In: Swiss Journal of Geosciences, 2015, vol. 108, no. 2-3, p. 327-343
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In: International Journal of Earth Sciences, 2014, vol. 103, no. 4, p. 1059-1082
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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: Swiss Journal of Geosciences, 2009, vol. 102, no. 1, p. 57-75
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In: Vegetation History and Archaeobotany, 2008, vol. 17, no. 2, p. 185-197
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In: Conservation Genetics, 2009, vol. 10, no. 2, p. 303-315
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 2, p. 293-312
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In: Swiss Journal of Geosciences, 2011, vol. 104, no. 1, p. 97-146
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 3, p. 407-429
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 3, p. 407-429
Detailed investigation of facies and sedimentary structures reveals that, during the Middle Oxfordian to Late Kimmeridgian, the shallow carbonate platform of the Swiss and French Jura Mountains recorded high-frequency sea-level fluctuations quite faithfully. The cyclostratigraphic analysis within the established biostratigraphic and sequence-chronostratigraphic framework implies that the...
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