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- W1963703022 abstract "In exposures of the Late Eocene Bembridge Limestone Formation at the west end of the Isle of Wight, calcareous ovoid-cylindrical trace fossils, ranging in length from 1 to over 47 mm long, but commonly 30 mm long and 15 mm in diameter, occur sparingly distributed in freshwater to pedogenically-modified limestones yielding calcitic casts of freshwater snails and land snails. Although specimens of the trace fossils having both ends entire are usually preserved as calcitic to calcite internal casts, the occurrence of rare hollow specimens lined by drusy calcite is evidence that they were chambers within the sediment. The majority of specimens were ruptured sub-terminally at one end before fossilization, probably by the escaping organism. Such specimens are partly to entirely filled by intraclastic lime mudstone. Rare specimens are attached to a short burrow-fill composed of similar lime mudstone and about the same diameter as the chamber. Most chambers have a surficial film of chalky micrite or microspar, with or without a cemented surficial micritic skin. In some specimens the micritic skin protects a surface ornament of lobate and composite tobate-linear ridges 0.5 mm wide and up to 5 mm long. When weathered-out in relief, these impart a wrinkle-like or fibrous surface texture, which can have a distinct helical trend. Whereas hitherto the chambers have been interpreted as tropical land snails' eggs, they differ from the latter in shape, surface texture, mode of rupture and mode of occurrence. The chambers also lack an egg-shell microstructure and cannot be reptile eggs. Although some analogous foreign specimens have been interpreted as simple hymenopteran brood chambers, fossil and Recent examples of these have a distinct terminal cap or seal, lacking in the Bembridge Limestone specimens. Instead, they may have been made by other kinds of insect for pupation, or by an unknown organism for aestivation or hibernation." @default.
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- W1963703022 date "1998-01-01" @default.
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- W1963703022 title "Cocoon-like trace fossils from the lacustrine-palustrine Bembridge Limestone Formation (Late Eocene), Southern England" @default.
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- W1963703022 doi "https://doi.org/10.1016/s0016-7878(98)80003-5" @default.
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