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 Realm base. The middle neritic seafloor between fairweather wave base and storm wave base is characterized by rippled sands, subaqueous dunes, and rocky reefs. The deeper outer neritic environment, only disturbed by occasional storms, is a zone of muddy locally reworked sediment. The upper slope is largely a burrowed mud barren.

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Diagenesisene carbonates. The most impressive karst is that on and beneath the Nullarbor Plain. The semi-arid climate also led to extensive pedogenic carbonate in the form of calcrete. The exposed Pleistocene carbonates were rapidly cemented because of abundant aragonite particles that were quickly blown into aeolianites from the nearby offshore.

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Sedimentary Attributesus sedimentation are controversial but seem to be related to terrestrially derived nutrient elements controlled by climate and again a modern equivalent is not a good geohistorical analog. Carbonate deposition in the epicratonic Murray Basin was closely tied to climate and trophic resources.

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etive diagrams.Offers extensive linkage to modern temperate .This book documents and interprets the onshore Cenozoic temperate carbonate depositional system along the southern margin of Australia.  These strata, deposited in four separate basins, together with the extensive modern marine system offs

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https://doi.org/10.1007/978-3-319-24489-1or shelf accommodation such that any sediment that accumulated was either swept landward or seaward, resulting in little long-term accumulation on the shelf proper. The sedimentary record was instead one of spectacular Pleistocene marginal marine aeolianite complexes and a massive slope accretionary wedge.

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Succession SA3: Late Oligocene—Middle Miocene—‘The Carbonate Shelf’ ~28–11 Maic Murray Basin. The middle Miocene was much different with comparatively warm ocean waters resulting in numerous large benthic foraminifers, abundant coralline algae, and even local reef-building corals in the deposits. The Murray Basin deposits accumulating in a centripetal ramp system also had local photozoan facies.

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Succession SA4: Plio-Pleistocene—“The Shaved Shelf” ~10.4 Ma–5.2 Kaor shelf accommodation such that any sediment that accumulated was either swept landward or seaward, resulting in little long-term accumulation on the shelf proper. The sedimentary record was instead one of spectacular Pleistocene marginal marine aeolianite complexes and a massive slope accretionary wedge.

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Book 2021, deposited in four separate basins, together with the extensive modern marine system offshore, comprise the largest such cool-water carbonate system on the globe.  The approach is classic and comparative but the information is a synthesis of recent research and new information.  A brief section of