In: Contributions to Mineralogy and Petrology, 2014, vol. 167, no. 6, p. 1-27
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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: Facies, 2010, vol. 56, no. 3, p. 385-397
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, p. S1-S20
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In: Metallurgical and Materials Transactions A, 2013, vol. 44, no. 9, p. 4119-4123
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In: Facies, 2011, vol. 57, no. 4, p. 605-612
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 1, p. 137-144
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In: Pure and Applied Chemistry, 2001, vol. 73, no. 2, p. 381-394
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In: Microscopy, 1999, vol. 48, no. 6, p. 717-723
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In: Journal of Materials Research, 1993, vol. 8, no. 1, p. 206-213
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