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- W2070502442 abstract "Charlotte Harbor is a complex lagoon and estuarine system in southwestern peninsular Florida that is underlain by Tertiary carbonates and Quaternary siliciclastic sedimentary sequences. High-resolution seismic profiling, vibracores, and sediment samples from modern environments have been used to interpret the Quaternary stratigraphy and evolution of this system. The underlying Tertiary carbonates have undergone extensive dissolution and collapse which has created isolated karst depressions and fracture-controlled, elongated troughs. Although late Neogene deposition infilled most of the pre-Quaternary relief, the Quaternary drainage system was controlled by the poorly integrated, vertical drainage of the karstified limestones which is unlike the well-integrated paleofluvial drainage systems of the mid-Atlantic and northern Gulf coastal plains. Despite these differences, paleotopography and sediment availability have controlled locations and sedimentary environments as has been noted in other published studies on purely siliciclastic systems. The distribution of three interpreted Quaternary depositional sequences (fluvial to upper estuarine point bar fining upward sequence (FUS), transitional estuarine sequence and tidal channel-delta FUS) and the mapped distribution of an early-middle Pleistocene seismic unconformity indicate that Quaternary sea-level fluctuations have repeatedly caused coastal systems to migrate through the area, leaving records of at least two Pleistocene barrier-lagoon systems. These systems straddled the infilled karst depressions and were apparently controlled by the availability of erodible sediment that infilled the depressions. The modern barrier system is perched upon one of the Pleistocene barrier platforms which has been preserved as a result of lithification of carbonate-rich inlet-tidal delta deposits. These platforms should preserve the backbarrier deposits from future shoreface incision but localized channelization will cause extensive reworking. Because the paleofluvial channels do not extend offshore, preservation on the inner shelf (> 5–7 km offshore) is limited to isolated karst depressions where Tertiary limestones are exposed." @default.
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- W2070502442 date "1989-08-01" @default.
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- W2070502442 title "Quaternary stratigraphy of the Charlotte Harbor estuarine-lagoon system, southwest Florida: Implications of the carbonate-siliciclastic transition" @default.
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- W2070502442 doi "https://doi.org/10.1016/0025-3227(89)90104-7" @default.
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