Browsing ELibrary by Author "Freeman K.H."
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Browsing ELibrary by Author "Freeman K.H."
Now showing items 1-7 of 7
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Joachimski M.M.; Pancost R.D.; Freeman K.H.; Ostertag-Henning C.; Buggisch W. (2002)Carbon isotope records for inorganic and total organic carbon (TOC) as well as for individual organic biomarkers show two positive excursions in the Late Frasnian with comparable shape and amplitude in δ13C. The positive ...
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Pedentchouk N.; Freeman K.H.; Harris N.B. (2006)This study investigates the extent of post-depositional alteration of δD values of n-alkyl lipids, isoprenoids, and kerogen isolated from a continuous 450 m core that covers the transition from thermally immature to early ...
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Dias R.F.; Freeman K.H.; Franks S.G. (2002)A new GC-Pyrolysis-IRMS method was developed for the δ13C determination of carboxyl carbon in low-molecular weight organic acids. By utilizing a palladium-wire reactor at 600<space>°C with a helium/hydrogen reactant gas, ...
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Smith F.A.; Freeman K.H. (2006)We measured hydrogen isotope compositions (δD) of high-molecular-weight n-alkanes (C27-C33) from grasses grown in greenhouses and collected from the US Great Plains. In both cases, n-alkanes from C4 grasses are enriched ...
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Pagani M.; Freeman K.H.; Arthur M.A. (2000)Carbon-isotope compositions of n-alkanes, pristane and phytane, and total organic carbon were measured and compared against isotopic trends of coeval alkadienones from Miocene sediments containing very low organic-carbon ...
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Freeman K.H. (2001)The ocean accounts for over 90% of the active pools of carbon on the Earth’s surface, with over 95% of marine carbon in the form of dissolved inorganic carbon (DIC) (Hedges and Keil 1995). Organic carbon dissolved in the ...
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Dias R.F.; Freeman K.H.; Lewan M.D.; Franks S.G. (2002)Low-molecular-weight (LMW) aqueous organic acids were generated from six oil-prone source rocks under hydrous-pyrolysis conditions. Differences in total organic carbon-normalized acid generation are a function of the initial ...
Now showing items 1-7 of 7
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