In: Geo-Marine Letters, 2014, vol. 34, no. 5, p. 399-417
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In: Swiss Journal of Geosciences, 2018, vol. 111, no. 3, p. 461–473
The ages obtained from planktonic foraminiferal assemblages retrieved from two exposures in the Gurnigel Flysch and from the re-examination of similar material gathered by previous researchers from the Voirons Flysch reveal only minor discrepancies with previous studies based on nannofossil biostratigraphy. In contrast, major divergences between this work and previous studies on the Voirons...
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In: Swiss Journal of Geosciences, 2018, vol. 111, no. 3, p. 511–522
Here we define a new morphospecies of planktonic foraminifera Globigerinoides eoconglobatus n. sp., identified from International Ocean Discovery Program (IODP) expedition 359 samples from drift deposits of the Maldives, Inner Sea. Through biostratigraphic analysis, we infer it may be the direct ancestor of Globigerinoides conglobatus evolving from Globigerinoides obliquus in the Late Miocene...
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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: Swiss Journal of Geosciences, 2011, vol. 104, no. 3, p. 367-408
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In: International Journal of Earth Sciences, 2013, vol. 102, no. 2, p. 493-515
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In: Swiss Journal of Geosciences, 2009, vol. 102, no. 2, p. 247-270
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In: Facies, 2009, vol. 55, no. 3, p. 401-419
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In: Swiss Journal of Geosciences, 2013, vol. 106, no. 2, p. 179-186
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In: International Journal of Earth Sciences, 2010, vol. 99, no. 1, p. 139-163
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