FISC - St. Petersburg
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Tile 6
Eastern Sambo: Eastern Sambo and Maryland Shoal flank Pelican Shoal (Fig. 91B). A single, moderately well developed outlier-reef tract is positioned at the seaward terrace edge off Eastern Sambo (Fig. 89, line 2) and Maryland Shoal (Fig. 95) but is absent off Pelican Shoal (Fig. 94A). Instead, a low-relief, bedrock dune-ridge type of accretion is present in the same location off Pelican Shoal. The low-relief feature is clearly part of the outlier-reef tract but a part that simply never experienced Pleistocene coral growth, as is judged from the smoothly rounded seismic reflection. Compare its smoothness (Fig. 94A) with the jaggedness of reflections over areas of known Holocene shelf-edge coral reefs (for example, Fig. 95). There is no seismic evidence that outlier reefs ever grew off Pelican Shoal. Lidz (2004) referred to the Pelican Shoal feature as a poorly developed reef or paleoshoreline beach-dune ridge. If the Pelican Shoal terrace feature does represent a beach-dune ridge, its presence would support the hypothesis (Lidz et al., 1997a) that beach-dune ridges served as nuclei for outlier-reef development. Confirmation of the origination of this feature would require coring. |