Organic-rich biolaminated facies from a Kimmeridgian lagoonal environment in the French Southern Jura mountains—A way of estimating accumulation rate variations
During Kimmeridgian times, the present-day Southern Jura was a carbonate platform. In the palaeolagoon at the village of Orbagnoux, organic matter was deposited, giving birth to calcareous laminites, with organic carbon reaching 12%. Three facies may be distinguished; two types of laminites are enco...
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Veröffentlicht in: | Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 1992-11, Vol.99 (1), p.163-177 |
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