By Ian Jarvis(eds.)
The Oligocene and Miocene Epochs include an important levels within the Cenozoic worldwide cooling that led from a greenhouse to an icehouse Earth.
Recent significant advances within the figuring out and time-resolution of weather occasions occurring at the present, in addition to the proliferation of experiences on Oligocene and Miocene shallow-water/neritic carbonate structures, invite us to re-examine the importance of those carbonate platforms within the context of adjustments in weather and Earth floor strategies. Carbonate structures, as a result of a large dependence at the ecological necessities of organisms generating the sediment, are delicate recorders of alterations in environmental stipulations on this planet surface.
The papers incorporated during this targeted e-book deal with the dynamic evolution of carbonate structures deposited throughout the Oligocene and Miocene within the context on climatic and Earth surfaces methods concentrating on climatic traits and controls over deposition; temporal adjustments in carbonate manufacturers and palaeoecology; carbonate terminology; facies; procedures and environmental parameters (including water temperature and construction intensity profiles); carbonate manufacturers and their spatial and temporal variability; and tectonic controls over architecture.
This publication is a part of the International organization of Sedimentologists (IAS) precise Publications.
The distinctive guides from the IAS are a suite of thematic volumes edited by means of experts on topics of relevant curiosity to sedimentologists. Papers are reviewed and revealed to a similar excessive criteria as these released within the magazine Sedimentology and several other of those volumes became normal works of reference.
Chapter 1 A Synthesis of overdue Oligocene via Miocene Deep Sea Temperatures as Inferred from Foraminiferal Mg/Ca Ratios (pages 1–16): Katharina Billups and Kathleen Scheiderich
Chapter 2 Latitudinal traits in Cenozoic Reef styles and their courting to weather (pages 17–33): Christine Perrin and Wolfgang Kiessling
Chapter three Carbonate Grain institutions: their Use and Environmental importance, a short evaluate (pages 35–47): Pascal Kindler and Moyra E.J. Wilson
Chapter four Temperate and Tropical Carbonatesedimentation Episodes within the Neogene Betic Basins (Southern Spain) associated with cLimatic Oscillations and adjustments in Atlantic?Mediterranean Connections: Constraints from Isotopic information (pages 49–69): Jose M. Martin, Juan C. Braga, Isabel M. Sanchez?Almazo and Julio Aguirre
Chapter five Facies types and Geometries of the Ragusa Platform (SE Sicily, Italy) close to the Serravallian–Tortonian Boundary (pages 71–88): Cyril Ruchonnet and Pascal Kindler
Chapter 6 The Sensitivity of a Tropical Foramol?Rhodalgal Carbonate Ramp to Relative Sea?Level switch: Miocene of the imperative Apennines, Italy (pages 89–105): Marco Brandano, Hildegard Westphal and Guillem Mateu?Vicens
Chapter 7 Facies and series structure of a Tropical Foramol?Rhodalgal Carbonate Ramp: Miocene of the relevant Apennines (Italy) (pages 107–127): Marco Brandano, Laura Corda and Francesca Castorina
Chapter eight Facies and Stratigraphic structure of a Miocene Warm?Temperate to Tropical Fault?Block Carbonate Platform, Sardinia (Central Mediterranean Sea) (pages 129–148): Merle?Friederike Benisek, Gabriela Marcano, Christian Betzler and Maria Mutti
Chapter nine Coralline Algae, Oysters and Echinoids – a Liaison in Rhodolith Formation from the Burdigalian of the Latium?Abruzzi Platform (Italy) (pages 149–163): Marco Brandano and Werner E. Piller
Chapter 10 Palaeoenvironmental importance of Oligocene–Miocene Coralline pink Algae – a evaluate (pages 165–182): Juan C. Braga, Davide Bassi and Werner E. Piller
Chapter eleven Molluscs as an important a part of Subtropical Shallow?Water Carbonate construction – an instance from a center Miocene Oolite Shoal (Upper Serravallian, Austria) (pages 183–199): Mathias Harzhauser and Werner E. Piller
Chapter 12 Echinoderms and Oligo?Miocene Carbonate platforms: power purposes in Sedimentology and Environmental Reconstruction (pages 201–228): Andreas Kroh and James H. Nebelsick
Chapter thirteen Coral variety and Temperature: a Palaeoclimatic standpoint for the Oligo?Miocene of the Mediterranean quarter (pages 229–244): Francesca R. Bosellini and Christine Perrin
Chapter 14 overdue Oligocene to Miocene Reef Formation on Kita?Daito?Jima, Northern Philippine Sea (pages 245–256): Y. Iryu, S. Inagaki, Y. Suzuki and ok. Yamamoto
Chapter 15 Carbonate construction in Rift Basins: types for Platform Inception, development and Dismantling, and for Shelf to Basin Sediment shipping, Miocene Sardinia Rift Basin, Italy (pages 257–282): Mario Vigorito, Marco Murru and Lucia Simone
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Additional resources for Carbonate Systems during the Oligocene-Miocene Climatic Transition
1997). Schlager (2000, 2003) named his carbonate factory types on a mixture of latitudinal (tropical), temperature (coolwater) and geological structure (mud mound) nomenclature, separating the three main factories based on the mode of carbonate precipitation. In deﬁning carbonate groupings or associations, the nomenclatures used are either descriptive or interpretative. However, interpretative environmental connotations, whether rightly or wrongly, are commonly attached to the original descriptive grain associations of Lees & Buller (1972).
Kiessling 0 Global number of reef sites Reef size Main reef-builders Reef-building assemblages Diversity of reef-builders Maximum number of reef sites 15 Langhian 20 Aquitanian 25 Chattian 30 Rupelian Number of reef sites increases in Mediterranean and Indo-Pacific regions Age (Ma) Burdigalian Most reefs outside intertropical zones are of low to moderate diversity Serravallian Preferential latitudinal distribution in Mediterranean and Indo-Pacific regions Tortonian Proportion of coral-dominated reefs increases 10 Preferential distribution of thickest reefs between tropics Messinian Number of reef sites declines Pliocene 5 Development of specific reef-building communities at high latitude Scleractinian corals dominate reef-building assemblages 35 Priabonian High-diversity reefs tend to develop in the median part of reef-belt High-latitude reefs dominated by specific reef-builders Bartonian 40 Fig.
James (1997) deﬁned an association as “a group of sedimentary particles occurring together under similar environmental conditions and havinguniform or distinctive aspects”. , 1997). Schlager (2000, 2003) named his carbonate factory types on a mixture of latitudinal (tropical), temperature (coolwater) and geological structure (mud mound) nomenclature, separating the three main factories based on the mode of carbonate precipitation. In deﬁning carbonate groupings or associations, the nomenclatures used are either descriptive or interpretative.
Carbonate Systems during the Oligocene-Miocene Climatic Transition by Ian Jarvis(eds.)