Carbonate Systems During the Olicocene-Miocene Climatic Transition (Special Publication 42 of the IAS) ( International Association Of Sedimentologists Series )

Publication series :International Association Of Sedimentologists Series

Author: Maria Mutti  

Publisher: John Wiley & Sons Inc‎

Publication year: 2010

E-ISBN: 9781444327434

P-ISBN(Hardback):  9781444337914

Subject: P588.24 Chemical and biochemical rock

Language: ENG

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Description

The Oligocene and Miocene Epochs comprise the most important phases in the Cenozoic global cooling that led from a greenhouse to an icehouse Earth.

Recent major advances in the understanding and time-resolution of climate events taking place at this time, as well as the proliferation of studies on Oligocene and Miocene shallow-water/neritic carbonate systems, invite us to re-evaluate the significance of these carbonate systems in the context of changes in climate and Earth surface processes. Carbonate systems, because of a wide dependence on the ecological requirements of organisms producing the sediment, are sensitive recorders of changes in environmental conditions on the Earth surface.

The papers included in this Special Publication address the dynamic evolution of carbonate systems deposited during the Oligocene and Miocene in the context on climatic and Earth surfaces processes focusing on  climatic trends and controls over deposition; temporal changes in carbonate producers and palaeoecology; carbonate terminology; facies; processes and environmental parameters (including water temperature and production depth profiles); carbonate producers and their spatial and temporal variability; and tectonic controls over architecture.

This book is part of the International Association of Sedimentologists (IAS) Special Publications.

The Special Publications from the IAS are a set of thematic volumes edited by specialists on subjects of central interest to sedimentologists. Papers are reviewed and printed to the same high standards as those published in the journal Sedimentology and several of these volumes have become standard works of reference.

Chapter

Contents

pp.:  1 – 7

Carbonate grain associations: their use and environmental significance, a brief review

pp.:  31 – 49

Temperate and tropical carbonate-sedimentation episodes in the Neogene Betic basins (southern Spain) linked to climatic oscillations and changes in Atlantic-Mediterranean connections: constraints from isotopic data

pp.:  49 – 63

Facies models and geometries of the Ragusa Platform (SE Sicily, Italy) near the Serravallian–Tortonian boundary

pp.:  63 – 85

The sensitivity of a tropical foramol-rhodalgal carbonate ramp to relative sea-level change: Miocene of the central Apennines, Italy

pp.:  85 – 103

Facies and sequence architecture of a tropical foramol-rhodalgal carbonate ramp: Miocene of the central Apennines (Italy)

pp.:  103 – 121

Facies and stratigraphic architecture of a Miocene warm-temperate to tropical fault-block carbonate platform, Sardinia (Central Mediterranean Sea)

pp.:  121 – 143

Coralline algae, oysters and echinoids – a liaison in rhodolith formation from the Burdigalian of the Latium-Abruzzi Platform (Italy)

pp.:  143 – 163

Palaeoenvironmental significance of Oligocene–Miocene coralline red algae – a review

pp.:  163 – 179

Molluscs as a major part of subtropical shallow-water carbonate production – an example from a Middle Miocene oolite shoal (Upper Serravallian, Austria)

pp.:  179 – 197

Echinoderms and Oligo-Miocene carbonate systems: potential applications in sedimentology and environmental reconstruction

pp.:  197 – 215

Coral diversity and temperature: a palaeoclimatic perspective for the Oligo-Miocene of the Mediterranean region

pp.:  215 – 243

Late Oligocene to Miocene reef formation on Kita-daito-jima, northern Philippine Sea

pp.:  243 – 259

Carbonate production in rift basins: models for platform inception, growth and dismantling, and for shelf to basin sediment transport, Miocene Sardinia Rift Basin, Italy

pp.:  259 – 271

Index

pp.:  271 – 297

LastPages

pp.:  297 – 314

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