In: Swiss Journal of Geosciences, 2014, vol. 107, no. 2-3, p. 223-250
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In: Newsletters on Stratigraphy, 2018, vol. 51, no. 3, p. 343–380
The upper Cenomanian – lower Turonian is a key-stratigraphic interval, as it encompasses the Late Cretaceous supergreenhouse and a major perturbation of the global carbon cycle (i. e., Oceanic Anoxic Event 2) as evidenced by a global positive carbon isotope excursion and by the nearly world-wide deposition of organic-rich marine facies. A turnover in planktonic foraminiferal assemblages and...
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In: Hydrogeology Journal, 2013, vol. 21, no. 2, p. 425-440
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In: European Journal of Plant Pathology, 2012, vol. 132, no. 1, p. 111-122
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, no. 2, p. 157-174
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In: Facies, 2009, vol. 55, no. 3, p. 401-419
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In: Graefe's Archive for Clinical and Experimental Ophthalmology, 2006, vol. 244, no. 9, p. 1104-1112
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In: Facies, 2010, vol. 56, no. 3, p. 385-397
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In: International Journal of Earth Sciences, 2013, vol. 102, no. 4, p. 1111-1129
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In: Facies, 2011, vol. 57, no. 4, p. 605-612
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