In: Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, vol. 235, p. 245-264
In the uppermost Hauterivian sediments of the western Tethys, a short-lived anoxic event (Faraoni event) is documented both in the form of an interval enriched in organic matter (pelagic realm) and in a condensed interval enriched in glauconite and phosphate (shelf realm). This latter interval represents the onset of a drowning episode on the Helvetic carbonate platform along the northern tethyan...
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In: International Journal of Earth Sciences, 2007, vol. 96, no. 2, p. 327-341
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In: International Journal of Earth Sciences, 2007, vol. 96, no. 2, p. 327-341
The Faraoni Level is a short-lived oxygen-deficient event that took place during the latest Hauterivian. In order to improve our understanding of the palaeoenvironmental conditions that occurred during this event, we have analysed the contents of several redox-sensitive trace elements (U, V, Mo, As, Co, Cd, Cu, Zn, Ni, Pb, Cr) from bulk limestone samples of late Hauterivian–early Barremian age...
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In: Swiss Journal of Geosciences, 2011, vol. 104, no. 1, p. 147-160
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In: Earth and Planetary Science Letters, 2006, vol. 242, p. 254-271
In order to improve our understanding of the relationships between the late Hauterivian oceanic anoxic Faraoni event, contemporaneous platform drowning along the northern Tethyan margin and global environmental change in general, we established high-resolution δ13C and δ18O curves for the late Hauterivian and the entire Barremian stage. These data were obtained from whole-rock carbonate samples...
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