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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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isoprenoids
Chemometric identification of crude oil families and deconvolution of mixtures in the surrounding Niuzhuang sag, Bohai Bay Basin, China
Hydrocarbon Molecular Markers as Indicators of the Late Cenozoic Sedimentation on the Amerasian Continental Margin (Arctic Ocean)
Source-rock reservoirs geochemistry of Devonian–Mississippian mudrocks in central Oklahoma
Geochemical characterization of the Upper Mississippian Goddard Formation, Noble Ranch Group, and related oils in the Anadarko Basin of Oklahoma
Oil retention and intrasource migration in the organic-rich lacustrine Chang 7 shale of the Upper Triassic Yanchang Formation, Ordos Basin, central China
Hydrocarbon migration in the multiple-sourced petroleum system in the northwestern Junggar Basin (northwestern China): Constraint from geochemical and phase fractionation analysis
Integrating heavy-mineral, geochemical and biomarker analyses of Plio-Pleistocene sandy and silty turbidites: a novel approach for provenance studies (Indus Fan, IODP Expedition 355)
How marine incursion influences the quality of lacustrine source rocks: The Paleogene Nanxiang Basin, eastern China
Recycling of archaeal biomass as a new strategy for extreme life in Dead Sea deep sediments
Geochemically distinct oil families in the onshore and offshore Santa Maria basins, California
Ahdeb oil field, Mesopotamian Basin, Iraq: Reservoir architecture and oil charge history
Organic geochemistry of the Eagle Ford Group in Texas
The development and extent of photic-zone euxinia concomitant with Woodford Shale deposition
AMBER EMBALMS ESSENTIAL OILS: A RARE PRESERVATION OF MONOTERPENOIDS IN FOSSIL RESINS FROM EASTERN HIMALAYA
The invasive diatom Pseudosolenia calcar-avis and specific C 25 isoprenoid lipids as a sedimentary time marker in the Black Sea
Hydrocarbon potential of the Lower Cretaceous mudstones in coastal southeastern China
The isotopic structures of geological organic compounds
Abstract: Organic compounds are ubiquitous in the Earth’s surface, sediments and many rocks, and preserve records of geological, geochemical and biological history; they are also critical natural resources and major environmental pollutants. The naturally occurring stable isotopes of volatile elements (D, 13 C, 15 N, 17,18 O, 33,34,36 S) provide one way of studying the origin, evolution and migration of geological organic compounds. The study of bulk stable isotope compositions (i.e. averaged across all possible molecular isotopic forms) is well established and widely practised, but frequently results in non-unique interpretations. Increasingly, researchers are reading the organic isotopic record with greater depth and specificity by characterizing stable isotope ‘structures’ – the proportions of site-specific and multiply substituted isotopologues that contribute to the total rare-isotope inventory of each compound. Most of the technologies for measuring stable isotope structures of organic molecules have been only recently developed and to date have been applied only in an exploratory way. Nevertheless, recent advances have demonstrated that molecular isotopic structures provide distinctive records of biosynthetic origins, conditions and mechanisms of chemical transformation during burial, and forensic fingerprints of exceptional specificity. This paper provides a review of this young field, which is organized to follow the evolution of molecular isotopic structure from biosynthesis, through diagenesis, catagenesis and metamorphism.