Bias in carbon concentration and δ13C measurements of organic matter due to cleaning treatments with organic solvents
Interpreting the organic carbon content (TOC) and stable carbon isotopic composition (δ13C) of organic matter in the sedimentary rock record depends on our capability to accurately measure them, while excluding sources of contamination. This however becomes increasingly problematic as we analyze sam...
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Veröffentlicht in: | Chemical geology 2018-08, Vol.493, p.405-412 |
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Sprache: | eng |
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