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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Lecture Notes in Computer Sciencemargin 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

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Diedrich Wolter,Arne Kreutzmann, oceanography, climate, and influence of Antarctica. Middle Eocene–early Oligocene SA2 biogenic shelf sediments accumulated during a time of at first warm, but then gradually cooling ocean waters under a relative quiescent tectonic regimen. The climate was mostly humid subtropical with extensive te

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