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  • 1
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    PANGAEA
    In:  Supplement to: Requejo, A G; Whelan, Jean K; Boehm, Paul D (1986): Hydrocarbon geochemistry and biological markers in Orca and Pigmy Basin sediments (Sites 618 and 619). In: Bouma, AH; Coleman, JM; Meyer, AW; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 96, 785-793, https://doi.org/10.2973/dsdp.proc.96.150.1986
    Publication Date: 2023-06-27
    Description: The C15+ hydrocarbon geochemistry of sediments from Sites 618 and 619 (Orca and Pigmy basins) has been examined as part of a biogeochemical study of microbial activity and biological markers in Leg 96 sediments. Total hydrocarbon concentrations (13-78 µg/g dry weight) are elevated in comparison to those reported for Recent sediments from the Gulf of Mexico continental shelf, but there is little evidence that these sediments contain petroleum hydrocarbons originating from seepage. The presence of weathered fossil hydrocarbons is suggested, however, by the unresolved envelope feature observed in gas chromatograms of most sediments and also by the distribution of C27-C29 steranes and triterpanes. Normal alkane distributions are consistent with a predominant input or preservation of terrestrial organic matter in these offshore basins. At Site 619 an enhanced terrestrial contribution below 113 m sub-bottom is indicated by an increase in the ratio of odd to even n-alkanes over the range C26 to C30. Pristane/phytane ratios at both sites range between 0.97 and 1.74 which, in conjunction with the occurrence of significant concentrations of perylene (10-500 ng/g dry weight), suggest the prevalence of reducing depositional conditions over the time period covered by the cores. A hydrocarbon tentatively identified as a C25 multibranched compound similar to those found in Recent sediments was detected in most samples.
    Keywords: 96-618; 96-618A; 96-619; Carbon, organic, total; Deep Sea Drilling Project; DEPTH, sediment/rock; DOC/DON high temperature catalytic combustion; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Gas chromatography; Glomar Challenger; Gulf of Mexico; Gulf of Mexico/BASIN; Hydrocarbons; Index; Latitude of event; Leg96; Longitude of event; n-C17/n-C29 ratio; Odd-even predominance index; Organic matter, extractable; Perylene; Pristane/Phytane ratio; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 181 data points
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 28 (1994), S. 1-15 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1520-5029
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The Western Canada and Williston basins contain source beds which have generated large quantities of oil and gas15. Remarkably, pyrolysates of the high-molecular-weight fractions of the Palaeozoic sediments and oils contain high abundances of 1,2,3,4-tetramethylbenzene (TMB, I in Fig. 1). This is ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 342 (1989), S. 670-673 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] We have analysed several tar-sand samples from the Miocene Pt Arena (Monterey) Formation in the Pt Arena Basin, California. Tar-stained sandstones are distributed throughout siliceous organic mudstones exposed at several locations along the northern California coastline. The thickest continuous ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 373 (1995), S. 293-294 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] HARTGERS ET AL. REPLY - Head et al. argue that heterotrophic bacterial biomass production in both the water column4'5 and surface sediments3 is important. We agree. However, this by no means implies that bacterial carbon will be ultimately preserved. Organic matter preserved in sediments ...
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract We used a research submersible to obtain 33 sediment samples from chemosynthetic communities at 541–650 m water depths in the Green Canyon (GC) area of the Gulf of Mexico slope. Sediment samples from beneath an isolated mat of H2S-oxidizing bacteria at GC 234 contain oil (mean = 5650 ppm) and C1–C5 hydrocarbons (mean = 12,979 ppm) that are altered by bacterial oxidation. Control cores away from the mat contain lower concentrations of oil (mean = 2966 ppm) and C1–C5 hydrocarbons (mean = 83.6 ppm). Bacterial oxidation of hydrocarbons depletes O2 in sediments and triggers bacterial sulfate reduction to produce the H2S required by the mats. Sediment samples from GC 185 (Bush Hill) contain high concentrations of oil (mean = 24,775 ppm) and C1–C5 hydrocarbons (mean = 11,037 ppm) that are altered by bacterial oxidation. Tube worm communities requiring H2S occur at GC 185 where the sea floor has been greatly modified since the Pleistocene by accumulation of oil, thermogenic gas hydrates, and authigenic carbonate rock. Venting to the water column is suppressed by this sea-floor modification, enhancing bacterial activity in sediments. Sediments from an area with vesicomyid clams (GC 272) contain lower concentrations of oil altered by bacterial oxidation (mean = 1716 ppm) but C1–C5 concentrations are high (mean = 28,766 ppm). In contrast to other sampling areas, a sediment associated with the methanotrophic Seep Mytilid I (GC 233) is characterized by low concentration of oil (82 ppm) but biogenic methane (C1) is present (8829 ppm).
    Type of Medium: Electronic Resource
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