Titlebook: Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean; Neritic Southern Aus Noel P. James,Yvonne Bone Book 2021 The Editor(s) (if applicable

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The Modern Carbonate Depositional Realmed by cool waters, a series of complex currents, and seasonal upwelling. Neritic sediments are composed of extraclasts, mainly relict and stranded particles, together with biofragments mostly from living bryozoans, benthic foraminifers, mollusks, echinoderms, brachiopods, coralline algae, and silice

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Succession SA2: Middle Eocene to Lower Oligocene—‘The Biogenic Shelf’?~?43-28 Maest but by the early Oligocene extended into the Otway Basin. SA2.1—Middle Eocene strata, are largely marginal, inner, and mid neritic siliciclastics passing outboard into carbonates with deep water bryozoan mounds. SA2.2—Mid to Upper Eocene rocks are mostly similar with carbonaceous inboard terrest

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Succession SA3: Late Oligocene—Middle Miocene—‘The Carbonate Shelf’?~28–11?Mavel fall, Upper Oligocene deposition was cool-water throughout with extensive heterozoan deposits in all neritic environments as well as the epicratonic Murray Basin. The middle Miocene was much different with comparatively warm ocean waters resulting in numerous large benthic foraminifers, abundant

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Diagenesismargin subsidence was largely characterized by seafloor carbonate dissolution, omission surface precipitation (hardgrounds) and burial alteration, there was no significant meteoric alteration. This latter aspect was largely due to the fact that there were few aragonitic components in the sediment an