Nuclear energy: Health impact of carbon-14

Summary Estimates are presented on the carbon-14 generation rates in several reactor types and in peaceful nuclear explosions. If the carbon-14 generated in light water reactors is released, the population radiationdose rate it causes initially will be comparable to that resulting from the krypton-85 and tritium generated in these reactors. Because of the long half-life, the radiationdose commitment and thedose rate resulting from the environmental build-up of carbon-14 are considerably larger than those of the two other radionuclides.This work received support from the Program on Science, Technology, and Society at Cornell University, with funds given them by the Sloan Foundation, Inc.     

Use of carbon-13 and carbon-14 natural abundances for stream food web studies

We review the use of stable carbon isotope ratios (δ¹³C) and radiocarbon natural abundances (Δ¹⁴C) for stream food web studies. The δ¹³C value of primary producers (e.g., periphytic algae, hereafter periphyton) in streams is controlled by isotopic fractionation during photosynthesis and variable δ¹³C of dissolved CO₂. When periphyton δ¹³C differs from that of terrestrial primary producers, the relative contribution of autochthony and allochthony to stream food webs can be calculated. Moreover, the variation in periphyton δ¹³C can reveal how much stream consumers rely on local resources because each stream habitat (e.g., riffle vs. pool, open vs. shaded) usually has a distinctive δ¹³C. However, periphyton δ¹³C often overlaps with that of terrestrial organic matter. On the other hand, periphyton Δ¹⁴C is less variable than δ¹³C among habitats, and reflects the Δ¹⁴C of dissolved CO₂, which could be a mixture of “aged” (Δ¹⁴C < 0 ‰) and “modern” (Δ¹⁴C > 0 ‰) carbon. This is because the Δ¹⁴C is corrected by its δ¹³C value for the isotopic fractionation during photosynthesis. Recent studies and our data indicate that many stream food webs are supported by “aged” carbon derived from the watershed via autochthonous production. The combined use of δ¹³C and Δ¹⁴C allows robust estimation of the carbon transfer pathway in a stream food web at multiple spatial scales ranging from the stream habitat level (e.g., riffle and pool) to watershed level (autochthony and allochthony). Furthermore, the Δ¹⁴C of stream food webs will expand our understanding about the time frame of carbon cycles in the watersheds.     

Microbial decomposition of leaf litter as influenced by fertilizers

Summary A urea and NPK-mixture at concentration of 5, 10 and 15 mg g^–1 air dry litter stimulated microbial populations, microbial activity and rate of decomposition of the litter. The stimulation was more pronounced as the concentration of the fertilizers was increased. However, this trend was reverse after two months in case of urea except for bacterial population. Fewer fungal species were isolated from the fertilizer-treated litter, together with a certain degree of alteration in the composition of mycoflora.     

The use of hair as an indicator of occupational 14C contamination

This paper presents a study in which the specific activity of ¹⁴C in hair has been investigated as an easily determined bio-indicator of the integrated ¹⁴C exposure (over several months). The study includes 28 Swedish workers handling ¹⁴C-labelled compounds, or working in a ¹⁴C-enriched environment. Hair samples from personnel at a Swedish nuclear power plant showed very low levels of ¹⁴C contamination, if any. In contrast, personnel at the investigated research departments showed ¹⁴C levels in hair of up to 60% above the natural specific activity of ¹⁴C. Much higher levels, up to 80 times the natural specific activity of ¹⁴C, were found in hair from individuals working at a pharmaceutical research laboratory. This contamination was, however, not solely an internal contamination. There were indications that most of the ¹⁴C in the hair originated from airborne ¹⁴C-compounds, which were adsorbed onto the hair. The difficulties in removing this external ¹⁴C contamination prior to analysis are discussed, as are the possibilities of using accelerator mass spectrometry to analyse various types of samples for retrospective dose assessment.     

Factors influencing leaf litter decomposition: an intersite decomposition experiment across China

The Long-Term Intersite Decomposition Experiment in China (hereafter referred to as LTIDE-China) was established in 2002 to study how substrate quality and macroclimate factors affect leaf litter decomposition. The LTIDE-China includes a wide variety of natural and managed ecosystems, consisting of 12 forest types (eight regional broadleaf forests, three needle-leaf plantations and one broadleaf plantation) at eight locations across China. Samples of mixed leaf litter from the south subtropical evergreen broadleaf forest in Dinghushan (referred to as the DHS sample) were translocated to all 12 forest types. The leaf litter from each of other 11 forest types was placed in its original forest to enable comparison of decomposition rates of DHS and local litters. The experiment lasted for 30 months, involving collection of litterbags from each site every 3 months. Our results show that annual decomposition rate-constants, as represented by regression fitted k-values, ranged from 0.169 to 1.454/year. Climatic factors control the decomposition rate, in which mean annual temperature and annual actual evapotranspiration are dominant and mean annual precipitation is subordinate. Initial C/N and N/P ratios were demonstrated to be important factors of regulating litter decomposition rate. Decomposition process may apparently be divided into two phases controlled by different factors. In our study, 0.75 years is believed to be the dividing line of the two phases. The fact that decomposition rates of DHS litters were slower than those of local litters may have been resulted from the acclimation of local decomposer communities to extraneous substrate.     

光降解在凋落物分解中的作用

近年来,越来越多的研究者认识到光降解可能在凋落物分解中发挥着重要作用.本文对光降解的作用机制,光降解在碳循环、养分循环中的作用,光降解与微生物分解的关系,以及影响光降解的因素进行了综述.光降解对凋落物分解过程同时具有正效应和负效应,正效应指光降解通过氧化有机质,或是改变凋落物自身理化性质使其更易淋溶和分解,负效应指高光辐射对分解者产生不利影响从而押制微生物分解.在光降解过程中光化学矿化产生CO2是生态系统碳流失的主要机制.除紫外光外,可见光中的蓝、绿光波段也对凋落物的降解产生影响.光降解作用的大小受到水分状况、凋落物化学性质和凋落物的暴露面积的影响.最后,讨论了该领域有待深入研究的方向,指出今后应当重点对光降解研究方法,光降解与环境因子的交互作用,光降解作用的空间差异,光降解与微生物分解的相互关系及其作用强度进行研究.     

Comparing intra- and inter-specific effects on litter decomposition in an old-field ecosystem

Plant species can differ in the quantity and quality of leaf litter they produce, and many studies have examined whether plant species diversity affects leaf-litter decomposition and nutrient release. A growing number of studies have indicated that intra-specific variation within plant species can also affect key ecosystem processes. However, the relative importance of intra- versus inter-specific variation for the functioning of ecosystems remains poorly known. Here, we investigate the effects of intra-specific variation in a dominant old-field plant species, tall goldenrod (Solidago altissima), and inter-specific variation among goldenrod species on litter quality, decomposition, and nitrogen (N) release. We found that the nutrient concentration of leaf litter varied among genotypes, which translated into ～50% difference in decomposition rates. Variation among other goldenrod species in decomposition rate was more than twice that of genetic variation within S. altissima. Furthermore, by manipulating litterbags to contain 1, 3, 6, or 9 genotypes, we found that S. altissima genotype identity had much stronger effects than did genotypic diversity on leaf-litter quality, decomposition, and N release. Taken together, these results suggest that the order of ecological importance for controlling leaf-litter decomposition and N release dynamics is plant species identity?genotype identity>genotypic diversity.     

Landscape patterns of litter decomposition in alpine tundra

A two-year study of the decomposition of alpine avens (Acomastylis rossii) foliage in alpine tundra of the Front Range of Colorado demonstrated a strong landscape-mediated effect on decay rates. Litter on sites with intermediate amounts of snowpack decayed more rapidly than litter on sites with larger or smaller amounts of snow. Annual decay constants (k-values) of this foliage ranged from-0.33 in dry tundra to-0.52 in moist tundra to-0.47 in the wettest habitat. No site differences in mass loss of litter were detected until late winter-early spring of the first year of decomposition, when significantly faster decomposition was observed for litter beneath the snowpack. In spite of obvious landscape-related patterns in rates of litter decomposition, total microarthropod densities in the top 5 cm of soil did not differ among habitats. However, the relative abundance of the oribatid and prostigmatid mites did vary significantly across the landscape in relation to the moisture gradient. Oribatid mites comprised a greater proportion of total mites in wetter areas. Microarthropod densities and composition, as well as patterns of decomposition, were compared with previous alpine, as well as arctic tundra, studies. The effects of soil invertebrates on decomposition rates in the alpine were evaluated with a mushroom litterbag decomposition experiment. Naphthalene was used to exclude fauna from a subset of litterbags placed in mesic and xeric habitats. Mushrooms without naphthalene additions decayed significantly faster in the mesic sites. Densities of invertebrates were also greater on mushrooms in these mesic sites. Mushrooms placed in xeric sites generally lacked fauna. Thus, both the activities and the composition of the detritus-based food web appear to change substantially across the moisture gradient found in alpine tundra.     

Physical determinants of microbial colonization and decomposition of plant litter in an Arctic Lake

Physical effects on the microbial colonization and decomposition of plant litter in an oligotrophic lake were studied in Toolik Lake, Alaska. Colonization, measured by adenosine triphosphate (ATP) analysis, and decomposition, measured by weight loss, were correlated with depth of incubation, light, and temperature. The effects of turbulence, light, and temperature were studied in microcosm experiments. A 10°C increase (above ambient) in temperature caused a doubling in the amount of microbial colonization and a 50% increase in decomposition. Light intensity had no quantitative effect on either colonization or decomposition. Turbulence experiments conducted in Toolik Lake showed significant differences in decomposition between natural turbulence and no turbulence. Elevated temperature (20°C, which was 10°C above ambient), high turbulence, and total darkness changed the composition of the litter microbiota, causing a shift from a bacterially dominated microbiota to one dominated by large filamentous forms, as revealed by scanning electron microscopy. This study shows the importance of these physical factors in determining the rate at which plant litter is colonized and degraded in aquatic environments.     

Fluorescence energy transfer as an indicator of Ca2+-ATPase interactions in sarcoplasmic reticulum.

Ca2+-ATPase molecules were labeled in intact sarcoplasmic reticulum (SR) vesicles, sequentially with a donor fluorophore, fluorescein-5'-isothiocyanate (FITC), and with an acceptor fluorophore, eosin-5'-isothiocyanate (EITC), each at a mole ratio of 0.25-0.5 mol/mol of ATPase. The resonance energy transfer was determined from the effect of acceptor on the intensity and lifetime of donor fluorescence. Due to structural similarities, the two dyes compete for the same site(s) on the Ca2+-ATPase, and under optimal conditions each ATPase molecule is labeled either with donor or acceptor fluorophore, but not with both. There is only slight labeling of phospholipids and other proteins in SR, even at concentrations of FITC or EITC higher than those used in the reported experiments. Efficient energy transfer was observed from the covalently bound FITC to EITC that is assumed to reflect interaction between ATPase molecules. Protein denaturing agents (8 M urea and 4 M guanidine) or nonsolubilizing concentrations of detergents (C12E8 or lysolecithin) abolish the energy transfer. These results are consistent with earlier observations that a large portion of the Ca2+-ATPase is present in oligomeric form in the native membrane. The technique is suitable for kinetic analysis of the effect of various treatments on the monomer-oligomer equilibrium of Ca2+-ATPase. A drawback of the method is that the labeled ATPase, although it retains conformational responses, is enzymatically inactive.     

Accumulation and release of nitrogen and phosphorus in relation to lignin decomposition in leaf litter of 14 tree species

Immobilization and mobilization of nitrogen and phosphorus were investigated in relation to the nitrogen (L/N) ratio and lignin to the phosphorus (L/P) ratio as indicators of the nitrogen and phosphorus dynamics. The present study was carried out on upper and lower parts of a forest slope in a cool temperate forest in Japan. Net immobilization and net mobilization characterized the dynamics of nitrogen and phosphorus in 14 litter types and were related to the changes in the L/N and L/P ratio. The critical values of the L/N and L/P ratio at which the mobilization began were 23–25 and 500–620, respectively. In litter types with the L/N and L/P ratio higher than critical values, nitrogen and phosphorus were immobilized until the ratios reached at the critical values and then nitrogen and phosphorus began decreasing. In litter types with initial L/N and L/P ratios lower than or equal to the critical values, nitrogen and phosphorus were released from litter. The critical values of the L/N and L/P ratios showed convergent trends among litter types as compared to their initial values, and were approached to those of underlying humus layers. These results indicated the usefulness of L/N and L/P ratios as indicators of the nitrogen and phosphorus dynamics in the study site. The general validity of the L/N ratio as an indicator of nitrogen dynamics and the convergent trend of critical L/N ratio at 25–30 were demonstrated by a review of literature on lignin and nitrogen dynamics in 47 litter types in temperate and boreal forests.     

Sap flow as an indicator of transpiration and the water status of young apricot trees

The relationship between water loss via transpiration and stem sap flow in young apricot trees was studied under different environmental conditions and different levels of soil water status. The experiment was carried out in a greenhouse over a 2-week period (November 2–14, 1997) using three-year-old apricot trees (Prunus armeniaca cv. Búlida) growing in pots. Diurnal courses of leaf water potential, leaf conductance and leaf turgor potential also were recorded throughout the experiment. Data from four days of different enviromental conditions and soil water availability have been selected for analysis. On each of the selected days the leaf water potential and the mean transpiration rates were well correlated. The slope of the linear regression of this correlation, taken to indicate the total hydraulic resistance of the tree, confirmed an increasing hydraulic resistance under drought conditions. When the trees were not drought stressed the diurnal courses of sap flow and transpiration were very similar. However, when the trees were droughted, measured of sap flow slightly underestimated actual transpiration. Our heat-pulse measurements suggest the amount of readily available water stored in the stem and leaf tissues of young apricot trees is sufficient to sustain the peak transpiration rates for about 1 hour. This revised version was published online in June 2006 with corrections to the Cover Date.     

A fungal endophyte slows litter decomposition in streams

1. Phyllosphere interactions are known to influence a variety of tree canopy community members, but less frequently have they been shown to affect processes across ecosystem boundaries. Here, we show that a fungal endophyte (Rhytisma punctatum) slows leaf litter decomposition of a dominant riparian tree species (Acer macrophyllum) in an adjacent stream ecosystem. 2. Patches of leaf tissue infected by R. punctatum show significantly slower decomposition compared to both nearby uninfected tissue from the same leaf, and completely uninfected leaves. These reduced rates of decomposition existed despite 50% greater nitrogen in infected tissues and may be driven by slower rates of decomposition for fungal tissues themselves or by endophyte–hyphomycete interactions. 3. Across a temperate forest in the Pacific Northwest, approximately 72% of all A. macrophyllum leaves were infected by R. punctatum. Since R. punctatum infection can influence leaf tissue on entire trees and large quantities of leaf litter at the landscape scale, this infection could potentially result in a mosaic of ‘cold spots’ of litter decomposition and altered nutrient cycling in riparian zones where this infection is prevalent.     

Bacterial diversity in agricultural soils during litter decomposition

Denaturing gradient gel electrophoresis (DGGE) of amplified fragments of genes coding for 16S rRNA was used to study the development of bacterial communities during decomposition of crop residues in agricultural soils. Ten strains were tested, and eight of these strains produced a single band. Furthermore, a mixture of strains yielded distinguishable bands. Thus, DGGE DNA band patterns were used to estimate bacterial diversity. A field experiment performed with litter in nylon bags was used to evaluate the bacterial diversity during the decomposition of readily degradable rye and more refractory wheat material in comparable luvisols and cambisols in northern, central, and southern Germany. The amount of bacterial DNA in the fresh litter was small. The DNA content increased rapidly after the litter was added to the soil, particularly in the rapidly decomposing rye material. Concurrently, diversity indices, such as the Shannon-Weaver index, evenness, and equitability, which were calculated from the number and relative abundance (intensity) of the bacterial DNA bands amplified from genes coding for 16S rRNA, increased during the course of decomposition. This general trend was not significant for evenness and equitability at any time. The indices were higher for the more degradation-resistant wheat straw than for the more easily decomposed rye grass. Thus, the DNA band patterns indicated that there was increasing bacterial diversity as decomposition proceeded and substrate quality decreased. The bacterial diversity differed for the sites in northern, central, and southern Germany, where the same litter material was buried in the soil. This shows that in addition to litter type climate, vegetation, and indigenous microbes in the surrounding soil affected the development of the bacterial communities in the litter.     

Searching for an indicator of N evolution during organic matter decomposition based on amino acids behaviour: a study on litter layers of pine forests

Soil microflora can directly take up the amino acids (Aas) released by decomposing plants and use them, together with de novo synthesized Aas, as building blocks for their own structures, which are expected to have an Aa composition that differs from plant-derived structures. The degree of change in the Aa composition during OM decomposition should reflect the degree of N evolution. Here we apply this concept to the study of three litter decomposition sequences in European forests: boreal (Pinus sylvestris L., Jädraås, Sweden), cool Atlantic (Pinus sylvestris L., La Gileppe, Belgium), and warm Atlantic (Pinus pinaster L., Montemor, Portugal). Litter was sorted into six decomposition stages according to morphological features: from intact, light-brown needles to dark needle fragments with faunal perforations. At each stage, the Aa composition of the litter was studied by acid hydrolysis plus liquid chromatography of the hydrolysates. Both the Aa content of the litter and the unhydrolyzable/total OC ratio increased with decomposition, but this was not the case with the unhydrolyzable/total N ratio. There is no sole pattern of Aa change with decomposition: in Jädraås and Montemor most of the changes occur in the initial and final steps, while in La Gileppe the changes seem quite evenly spread throughout the decomposition. The fact that the Aa composition of the litter did not converge with decomposition suggests the existence of site-specific biotas with contrasted Aa fingerprints. The abundance of a given Aa relative to the total differed among Aas and sites; but for some Aas it was possible to detect common patterns of decomposition behaviour (either a consistent increase or a consistent decrease). The aa/total ratio for Gly, Ala and Thr consistently increased with decomposition. These Aas were used to search for a numerical index, the Aa signature (Aa_SIG), which would reflect the changes in Aa composition from fresh debris to highly decomposed organic materials. The change in the proposed Aa_SIG was found to correlate well with the mathematical distance from the starting point (calculated as the euclidean distance); this suggests that it could be potentially useful as an indicator of N evolution during litter decomposition, at least in its first stages.     

Interacting effects of leaf litter species and macrofauna on decomposition in different litter environments

The leaf litter environment (single species versus mixed species), and interactions between litter diversity and macrofauna are thought to be important in influencing decomposition rates. However, the role of soil macrofauna in the breakdown of different species of leaf litter is poorly understood. In this study we examine the multiple biotic controls of decomposition – litter quality, soil macrofauna and litter environment and their interactions. The influence of soil macrofauna and litter environment on the decomposition of six deciduous tree species (Fraxinus excelsior L., Acer pseudoplatanus L., Acer campestre L., Corylus avellana L., Quercus robur L., Fagus sylvatica L.) was investigated in a temperate forest, Wytham Woods, Southern England. We used litterbags that selectively excluded macrofauna to assess the relative importance of macrofauna versus microbial, micro and mesofauna decomposition, and placed single species bags in either conspecific single species or mixed species litter environments. The study was designed to separate plant species composition effects on litter decomposition rates, allowing us to evaluate whether mixed species litter environments affect decomposition rates compared to single species litter environments, and if so whether the effects vary among litter species, over time, and with regard to the presence of soil macrofauna. All species had faster rates of decomposition when macrofauna were present, with 22–41% of the total mass loss attributed to macrofauna. Macrofauna were most important for easily decomposable species as soon as the leaves were placed on the ground, but were most important for recalcitrant species after nine months in the field. The mass loss rates did not differ between mixed and single species litter environments, indicating that observed differences between single species and mixed species litterbags in previous field studies are due to the direct contact of neighbouring species inside the litterbag rather than the litter environment in which they are placed.