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: Swiss Journal of Geosciences, 2011, vol. 104, no. 3, p. 367-408
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In: Paläontologische Zeitschrift, 2010, vol. 84, no. 2, p. 259-292
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In: International Journal of Earth Sciences, 2004, vol. 93, no. 3, p. 384-399
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In: International Journal of Earth Sciences, 2013, vol. 102, no. 1, p. 207-233
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In: Paläontologische Zeitschrift, 2008, vol. 82, no. 1, p. 55-84
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, p. III-V
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In: Swiss Journal of Geosciences, 2013, vol. 106, no. 2, p. 179-186
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, p. S1-S20
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, no. 3, p. 295-299
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