A review of nitrogen isotopic alteration in marine sediments

Nitrogen isotopes are an important tool for evaluating past biogeochemical cycling from the paleoceanographic record. However, bulk sedimentary nitrogen isotope ratios, which can be determined routinely and at minimal cost, may be altered during burial and early sedimentary diagenesis, particularly...

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Veröffentlicht in:	Paleoceanography 2012-12, Vol.27 (4), p.np-n/a
Hauptverfasser:	Robinson, Rebecca S., Kienast, Markus, Luiza Albuquerque, Ana, Altabet, Mark, Contreras, Sergio, De Pol Holz, Ricardo, Dubois, Nathalie, Francois, Roger, Galbraith, Eric, Hsu, Ting-Chang, Ivanochko, Tara, Jaccard, Samuel, Kao, Shuh-Ji, Kiefer, Thorsten, Kienast, Stephanie, Lehmann, Moritz, Martinez, Philippe, McCarthy, Matthew, Möbius, Jürgen, Pedersen, Tom, Quan, Tracy M., Ryabenko, Evgeniya, Schmittner, Andreas, Schneider, Ralph, Schneider-Mor, Aya, Shigemitsu, Masahito, Sinclair, Dan, Somes, Christopher, Studer, Anja, Thunell, Robert, Yang, Jin-Yu
Format:	Artikel
Sprache:	eng
Schlagworte:	Biogeochemical cycles Biogeochemistry Continental margins Diagenesis Geobiology isotopic alteration Marine Marine sediments Nitrogen Ocean floor Oceanography organic matter diagenesis Scientific apparatus & instruments sediment trap δ15N database sedimentary N isotopes Water depth
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