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: International Journal of Earth Sciences, 2013, vol. 102, no. 2, p. 493-515
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In: Facies, 2007, vol. 53, no. 4, p. 535-552
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In: Cretaceous Research, 2013, vol. 41, p. 217-236
Syn-rift shallow-marine carbonates of Late Aptian to Early Albian age in the southern Maestrat Basin (E Spain) register the thickest Aptian sedimentary record of the basin, and one of the most complete carbonate successions of this age reported in the northern Tethyan margin. The host limestones (Benassal Formation) are partially replaced by dolostones providing a new case study of...
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In: Sedimentology, 2012, vol. 59, no. 1, p. 185–211
Recent global change occurs within decades and leaves a significant imprint on shallow carbonate platforms. To what extent can rate and synchronicity of environmental changes in the past be evaluated in order to allow comparisons with the processes and products of today? Sections of a carbonate-dominated platform of Late Oxfordian age have been logged in detail in the Swiss Jura Mountains. The...
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