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Delile in a Mediterranean shallow environment (Stagnone di Marsala, western Sicily) were investigated seasonally throughout 1998.
Whether similar ligands and/or ligands in the surface ocean seawater can explain the persistence of DFe in shallow environment is unknown.
Development in a protected setting, together with rapid burial due to progradation of siliciclastics on top of the palaeotopographic high, accounts for this exceptional preservation in such a shallow environment.
The original data acquired by the hydrophone array from the shallow environment are analyzed and processed by the following steps.
The first aquifer is buried in shallow environment (<40 m) and the wall rocks are dominated by siltstone and clay.
Moreover, we can see the clutter and noise are noticeable, owing to the little distance from sound source, and shallow environment of the exploration.
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Rudist biostromes were preserved in seaward areas of these protected shallow environments of overall moderate to low hydrodynamic gradient, which was punctuated by storms.
The physical conditions of deep and shallow environments may create disparate fertilization conditions for corals in a number of ways, the most obvious being for broadcast spawning species such as O. faveolata.
Wind waves in shallow environments affect the movement of bottom sediment, coastal erosion, and overtopping and breaching of shore defenses and coastal evolution: forming beaches, sandbanks, and ebb shoals in estuaries.
Storm deposits (tem-pestites) in shallow environments may reveal many various features depending on local conditions.
This is also evidenced by the slight oversaturation in SiO2 (mainly chalcedony) that groundwater presents when it reaches lower temperatures in more shallow environments.
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