Aerobic Biotransformation of N-Nitrosodimethylamine and N-Nitrodimethylamine by Benzene-, Butane-, Methane-, Propane-, and Toluene-Fed Cultures

N-Nitrosodimethylamine (NDMA) is an emerging contaminant of concern. N-nitrodimethylamine (DMNA) is a structural analog to NDMA. NDMA and DMNA have been found in drinking water, groundwater, and other media and are of concern due their toxicity. The authors evaluated biotransformation of NDMA and DMNA by cultures enriched from contaminated groundwater growing on benzene, butane, methane, propane, or toluene. Maximum specific growth rates of enriched cultures on butane (μ_max = 1.1 h^?1) and propane (μ_max = 0.65 h^?1) were 1 to 2 orders of magnitude higher than those presented in the literature. Growth rates of mixed cultures grown on benzene (μ_max = 1.3 h^?1), methane (μ_max = 0.09 h^?1), and toluene (μ_max = 0.99 h^?1) in these studies were similar to those presented in the literature. NDMA biotransformation rates for methane oxidizers (υ_max = 1.4 ng min^?1 mg^?1) and toluene oxidizers (υ_max = 2.3 ng min^?1 mg^?1) were comparable to those presented in the literature, whereas the biotransformation rate for propane oxidizers (υ_max = 0.37 ng min^?1 mg^?1) was lower. NDMA biotransformation rates for benzene oxidizers (υ_max = 1.02 ng min^?1 mg^?1) and butane oxidizers (υ_max = 1.2 ng min^?1 mg^?1) were comparable to those reported for other primary substrates. These studies showed that DMNA biotransformation rates for benzene (υ_max = 0.79 ng min^?1 mg^?1), butane (υ_max = 1.0 ng min^?1 mg^?1), methane (υ_max = 2.1 ng min^?1 mg^?1), propane (υ_max = 1.46 ng min^?1 mg^?1), and toluene (υ_max = 0.52 ng min^?1 mg^?1) oxidizers were all comparable. These studies highlight potential bioremediation methods for NDMA and DMNA in contaminated groundwater.     

Comprehensive RNAA of cadmium,cobalt, nickel,and copper using109Cd,57Co,and reactor-produced67Cu as radioisotopic yield monitors

An existing radiochemical NAA procedure for Cd, Co, and Cu was improved to allow determination of individual radiochemical yields by the radioisotopic tracer technique, thus eliminating errors owing to variable recovery.¹⁰⁹Cd was used as tracer for Cd determination via¹¹⁵Cd/^115mIn,⁵⁷Co for Co via⁶⁰Co, and potentially for Ni via⁵⁸Co, whereas as a novelty⁶⁷Cu, produced by reactor irradiation of ZnO of natural isotopic composition (by the⁶⁷Zn [n,p]⁶⁷Cu reaction) was used for Cu via the indicator nuclide⁶⁴Cu. The simple production and purification of⁶⁷Cu by anion exchange is described. Results for biological RMs are given and discussed.     

STIM proteins,Orai1, and gene expression

Cytoplasmic Ca²⁺ is an universal intracellular messenger that activates cellular responses over a broad temporal range, from neurotransmitter release to cell growth and proliferation.^1,2 Inherent to the use of the multifarious Ca²⁺ signal is the question of specificity: how can some Ca²⁺-dependent responses be activated in a cell and not others? A rise in cytoplasmic Ca²⁺ can evoke a response either by binding directly to the target (as occurs with certain Ca²⁺-activated K⁺ and Cl⁻ channels, for example) or through recruitment of intermediary proteins, such as calmodulin and troponin C. A substantial body of evidence has now established that Ca²⁺-binding proteins differ both in their affinities for Ca²⁺ and in their on- and off-rates for Ca²⁺ binding/unbinding. Furthermore, different Ca²⁺-binding proteins often occupy distinct locations within the cell. Therefore, the size, kinetics and spatial profile of a cytoplasmic Ca²⁺ signal are all important in determining which Ca²⁺-dependent response will be activated, when and for how long.³     

Major Ion Chemistry of Soil Solution of Mountainous Soils,Alvand, Hamedan,Western Iran

Soil solution chemistry reflects the most dynamic processes occurring in soils and is responsible for their current status. This study was undertaken to determine the soil solution status in 25 mountainous soils. The major cations in the studied soil solutions are in the decreasing order of Ca²⁺ > Mg²⁺ > Na⁺ > K⁺. The anions are also arranged in decreasing order as HCO^? ₃ > Cl^? > NO^? ₃ > SO ^2? ₄ . Concentrations of NO^? ₃ , P, and K⁺ in soil solutions were in the range of 12–364 mg l^?1, 1.75–34.8 mg l^?1, and 0.78– 198 mg l^?1, respectively. Results suggest that the concentration of P in the soil solutions could be primarily controlled by of the solubility of octacalcium phosphate and ß-tricalcium phosphate. In general, the greater the dissolved P concentration in the soil solution, the closer the solution was to equilibrium with respect to the more soluble Ca²⁺ phosphate minerals. Surface soil accumulations of P, NO^? ₃ , and K⁺ have occurred in these soils to such an extent that loss of these nutrients in surface runoff and the high risk for nutrient transfer into groundwater in concentrations exceeding the groundwater quality standard has become a priority management concern.     

Distribution of nitrogen-15 tracers applied to the canopy of a mature spruce-hemlock stand,Howland, Maine,USA

In N-limited ecosystems, fertilization by N deposition may enhance plant growth and thus impact C sequestration. In many N deposition–C sequestration experiments, N is added directly to the soil, bypassing canopy processes and potentially favoring N immobilization by the soil. To understand the impact of enhanced N deposition on a low fertility unmanaged forest and better emulate natural N deposition processes, we added 18 kg N ha⁻¹ year⁻¹ as dissolved NH₄NO₃ directly to the canopy of 21 ha of spruce-hemlock forest. In two 0.3-ha subplots, the added N was isotopically labeled as ¹⁵NH₄ ⁺ or ¹⁵NO₃ ⁻ (1% final enrichment). Among ecosystem pools, we recovered 38 and 67% of the ¹⁵N added as ¹⁵NH₄ ⁺ and ¹⁵NO₃ ⁻, respectively. Of ¹⁵N recoverable in plant biomass, only 3–6% was recovered in live foliage and bole wood. Tree twigs, branches, and bark constituted the most important plant sinks for both NO₃ ⁻ and NH₄ ⁺, together accounting for 25–50% of ¹⁵N recovery for these ions, respectively. Forest floor and soil ¹⁵N retention was small compared to previous studies; the litter layer and well-humified O horizon were important sinks for NH₄ ⁺ (9%) and NO₃ ⁻ (7%). Retention by canopy elements (surfaces of branches and boles) provided a substantial sink for N that may have been through physico-chemical processes rather than by N assimilation as indicated by poor recoveries in wood tissues. Canopy retention of precipitation-borne N added in this particular manner may thus not become plant-available N for several years. Despite a large canopy N retention potential in this forest, C sequestration into new wood growth as a result of the N addition was only ~16 g C m⁻² year⁻¹ or about 10% above the current net annual C sequestration for this site.     

Monovalent Cation Permeation through the Connexin40 Gap Junction Channel : Cs,Rb, K,Na, Li,TEA, TMA,TBA, and Effects of Anions Br,Cl, F,Acetate, Aspartate,Glutamate, and NO3

The unitary conductances and permeability sequences of the rat connexin40 (rCx40) gap junction channels to seven monovalent cations and anions were studied in rCx40-transfected neuroblastoma 2A (N2A) cell pairs using the dual whole cell recording technique. Chloride salt cation substitutions (115 mM principal salt) resulted in the following junctional maximal single channel current-voltage relationship slope conductances (γ_j in pS): CsCl (153), RbCl (148), KCl (142), NaCl (115), LiCl (86), TMACl (71), TEACl (63). Reversible block of the rCx40 channel was observed with TBA. Potassium anion salt γ_j are: Kglutamate (160), Kacetate (160), Kaspartate (158), KNO₃ (157), KF (148), KCl (142), and KBr (132). Ion selectivity was verified by measuring reversal potentials for current in rCx40 gap junction channels with asymmetric salt solutions in the two electrodes and using the Goldman-Hodgkin-Katz equation to calculate relative permeabilities. The permeabilities relative to Li⁺ are: Cs⁺ (1.38), Rb⁺ (1.32), K⁺ (1.31), Na⁺ (1.16), TMA⁺ (0.53), TEA⁺ (0.45), TBA⁺ (0.03), Cl⁻ (0.19), glutamate⁻ (0.04), and NO₃− (0.14), assuming that the monovalent anions permeate the channel by forming ion pairs with permeant monovalent cations within the pore thereby causing proportionate decreases in the channel conductance. This hypothesis can account for why the predicted increasing conductances with increasing ion mobilities in an essentially aqueous channel were not observed for anions in the rCx40 channel. The rCx40 effective channel radius is estimated to be 6.6 Å from a theoretical fit of the relationship of relative permeability and cation radius.     

Caesium accumulation by microorganisms: uptake mechanisms,cation competition,compartmentalization and toxicity

Summary The continued release of caesium radioisotopes into the environment has led to a resurgence of interest in microbe-Cs interactions. Caesium exists almost exclusively as the monovalent cation Cs⁺ in the natural environment. Although Cs⁺ is a weak Lewis acid that exhibits a low tendency to form complexes with ligands, its chemical similarity to the biologically essential alkali cation K⁺ facilitates high levels of metabolism-dependent intracellular accumulation. Microbial Cs⁺ (K⁺) uptake is generally mediated by monovalent cation transport systems located on the plasma membrane. These differe widely in specificity for alkali cations and consequently microorganisms display large differences in their ability to accumulate Cs⁺; Cs⁺ appears to have an equal or greater affinity than K⁺ for transport in certain microorganisms. Microbial Cs⁺ accumulation is markedly influenced by the presence of external cations, e.g. K⁺, Na⁺, NH₄ ⁺ and H⁺, and is generally accompanied by an approximate stoichiometric exchange for intracellular K⁺. However, stimulation of growth of K⁺-starved microbial cultures by Cs⁺ is limited and its has been proposed that it is not the presence of Cs⁺ in cells that is growth inhibitory but rather the resulting loss of K⁺. Increased microbial tolerance to Cs⁺ may result from sequestration of Cs⁺ in vacuoles or changes in the activity and/or specificity of transport systems mediating Cs⁺ uptake. The precise intracellular target(s) for Cs⁺-induced toxicity has yet to be clearly defined, although certain internal structures, e.g. ribosomes, become unstable in the presence of Cs⁺ and Cs⁺ is known to substitute poorly for K⁺ in the activation of many K⁺-requiring enzymes.     

Effects of the probiotic,Bacillus subtilis E20, on the survival,development, stress tolerance,and immune status of white shrimp,Litopenaeus vannamei larvae

In this study, the probiotic, Bacillus subtilis E20, isolated from the human health food, natto, was used for white shrimp, Litopenaeus vannamei, larvae breeding to improve the larval survival rate and development by adding probiotic to the rearing water at (control), 10⁸, and 10⁹ cfu L^?1 salt water once every 3 days during the 14 days of breeding experiment. Thereafter, stress tolerance and immune status of postlarvae were evaluated. Shrimp larval development was significantly accelerated after adding the probiotic to the larval rearing water at a level of 10⁹ cfu L^?1. The survival rate of larvae was significantly higher in the treatment with 10⁹ cfu L^?1 compared to the control and the treatment with 10⁸ cfu L^?1 after all larvae had metamorphosed to postlarvae. Adding the probiotic to the shrimp larvae rearing water produced a weak inhibition of bacterial growth by an analysis of the total bacterial count and presumptive Vibrio count. For stress tests, no postlarvae died when they were reared in water in which the temperature was decreased from 30 to 2 °C at a rate of 0.1 °C min^?1. Postlarvae had significantly lower cumulate mortality in the treatments with 10⁸ and 10⁹ cfu L^?1 compared to the control when they were suddenly exposed to fresh water and 60‰ salt water. A significant decrease in the cumulative mortality of postlarvae treated with the probiotic at a level of 10⁹ cfu L^?1 was recorded after the sudden transfer to 300 mg L^?1 nitrite-N compared to the control and treatment with 10⁸ cfu L^?1. The analysis of immune-related gene expressions showed that the gene expression of prophenoloxidase I, prophenoloxidase II, and lysozyme of larvae were significantly increased after being reared in probiotic-containing water at the levels of 10⁸ and 10⁹ cfu L^?1. However, no significant difference in serine proteinase or glutathione peroxidase gene expressions was recorded in this study. It is therefore suggested that 10⁹ cfu L^?1 of probiotic, B. subtilis E20 adding to rearing water for shrimp larva breeding.     

Photosynthesis, growth, and the role of chloride

Previous studies with isolated chloroplasts have indicated that Cl⁻ is an essential cofactor for photosynthesis. Considerable support for the postulated Cl⁻ requirement in photosynthesis came from the observation that Cl⁻ is essential for growth. Data are presented which show that a 60% reduction in growth which occurred in Cl⁻ -deficient sugar beet (Beta vulgaris L.) was not due to an effect of Cl⁻ on the rate of photosynthesis in vivo (net CO₂ uptake per unit area of attached leaves). The principal effect of Cl⁻ deficiency was to lower cell multiplication rates in leaves, thus slowing down their growth and ultimately decreasing their area. The absence of an effect of Cl⁻ on photosynthesis in vivo was unlikely to have been due to Cl⁻ retention by the chloroplasts because their Cl⁻ concentration (measured after nonaqueous isolation) decreased progressively with decrease in leaf Cl⁻.     

Caprine blood groups. 2. The C,G, H,I, J,K, L,N, and Q systems

Nine blood group systems of goats were identified using 12 caprine reagents produced by absorption of alloimmune antisera. The caprine C blood group system, possibly homologous to the ovine C blood group system, was characterized by two reagents and shown to be controlled by three alleles,C ¹²,C ²⁵, andC ⁻. A more complex blood group system of goats, designated G, was identified using three reagents and shown to be controlled by six codominant alleles (G ^10.19.20,G ^10.19,G ^10.20,G ¹⁰,G ¹⁹,G ²⁰) and a recessive allele (G ⁻). A further seven one-factor two-allelic systems were identified by seven reagents. The nine genetic systems provided exclusion probabilities of 0.479, 0.492, 0.548, and 0.572 in Australian Angora, Dairy, Cashmere, and Texan Angora goat breeds, respectively. This work was supported by a grant from the Australian Stud Book, Alison Road, Randwick, New South Wales 2031, Australia.     

Minimum energy conformations of DNA dimeric subunits: Potential energy calculations for dGpdC,dApdA, dCpdC,dGpdG, and dTpdT

Minimum energy conformations have been calculated for the deoxydinucleoside phosphates dGpdC, dApdA, dCpdC, dGpdG, and dTpdT. In these potential energy calculations the eight diheldral angles and the sugar pucker were flexible parameters. A substantial survey of conformation space was made in which all staggred combination ofthe dihedral angles ω′,ω, and ψ, in conjuction with C(2′)-endo puker, were used as starting conformers for the energy minimization. The most important conformations in the C(3′)-endo-puckering domain have ψ = g⁺; ω′,ω = g^?,g^?(A-form),g⁺, g⁺, and g^?,t. With C(2′)-endo-type puker the most important conformations have ψ = g⁺; ω′,ω =g^_,g^_(B-form) and g⁺,t; and ψ =t; ω′,ω =g^_,t(Watson-Crick from) and t,g⁺ (skewed). Stacked bases are a persistent feature of the low-energy conformations, the g⁺ conformer being an exception. Freeing the suger puker allowed this conformation to become low energy, with C(3′)-exo puker. It also caused other low-energy forms, such and the Waston-Crick conformation, to become more favourable. Conformation flexibility in the sugar puker and in ψ, as well as the ω′,ω angle pair, is indicated for the dimeric subunits of DNA.     

Chromosomal assignment of a large tRNA gene cluster (tRNALeu,tRNAGln, tRNALys,tRNAArg, tRNAGly) to 17p13.1

Summary A cluster of tRNA genes (tRNA _UAG ^Leu , tRNA _CUG ^Gln , tRNA _UUU ^Lys , tRNA _UCU ^Arg ) and an adjacent tRNA _GCC ^Gly have been assigned to human chromosome 17p12–p13.1 by in situ hybridization using a 4.2 kb human DNA fragment for tRNA^Leu, tRNA^Gln, tRNA^Lys, tRNA^Arg, and, for tRNA^Gly, 1.3 kb and 0.58 kb human DNA fragments containing these genes as probes. This localization was confirmed and refined to 17p13.100–p13.105 using a somatic cell hybrid mapping panel. Preliminary experiments with the biotiny lated tRNA Leu, Gln, Lys, Arg probe and metaphase spreads from other great apes suggest the presence of a hybridization site on the long arm of gorilla (Gorilla gorilla) chromosome 19 and the short arm of orangutan (Pongo pygmaeus) chromosome 19 providing further support for homology between HSA17, GGO19 and PPY19.     

Biotic and abiotic immobilization of ammonium, nitrite, and nitrate in soils developed under different tree species in the Catskill Mountains, New York, USA

Nitrogen retention in soil organic matter (SOM) is a key process influencing the accumulation and loss of N in forest ecosystems, but the rates and mechanisms of inorganic N retention in soils are not well understood. The primary objectives of this study were to compare ammonium (NH₄⁺), nitrite (NO₂^?), and nitrate (NO₃^?) immobilization among soils developed under different tree species in the Catskill Mountains of New York State, and to determine the relative roles of biotic or abiotic processes in soil N retention. A laboratory experiment was performed, where ¹⁵N was added as NH₄⁺, NO₂^?, or NO₃^? to live and mercury‐treated O horizon soils from three tree species (American beech, northern red oak, sugar maple), and ¹⁵N recoveries were determined in the SOM pool. Mercuric chloride was used to treat soils as this chemical inhibits microbial metabolism without significantly altering the chemistry of SOM. The recovery of ¹⁵N in SOM was almost always greater for NH₄⁺ (mean 20%) and NO₂^? (47%) than for NO₃^? (10%). Ammonium immobilization occurred primarily by biotic processes, with mean recoveries in live soils increasing from 9% at 15 min to 53% after 28 days of incubation. The incorporation of NO₂^? into SOM occurred rapidly (<15 min) via abiotic processes. Abiotic immobilization of NO₂^? (mean recovery 58%) was significantly greater than abiotic immobilization of NH₄⁺ (7%) or NO₃^? (7%). The incorporation of NO₂^? into SOM did not vary significantly among tree species, so this mechanism likely does not contribute to differences in soil NO₃^? dynamics among species. As over 30% of the ¹⁵NO₂^? label was recovered in SOM within 15 min in live soils, and the products of NO₂^? incorporation into SOM remained relatively stable throughout the 28‐day incubation, our results suggest that NO₂^? incorporation into SOM may be an important mechanism of N retention in forest soils. The importance of NO₂^? immobilization for N retention in field soils, however, will depend on the competition between incorporation into SOM and nitrification for transiently available NO₂^?. Further research is required to determine the importance of this process in field environments.     

Ammonium, nitrate, and proton fluxes along the maize root

Ion-selective microelectrodes were used to measure NH₄⁺, NO₃^– and H⁺ fluxes along the primary root of maize seedlings. Plants were exposed to nutrient solutions containing NH₄⁺, NO₃^– or both ions. Nitrogen fluxes along the root varied substantially among the different treatments. Net NH₄⁺ and NO₃^– uptake and H⁺ extrusion were low at the very apex of the root and generally increased in the more basal regions. In the absence of nitrogen or in the presence of NO₃^– alone, net H⁺ uptake (and root surface alkalinization) occurred at the root tip (0–1 mm), whereas net H⁺ extrusion occurred in all other regions. In the presence of NH₄⁺ alone, a dramatic increase in net H⁺ extrusion was detected in all regions except for the region 6–11 mm from the apex. In contrast, when NO₃^– alone was supplied, net H⁺ extrusion was depressed at all locations except for the tip (0–1 mm). When both NH₄⁺ and NO₃^– were supplied, NO₃^– uptake was suppressed at all locations while net H⁺ extrusion was increased relative to NO₃^– alone. The capacities to absorb NH₄⁺ and NO₃^– at the tip were similar, as indicated by flux rates when NH₄⁺ or NO₃^– were supplied as sole sources, but when supplied together, net NO₃^– uptake was half that of net NH₄⁺ uptake, indicating that NH₄⁺ may satisfy the nitrogen requirements of the poorly vascularized apical tissue in the most energy-efficient way. The high spatial resolution of the measurements enabled us to establish that acidification in the root expansion zone is maintained regardless of nitrogen source.     

Lysophosphatidylcholine-activated,vanadate-inhibited,Mg2+-ATPase from radish microsomes

An orthovanadate-inhibited, nitrate-insensitive, phospholipid-requiring Mg²⁺-ATPase has been partially purified (approx. 40-fold) from microsomal preparations from 24 h germinated radish seedlings. The specific activity obtained was 10–13 μmol P_i · min^?1 per mg protein, namely by 4- to 10-fold higher than that reported for the known similar enzyme preparations from corn and oat roots, and by 3- to 10-fold lower than that of the extensively purified plasmalemma enzymes from Neurospora and yeast. The partially purified activity was fairly specific for ATP, other nucleotide triphosphates being hydrolysed at less than 10% the rate with ATP; no activity was present towards ADP, AMP, p-nitrophenyl phosphate and other phosphate esters. The activity was strongly dependent on the presence of phospholipids with a marked preference for lysophosphatidylcholine, and showed an absolute requirement for Mg²⁺ or some other divalent cations (CO²⁺, Mn²⁺, Mg²⁺, Ni²⁺, Zn²⁺ in order of decreasing effectiveness); Ca²⁺ could not substitute for Mg²⁺ and was strongly inhibitory in its presence. K⁺, Rb⁺ and Na⁺ and also to a lesser extent NH₄⁺ and Li⁺ were significantly stimulatory, while the anions NO₃^?, H₂PO₄^?, Cl^? and SO₄^2? were ineffective. Orthovanadate, N,N′-dicyclohexylcarbodiimide, diethylstilbestrol, p-chloromercuribenzensulfonate, tetraiodofluorescein and tetrachlorotetraiodofluorescein were strongly inhibitory. The coincidence of the K_m for ATP with that for Mg²⁺ suggested that ATP-Mg is the true substrate. Accordingly, the enzyme showed a normal Michaelis-Menten kinetics for ATP-Mg with an apparent K_m of approx. 0.5 mM. The similarity of the characteristics of this enzyme with those of the plasmalemma enzymes from lower plants suggests its location at the plasma membrane, while some data ‘in vivo’ and in native sealed vesicle systems indicate its involvement in active proton transport.     

COMPARISONS OF NITRATE UPTAKE, STORAGE, AND REDUCTION IN MARINE DIATOMS AND FLAGELLATES

Diatoms, but not flagellates, have been shown to increase rates of nitrogen release after a shift from a low growth irradiance to a much higher experimental irradiance. We compared NO₃ ^? uptake kinetics, internal inorganic nitrogen storage, and the temperature dependence of the NO₃ ^? reduction enzymes, nitrate (NR) and nitrite reductase (NiR), in nitrogen‐replete cultures of 3 diatoms (Chaetoceros sp., Skeletonema costatum, Thalassiosira weissflogii) and 3 flagellates (Dunaliella tertiolecta, Pavlova lutheri, Prorocentrum minimum) to provide insight into the differences in nitrogen release patterns observed between these species. At NO₃ ^? concentrations <40 μmol‐N·L ^{? 1}, all the diatom species and the dinoflagellate P. minimum exhibited saturating kinetics, whereas the other flagellates, D. tertiolecta and P. lutheri, did not saturate, leading to very high estimated K _s values. Above ～60 μmol‐N·L ^{? 1}, NO₃ ^? uptake rates of all species tested continued to increase in a linear fashion. Rates of NO₃ ^? uptake at 40 μmol‐N·L ^{? 1}, normalized to cellular nitrogen, carbon, cell number, and surface area, were generally greater for diatoms than flagellates. Diatoms stored significant amounts of NO₃ ^? internally, whereas the flagellate species stored significant amounts of NH₄ ⁺ . Half‐saturation concentrations for NR and NiR were similar between all species, but diatoms had significantly lower temperature optima for NR and NiR than did the flagellates tested in most cases. Relative to calculated biosynthetic demands, diatoms were found to have greater NO₃ ^? uptake and NO₃ ^? reduction rates than flagellates. This enhanced capacity for NO₃ ^? uptake and reduction along with the lower optimum temperature for enzyme activity could explain differences in nitrogen release patterns between diatoms and flagellates after an increase in irradiance.     

Seasonal respiration of foliage, fine roots, and woody tissues in relation to growth, tissue N, and photosynthesis

Autotrophic respiration may regulate how ecosystem productivity responds to changes in temperature, atmospheric [CO₂] and N deposition. Estimates of autotrophic respiration are difficult for forest ecosystems, because of the large amount of biomass, different metabolic rates among tissues, and seasonal variation in respiration rates. We examined spatial and seasonal patterns in autotrophic respiration in a Pinus strobus ecosystem, and hypothesized that seasonal patterns in respiration rates at a common temperature would vary with [N] for fully expanded foliage and fine roots, with photosynthesis for foliage, and with growth for woody tissues (stems, branches, and coarse roots). We also hypothesized that differences in [N] would largely explain differences in maintenance or dormant‐season respiration among tissues. For April–November, mean respiration at 15 °C varied from 1.5 to 2.8 μmol kg^?1 s^?1 for fully expanded foliage, 1.7–3.0 for growing foliage, 0.8–1.6 for fine roots, 0.6–1.1 (sapwood) for stems, 0.5–1.8 (sapwood) for branches, and 0.2–1.5 (sapwood) for coarse roots. Growing season variation in respiration for foliage produced the prior year was strongly related to [N] (r² = 0.94), but fine root respiration was not related to [N]. For current‐year needles, respiration did not covary with [N]. Night‐time foliar respiration did not vary in concert with previous‐day photosynthesis for either growing or fully expanded needles. Stem growth explained about one‐third of the seasonal variation in stem respiration (r² = 0.38), and also variation among trees (r² = 0.43). We did not determine the cause of seasonal variation in branch and coarse root respiration, but it is unlikely to be directly related to growth, as the pattern of respiration in coarse roots and branches was not synchronized with stem growth. Seasonal variations in temperature‐corrected respiration rates were not synchronized among tissues, except foliage and branches. Spatial variability in dormant‐season respiration rates was significantly related to tissue N content in foliage (r² = 0.67), stems (r² = 0.45), coarse roots (r² = 0.36), and all tissues combined (r² = 0.83), but not for fine roots and branches. Per unit N, rates for P. strobus varied from 0.22 to 3.4 μmol molN^?1 s^?1 at 15 °C, comparable to those found for other conifers. Accurate estimates of annual autotrophic respiration should reflect seasonal and spatial variation in respiration rates of individual tissues.     

An adapid primate,sinoadapis, from lufeng,latest miocene,Yunnan, China

The paper deals with a new form ofSinoadapis from the Lufeng hominoid Locality, assigned toSinoadapis shihuibaensis sp. nov. Holotype PA 882 A fragment of right mandible with C,−M₃. Other materials. PA 903 A fragment of left maxilla with P³−M³. PA 959 Left lower tooth row with I₁−P², P₄. PA 902 Right upper tooth row with C′−P³. PA 964 An isolated left I¹. PA 907 An isolated right I³. PA 972 An isolated right M³.     

Estimated feeding rates and energy requirements of gentoo penguins,Pygoscelis papua,at Macquarie Island

Summary Water and sodium turnovers of 6–7 week old gentoo penguin chicks and breeding adults were measured using isotopically labelled water and sodium. Influx rates for chicks averaged 188 ml·kg^-1·day^-1 and 13.9 mmol·kg^-1·day^-1 for water and sodium, respectively. Chicks consumed an estimated 228 g·kg^-1·day^-1 fresh food or 886 kJ kg^-1 day. These values correspond to 761 g·day^-1 or 2945 kJ·day^-1 for a gentoo chick mid-way through the growth period. Flux rates for adults attending chicks ranged from 199 to 428 ml·kg^-1·day^-1 for water and from 15 to 36 mmol·kg^-1·ay^-1 for sodium.