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- W2025787739 abstract "The Duntulm and Kilmaluag formations of the Middle Jurassic (Bathonian) Great Estuarine Group represent deposition in brackish-marine and fresh-brackish lagoons respectively. Deposition of ostracod valves at or near to the shoreline of these lagoons is described. Populations of Darwinula and Paracypris , composed almost entirely of carapaces of adults and older juveniles, are ascribed to storm deposition above the normal water level. Desiccation cracks and ‘cup-in-cup’ preservation, the latter indicative of wave reworking, are used to document fluctuations between subaqueous and subaerial conditions during deposition of the Kilmaluag Formation." @default.
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- W2025787739 date "1995-01-01" @default.
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- W2025787739 title "Ostracod biostratinomy at lagoonal shorelines: examples from the Great Estuarine Group, Middle Jurassic, Scotland" @default.
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- W2025787739 doi "https://doi.org/10.1016/s0016-7878(08)80024-7" @default.
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