Contribution of winter processes to soil nitrogen flux in taiga forest ecosystems

We measured annual net nitrogen (N) mineralization, nitrification, and amino acid production in situ across a primary successional sequence in interior Alaska, USA. Net N mineralization per gram dry soil increased across the successional sequence, but with a sharp decline in the oldest stage (black spruce). Net N mineralization expressed per gram soil organic matter exhibited the opposite pattern, suggesting that soil organic matter quality decreases significantly across succession. Net N mineralization rates during the growing season from green-up (early May) through freeze-up (late September–early October) accounted for approximately 60% of the annual inorganic N flux, whereas the remaining N was released during the apparent dormant season. Nitrogen release during winter occurred primarily during October–January with only negligible N mineralization during early spring in stands of willow, alder, balsam poplar and white spruce. By contrast, black spruce stands exhibited substantial mineralization after snow melt during early spring. The high rates of N mineralization in late autumn through early winter coincide with high turnover of fine root biomass in these stands, suggesting that labile substrate production, rather than temperature, is a major controlling factor over N release in these ecosystems. We suggest that the convention of restricting measurements of soil processes to the growing season greatly underestimate annual flux rates of inorganic nitrogen in these high-latitude ecosystems.     

Site factors controlling epiphytic lichen abundance in northern coniferous forests

Epiphytic lichens are an important part of the vegetation of northern coniferous forests of Eurasia and North America. Much progress has been made during recent decades at disentangling relevant site factors, which control the diversity and distribution of epiphytic lichens in boreal and oroboreal forests. The present paper aims at summarizing the present state of knowledge. Relevant site factors include the microclimate, nutrient supply, structural diversity and, if applicable, air pollution. The continuity of site conditions decides over the presence of species with dispersal limitations. The effects of fire on epiphytic lichens are largely unstudied, although fire is an important ecological factor in boreal forests.     

Amino acid uptake systems in lizard and chick brain cells

The uptake of seven amino acids, -aminoisobutyric acid (AIB), cyclo-leucine (cyclo-Leu), -aminobutyric acid (GABA), glycine (Gly), glutamic acid (Glu), lysine (Lys), and taurine (Tau), representatives of different amino acid transport systems, was studied in slices of brain from Tokay lizards and White Leghorn chicks. In descending order, the rate of the initial uptake of the amino acids in both species was Glu>Gly>GABA>Cyclo-Leu>AIB>Lys>Tau. The substrate specificities and the differences in sodium and temperature dependence of the uptake of the amino acids indicate the presence of several distinct amino acid transport systems, some sodium-dependent and some sodium-independent. The structural specificity of amino acid transport classes in the brain of these species is similar to that in other vertebrate brain preparations.Special issue dedicated to Dr. Santiago Grisolia.     

寒温带针叶林土壤CH4吸收对模拟大气氮沉降增加的初期响应

N沉降作为驱动因子会改变森林土壤－大气界面CH4净交换通量和方向。然而,对引起北方森林土壤CH4吸收发生转变的大气N沉降临界负荷及其响应机制知之甚少。为此,本研究以我国大兴安岭北方寒温带针叶林土壤作为研究对象,参照大兴安岭站实际大气N沉降通量,构建了低剂量、多形态和高频率的大气N沉降模拟增加控制实验,研究了2010年6-10月生长季土壤CH4吸收通量及其驱动因子对增N的初期响应。研究表明：整个生长季,大兴安岭寒温带针叶林土壤作为大气CH4净汇,CH4平均吸收通量为51.5?4.70 ugm-2h-1,主要受0-10cm土壤水分驱动。短期内,0-10cm矿质土壤NH4 -N含量对增N响应敏感;0-10cm矿质土壤NO3--N含量则受NO3--N输入影响较为明显。相反,0-10cm矿质土壤pH对增N的响应不敏感。总体上,低剂量的N输入对大兴安岭寒温带针叶林生长季土壤－大气界面CH4净交换通量影响不显著,而不排除NO3--N 输入尤其是低N处理情形所呈现出促进土壤CH4氧化的趋势。大兴安岭寒温带针叶林土壤CH4吸收对增N的响应敏感程度可能和土壤CH4活性氧化区域,土壤NH4 -N、NO3--N含量空间分布格局和相对比例有关。未来长期低水平的大气N沉降是否会改变大兴安岭北方森林土壤氧化大气CH4趋势,有待研究。     

Amino acid uptake and protein synthesis during early meiosis in Saccharomyces cerevisiae

Uptake and incorporation into proteins of an externally supplied amino acid were followed during early meiosis in yeast. Under conditions optimal for development, an insufficient permeability of the cell leads to an incorporation pattern which reflects the changes in the activity of the amino acid transporting system rather than those in protein synthesis. A more correct picture of protein synthesis during early meiosis is obtained by the use of a mutant with an enhanced level of amino acid uptake.Abbreviation SPM Sporulation medium     

Impacts of climate and land use on N2O and CH4 fluxes from tropical ecosystems in the Mt. Kilimanjaro region,Tanzania

In this study, we quantify the impacts of climate and land use on soil N₂O and CH₄ fluxes from tropical forest, agroforest, arable and savanna ecosystems in Africa. To do so, we measured greenhouse gases (GHG) fluxes from 12 different ecosystems along climate and land‐use gradients at Mt. Kilimanjaro, combining long‐term in situ chamber and laboratory soil core incubation techniques. Both methods showed similar patterns of GHG exchange. Although there were distinct differences from ecosystem to ecosystem, soils generally functioned as net sources and sinks for N₂O and CH₄ respectively. N₂O emissions correlated positively with soil moisture and total soil nitrogen content. CH₄ uptake rates correlated negatively with soil moisture and clay content and positively with SOC. Due to moderate soil moisture contents and the dominance of nitrification in soil N turnover, N₂O emissions of tropical montane forests were generally low (<1.2 kg N ha^?1 year^?1), and it is likely that ecosystem N losses are driven instead by nitrate leaching (~10 kg N ha^?1 year^?1). Forest soils with well‐aerated litter layers were a significant sink for atmospheric CH₄ (up to 4 kg C ha^?1 year^?1) regardless of low mean annual temperatures at higher elevations. Land‐use intensification significantly increased the soil N₂O source strength and significantly decreased the soil CH₄ sink. Compared to decreases in aboveground and belowground carbon stocks enhanced soil non‐CO₂ GHG emissions following land‐use conversion from tropical forests to homegardens and coffee plantations were only a small factor in the total GHG budget. However, due to lower ecosystem carbon stock changes, enhanced N₂O emissions significantly contributed to total GHG emissions following conversion of savanna into grassland and particularly maize. Overall, we found that the protection and sustainable management of aboveground and belowground carbon and nitrogen stocks of agroforestry and arable systems is most crucial for mitigating GHG emissions from land‐use change.     

Litterflow chemistry and nutrient uptake from the forest floor in northwest Amazonian forest ecosystems

Samples of the fraction of net rainfall passing through the forest floor collected at monthly intervals in four pristine forests in Colombian Amazonia, during the period between 1995–1997 were analysed for solute concentrations to estimate the element fluxes from the forest floor into the mineral soil and root nutrient uptake from these forest floors. Results were compared with inputs by throughfall, stemflow, litterfall and fine root decay. Element concentrations were tested for their relationship with litterflow amounts, rainfall intensity and length of the antecedent dry period and differences in element fluxes between ecosystems were assessed. Concentrations of elements in litterflow followed a similar pattern as those in throughfall, which indicates that element outputs from the forest floor are strongly related to those inputs in throughfall. In the forests studied, the average concentrations of elements as K, Mg, orthoP and the pH of the litterflow decreased relative to that in throughfall in most events, while the concentration of elements such as dissolved organic carbon, H, SO₄ and Si increased in litterflow from these forests. Element concentrations in litterflow showed a poor correlation with variables such as litterflow amounts, rainfall intensity and antecedent dry period, except for K which showed a significant correlation (p>0.95) with analysed variables in all forests. Outputs were significantly different between forests (p>0.95); these fluxes, which particularly concerned cations, being the largest in the flood plain, while for anions outputs increased from the flood plain to the sedimentary plain. After adding the nutrient contributed by litter decomposition and fine root decay, the net outputs of main elements from the forest floors were still smaller than inputs by net precipitation (throughfall+stemflow) indicating that the litter layers clearly acted as a sink for most nutrients. Accordingly, the element balances confirm that the forest floors acted as a sink for nutrients coming in by throughfall, stemflow, litterfall and fine root decomposition. P, Mg and N appeared to be the most limiting nutrients and the forests studied efficiently recycled these nutrients.     

Amino acid determination in some edible Mexican insects

Summary The amino acid contents of edible insects from different provinces of Mexico and reference proteins were analysed by reversed-phase high-performance liquid chromatography and ion exchange chromatography. The insect amino acid contents were higher than the adult requirements indicated by the WHO/FAO pattern.     

Nutrient cycling in a tropical seasonal rain forest of Xishuangbanna, Southwest China. Part 1: tree species: nutrient distribution and uptake

Tropical rain forests are characterized by large numbers of the species with diverse growth habits. The objective of the present study was to determine the distribution of nutrient content in the major trees of the tropical rain forests in Xishuangbanna. This will improve the understanding of the nutrient losses from such sites that result from harvesting and flow of nutrients within the ecosystem and lead to the development of effective and rational forest management strategies. Based on the results in this study, the distribution of nutrients among biomass components of trees varied: The ordering of major elements concentrations was K>N>Mg>Ca>P in branch, stem and root tissues but was N>K>Mg>Ca>P in leaves. The maximum amount of all nutrients per ha occurred in the stems followed by branches, roots and leaves. Of the total uptake of 6167.7 kg ha⁻¹ of all nutrients, the contribution of various nutrients was found to be N (2010.6 t ha⁻¹), P (196.3 t ha⁻¹), K (2123.8 kg ha⁻¹), Ca (832 kg ha⁻¹) and Mg (1005 kg ha⁻¹). However, comparing the nutrient uptake of other tropical and sub tropical forests, the results indicated that rates for the Xishuangbanna forests were 20–35% lower than previously reported values.     

Amino acid uptake in plasma membrane vesicles isolated from proliferating tumor cells and tissues

Summary The transport of L-alanine, a natural substrate of system A, across plasma membrane vesicle preparations has been studied in the early stages of rat DENA-PH hepato-carcinogenesis and in a very undifferentiated rat ascites hepatoma cell line (Yoshida AH-130) in the exponential and stationary phase of growth.Kinetic analyses indicated an increase of the V_max value in DENA-PH-treated rats 30 h after partial hepatectomy as well as in exponential growing Yoshida ascites cells. In DENA-PH-treated rats the Km value was drastically reduced 7 and 60 days after surgery, when enzyme-altered hyperplastic and preneoplastic lesions were present in rat liver. Drastically reduced Km values were also found in Yoshida ascites cells.The results suggest that an altered alanine transporter might take place in liver plasma membranes from carcinogen-treated rats. This appears to occur also in an established tumor cell line, grown in vivo.Abbreviations AAF 2-acetylaminofluorene - DENA diethylnitrosamine - PH partial hepatectomy - PMSF phenylmethanesulfonyl fluoride     

Characteristics of amino acid uptake in barley

Plants have the ability to take up organic nitrogen (N) but this has not been thoroughly studied in agricultural plants. A critical question is whether agricultural plants can acquire amino acids in a soil ecosystem. The aim of this study was to characterize amino acid uptake capacity in barley (Hordeum vulgare L.) from a mixture of amino acids at concentrations relevant to field conditions. Amino acids in soil solution under barley were collected in microlysimeters. The recorded amino acid composition, 0–8.2 μM of l-Serine, l-Glutamic acid, Glycine, l-Arginine and l-Alanine, was then used as a template for uptake studies in hydroponically grown barley plants. Amino acid uptake during 2 h was studied at initial concentrations of 2–25 μM amino acids and recorded as amino acid disappearance from the incubation solution, analysed with HPLC. The uptake was verified in control experiments using several other techniques. Uptake of all five amino acids occurred at 2 μM and below. The concentration dependency of the uptake rate could be described by Michaelis–Menten kinetics. The affinity constant (K _m) was in the range 19.6–33.2 μM. These K _m values are comparable to reported values for soil micro-organisms.     

Amino acid uptake by Ricinus communis roots: characterization and physiological significance

Abstract Roots of sterile-grown, intact 6-day-old seedlings of Ricinus communis possess at least two independent active amino acid uptake systems, one for neutral and one for basic amino acids. The kinetics of uptake of L-proline and L-arginine, which were taken as representative substrates for the two systems, are biphasic. At low concentrations (0.01–0.5 mol m^?3) Michaelis -Menten kinetics prevail, changing to a linear concentration dependence at higher substrate concentrations (1–50 mol m^?3). L-glutamate uptake velocity is linear over the whole substrate concentration range. For comparison the uptake kinetics of nitrate and ammonium were determined as well as interactions among the different nitrogen sources. The K_m value for nitrate uptake was 0.4 mol m^?3, and for ammonium 0.1 mol m^?3. The uptake capacity for nitrate or ammonium was approximately the same as for amino acids. The interaction between the uptake systems for organic and inorganic nitrogen is small. Two hypotheses for the physiological significance of amino acid uptake by roots were considered: (i) Uptake of amino acids from the soil-determination of amino acids in soil and in soil water indicates that they might contribute 15–25% to the nitrogen nutrition of the plant. (ii) Amino acid uptake systems of root cells serve primarily as retrieval of amino acids delivered from the phloem- it was found that ¹⁴C L-glutamine, which was delivered to the cotyledon and transported to the root via the phloem, was not lost by the roots, whereas it appeared in the bathing medium if L-glutamine was applied externally to the root to compete for the uptake sites; this suggests that an apoplastic pool of amino acids in the root exists due to their efflux from the phloem.     

Effects of perennial neighbors and nitrogen pulses on growth and nitrogen uptake by Bromus tectorum

An experiment was conducted to determine if growth and biomass responsesof the annual grass Bromus tectorum are affected by themagnitude and timing of nitrogen (N) pulses and if these responses areinfluenced by different perennial neighbor species. Nitrogen(NH₄:NO₃) was applied in three pulse treatments of varyinginterpulse length (3-d, 9-d, or 21-d between N additions). The total amount of Nadded was the same among treatments; hence, both the frequency and magnitude ofN pulses varied (i.e., the longer the interpulse period,the greater the amount of N added for a single pulse).Bromus showed little response to the different N-pulsetreatments. The only characteristic that varied among pulse treatments wasspecific leaf area (SLA), which was significantly greater whenBromus was grown under the 21-d N pulse than when grownunder the 3-d or 9-d N pulses. Bromus height, leaf andtiller numbers, leaf area and aboveground biomass were not affected by theN-pulse treatments nor were tissue-N contents and concentrations. However,Bromus production and tissue-N were significantly differentwhen Bromus was grown with different perennial neighborspecies. Tiller production, aboveground biomass, and seed numbers ofBromus were lowest when the perennial neighbor was thetussock grass Agropyron desertorum, intermediate when theneighbor was the evergreen shrub Artemisia tridentata, andgreatest when the neighbor was the deciduous shrub Chrysothamnusnauseosus. N contents of Bromus leaves were alsolowest when the neighbor was Agropyron. In contrast, root Nuptake capacities were greatest for Agropyron-Bromus rootmixes and lowest for Chrysothamnus-Bromus root mixes. Theseresults suggest that perennial neighbors affect growth, seed production, and Nuptake of Bromus to a greater extent than the timing andmagnitude of N pulses.     

Amino acid and vitamin requirements in mammalian cultured cells

Summary The development of the tissue culture technique has enabled us to cultivate mammalian cells in a way which is similar to that in use with bacterial cells. As such, the nutritional requirements of mammalian cells in culture have been studied with simplicity and exactness. According to Eagle's extensive works it is accepted that cultured cells generally require 13 amino acids, 8 or 9 vitamins, glucose and 6 inorganic salts. However, although some cultured cells have a capacity for the biosynthesis of Eagle's essential nutrients and others require non-essential nutrients.In this review we will discuss the amino acid and vitamin requirements of cultured cells, and a cell line (R-Y121B · cho) which propagates continuously in a chemically defined medium containing 11 amino acids, 7 vitamins, glucose and 6 ionic salts. Arginine, glutamine, tyrosine and choline are synthesized in the R-Y121B · cho cells.     

Nutrient uptake as a contributing explanation for deep rooting in arid and semi-arid ecosystems

Explanations for the occurrence of deep-rooted plants in arid and semi-arid ecosystems have traditionally emphasized the uptake of relatively deep soil water. However, recent hydrologic data from arid systems show that soil water potentials at depth fluctuate little over long time periods, suggesting this water may be rarely utilized or replenished. In this study, we examine the distributions of root biomass, soil moisture and nutrient contents to 10-m depths at five semi-arid and arid sites across southwestern USA. We couple these depth distributions with strontium (Sr) isotope data that show deep (>1 m) nutrient uptake is prevalent at four of the five sites. At all of the sites, the highest abundance of one or more of the measured nutrients occurred deep within the soil profile, particularly for P, Ca²⁺ and Mg²⁺. Phosphate contents were greater at depth than in the top meter of soil at three of five sites. At Jornada, for example, the 2–3 m depth increment had twice the extractable P as the top meter of soil, despite the highest concentrations of P occurring at the surface. The prevalence of such deep resource pools, and our evidence for cation uptake from them, suggest nutrient uptake as a complementary explanation for the occurrence of deep-rooted plants in arid and semi-arid systems. We propose that hydraulic redistribution of shallow surface water to deep soil layers by roots may be the mechanism through which deep soil nutrients are mobilized and taken up by plants.Electronic Supplementary Material Supplementary material is available for this article at     

稻鸭、稻鱼共作生态系统土壤可溶性有机N的动态和损失

通过田间试验研究了稻鸭、稻鱼共作生态系统土壤可溶性有机N(SON)的动态和损失,及其与土壤微生物量N和水稻吸N量的相关性.结果表明,(1)土壤SON是稻田土壤主要的可溶性N,其中处理CK,RD和RF土壤SON库分别为121.16, 109 30 和113.71 kg/hm2,高于土壤无机N库.(2)土壤SON与土壤可溶性无机N显著正相关(p<0.01);在水稻生育期间,土壤SON含量随水稻的生长而逐渐降低;同时由于鸭和鱼的存在,处理RD和RF土壤SON含量显著低于处理CK;土壤SON与水稻累积吸N量呈显著负相关(p<0.01),表明水稻生长强烈影响着土壤SON.(3)在水稻生长前期,渗漏水各形态N含量最大;溶解性有机N(DON)是稻田渗漏水N素的主要形态;同时,统计分析显示,相对于处理CK,RF土壤SON的下渗淋失量显著降低,RD土壤SON的下渗淋失量则略为降低.(4)水稻生育期间,土壤微生物量N不断地变化着,此外,由于鸭和鱼的存在,相对与处理CK,处理RD和RF土壤显著的提高了土壤MBN.同时,由于水稻吸收和N的淋失,土壤微生物量N与土壤SON不相关.总之,在水稻生长期间,土壤可溶性有机N受水稻吸N、微生物吸N与分解和N淋失的共同作用.     

Amino acid profiles in some scented rice varieties

Summary Twelve scented (basmati) and one non-scented variety were analysed for their amino acid composition. The essential amino acid profiles of scented varieties when compared with non-scented, revealed that these varieties exhibited higher values, which ranged from 2.82 to 4.86 gm/100 gm protein for lysine, 1.92 to 3.13 for methionine, 1.67 to 4.23 for tyrosine, 3.65 to 4.91 for phenylalanine, 5.50 to 8.95 for leucine, 2.25 to 3.40 for isoleucine, 2.84 to 3.46 for threonine, 3.36 to 5.33 for valine. When these values were compared to FAO recommended standards, it was observed that most of the scented varieties had comparable or superior values, while varieties such as, Type 3, Basmati sufaid 100, Likitimachi, Randhunipagalu and Basmati 370 showed superior lysine, phenylalanine, leucine, and methionine content. These observations suggest that the scented varieties posses better amino acid profiles and exhibit superior nutritional qualities, which could be utilised in breeding varieties with improved amino acid composition.     

Amino acid studies in transient acute polymorphic psychosis

Summary Data are reviewed on the amino acid metabolism in patients suffering from transient acute polymorphic psychoses according to ICD-10. The psychotic episodes of many of these patients are characterized by distorted sensory perceptions and intense emotional states; plasma amino acid analysis revealed a disturbed serine-glycine metabolism.In remitted patients oral loading with serine induced the characteristic dysperceptions and psychedelic symptoms. Plasma concentrations of serine and methionine were decreased, and the concentration of taurine was increased. Fibroblast experiments suggest that the activities of the serine metabolizing enzymes serine hydroxymethyltransferase and cystathionine-synthase are increased in these patients.The determination of plasma amino acid concentrations proved to be useful in discriminating these patients. The prevalence of this transient psychosis in a psychiatric in-patient population ranged between 1.4 and 3.6%.     

Amino acid modifications in canine, equine and porcine pituitary growth hormones, identified by peptide-mass mapping

Modified amino acid residues in porcine, canine and equine growth hormones purified from pituitary glands were characterised by tryptic mapping and high-performance liquid chromatography with on-line coupled electrospray ionisation mass spectrometry (HPLC–ESI-MS) detection. Hormones from all three species showed the same changes. Conversion of Asp¹²⁸ to iso-Asp¹²⁸ was a component of native hormones, while deamidation of Asn¹² and Asn⁹⁸ to Asp and iso-Asp, oxidation of Met⁴, and cyclisation to the pyroglutamyl derivative of Gln¹³⁹, probably occurred in vitro, during isolation, storage or hydrolysis. Porcine and canine hormones had indistinguishable protein fingerprints, confirming the assumption, based on their cDNA sequences, that their mature primary structures are identical.