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• W2102474137 abstract "Ar39 Ar age for the basal Berriasian suggest that the duration of the Kimmeridgian and Tithonian were nominally ~650 k.y. shorter than previously determined. The Re-Os data for the Staffin black shale indicates that the seawater Os isotope composition at the Oxfordian/Kimmeridgian boundary was radiogenic ( 187 Os/ 188 Os = 0.53), similar to that for the Early Tithonian, but much higher than the Late Callovian ( 187 Os/ 188 Os = 0.27). These Os isotope compositions suggest that the rate of continental weathering had increased from the Callovian to Kimmeridgian/Tithonian." @default.
• W2102474137 created "2016-06-24" @default.
• W2102474137 creator A5081959981 @default.
• W2102474137 date "2007-01-01" @default.
• W2102474137 modified "2023-09-25" @default.
• W2102474137 title "Direct Rhenium-Osmium age of the Oxfordian-Kimmeridgian boundary, Staffin bay, Isle of Skye, U.K., and the Late Jurassic time scale" @default.
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• W2102474137 hasPublicationYear "2007" @default.
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