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Record Nr. |
UNINA9910140772203321 |
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Titolo |
Carbonate systems during the Oligocene-Miocene climatic transition [[electronic resource] /] / edited by Maria Mutti, Werner Piller, Christian Betzler |
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Pubbl/distr/stampa |
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Hoboken, NJ, : Blackwell Pub., 2010 |
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ISBN |
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1-282-72925-X |
9786612729256 |
1-118-39836-X |
1-4443-2743-7 |
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Descrizione fisica |
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1 online resource (314 p.) |
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Collana |
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Special publication ... of the international association of sedimentologists ; ; no. 42 |
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Altri autori (Persone) |
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MuttiM (Maria) |
PillerWerner E |
BetzlerChristian |
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Disciplina |
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Soggetti |
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Carbonate rocks |
Geology, Stratigraphic - Oligocene |
Geology, Stratigraphic - Miocene |
Paleoclimatology - Oligocene |
Paleoclimatology - Miocene |
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Lingua di pubblicazione |
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Formato |
Materiale a stampa |
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Livello bibliografico |
Monografia |
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Note generali |
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Description based upon print version of record. |
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Nota di bibliografia |
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Includes bibliographical references and index. |
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Nota di contenuto |
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Carbonate Systems During the Oligocene-Miocene Climatic Transition; Contents; Miocene carbonate systems: an introduction; A synthesis of Late Oligocene through Miocene deep sea temperatures as inferred from foraminiferal Mg/Ca ratios; Latitudinal trends in Cenozoic reef patterns and their relationship to climate; Carbonate grain associations: their use and environmental significance, a brief review |
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 dataFacies models and geometries of the Ragusa Platform (SE Sicily, Italy) near the Serravallian-Tortonian boundary; The sensitivity of a tropical foramol-rhodalgal carbonate ramp to relative sea-level |
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change: Miocene of the central Apennines, Italy; Facies and sequence architecture of a tropical foramol-rhodalgal carbonate ramp: Miocene of the central Apennines (Italy) |
Facies and stratigraphic architecture of a Miocene warm-temperate to tropical fault-block carbonate platform, Sardinia (Central Mediterranean Sea)Coralline algae, oysters and echinoids - a liaison in rhodolith formation from the Burdigalian of the Latium-Abruzzi Platform (Italy); Palaeoenvironmental significance of Oligocene-Miocene coralline red algae - a review; Molluscs as a major part of subtropical shallow-water carbonate production - an example from a Middle Miocene oolite shoal (Upper Serravallian, Austria) |
Echinoderms and Oligo-Miocene carbonate systems: potential applications in sedimentology and environmental reconstructionCoral diversity and temperature: a palaeoclimatic perspective for the Oligo-Miocene of the Mediterranean region; Late Oligocene to Miocene reef formation on Kita-daito-jima, northern Philippine Sea; Carbonate production in rift basins: models for platform inception, growth and dismantling, and for shelf to basin sediment transport, Miocene Sardinia Rift Basin, Italy; Index |
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Sommario/riassunto |
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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 |
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