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• W1521624074 abstract "The sedimentary facies characterizing the shoreface-connected ridges off the East Frisian barrier-island coast, southern North Sea, were analyzed by means of high-resolution multi-beam bathymetry, sediment characteristics, and internal sedimentary structures derived from vibracores and box-cores. Particular attention was given to the contrasting sedimentary characteristics associated with seasonal storm and calm-weather situations, and how this was reflected in the preservation potential of the respective deposits. The internal sedimentary structures of the ridges are clearly related to the local wave climate and tidal regime. Under calm-weather conditions (summer months), partly bioturbated ripple cross-laminated sands dominate the deposits. In addition, tide-generated features such as small dune cross-stratification, herring-bone crossbeds, and flaser structures can be recognized. Particularly on the inner ridges, most of the physical structures in the upper sediment layer are strongly bioturbated by burrowing sea urchins (Echinocardium cordatum) and polychaete worms such as Lanice conchilega and Arenicola marina, whereas towards the outer ridges, the rate of bioturbation decreases rapidly, bi-directional large-scale crossbeds and climbing-ripple crossbeds being the dominant sedimentary structures. However, during the storm period (autumn — spring) most of these structures are replaced by hummocky cross-stratifications, low-angle laminations, and upper-flow-regime plane beds indicative of storm events. According to vibracore data, most of the preserved down-core sedimentary structures reflect storm influence, although a few structures possibly relate to fair-weather conditions, e.g. occasionally preserved bioturbated beds and ripple crossbedding. This may be due to a change in the effective wave-base in response to changing weather conditions during the waning storm phase rather than to a prolonged fair-weather period. Modern facies models based solely on short box-cores must be applied with great caution to the interpretation of the rock record." @default.
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• W1521624074 date "2012-01-26" @default.
• W1521624074 modified "2023-10-01" @default.
• W1521624074 title "Sedimentary Facies of Shoreface‐Connected Sand Ridges off the East Frisian Barrier‐Island Coast, Southern North Sea: Climatic Controls and Preservation Potential" @default.
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• W1521624074 doi "https://doi.org/10.1002/9781118311172.ch7" @default.
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