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- W1573161986 abstract "Detailed sequence and facies analyses of ten stratigraphic sections, positioned on two platform to basin transects across the Ragusa ramp (Sicily, Italy), demonstrate that two models of facies zones must be used to describe the internal architecture of this carbonate edifice near the Serravallian/Tortonian boundary. Seven facies zones, based on the palaeobathymetric position of the carbonate-producing biota, have been defined and described for each of these stages. During the late Serravallian, the inner ramp was characterized mainly by small epiphytic biota of the foramol association, whereas the middle ramp was dominated by rhodoliths and minor benthic foraminifera, bryozoans, barnacles, serpulids and echinoids. In contrast, during the early Tortonian, the inner ramp was characterized by a chlorozoan biota (Halimeda and Porites) and the middle ramp by branching Corallinacea and rhodoliths. This seemingly minor modification in the type and locus of carbonate production, and the associated changes in hydrodynamics, had profound consequences on the overall geometry of the platform, which evolved from a distally steepened ramp in the late Serravallian, to a geometry approaching that of a flat-topped platform in the early Tortonian." @default.
- W1573161986 created "2016-06-24" @default.
- W1573161986 creator A5025045125 @default.
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- W1573161986 date "2012-04-03" @default.
- W1573161986 modified "2023-10-14" @default.
- W1573161986 title "Facies Models and Geometries of the Ragusa Platform (SE Sicily, Italy) Near the Serravallian–Tortonian Boundary" @default.
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- W1573161986 doi "https://doi.org/10.1002/9781118398364.ch5" @default.
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