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- W2022132363 abstract "Systematic variations in the 13C contents of individual extractable n-alkanes (C16–C29) can be modelled quantitatively and interpreted as indicating contributions from at least five distinct sources. These appear to be cyanobacterial (C16–C18, δ13C = − 37000vs PDB), phytoplanktonic C16–C23, δ = −32000), chemoautotrophic bacterial (C20–C29, δ = −38000), phytoplanktonic or heterotrophic bacterial (C20–C29, δ = −30‰), and vascular plants (C23–C29, δ = −29‰). Hydrous pyrolysis of related kerogens yields large quantities of additional n-alkanes with different and much more uniform δ values. The latter materials are apparently derived from the thermolysis of aliphatic biopolymers whose presence in the Green River Oil Shale has been recognized visually." @default.
- W2022132363 created "2016-06-24" @default.
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- W2022132363 date "1994-06-01" @default.
- W2022132363 modified "2023-10-02" @default.
- W2022132363 title "Partial resolution of sources of n-alkanes in the saline portion of the Parachute Creek Member, Green River Formation (Piceance Creek Basin, Colorado)" @default.
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- W2022132363 doi "https://doi.org/10.1016/0146-6380(94)90010-8" @default.
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