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Environmental fluctuations in the Olenus Zone (Upper Cambrian), southern Scandinavia: A geochemical approach
Bulletin of the Geological Society of Denmark
The Scandinavian Alum Shale Formation (Middle Cambrian to Lower Ordovician) was deposited under generally low bottom water oxygen levels. In the formation there is a covariance between faunal composition and the level of trace element enrichment caused by their mutual dependence upon changes in the bottom water oxygen levels. A detailed profile of the V/(V+Ni) ratio through the Upper Cambrian Olenus Zone in the Gislövshammar-2 core, Scania, Sweden, is described. Environmental information fromdoi:10.37570/bgsd-2000-47-03 fatcat:evooru3ig5d2fj7nlfyp7srmei