In: Swiss Journal of Geosciences, 2015, vol. 108, no. 2-3, p. 213-224
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In: Stratigraphy & Timescales, 2018, vol. 3, p. 151–187
The sedimentary record of ancient shallow-marine carbonate platforms commonly displays a stacking of different facies, which reflects repetitive changes of depositional environments through time. These changes can be induced by external factors such as cyclical changes in climate and/or sea level, but also by internal factors such as lateral migration of sediment bodies and/or changes in the...
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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: The International Journal of Life Cycle Assessment, 2005, vol. 10, no. 2, p. 120-130
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In: Facies, 2010, vol. 56, no. 2, p. 249-278
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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. 3, p. 515-518
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In: Swiss Journal of Geosciences, 2009, vol. 102, no. 2, p. 247-270
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, no. 2, p. 157-174
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In: Mineralium Deposita, 2006, vol. 41, no. 3, p. 259-280
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