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Lookup NU author(s): Dr Richard Tyson
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Bulk geochemical data from the NERC Rapid Global Geological Events project are used to appraise the pattern of variation in mean organic content through the cymodoce to rotunda zones of the type Kimmeridge Clay Formation in southern Dorset. There is a symmetrical stratigraphic pattern in mean and modal total organic carbon (TOC) values, which increase from 1-2% at the top and base to a peak of 8-9% in the middle of the formation. To remove distortion caused by the strong positive skewness of the TOC values, the mean TOC per zone was recalculated for the first mode of the TOC distribution only, and combined pragmatically with pyrolysis estimates of the reactive (marine) TOC fraction to derive marine TOC values; these also vary symmetrically from c. 0.5% to peak values of c. 5.0%. The mean TOC is negatively correlated with sedimentation rate, indicating that dilution is a significant controlling variable. Mean palaeoproductivity was assessed using modern marine sediment relationships between carbon burial efficiency, sedimentation rate (derived from RGGE cyclostratigraphic analyses), the likely dissolved oxygen range, and water depth. Best estimates of palaeoproductivity range from 40 to 150 g Cm-2 a-1 (low to moderate by comparison with present-day shelves) and are positively but nonlinearly correlated with mean δ13 CTOC values.
Author(s): Tyson RV
Publication type: Article
Publication status: Published
Journal: Journal of the Geological Society
Year: 2004
Volume: 161
Issue: 4
Pages: 667-673
Print publication date: 01/07/2004
ISSN (print): 0016-7649
ISSN (electronic):
Publisher: Geological Society Publishing House
URL: http://dx.doi.org/10.1144/0016-764903-078
DOI: 10.1144/0016-764903-078
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