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    Molecular, Radioactive and Stable Isotope Characterization of Estuarine Particulate Organic Matter

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    Author
    Megens, Luc
    van der Plicht, Johannes
    D Leeuw, J. W.
    Issue Date
    1998-01-01
    Keywords
    Ems Dollard Estuary
    suspended materials
    particulate materials
    gas chromatograms
    estuarine environment
    pyrolysis
    total organic carbon
    North Sea
    fatty acids
    lipids
    Atlantic Ocean
    North Atlantic
    marine environment
    Germany
    mass spectra
    spectra
    organic acids
    isotope ratios
    Central Europe
    Netherlands
    organic compounds
    Europe
    Western Europe
    sediments
    C 14
    carbon
    isotopes
    radioactive isotopes
    C 13 C 12
    stable isotopes
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    Citation
    Megens, L., van der Plicht, J., & De Leeuw, J. W. (1998). Molecular, radioactive and stable carbon isotope characterization of estuarine particulate organic matter. Radiocarbon, 40(2), 985-990.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 16th International Radiocarbon Conference held in Gronigen, Netherlands, June 16-20, 1997.
    URI
    http://hdl.handle.net/10150/654535
    DOI
    10.1017/S0033822200018956
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Organic matter in sediments and suspended matter is a complex mixture of constituents with different histories, sources and stabilities. To study these components in a suspended matter sample from the Ems-Dollard Estuary, we used combined molecular analysis with pyrolysis/gas chromatography/mass spectrometry and stable and radioactive carbon isotope analyses of the bulk and separated chemical fractions. Carbohydrates and proteins, ca. 50% of the total organic carbon (TOC), are much younger than the bulk sample and have a somewhat higher delta-13C value. Lipids and the final residue are considerably older and have lower delta-13C values. The final residue, ca. 17% of the total carbon, consists mainly of aliphatic macromolecules that could be derived from algae or terrestrial plants. The delta-13C value points to a marine origin.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200018956
    Scopus Count
    Collections
    Radiocarbon, Volume 40, Number 2 (1998)

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