Thèse de doctorat : Université de Fribourg, 1999 ; no 1240.
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Thèse de doctorat : Université de Fribourg, 2007 ; no 1579.
The main goal of this study is to monitor the highfrequency palaeoenvironmental changes occurring during a marine transgression in mixed carbonatesiliciclastic sedimentary systems. Based on a wellestablished bio- and sequence-stratigraphic framework, a narrow time window in the Bimammatum Zone of the Late Oxfordian is investigated. Seven shallow platform sections (Swiss Jura, Lorraine), two deep...
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Thèse de doctorat : Université de Fribourg, 2003 ; Nr. 1407.
During the Late Oxfordian and earliest Kimmeridgian, today’s central Swiss Jura Mountains developed as a shallow carbonate-dominated plat form. At the threshold between boreal depositional areas to the north and the Tethys ocean to the south, dynamic sedimentatary systems developed under a subtropical and semiarid to arid climate (palaeolatitude 33°to38°N). Sedimentological analyses of the 6...
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