First indications of the formation of kerogen amorphous fractions by selective preservation. Role of non-hydrolysable macromolecular constituents of Eubacterial cell walls
- 31 December 1994
- journal article
- Published by Elsevier in Organic Geochemistry
- Vol. 22 (3-5) , 759-IN12
- https://doi.org/10.1016/0146-6380(94)90137-6
Abstract
No abstract availableThis publication has 22 references indexed in Scilit:
- Mechanisms of flash pyrolysis of ether lipids isolated from the green microalga Botryococcus braunii race AJournal of Analytical and Applied Pyrolysis, 1993
- Occurrence of non-hydrolysable amides in the macromolecular constituent of Scenedesmus quadricauda cell wall as revealed by 15N NMR: Origin of n-alkylnitriles in pyrolysates of ultralaminae-containing kerogensGeochimica et Cosmochimica Acta, 1993
- Formation of ultralaminae in marine kerogens via selective preservation of thin resistant outer walls of microalgaeOrganic Geochemistry, 1992
- Structure of Chlorella fusca algaenan: relationships with ultralaminae in lacustrine kerogens; species- and environment-dependent variations in the composition of fossil ultralaminaeOrganic Geochemistry, 1992
- Non-hydrolysable macromolecular constituents from outer walls of Chlorella fusca and Nanochlorum eucaryotumPhytochemistry, 1992
- Organic Matter in the Early Toarcian Shales, Paris Basin, France: a Response to Environmental ChangesRevue de l'Institut Français du Pétrole, 1991
- Chemical evidence of kerogen formation in source rocks and oil shales via selective preservation of thin resistant outer walls of microalgae: Origin of ultralaminaeGeochimica et Cosmochimica Acta, 1991
- Origin of Messel Oil Shale kerogenNature, 1988
- Geochemical significance of lipids and lipid-derived substructures interlaced in kerogenOrganic Geochemistry, 1988
- Chemistry and petrography of the Marl Slate of S. E. Durham, EnglandEconomic Geology, 1963