incubation at a range of temperatures from 8°C to 28°C. The soil organic carbon, water contents and mineralisation rates of soil samples from the 0–5 cm layer were higher in the native forest than in the Douglas fir plantation. During incubation, a temperature-dependent shift in the δ¹³C of respired CO₂ was observed, suggesting that different carbon compounds were mineralised at different temperatures. The initial size of the WEOC pool was not affected by forest type. The WEOC pool size of samples from the native forest did not change consistently over time whereas it decreased significantly in samples from the Douglas plantation, irrespective of soil temperature. No clear changes in the δ¹³C values of the WEOC were observed, irrespective of soil origin. The fate of the WEOC, independent of soil organic carbon content or mineralisation rates, appeared to relate to forest types. Replacement of native oak-beech forest with Douglas fir plantation impacts carbon input to the soil, mineralisation rates and production of dissolved organic carbon.     

Temporal dynamics of the carbon isotope composition in a Pinus sylvestris stand: from newly assimilated organic carbon to respired carbon dioxide

The (13)C isotopic signature (C stable isotope ratio; delta(13)C) of CO(2) respired from forest ecosystems and their particular compartments are known to be influenced by temporal changes in environmental conditions affecting C isotope fractionation during photosynthesis. Whereas most studies have assessed temporal variation in delta(13)C of ecosystem-respired CO(2) on a day-to-day scale, not much information is available on its diel dynamics. We investigated environmental and physiological controls over potential temporal changes in delta(13)C of respired CO(2) by following the short-term dynamics of the (13)C signature from newly assimilated organic matter pools in the needles, via phloem-transported organic matter in twigs and trunks, to trunk-, soil- and ecosystem-respired CO(2). We found a strong 24-h periodicity in delta(13)C of organic matter in leaf and twig phloem sap, which was strongly dampened as carbohydrates were transported down the trunk. Periodicity reappeared in the delta(13)C of trunk-respired CO(2), which seemed to originate from apparent respiratory fractionation rather than from changes in delta(13)C of the organic substrate. The diel patterns of delta(13)C in soil-respired CO(2) are partly explained by soil temperature and moisture and are probably due to changes in the relative contribution of heterotrophic and autotrophic CO(2) fluxes to total soil efflux in response to environmental conditions. Our study shows that direct relations between delta(13)C of recent assimilates and respired CO(2) may not be present on a diel time scale, and other factors lead to short-term variations in delta(13)C of ecosystem-emitted CO(2). On the one hand, these variations complicate ecosystem CO(2) flux partitioning, but on the other hand they provide new insights into metabolic processes underlying respiratory CO(2) emission.     

Can isotopic fractionation during respiration explain the 13C-enriched sporocarps of ectomycorrhizal and saprotrophic fungi?

The mechanism behind the (13)C enrichment of fungi relative to plant materials is unclear and constrains the use of stable isotopes in studies of the carbon cycle in soils. Here, we examined whether isotopic fractionation during respiration contributes to this pattern by comparing delta(13)C signatures of respired CO(2), sporocarps and their associated plant materials, from 16 species of ectomycorrhizal or saprotrophic fungi collected in a Norway spruce forest. The isotopic composition of respired CO(2) and sporocarps was positively correlated. The differences in delta(13)C between CO(2) and sporocarps were generally small, < +/-1 per thousand in nine out of 16 species, and the average shift for all investigated species was 0.04 per thousand. However, when fungal groups were analysed separately, three out of six species of ectomycorrhizal basidiomycetes respired (13)C-enriched CO(2) (up to 1.6 per thousand), whereas three out of five species of polypores respired (13)C-depleted CO(2) (up to 1.7 per thousand; P < 0.05). The CO(2) and sporocarps were always (13)C-enriched compared with wood, litter or roots. Loss of (13)C-depleted CO(2) may have enriched some species in (13)C. However, that the CO(2) was consistently (13)C-enriched compared with plant materials implies that other processes must be found to explain the consistent (13)C-enrichment of fungal biomass compared with plant materials.     

Biodegradation of TNT (2,4,6-trinitrotoluene) by Phanerochaete chrysosporium.

Extensive biodegradation of TNT (2,4,6-trinitrotoluene) by the white rot fungus Phanerochaete chrysosporium was observed. At an initial concentration of 1.3 mg/liter, 35.4 +/- 3.6% of the [14C]TNT was degraded to 14CO2 in 18 days. The addition of glucose 12 days after the addition of TNT did not stimulate mineralization, and, after 18 days of incubation with TNT only, about 3.3% of the initial TNT could be recovered. Mineralization of [14C]TNT adsorbed on soil was also examined. Ground corncobs served as the nutrient for slow but sustained degradation of [14C]TNT to 14CO2 such that 6.3 +/- 0.6% of the [14C]TNT initially present was converted to 14CO2 during the 30-day incubation period. Mass balance analysis of liquid cultures and of soil-corncob cultures revealed that polar [14C]TNT metabolites are formed in both systems, and high-performance liquid chromatography analyses revealed that less than 5% of the radioactivity remained as undegraded [14C]TNT following incubation with the fungus in soil or liquid cultures. When the concentration of TNT in cultures (both liquid and soil) was adjusted to contamination levels that might be found in the environment, i.e., 10,000 mg/kg in soil and 100 mg/liter in water, mineralization studies showed that 18.4 +/- 2.9% and 19.6 +/- 3.5% of the initial TNT was converted to 14CO2 in 90 days in soil and liquid cultures, respectively. In both cases (90 days in water at 100 mg/liter and in soil at 10,000 mg/kg) approximately 85% of the TNT was degraded. These results suggest that this fungus may be useful for the decontamination of sites in the environment contaminated with TNT.     

Physiological girdling of pine trees via phloem chilling: proof of concept

Quantifying below-ground carbon (C) allocation is particularly difficult as methods usually disturb the root-mycorrhizal-soil continuum. We reduced C allocation below ground of loblolly pine trees by: (1) physically girdling trees and (2) physiologically girdling pine trees by chilling the phloem. Chilling reduced cambium temperatures by approximately 18 degrees C. Both methods rapidly reduced soil CO2 efflux, and after approximately 10 days decreased net photosynthesis (P(n)), the latter indicating feedback inhibition. Chilling decreased soil-soluble C, indicating that decreased soil CO2 efflux may have been mediated by a decrease in root C exudation that was rapidly respired by microbes. These effects were only observed in late summer/early autumn when above-ground growth was minimal, and not in the spring when above-ground growth was rapid. All of the effects were rapidly reversed when chilling was ceased. In fertilized plots, both chilling and physical girdling methods reduced soil CO2 efflux by approximately 8%. Physical girdling reduced soil CO2 efflux by 26% in non-fertilized plots. This work demonstrates that phloem chilling provides a non-destructive alternative to reducing the movement of recent photosynthate below the point of chilling to estimate C allocation below ground on large trees.     

Effects of lipid removal and preservatives on carbon and nitrogen stable isotope ratios of squid tissues: Implications for ecological studies

Stable isotope analysis of carbon (C) and nitrogen (N) in animal tissues is an important approach to investigate the tropic status and habitat of marine species. Some biases due to lipid extractions and preservation can hinder the interpretation of results, yet their effects have not been investigated in squid. In this study, we evaluated the effects of lipid extraction and preservatives (dimethylsulfoxide (DMSO), 70% ethanol, and 10% buffered formaldehyde) on the δ¹³C, δ¹⁵N and C:N ratios in squid muscle. Beaks were placed under the same treatments with the exception of DMSO. Muscle and beak samples remained under treatment for 375 days and 416 days, respectively. Our results indicate that lipid extractions increased the mean values of unpreserved samples by 0.8‰ for δ¹³C and by 0.68‰ for δ¹⁵N. Preservatives also affected the isotopic composition in muscle at different magnitudes. DMSO remarkably reduced and increased the variability for δ¹³C and δ¹⁵N values among samples, formalin mainly reduced δ¹³C values by 1.5‰, whereas ethanol increased both δ¹³C and δ¹⁵N by ≤ 0.8‰. Lipid extractions eliminated the effect of DMSO and ethanol for δ¹³C and δ¹⁵N, and formalin only for δ¹⁵N. In beak, negligible shifts in δ¹³C, δ¹⁵N and C:N ratios were recorded after preservation in ethanol and formalin. Although lipid extractions can be recommended to reduce the effect of preservation, further research is needed to develop correction models for isotopic shifts associated with both lipid extractions in unpreserved and preserved muscle tissues. Lipid extractions per se could introduce a bias that may have important implications for ecological studies.     

Diet‐switching experiments show rapid accumulation and preferential retention of highly unsaturated fatty acids in Daphnia

Zooplankton transfer ecologically important fatty acids (FA) from their diets to upper trophic levels. We used diet‐switching experiments with ¹³C‐labeled food sources to determine the time scale at which dietary uptake is manifested in the FA profiles of Daphnia magna. Daphnia dramatically shifted their FA composition in response to diet change within only four days, however Daphnia switched from a high quality (i.e. Cryptomonas) to a moderate quality (Scenedesmus) diet retained the most physiologically important FA from their original diet source even after 14 days. In particular, Daphnia exhibited long‐term retention of eicosapentaenoic (EPA; 20:5ω3) and arachidonic acid (ARA; 20:4ω6) when switched from Cryptomonas to Scenedesmus. Similarly, when switched from Scenedesmus to Cryptomonas, Daphnia took up a high proportion of EPA and ARA after only two days. The phospholipid fatty acid (PLFA) fraction in Daphnia was preferentially enriched with stearic (18:0), oleic (18:1ω9), and linoleic acid (LIN; 18:2ω6). In contrast with studies of marine copepods, dietary FA also strongly affected the PLFA composition (structural lipids) of Daphnia. Results of δ¹³C signatures of individual FA provided evidence of elongation and desaturation of α‐linolenic (ALA; 18:3ω3) or stearidonic acid (SDA; 18:4ω3) to EPA 10 days after a diet switch to EPA‐deficient Scenedesmus. Differences in the ARA content of Daphnia fed Cryptomonas and Scenedesmus suggest Daphnia consuming Cryptomonas synthesized ARA via retroconversion of ω6‐docosapentaenoic acid (ω6‐DPA; 22:5ω6). Daphnia preferentially accumulate and retain, as well as bioconvert, those FA that are also most physiologically important for fish production. Our results also indicate Daphnia FA composition responds to their diet on a short temporal scale and analyses of lipid biomarkers in zooplankton provide strong insights into the food sources that support their production.     

海北高寒草甸土壤有机碳同位素组成及C3/C4碳源的变化

通过对高寒嵩草草甸土壤剖面不同深度(0～5cm,5～15cm,15～25cm,25～35cm,35～50cm,50～65cm)有机碳稳定性碳同位素的测定发现,土壤有机碳稳定性同位素(δ^13C)随土壤深度的增加而变大。表层土壤(0～5cm,定义为现代土壤)的δ^13C值最小,基本上接近现代植被的碳同位素特征。在土层5～10cm深度以下(粗略地定为古土壤),土壤有机碳稳定性同位素骤然上升,与表层土壤的同位素特征明显不同。考虑到影响土壤碳同位素的诸多因素,通过稳定性碳同位素的质量平衡模型计算,得出初步结果：来自C4(或CAM)植物的碳源随土壤深度的增加而增大。进一步推测,该地区植被可能经历由C4植物占优势的群落向C3植物占优势的群溶演化的过程。在这个过程中,大气碳同位素的变化和土壤有机质的形成过程(有机质淋溶过程)等也会引起土壤碳同位素的升高,因此质量平衡模型可能会过多地估算C4组分,而低估C3组分。     

Syntrophic acetate oxidation under thermophilic methanogenic condition in Chinese paddy field soil

The aim of the present work was to determine and compare the degradation of acetate in a Chinese rice field soil at 25°C and 50°C, respectively, and to identify specifically the active organisms involved in syntrophic acetate oxidation. Soil was preincubated anaerobically for 30 days to reduce alternative electron acceptors other than CO(2). The [2-(13)C] acetate (99% (13)C) was added twice: 0 day and 19 days after preincubation. Addition of [2-(13)C] acetate resulted in an immediate increase of (13)C labeled CH(4) but non-labeling of CO(2) at 25°C. The methanogen community was dominated by Methanosarcinaceae and Methanocellales at 25°C. In contrast, the addition of [2-(13)C] acetate at 50°C resulted in a rapid increase of (13)CO(2). The (13)C labeling of CH(4) gradually increased and reached a similar value to CO(2) (13% (13)C) at the end of incubation (40 days). Nearly all archaeal 16S rRNA genes detected at 50°C belonged to hydrogenotrophic Methanocellales. DNA-based stable isotope probing analysis revealed that the organisms related to Thermacetogenium lineage and the unclassified Thermoanaerobacteraceae group were intensively labeled with (13)C in the incubations at 50°C. Thus, acetate was converted to CH(4) and CO(2) through aceticlastic methanogenesis at 25°C, while syntrophic acetate oxidation occurred at 50°C.     

Biodegradation of TNT (2,4,6-trinitrotoluene) by Phanerochaete chrysosporium

Extensive biodegradation of TNT (2,4,6-trinitrotoluene) by the white rot fungus Phanerochaete chrysosporium was observed. At an initial concentration of 1.3 mg/liter, 35.4 +/- 3.6% of the [14C]TNT was degraded to 14CO2 in 18 days. The addition of glucose 12 days after the addition of TNT did not stimulate mineralization, and, after 18 days of incubation with TNT only, about 3.3% of the initial TNT could be recovered. Mineralization of [14C]TNT adsorbed on soil was also examined. Ground corncobs served as the nutrient for slow but sustained degradation of [14C]TNT to 14CO2 such that 6.3 +/- 0.6% of the [14C]TNT initially present was converted to 14CO2 during the 30-day incubation period. Mass balance analysis of liquid cultures and of soil-corncob cultures revealed that polar [14C]TNT metabolites are formed in both systems, and high-performance liquid chromatography analyses revealed that less than 5% of the radioactivity remained as undegraded [14C]TNT following incubation with the fungus in soil or liquid cultures. When the concentration of TNT in cultures (both liquid and soil) was adjusted to contamination levels that might be found in the environment, i.e., 10,000 mg/kg in soil and 100 mg/liter in water, mineralization studies showed that 18.4 +/- 2.9% and 19.6 +/- 3.5% of the initial TNT was converted to 14CO2 in 90 days in soil and liquid cultures, respectively. In both cases (90 days in water at 100 mg/liter and in soil at 10,000 mg/kg) approximately 85% of the TNT was degraded. These results suggest that this fungus may be useful for the decontamination of sites in the environment contaminated with TNT.     

Aerial decay influence on the stable oxygen and carbon isotope ratios in tree ring cellulose

Sub-fossil wood is often affected by the decaying process that introduces uncertainties in the measurement of oxygen and carbon stable isotope composition in cellulose. Although the cellulose stable isotopes are widely used as climatic proxies, our understanding of processes controlling their behavior is very limited. We present here a comparative study of stable oxygen and carbon isotope ratios in tree ring cellulose in decayed and non-decayed wood samples of Swiss stone pine (Pinus cembra) trees. The intra-ring stable isotope variability (around the circumference of a single ring) was between 0.1 and 0.5‰ for δ¹⁸O values and between 0.5 and 1.6‰ for δ¹³C values for both decayed and non-decayed wood. Observed intra-tree δ¹⁸O variability is less than that reported in the literature (0.5–1.5‰), however, for δ¹³C it is larger than the reported values (0.7–1.2‰). The inter-tree variability for non-decayed wood ranges between 1.1 and 2.3‰ for δ¹⁸O values, and between 2 and 4.7‰ for δ¹³C values. The inter-tree differences for δ¹⁸O values are similar to those reported in the literature (1–2‰ for oxygen and 1–3‰ for carbon) but are larger for δ¹³C values. We have found that the differences for δ¹⁸O and δ¹³C values between decayed and non-decayed wood are smaller than the variation among different trees from the same site, suggesting that the decayed wood can be used for isotopic paleoclimate research.     

树木年轮 δ13C 值及其对我国北方大气CO2浓度变化的指示意义

 本文采样分析了承德市油松年轮中δ13C值自工业革命以来的变化,用以揭示我国北方大气CO2浓度的变化规律。结果表明：承德市油松年轮中的δ13C值自1810年以来平均下降了0.839‰,下降范围0.682‰～1.120‰,指示了大气CO2浓度逐渐升高的特点。δ13C值与历史时期全球大气CO2浓度之间存在显著相关关系(r＝ –0.5609,P<0.01)。应用树木年轮δ13C值与大气CO2浓度之间的关系式,推测出我国北方大气CO2浓度从工业革命以前的约278.4μmol·mol-1上升到目前的340μmol·mol-1。从而为我国的全球变化研究提供了CO2浓度历史变迁方面的证据。     

Rapid changes in δ¹³C of ecosystem-respired CO₂ after sunset are consistent with transient ¹³C enrichment of leaf respired CO₂

The CO? respired by darkened, light-adapted, leaves is enriched in 13C during the first minutes, and this effect may be related to rapid changes in leaf respiratory biochemistry upon darkening. We hypothesized that this effect would be evident at the ecosystem scale. High temporal resolution measurements of the carbon isotope composition of ecosystem respiration were made over 28 diel periods in an abandoned temperate pasture, and were compared with leaf-level measurements at differing levels of pre-illumination. At the leaf level, CO? respired by darkened leaves that had been preadapted to high light was strongly enriched in 13C, but such a 13C-enrichment rapidly declined over 60-100 min. The 13C-enrichment was less pronounced when leaves were preadapted to low light. These leaf-level responses were mirrored at the ecosystem scale; after sunset following clear, sunny days respired CO? was first 13C enriched, but the 13C-enrichment rapidly declined over 60-100 min. Further, this response was less pronounced following cloudy days. We conclude that the dynamics of leaf respiratory isotopic signal caused variations in ecosystem-scale 12CO?/13) CO? exchange. Such rapid isotope kinetics should be considered when applying 13C-based techniques to elucidate ecosystem carbon cycling.     

Carbon dioxide evolution as a measure of attack of wood by fungi and its application to testing wood preservatives and sap stain preventives

A method of assessing fungal attack on wood, using a conductivity respirometer to measure the CO₂ evolution of the attacking fungus, is described and its application to the testing of wood preservatives and sapstain preventives is explored. Tests made by this method established in 9–13 days that the minimum fungitoxic concentration of Timbor (disodium octaborate decahydrate) was between 0·05 and 0·1%—a value agreeing with that given by the standard wood-block test lasting 12 weeks. The use of the CO₂-measurement method for fungitoxicity determinations on a copper-chrome-arsenate wood preservative and on the sapstain preventive, Santobrite (a sodium pentachlorophenate preparation), gave unsatisfactory results.