Dual isotope labeling: Conjugation of 32P-oligonucleotides with 18F-aryltrifluoroborate via copper(I) catalyzed cycloaddition

A one-pot-two-step labeling of an oligonucleotide with an ¹⁸F-ArBF₃^?(aryltrifluoroborate) radioprosthetic is reported herein. In order to characterize labeling in terms of radiochemistry, phosphorus-32 was also introduced to the 5′-terminus of the oligonucleotide via enzymatic phosphorylation. A pendant azide group was subsequently conjugated to the 5′-phosphate of the oligonucleotide. Copper(I) catalyzed [2+3] cycloaddition was undertaken to conjugate an alkyne-bearing¹⁸F-ArBF₃^? to the oligonucleotide. Following polyacrylamide gel electrophoresis, this doubly-labeled bioconjugate exhibited decay properties of both the phosphorus-32 and fluorine-18, that were confirmed by autoradiography at selected lengths of time, which in turn provided concrete evidence of successful conjugation. These results are corroborated by HPLC analysis of the labeled material. Taken together this work demonstrates viable use of ¹⁸F-ArBF₃^? prosthetics for labeling oligonucleotides for use in PET imaging.     

Stable and radiogenic isotope analyses on shark teeth from the Early to the Middle Permian (Sakmarian–Roadian) of the southwestern USA

δ¹⁸O_P values and ⁸⁷Sr/⁸⁶Sr ratios were determined on disarticulated xenacanthiform, hybodontid and ctenacanthid shark tooth material from several Early Permian (Sakmarian–Kungurian) continental bone beds of northern Texas and southern Oklahoma as well as from the marine Middle Permian (Roadian) of northern Arizona. The δ¹⁸O_P values derived from the teeth of bone beds are in the range of 17.6–23.5‰ VSMOW, and are mostly depleted in ¹⁸O by 0.5–5‰ relative to proposed coeval marine δ¹⁸O_P values. This indicates an adaptation to freshwater habitats on the Early Permian coastal plain by several sharks. Distinctly higher δ¹⁸O_P values from two bone beds are attributed to significant evaporative enrichment in ¹⁸O in flood plain ponds. ⁸⁷Sr/⁸⁶Sr ratios of around 0.71077 are notably more radiogenic than ⁸⁷Sr/⁸⁶Sr of contemporaneous seawater. In contrast, the isotopic composition of teeth from the marine Kaibab Formation is characterised by low δ¹⁸O_P values in the range of 13.4–15.6‰ VSMOW while ⁸⁷Sr/⁸⁶Sr ratios of around 0.70821 are closer to the Roadian seawater value. The distinctly depleted δ¹⁸O_P values cannot be readily explained by fluvially affected freshening in a nearshore marine environment, so a diagenetic alteration of the Kaibab material seems to be more likely, excluding it from further interpretation.     

Measurements of 18O‐Pi uptake indicate fast metabolism of phosphate in tree roots

Phosphorus (P) nutrition of beech ecosystems depends on soil processes, plant internal P cycling and P acquisition. P uptake of trees in the field is currently not validated due to the lack of an experimental approach applicable in natural forests. Application of radiolabelled tracers such as ³³P and ³²P is limited to special research sites and not allowed in natural environments. Moreover, only one stable isotope of P, namely ³¹P, exists. One alternative tool to measure P acquisition in the field could be the use of ¹⁸O‐labelled ³¹P‐phosphate (³¹P¹⁸O₄ ^3?). Phosphate (P_i) uptake rates calculated from the ¹⁸O enrichment of dried root material after application of ³¹P_i ¹⁸O₄ ^3? via nutrient solution was always lower compared to ³³P incorporation, did not show increasing rates of P_i uptake at P deficiency under controlled conditions, and did not reveal seasonal fluctuations in the field. Consequently, a clear correlation between ³³P‐based and ¹⁸O‐based P_i uptake by roots could not be established. Comparison of P_i uptake rates achieved from ³³P‐P_i and ¹⁸O‐P_i application led to the conclusion of high P_i metabolism in roots after P_i uptake. The replacement of ¹⁸O by ¹⁶O from water in ¹⁸O‐P_i during root influx, but most probably after P_i uptake into roots, due to metabolic activities, indicates high and fast turnover of P_i. Hence, the use of ¹⁸O‐P_i as an alternative tool to estimate P_i acquisition of trees in the field must consider the increase of ¹⁸O abundance in root water that was disregarded in dried root material.     

Oxygen isotope analysis of human bone phosphate evidences weaning age in archaeological populations

Here we report bone phosphate oxygen (δ¹⁸O_p) values from perinates/neonates and infants (<3.5 years; n = 32); children (4–12 years; n = 12); unsexed juveniles (16–18 years; n = 2); and adult bones (n = 17) from Wharram Percy, North Yorkshire, England, in order to explore the potential of this method to investigate patterns of past breastfeeding and weaning. In prior studies, δ¹⁵N and δ¹³C analyses of bone collagen have been utilized to explore weaning age in this large and well‐studied assemblage, rendering this material highly appropriate for the testing and development of this alternative method targeting the inorganic phase of bone. Data produced reveal ¹⁸O‐enrichment in the youngest perinatal/neonatal and infant samples, and an association between age and bone δ¹⁸O_p (and previously‐published δ¹⁵N values), with high values in both these isotope systems likely due to breastfeeding. After the age of 2–3 years, δ¹⁸O_p values are lower, and all children between the ages of 4 and 12, along with the vast majority of sub‐adults and adults sampled (aged 16 to >50 years), have δ¹⁸O_p values consistent with the consumption of local modern drinking water. The implications of this study for the reconstruction of weaning practices in archaeological populations are discussed, including variations observed with bone δ¹⁵N_coll and δ¹⁸O_p co‐analysis and the influence of culturally‐modified drinking water and seasonality. The use of this method to explore human mobility and palaeoclimatic conditions are also discussed with reference to the data presented. Am J Phys Anthropol 157:226–241, 2015. © 2015 Wiley Periodicals, Inc.     

The 18O-signal transfer from water vapour to leaf water and assimilates varies among plant species and growth forms

The ¹⁸O signature of atmospheric water vapour (δ¹⁸O_V) is known to be transferred via leaf water to assimilates. It remains, however, unclear how the ¹⁸O-signal transfer differs among plant species and growth forms. We performed a 9-hr greenhouse fog experiment (relative humidity ≥ 98%) with ¹⁸O-depleted water vapour (−106.7‰) on 140 plant species of eight different growth forms during daytime. We quantified the ¹⁸O-signal transfer by calculating the mean residence time of O in leaf water (MRT_LW) and sugars (MRT_Sugars) and related it to leaf traits and physiological drivers. MRT_LW increased with leaf succulence and thickness, varying between 1.4 and 10.8 hr. MRT_Sugars was shorter in C₃ and C₄ plants than in crassulacean acid metabolism (CAM) plants and highly variable among species and growth forms; MRT_Sugars was shortest for grasses and aquatic plants, intermediate for broadleaf trees, shrubs, and herbs, and longest for conifers, epiphytes, and succulents. Sucrose was more sensitive to δ¹⁸O_V variations than other assimilates. Our comprehensive study shows that plant species and growth forms vary strongly in their sensitivity to δ¹⁸O_V variations, which is important for the interpretation of δ¹⁸O values in plant organic material and compounds and thus for the reconstruction of climatic conditions and plant functional responses.     

Biologically driven isotopic fractionations in bivalves: from palaeoenvironmental problem to palaeophysiological proxy

Traditional bulk stable isotope (δ¹⁸O and δ¹³C) and clumped isotope (Δ₄₇) records from bivalve shells provide invaluable histories of Earth's local and global climate change. However, biologically driven isotopic fractionations (BioDIFs) can overprint primary environmental signals in the shell. Here, we explore how conventional measurements of δ¹⁸O, δ¹³C, and Δ₄₇ in bivalve shells can be re-interpreted to investigate these physiological processes deliberately. Using intrashell Δ₄₇ and δ¹⁸O alignment as a proxy for equilibrium state, we separately examine fractionations and/or disequilibrium occurring in the two major stages of the biomineralisation process: the secretion of the extrapallial fluid (EPF) and the precipitation of shell material from the EPF. We measured δ¹⁸O, δ¹³C, and Δ₄₇ in fossil shells representing five genera (Lahillia, Dozyia, Eselaevitrigonia, Nordenskjoldia, and Cucullaea) from the Maastrichtian age [66–69 million years ago (Ma)] López de Bertodano Formation on Seymour Island, Antarctica. Material was sampled from both the outer and inner shell layers (OSL and ISL, respectively), which precipitate from separate EPF reservoirs. We find consistent δ¹⁸O values across the five taxa, indicating that the composition of the OSL can be a reliable palaeoclimate proxy. However, relative to the OSL baseline, ISLs of all taxa show BioDIFs in one or more isotopic parameters. We discuss/hypothesise potential origins of these BioDIFs by synthesising isotope systematics with the physiological processes underlying shell biomineralisation. We propose a generalised analytical and interpretive framework that maximises the amount of palaeoenvironmental and palaeobiological information that can be derived from the isotopic composition of fossil shell material, even in the presence of previously confounding ‘vital effects’. Applying this framework in deep time can expand the utility of δ¹⁸O, δ¹³C, and Δ₄₇ measurements from proxies of past environments to proxies for certain biomineralisation strategies across space, time, and phylogeny among Bivalvia and other calcifying organisms.     

Determinants of isotopic coupling of CO2 and water vapour within a Quercus petraea forest canopy

Concentration and isotopic composition (δ¹³C and δ¹⁸O) of ambient CO₂ and water vapour were determined within a Quercus petraea canopy, Northumberland, UK. From continuous measurements made across a 36-h period from three heights within the forest canopy, we generated mixing lines (Keeling plots) for δ_a ¹³CO₂, δ_a C¹⁸O¹⁶O and δ_a H₂ ¹⁸O, to derive the isotopic composition of the signal being released from forest to atmosphere. These were compared directly with measurements of different respective pools within the forest system, i.e. δ¹³C of organic matter input for δ_a ¹³CO₂, δ¹⁸O of exchangeable water for δ_a C¹⁸O¹⁶O and transpired water vapour for δ_a H₂ ¹⁸O. [CO₂] and δ_a ¹³CO₂ showed strong coupling, where the released CO₂ was, on average, 4 per mil enriched compared to the organic matter of plant material in the system, suggesting either fractionation of organic material before eventual release as soil-respired CO₂, or temporal differences in ecosystem discrimination. δ_a C¹⁸O¹⁶O was less well coupled to [CO₂], probably due to the heterogeneity and transient nature of water pools (soil, leaf and moss) within the forest. Similarly, δ_a H₂ ¹⁸O was less coupled to [H₂O], again reflecting the transient nature of water transpired to the forest, seen as uncoupling during times of large changes in vapour pressure deficit. The δ¹⁸O of transpired water vapour, inferred from both mixing lines at the canopy scale and direct measurement at the leaf level, approximated that of source water, confirming that an isotopic steady state held for the forest integrated over the daily cycle. This demonstrates that isotopic coupling of CO₂ and water vapour within a forest canopy will depend on absolute differences in the isotopic composition of the respective pools involved in exchange and on the stability of each of these pools with time. Received: 21 March 1998 / Accepted: 10 December 1998     

How useful are vibrational frequencies of isotopomeric O2 fragments for assessing local symmetry? Some simple systems and the vexing case of a galactose oxidase model

The tendency for mixed-isotope O₂ fragments to exhibit different stretching frequencies in asymmetric environments is examined with various levels of electronic structure theory for simple peroxides and peroxyl radicals, as well as for a variety of monocopper–O₂ complexes. The study of the monocopper species is motivated by their relevance to the active site of galactose oxidase. Extensive theoretical work with an experimental model characterized by Jazdzewski et al. (J. Biol. Inorg. Chem. 8:381–393, 2003) suggests that the failure to observe a splitting between ¹⁶O¹⁸O and ¹⁸O¹⁶O isotopomers cannot be taken as evidence against end-on O₂ coordination. Conformational analysis on an energetic basis, however, is complicated by biradical character inherent in all of the copper–O₂ singlet structures. Electronic Supplementary Material Supplementary material is available for this article at .     

Relative humidity- and ABA-induced variation in carbon and oxygen isotope ratios of cotton leaves

Cotton (Gossypium hirsutum L. cv. CS50) plants were grown at two levels of relative humidity (RH) and sprayed daily with abscisic acid (ABA) at four concentrations. Plants grown at lower humidity had higher transpiration rates, lower leaf temperatures and lower stomatal conductance. Plant biomass was also reduced at low humidity. Within each humidity environment, increasing ABA concentration generally reduced stomatal conductance, evaporation rates, superficial leaf density and plant biomass, and increased leaf temperature and specific leaf area. As expected, decreased stomatal conductance resulted in decreased carbon isotope discrimination in leaf material ( Δ ¹³C_l). Plants grown at low humidity were more enriched in ¹⁸O than those grown at high RH, as theory predicts. Within each humidity environment, increasing ABA concentration increased oxygen isotope enrichment of leaf cellulose ( Δ ¹⁸O_c) and whole‐leaf tissue ( Δ ¹⁸O_l). Values of Δ ¹³C_l and Δ ¹⁸O_l predicted by theoretical models were close to those observed, accounting for 79% of the measured variation in Δ ¹³C_l and 95% of the measured variation in Δ ¹⁸O_l. Supporting theory, Δ ¹³C_l and Δ ¹⁸O_l in whole‐leaf tissue were negatively related.     

Reconstructing the δ18O of atmospheric water vapour via the CAM epiphyte Tillandsia usneoides: seasonal controls on δ18O in the field and large‐scale reconstruction of δ18Oa

Using both oxygen isotope ratios of leaf water (δ¹⁸O_L) and cellulose (δ¹⁸O_C) of Tillandsia usneoides in situ, this paper examined how short‐ and long‐term responses to environmental variation and model parameterization affected the reconstruction of the atmospheric water vapour (δ¹⁸O_a). During sample‐intensive field campaigns, predictions of δ¹⁸O_L matched observations well using a non‐steady‐state model, but the model required data‐rich parameterization. Predictions from the more easily parameterized maximum enrichment model (δ¹⁸O_L–M) matched observed δ¹⁸O_L and observed δ¹⁸O_a when leaf water turnover was less than 3.5 d. Using the δ¹⁸O_L–M model and weekly samples of δ¹⁸O_L across two growing seasons in Florida, USA, reconstructed δ¹⁸O_a was ?12.6 ± 0.3‰. This is compared with δ¹⁸O_a of ?12.4 ± 0.2‰ resolved from the growing‐season‐weighted δ¹⁸O_C. Both of these values were similar to δ¹⁸O_a in equilibrium with precipitation, ?12.9‰. δ¹⁸O_a was also reconstructed through a large‐scale transect with δ¹⁸O_L and the growing‐season‐integrated δ¹⁸O_C across the southeastern United States. There was considerable large‐scale variation, but there was regional, weather‐induced coherence in δ¹⁸O_a when using δ¹⁸O_L. The reconstruction of δ¹⁸O_a with δ¹⁸O_C generally supported the assumption of δ¹⁸O_a being in equilibrium with precipitation δ¹⁸O (δ¹⁸O_ppt), but the pool of δ¹⁸O_ppt with which δ¹⁸O_a was in equilibrium – growing season versus annual δ¹⁸O_ppt – changed with latitude.     

Deciphering the oxygen isotope composition of nitrous oxide produced by nitrification

The ability to use δ¹⁸O values of nitrous oxide (N₂O) to apportion environmental emissions is currently hindered by a poor understanding of the controls on δ¹⁸O–N₂O from nitrification (hydroxylamine oxidation to N₂O and nitrite reduction to N₂O). In this study fertilized agricultural soils and unfertilized temperate forest soils were aerobically incubated with different ¹⁸O/¹⁶O waters, and conceptual and mathematical models were developed to systematically explain the δ¹⁸O–N₂O formed by nitrification. Modeling exercises used a set of defined input parameters to emulate the measured soil δ¹⁸O–N₂O data (Monte Carlo approach). The Monte Carlo simulations implied that abiotic oxygen (O) exchange between nitrite (NO₂^?) and H₂O is important in all soils, but that biological, enzyme‐controlled O‐exchange does not occur during the reduction of NO₂^? to N₂O (nitrifier‐denitrification). Similarly, the results of the model simulations indicated that N₂O consumption is not characteristic of aerobic N₂O formation. The results of this study and a synthesis of the published literature data indicate that δ¹⁸O–N₂O formed in aerobic environments is constrained between +13‰ and +35‰ relative to Vienna Standard Mean Ocean Water (VSMOW). N₂O formed via hydroxylamine oxidation and nitrifier‐denitrification cannot be separated using δ¹⁸O unless ¹⁸O tracers are employed. The natural range of nitrifier δ¹⁸O–N₂O is discussed and explained in terms of our conceptual model, and the major and minor controls that define aerobically produced δ¹⁸O–N₂O are identified. Despite the highly complex nature of δ¹⁸O–N₂O produced by nitrification this δ¹⁸O range is narrow. As a result, in many situations δ¹⁸O values may be used in conjunction with δ¹⁵N–N₂O data to apportion nitrifier‐ and denitrifier‐derived N₂O. However, when biological O‐exchange during denitrification is high and N₂O consumption is low, there may be too much overlap in δ¹⁸O values to distinguish N₂O formed by these pathways.     

Nitrogen fertilization and δ18O of CO2 have no effect on 18O‐enrichment of leaf water and cellulose in Cleistogenes squarrosa (C4) – is VPD the sole control?

The oxygen isotope composition of cellulose (δ¹⁸O_Cel) archives hydrological and physiological information. Here, we assess previously unexplored direct and interactive effects of the δ¹⁸O of CO₂ (δ¹⁸O_CO2), nitrogen (N) fertilizer supply and vapour pressure deficit (VPD) on δ¹⁸O_Cel, ¹⁸O‐enrichment of leaf water (Δ¹⁸O_LW) and cellulose (Δ¹⁸O_Cel) relative to source water, and p_exp_x, the proportion of oxygen in cellulose that exchanged with unenriched water at the site of cellulose synthesis, in a C₄ grass (Cleistogenes squarrosa). δ¹⁸O_CO2 and N supply, and their interactions with VPD, had no effect on δ¹⁸O_Cel, Δ¹⁸O_LW, Δ¹⁸O_Cel and p_exp_x. Δ¹⁸O_Cel and Δ¹⁸O_LW increased with VPD, while p_exp_x decreased. That VPD‐effect on p_exp_x was supported by sensitivity tests to variation of Δ¹⁸O_LW and the equilibrium fractionation factor between carbonyl oxygen and water. N supply altered growth and morphological features, but not ¹⁸O relations; conversely, VPD had no effect on growth or morphology, but controlled ¹⁸O relations. The work implies that reconstructions of VPD from Δ¹⁸O_Cel would overestimate amplitudes of VPD variation, at least in this species, if the VPD‐effect on p_exp_x is ignored. Progress in understanding the relationship between Δ¹⁸O_LW and Δ¹⁸O_Cel will require separate investigations of p_ex and p_x and of their responses to environmental conditions.     

Synthesis of 6-[18F]fluoropyridoxal and radioactivity distribution in rat at 60 min

6-[¹⁸F]Fluoropyridoxal was synthesized by the flourination of a propylamine derivative of pyridoxal (pyridoxal Schiff base) with ¹⁸F-labelled acetylhypofluorite. Two different fluorinating agents, 5% F₂ in N₂ and acetylhypofluorite, were investigated with nonradioactive material. The evaluation of reactions in CH₃CN and chloroform showed CH₃CN to be the better solvent and CH₃COOF to be the better fluorinating reagent. The synthesis gave a radiochemical yield of about 18% (expressed at the end of synthesis) and required 35–40 min to complete. The specific activity of the final radiopharmaceutical at the end of the synthesis was about 25.9 GBq/mmol (700 mCi/mmol).The tissue distribution of 6-fluoropyridoxal in rat at 60 min is also reported. A large concentration in liver and kidney indicates that this radiopharmaceutical could be of special interest in the imaging of liver functions. The concentration in the brain might also allow in vivo PET imaging of the 6-(fluoropyridoxal) uptake if a high efficiency PET scanner is used.     

The Metabolism of the Germinating Oil Palm (Elaeis guineensis) Seedling : In Vivo Studies

The metabolism of ¹⁴C-labeled fatty acids and triacylglycerols was followed in intact germinating oil palm seedlings as well as in tissue slices. In the germinating seedling, the shoot contained a normal pattern of membrane fatty acids (mainly C₁₆, C_18:1, C_18:2) but the kernel contained about 68% C₁₂ and C₁₄ fatty acids. Haustorium fatty acids were intermediate between the two. [¹⁴C]Acetate was actively metabolized by shoot and haustorium slices but not so actively by the kernel. Approximately 9% to 17% was converted to water-soluble substances, 4% to 6% to CO₂, and 0.5% to 5.9% to lipids. The fatty acids synthesized in the shoot and haustorium were mainly C₁₆, C₁₈, and C_18:1 fatty acids but in the kernel about 18% to 32% of the ¹⁴C-fatty acids were C₁₂ fatty acids.

[¹⁴C]Lauric acid was absorbed and metabolized by haustorium slices and by the haustorium in intact seedlings; it was partly esterified to triacylglycerols and also converted to water-soluble substances and insoluble tissue material. In contrast, tri-[¹⁴C]laurin was absorbed but not metabolized. The haustorium also absorbed other fatty acids but the longer chain (C₁₆ and C₁₈) fatty acids were not esterified or metabolized further. Preincubation of the haustorium with plant hormones or in the presence of kernel tissue did not alter its inactivity towards tri-[¹⁴C]laurin.

When tri-[¹⁴C]laurin or [¹⁴C]lauric acid were injected into the seed or the shoot, there was no movement or radioactivity to other parts of the seedling. When injected into the shoot, but not into the seed, tri-[¹⁴C] laurin was hydrolyzed and partly metabolized to water-soluble substances.

     

The geochemistry of methane in Lake Fryxell,an amictic,permanently ice-covered,antarctic lake

The abundance and distribution of dissolved CH₄ were determined from 1987–1990 in Lake Fryxell, Antarctica, an amictic, permanently ice-covered lake in which solute movement is controlled by diffusion. CH₄ concentrations were < 1 υM in the upper oxic waters, but increased below the oxycline to 936 μM at 18 m. Sediment CH₄ was 1100 μmol (1 sed)⁻¹ in the 0–5 cm zone. Upward flux from the sediment was the source of the CH₄, NH₄ ⁺, and DOC in the water column; CH₄ was 27% of the DOC+CH₄ carbon at 18 m. Incubations with surficial sediments indicated that H¹⁴CO₃ ⁻ reduction was 0.4 μmol (1 sed)⁻¹ day⁻¹ or 4× the rate of acetate fermentation to CH₄. There was no measurable CH₄ production in the water column. However, depth profiles of CH₄, NH₄, and DIC normalized to bottom water concentrations demonstrated that a significant CH₄ sink was evident in the anoxic, sulfate-containing zone of the water column (10–18 m). The δ¹³CH₄ in this zone decreased from −72 % at 18 m to −76% at 12 m, indicating that the consumption mechanism did not result in an isotopic enrichment of ¹³CH₄. In contrast, δ¹³CH₄ increased to −55 % at 9 m due to aerobic oxidation, though this was a minor aspect of the CH₄ cycle. The water column CH₄ profile was modeled by coupling diffusive flux with a first order consumption term; the best-fit rate constant for anaerobic CH₄ consumption was 0.012 yr⁻¹. On a total carbon basis, CH₄ consumption in the anoxic water column exerted a major effect on the flux of carbonaceous material from the underlying sediments and serves to exemplify the importance of CH₄ to carbon cycling in Lake Fryxell.     

Chemical alterations of hyaluronic acid and dermatan sulfate detected in aging human skin by infrared spectroscopy

Age-mediated deacetylation of hyaluronic acid and dermatan sulfate, and shift of sulfate ester configuration were indicated by infrared spectroscopy. Hyaluronic acid and the three dermatan sulfates (DS₁₈, DS₁₈ and DS₃₅), sequentially precipitated from adult skin with 18%, 28% and 35% ethanol, were analyzed at varying ages. At age 75 years, loss of infrared bands in the 1650-1600 cm⁻¹ region, at 1380 cm⁻¹ and 1320 cm⁻¹ and appearance of a band at 1560 cm⁻¹ were characteristic of hyaluronic acid and DS₃₅,·moreover, in DS₂₈ and DS₃₅ the intensities of the bands at 840 cm⁻¹ and 860 cm⁻ were, respectively, decreased and increased. A low intensity band in the 805-785 cm⁻¹ region was observed in the spectra of DS₁₈ (19–35 years), DS₂₈ (70–80 years) and DS₃₅ (all ages). It intensified in DS₂₈ of the 80-years-olds. In the 75±5-year-old group. ninhydrin-positive material of hyaluronic acid and DS₃₅ increased, while reducing GlcNAc of hyaluronic acid decreased. The data demonstrated hyaluronic acid and DS₃₅ deacetylation and suggested a decrease of equatorial sulfates with infrared band at 840 cm⁻¹ and an incrase of axial sulfates with band at 860 cm⁻¹ in DS₂₈ and DS₃₅ of the 75±5-yearl-old set. Equatorial sulfates with band in the 805±785 cm⁻¹ region apparently decreased in DS₁₈ after 35 years and increased in DS₂₈ of the oldest group.     

Utilization of a Stable Isotope of Oxygen by Pseudomonas fluorescens

Oxygen utilization is defined in this investigation as the terminal use of oxygen in respiration, i.e., the formation of water. A culture of Pseudomonas fluorescens was allowed to respire in an atmosphere of O¹⁸. The production of H₂O¹⁸ was measured during two test runs of 124 and 232 min each. During the first run, 0.505 mmole of H₂O¹⁸ was produced. The second run produced 0.460 mmole of H₂O¹⁸. H₂O¹⁸ production took place throughout the course of each of the runs.     

Synthesis and evaluation of an 18F-labeled boramino acid analog of aminosuberic acid for PET imaging of the antiporter system xC−

In this study, we synthesized ¹⁸F-ASu-BF₃, a close boramino acid analog of 5-[¹⁸F]fluoro-aminosuberic acid (¹⁸F-ASu), via ¹⁸F-¹⁹F isotope exchange reaction and evaluated its potential for imaging with positron emission tomography (PET). ¹⁸F-ASu-BF₃ was stable in mouse plasma and taken up into PC3 prostate cancer cells via the system x_C^? amino acid transporter. The continuous use of isoflurane for anesthesia during dynamic imaging acquisition slowed down the excretion of ¹⁸F-ASu-BF₃ and enabled visualization of PC3 tumor xenografts in mice. In contrast, no tumor visualization was observed from static images of ¹⁸F-BF₃-ASu due to its rapid renal excretion mediated in part by the organic anion transporter. Our data indicate that the pharmacokinetics of amino acids could be altered after being converted into their boramino acid analogs. Therefore, care should be taken when using the boramino acid strategy to design and prepare ¹⁸F-labeled tracers for imaging amino acid transporters/receptors with PET.     

Assessment of radionuclide impurities in [18F]fluoromethylcholine ([18F]FMCH)

Purpose[¹⁸F]Fluoromethylcholine ([¹⁸F]FMCH) is a radiopharmaceutical used in positron emission tomography (PET) imaging for the study of prostate, breast, and brain tumors. It is usually synthesized in cyclotron facilities where ¹⁸F is produced by proton irradiation of [¹⁸O]H₂O through ¹⁸O(p,n)¹⁸F reaction. Due to the activation of target materials, the bombardment causes unwanted radionuclidic impurities in [¹⁸O]H₂O, that need to be removed during the radiopharmaceutical synthesis. Thus, the aim of this study is to quantify the radionuclide impurities in the ¹⁸F production process and in the synthesized [¹⁸F]FMCH, demonstrating the radionuclidic purity of this radiopharmaceutical.MethodsLong-lived radionuclide impurities were experimentally assessed using high-resolution gamma and liquid scintillation spectrometries, while short-lived impurities were monitored analyzing the decay curve of the irradiated [¹⁸O]H₂O with an activity calibrator. As spectrometric radionuclide library, a Geant4 Monte Carlo simulation of the ¹⁸F-target assembly was previously performed.Results³H, ^52,54Mn, ^56,57,58Co, ^95m,96Tc, ¹⁰⁹Cd, and ¹⁸⁴Re were found in the irradiated [¹⁸O]H₂O, but no radionuclide was found in the non-irradiated [¹⁸O]H₂O neither in the final [¹⁸F]FMCH solution with an activity concentration greater than the minimum detectable activity concentration. A total impurity activity <6.2 kBq was measured in the irradiated [¹⁸O]H₂O, whereas a [¹⁸F]FMCH radionuclide purity >99.9999998% was estimated. Finally, the decay curve of the irradiated [¹⁸O]H₂O revealed a very low maximum of ¹³N activity (<0.03% of ¹⁸F) even immediately after the end of bombardment.ConclusionsThis study demonstrated the radionuclidic purity of [¹⁸F]FMCH according to the EU Pharmacopeia.