D-[6-13C]glucose - CAS 106032-62-6
Molecular Formula:
13CC5H12O6
Molecular Weight:
181.15
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Tag:
13C-labelled Carbohydrates
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1.13C-phenylalanine breath test detects altered phenylalanine kinetics in schizophrenia patients.
Teraishi T1, Ozeki Y, Hori H, Sasayama D, Chiba S, Yamamoto N, Tanaka H, Iijima Y, Matsuo J, Kawamoto Y, Kinoshita Y, Hattori K, Ota M, Kajiwara M, Terada S, Higuchi T, Kunugi H. Transl Psychiatry. 2012 May 22;2:e119. doi: 10.1038/tp.2012.48.
Phenylalanine is an essential amino acid required for the synthesis of catecholamines including dopamine. Altered levels of phenylalanine and its metabolites in blood and cerebrospinal fluid have been reported in schizophrenia patients. This study attempted to examine for the first time whether phenylalanine kinetics is altered in schizophrenia using L-[1-(13)C]phenylalanine breath test ((13)C-PBT). The subjects were 20 chronically medicated schizophrenia patients (DSM-IV) and the same number of age- and sex-matched controls. (13)C-phenylalanine (99 atom% (13)C; 100 mg) was administered orally and the breath (13)CO(2) /(12)CO(2) ratio was monitored for 120 min. The possible effect of antipsychotic medication (risperidone (RPD) or haloperidol (HPD) treatment for 21 days) on (13)C-PBT was examined in rats. Body weight (BW), age and diagnostic status were significant predictors of the area under the curve of the time course of Δ(13)CO(2) (‰) and the cumulative recovery rate (CRR) at 120 min.
2.Bacteria and fungi respond differently to multifactorial climate change in a temperate heathland, traced with 13C-glycine and FACE CO2.
Andresen LC1, Dungait JA2, Bol R3, Selsted MB4, Ambus P4, Michelsen A1. PLoS One. 2014 Jan 15;9(1):e85070. doi: 10.1371/journal.pone.0085070. eCollection 2014.
It is vital to understand responses of soil microorganisms to predicted climate changes, as these directly control soil carbon (C) dynamics. The rate of turnover of soil organic carbon is mediated by soil microorganisms whose activity may be affected by climate change. After one year of multifactorial climate change treatments, at an undisturbed temperate heathland, soil microbial community dynamics were investigated by injection of a very small concentration (5.12 µg C g(-1) soil) of (13)C-labeled glycine ((13)C2, 99 atom %) to soils in situ. Plots were treated with elevated temperature (+1°C, T), summer drought (D) and elevated atmospheric carbon dioxide (510 ppm [CO2]), as well as combined treatments (TD, TCO2, DCO2 and TDCO2). The (13)C enrichment of respired CO2 and of phospholipid fatty acids (PLFAs) was determined after 24 h. (13)C-glycine incorporation into the biomarker PLFAs for specific microbial groups (Gram positive bacteria, Gram negative bacteria, actinobacteria and fungi) was quantified using gas chromatography-combustion-stable isotope ratio mass spectrometry (GC-C-IRMS).
3.Tracking the flow of bacterially derived 13C and 15N through soil faunal feeding channels.
Crotty FV1, Blackshaw RP, Murray PJ. Rapid Commun Mass Spectrom. 2011 Jun 15;25(11):1503-13. doi: 10.1002/rcm.4945.
The soil food web has been referred to as a 'black box', a 'poor man's tropical rainforest' and an 'enigma', due to its opacity, diversity and the limited insight into feeding specificity. Here we investigate the flow of C and N through the soil food web as a way to gain understanding of the feeding interactions occurring. A bacterium, Pseudomonas lurida, was introduced to soil cores from two different habitats, a grassland and a woodland with the same soil type, enriched to 99 atom% in (13)C and (15)N, to trace the flow of bacterial C and N through the soil food web. Throughout the experiment the soil remained enriched in (13)C and (15)N. Almost all the invertebrates tested gained C and N enrichment indicative of the labelled bacteria, implying that bacterial feeding is a common mechanism within the soil. Only three groups were significantly enriched in both (13)C and (15)N in both habitats. These were Collembola (Entomobryomorpha), Acari (Oribatida), and Nematoda, indicating that these organisms are consuming the most bacteria within both systems.
4.Determination of 13C isotopic enrichment of glutathione and glycine by gas chromatography/combustion/isotope ratio mass spectrometry after formation of the N- or N,S-ethoxycarbonyl methyl ester derivatives.
Tea I1, Ferchaud-Roucher V, Küster A, Darmaun D, Robins RJ. Rapid Commun Mass Spectrom. 2007;21(20):3245-52.
The depletion of glutathione (GSH) reported in very-low-birth-weight infants is implicated in several pathologies, especially if deficiency occurs during foetal development. The cause of this depletion is suggested to be modification of GSH turnover. To probe the role of GSH, a reliable non-invasive method adapted to very-low-birth-weight infants is required. In this paper, we report the preparation of the N,S-ethoxycarbonyl methyl ester derivatives of GSH and glycine and their application to the measurement of (13)C/(12)C ratios at natural abundance in erythrocyte samples by gas chromatography/combustion/isotope ratio mass spectrometry (GC/C/IRMS). The technique allowed the determination of (13)C/(12)C ratios at natural abundance with a precision <3% and within-day and between-day variabilities both <4%. The method is able to determine accurately low (13)C-enrichments in GSH (0.00241 to 0.00753 Atom Percent Excess) in erythrocyte extracts following incubation with (13)C-glycine at low specific enrichment (approx.
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CAS 106032-62-6 D-[6-13C]glucose

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