04924nam 2200745Ia 450 991080929450332120240509021013.01-282-72925-X97866127292561-118-39836-X1-4443-2743-7(CKB)2670000000034961(EBL)573944(OCoLC)659500858(SSID)ssj0000434137(PQKBManifestationID)11311350(PQKBTitleCode)TC0000434137(PQKBWorkID)10395089(PQKB)11684628(MiAaPQ)EBC573944(Au-PeEL)EBL573944(CaPaEBR)ebr10419467(CaONFJC)MIL272925(EXLCZ)99267000000003496120100511d2010 uy 0engur|n|---|||||txtccrCarbonate systems during the Oligocene-Miocene climatic transition /edited by Maria Mutti, Werner Piller, Christian Betzler1st ed.Hoboken, NJ Blackwell Pub.20101 online resource (314 p.)Special publication ... of the international association of sedimentologists ;no. 42Description based upon print version of record.1-4443-3791-2 Includes bibliographical references and index.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 reviewTemperate 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 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; IndexThe 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 producingSpecial publication ... of the International Association of Sedimentologists ;no. 42.Carbonate rocksGeology, StratigraphicOligoceneGeology, StratigraphicMiocenePaleoclimatologyOligocenePaleoclimatologyMioceneCarbonate rocks.Geology, StratigraphicGeology, StratigraphicPaleoclimatologyPaleoclimatology552/.58Mutti M(Maria)889570Piller Werner E799186Betzler Christian889571MiAaPQMiAaPQMiAaPQBOOK9910809294503321Carbonate systems during the Oligocene-Miocene climatic transition1987157UNINA