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  • Reactive oxygen species  (4)
  • Inorganic Chemistry  (3)
  • 306-U1313; AGE; Cibicidoides mundulus, δ13C; Cibicidoides mundulus, δ18O; Cibicidoides sp., δ13C; Cibicidoides sp., δ18O; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Exp306; Integrated Ocean Drilling Program / International Ocean Discovery Program; Intercore correlation; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 252; North Atlantic Climate 2; Sample code/label; Uvigerina sp., δ13C; Uvigerina sp., δ18O  (2)
  • Lung surfactant secretion
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Keywords
  • 1
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Biochimica et Biophysica Acta (BBA)/Biomembranes 939 (1988), S. 449-458 
    ISSN: 0005-2736
    Keywords: (Rat lung) ; Fluorescent probe ; Lung surfactant secretion ; Sodium ion/proton antiport ; Type II cell ; pH, intracellular
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology , Chemistry and Pharmacology , Medicine , Physics
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Biochimica et Biophysica Acta (BBA)/Biomembranes 902 (1987), S. 317-326 
    ISSN: 0005-2736
    Keywords: (Rat lung) ; Carbocyanine dye ; Lung surfactant secretion ; Terbutaline ; Tetradecanoylphorbol acetate ; Tetraphenylmethylphosphonium ion ; Transmembrane potential ; Type II cell
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology , Chemistry and Pharmacology , Medicine , Physics
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Berichte der deutschen chemischen Gesellschaft 107 (1974), S. 3818-3834 
    ISSN: 0009-2940
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Systematic Investigations on the Behaviour of Organotin Compounds toward. Liquid Sulfur Dioxide, VII. Cleavage of Tin-Oxygen Bond with So2The hexaorganodistannoxanes 1a and b react with SO2 to yield bis(triorganotin) sulfites 2a, b. At higher temperatures, a disproportionation takes place yielding the sulfinates 3a, b resp. 5a, b and diorganotin sulfites 4a, b; possible reaction mechanisms are discussed. As by-products result the sulfates 6a and 8a as well as the thioester 7a. Triorganotin hydroxides 10a-c react in the same way. 4a-c are also obtained by addition of SO2 to diorganotin oxides 9a-c. The triorganotin alkoxides and phenoxides 11 and 13 add 1 mole of SO2 yielding the very sensitive triorganotin organylsulfites of which only 12 could be isolated. The constitution of the newly prepared compounds has been established by means of their i.r. and 1H n.m.r. spectra.
    Notes: Die Hexaorganodistannoxane 1a und b reagieren mit SO2 unter milden Bedingungen zu den Bis(triorganozinn)-sulfiten 2a, b. Bei höheren Temperaturen erfolgt dagegen eine Disproportionierung zu den Sulfinaten 3a, b bzw. 5a, b und Diorganozinn-sulfiten 4a, b; mögliche Reaktionsmechanismen werden diskutiert. Als Nebenprodukte entstehen die Sulfate 6a und 8a sowie der Thioester 7a. Analog verhalten sich die Triorganozinn-hydroxide 10a-c. 4a-c erhält man auch durch Addition von SO2 an Diorganozinn-oxide 9a-c. Die Triorganozinn-alkoxide und -phenoxide 11 und 13 addieren 1 mol SO2 unter Bildung der sehr hydrolyseempfindlichen Triorganozinn-organylsulfite, von denen nur 12 isoliert werden konnte. Die Konstitution der neu dargestellten Verbindungen wurde mit Hilfe ihrer IR- und 1H-NMR-Spektren gesichert.
    Additional Material: 4 Tab.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Berichte der deutschen chemischen Gesellschaft 94 (1961), S. 392-397 
    ISSN: 0009-2940
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: Tertiäre aromatische sowie aliphatisch- bzw. cycloaliphatisch-aromatische Phosphine reagieren mit Kalium oder Natrium unter Abspaltung eines Aryl oder Alkylrestes und Bildung von Alkaliphosphiden des Typs MePR2 bzw. MePRR'. Für eine Spaltungsreaktion ist die Anwesenheit eines aromatischen Restes im tert. Phosphin Voraussetzung. Während sich tert. aliphatische und cycloaliphatische Phosphine gegenüber Kalium indifferent verhalten, liefert bei analoger Reaktion beispielsweise Diäthylphenylphosphin Kalium-äthyl-phenyl-phosphid. Die Alkali-phosphide sind sehr reaktionsfähig und dienen zur Synthese weiterer phosphororganischer Verbindungen. Sie liefern bei der oxydativen Hydrolyse die entsprechenden Phosphinsäuren und mit Alkylhalogeniden Phosphoniumsalze.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 0044-2313
    Keywords: Silanediyldiphosphinite ; chelate complexes ; synthesis ; structure, multinuclear NMR spectroscopy ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Synthese eines neuen Silandiyldiphosphinits tBu2Si(OPPh2)2 und seine Reaktionen mit den Norbornadien-Komplexen C7H8M(CO)4 (M = Cr, Mo, W). Kristallstrukturen von cis-M(CO)4[tBu2Si(OPPh2)2] (M = Cr, Mo)Silandiyldiphosphinit tBu2Si(OPPh2)2 1 wurde dargestellt. 1 reagiert mit den Norbornadienkomplexen C7H8M(CO)4 (M = Cr, Mo, W) zu sechsgliedrigen Chelaten des Typs cis-M(CO)4[tBu2Si(OPPh2)2] 2-4. Die Kristallstrukturen des Chromkomplexes Cr(CO)4[tBuSi(OPPh2)2] 2 und des Molybdänkomplexes Mo(CO)4[tBuSi(OPPh2)2] 3 wurden bestimmt. Beide kristallisieren triklin (Raumgruppe P1) mit den Zellkonstanten: (2) a = 1 093(3) pm, b = 1 477(5) pm und c = 1 542(5) pm; α = 108.4(2)°, b̃ = 103.87(11)° und b̃ = 104.57(10)°; U = 2.143(12) nm3; Z = 2; (3) a = 1097.8(2) pm, b = 1 483.7(2) pm und c = 1 554.3(2) pm; α = 108.10(1)°, b̃ = 103.956(6)° und γ = 104.213(7)°; U = 2.1899(6) nm3; Z = 2. Beide Komplexe bestehen aus diskreten, leicht verdrillten oktaedrischen Monomeren mit annähernd planaren Chelatringen. Im Gegensatz hierzu wurde bei den Röntgenstrukturanalysen verwandter Komplexe Konformationen ermittelt, die von Twistboot zu „Chaiselongue“ variieren.
    Notes: Silanediyldiphosphinite tBu2Si(OPPh2)2 1 has been synthesised. 1 reacts with the norbornadiene complexes C7H8M(CO)4 (M = Cr, Mo, W) to give six-membered chelate rings of the type cis-M(CO)4[tBu2Si(OPPh2)2] 2-4. The crystal structures of the chromium and molybdenum complexes cis-Cr(CO)4[tBu2Si(OPPh2)2] 2 and cis-Mo(CO)4[tBu2Si(OPPh2)2] 3 have been determined. Both complexes crystallise in the triclinic system (space group P1) with unit cell parameters: (2) a = 1 093(3) pm, b = 1 477(5) pm and c = 1 542(5) pm; α = 108.4(2)°, b̃ = 103.87(11)° and b̃ = 104.57(10)°; U = 2.143(12) nm3; Z = 2; (3) a = 1 097.8(2) pm, b = 1 483.7(2) pm and c = 1 554.3(2) pm; α = 108.10(1)°, b̃ = 103.956(6)° and γ = 104.213(7)°; U = 2.1899(6) nm3; Z = 2. Both 2 and 3 consist of discrete, slightly distorted, octahedral monomers in which the six-membered chelate rings are essentially planar. In contrast, the conformations of the chelate rings found in crystal structures of analogous complexes vary from twist-boat to “chaise longue”.
    Additional Material: 1 Ill.
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  • 6
    Publication Date: 2024-03-02
    Keywords: 306-U1313; AGE; Cibicidoides mundulus, δ13C; Cibicidoides mundulus, δ18O; Cibicidoides sp., δ13C; Cibicidoides sp., δ18O; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Exp306; Integrated Ocean Drilling Program / International Ocean Discovery Program; Intercore correlation; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 252; North Atlantic Climate 2; Sample code/label; Uvigerina sp., δ13C; Uvigerina sp., δ18O
    Type: Dataset
    Format: text/tab-separated-values, 2672 data points
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  • 7
    Publication Date: 2024-03-02
    Keywords: 306-U1313; AGE; Cibicidoides mundulus, δ13C; Cibicidoides mundulus, δ18O; Cibicidoides sp., δ13C; Cibicidoides sp., δ18O; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Exp306; Integrated Ocean Drilling Program / International Ocean Discovery Program; Intercore correlation; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 252; North Atlantic Climate 2; Sample code/label; Uvigerina sp., δ13C; Uvigerina sp., δ18O
    Type: Dataset
    Format: text/tab-separated-values, 2672 data points
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  • 8
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 4 (2013): 262, doi:10.3389/fmicb.2013.00262.
    Description: Manganese (Mn) oxides are among the most reactive sorbents and oxidants within the environment, where they play a central role in the cycling of nutrients, metals, and carbon. Recent discoveries have identified superoxide (O−2) both of biogenic and abiogenic origin as an effective oxidant of Mn(II) leading to the formation of Mn oxides. Here we examined the conditions under which abiotically produced superoxide led to oxidative precipitation of Mn and the solid-phases produced. Oxidized Mn, as both aqueous Mn(III) and Mn(III/IV) oxides, was only observed in the presence of active catalase, indicating that hydrogen peroxide (H2O2), a product of the reaction of O−2 with Mn(II), inhibits the oxidation process presumably through the reduction of Mn(III). Citrate and pyrophosphate increased the yield of oxidized Mn but decreased the amount of Mn oxide produced via formation of Mn(III)-ligand complexes. While complexing ligands played a role in stabilizing Mn(III), they did not eliminate the inhibition of net Mn(III) formation by H2O2. The Mn oxides precipitated were highly disordered colloidal hexagonal birnessite, similar to those produced by biotically generated superoxide. Yet, in contrast to the large particulate Mn oxides formed by biogenic superoxide, abiotic Mn oxides did not ripen to larger, more crystalline phases. This suggests that the deposition of crystalline Mn oxides within the environment requires a biological, or at least organic, influence. This work provides the first direct evidence that, under conditions relevant to natural waters, oxidation of Mn(II) by superoxide can occur and lead to formation of Mn oxides. For organisms that oxidize Mn(II) by producing superoxide, these findings may also point to other microbially mediated processes, in particular enzymatic hydrogen peroxide degradation and/or production of organic ligand metabolites, that allow for Mn oxide formation.
    Description: This project was supported by the National Science Foundation, grants EAR-1245919/1025077 (awarded to Colleen M. Hansel and Bettina M. Voelker), and by the Radcliffe Institute for Advanced Study at Harvard University (through a fellowship to Bettina M. Voelker).
    Keywords: Manganese oxidation ; Manganese oxides ; Superoxide ; Reactive oxygen species ; Mn(III) complexes ; Organic ligands
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 9
    Publication Date: 2022-05-25
    Description: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Chemistry 4 (2016): 5, doi:10.3389/fchem.2016.00005.
    Description: Biological production and decay of the reactive oxygen species (ROS) hydrogen peroxide (H2O2) and superoxide (O−2) likely have significant effects on the cycling of trace metals and carbon in marine systems. In this study, extracellular production rates of H2O2 and O−2 were determined for five species of marine diatoms in the presence and absence of light. Production of both ROS was measured in parallel by suspending cells on filters and measuring the ROS downstream using chemiluminescence probes. In addition, the ability of these organisms to break down O−2 and H2O2 was examined by measuring recovery of O−2 and H2O2 added to the influent medium. O−2 production rates ranged from undetectable to 7.3 × 10−16 mol cell−1 h−1, while H2O2 production rates ranged from undetectable to 3.4 × 10−16 mol cell−1 h−1. Results suggest that extracellular ROS production occurs through a variety of pathways even amongst organisms of the same genus. Thalassiosira spp. produced more O−2 in light than dark, even when the organisms were killed, indicating that O−2 is produced via a passive photochemical process on the cell surface. The ratio of H2O2 to O−2 production rates was consistent with production of H2O2 solely through dismutation of O−2 for T. oceanica, while T. pseudonana made much more H2O2 than O−2. T. weissflogii only produced H2O2 when stressed or killed. P. tricornutum cells did not make cell-associated ROS, but did secrete H2O2-producing substances into the growth medium. In all organisms, recovery rates for killed cultures (94–100% H2O2; 10–80% O−2) were consistently higher than those for live cultures (65–95% H2O2; 10–50% O−2). While recovery rates for killed cultures in H2O2 indicate that nearly all H2O2 was degraded by active cell processes, O−2 decay appeared to occur via a combination of active and passive processes. Overall, this study shows that the rates and pathways for ROS production and decay vary greatly among diatom species, even between those that are closely related, and as a function of light conditions.
    Description: This research was supported by NSF grant OCE-1131734/1246174 to BV and CH.
    Keywords: Reactive oxygen species ; Superoxide ; Hydrogen peroxide ; Diatoms ; Culture
    Repository Name: Woods Hole Open Access Server
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  • 10
    Publication Date: 2022-10-26
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Bond, R. J., Hansel, C. M., & Voelker, B. M. Heterotrophic bacteria exhibit a wide range of rates of extracellular production and decay of hydrogen peroxide. Frontiers in Marine Science, 7, (2020): 72, doi:10.3389/fmars.2020.00072.
    Description: Bacteria have been implicated as both a source and sink of hydrogen peroxide (H2O2), a reactive oxygen species which can both impact microbial growth and participate in the geochemical cycling of trace metals and carbon in natural waters. In this study, simultaneous H2O2 production and decay by twelve species of heterotrophic bacteria were evaluated in both batch and flow-through incubations. While wide species-to-species variability of cell-normalized H2O2 decay rate coefficients [2 × 10–8 to 5 × 10–6 hr–1 (cell mL–1)–1] was observed, these rate coefficients were relatively consistent for a given bacterial species. By contrast, observed production rates (below detection limit to 3 × 102 amol cell–1 hr–1) were more variable even for the same species. Variations based on incubation conditions in some bacterial strains suggest that external conditions may impact extracellular H2O2 levels either through increased extracellular production or leakage of intracellular H2O2. Comparison of H2O2 production rates to previously determined superoxide (O2–) production rates suggests that O2– and H2O2 production are not necessarily linked. Rates measured in this study indicate that bacteria could account for a majority of H2O2 decay observed in aqueous systems but likely only make a modest contribution to dark H2O2 production.
    Description: This research was supported by NSF grant OCE-1131734/1246174 to BV and CH.
    Keywords: Reactive oxygen species ; Hydrogen peroxide ; Heterotrophic bacteria ; H2O2 production ; H2O2 decomposition
    Repository Name: Woods Hole Open Access Server
    Type: Article
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