Cyclic and Event Stratification [electronic resource] /

I. Limestone-Marl Rhythms and Climate-controlled Facies Changes -- General Remarks About the Nature, Occurrence, and Recognition of Cyclic Sequences (Periodites) -- Limestone-Marl Cycles (Periodites): Diagnosis, Significance, Causes — a Review -- Observations on Well-bedded Upper Jurassic Limestones -- Origin of Marl-Limestone Alternation (Oxford 2) in Southwest Germany -- Limestone-Shale Bedding and Perturbations of the Earth’s Orbit -- Rhythmic Sedimentation Documented in a Late Cretaceous Core (Abstract) -- Ecology and Depositional Environments of Chalk-Marl and Limestone-Shale Rhythms in the Cretaceous of North America (Abstract) -- Diagenetic Redistribution of Carbonate, a Process in Forming Limestone-Marl Alternations (Devonian and Carboniferous, Rheinisches Schiefergebirge, W. Germany) -- A Contribution to the Origin of Limestone-Shale Sequences -- Deep-Sea Stratigraphy: Cenozoic Climate Steps and the Search for Chemo-Climatic Feedback -- IIA. Event Stratification. Calcareous and Quartz-Sandy Tempestites -- General Remarks About Event Deposits -- Experiments on the Distinction of Wave and Current Influenced Shell Accumulations -- Calcareous Tempestites: Storm-dominated Stratification in Upper Muschelkalk Limestones (Middle Trias, SW-Germany) -- Allochthonous Coquinas in the Upper Muschelkalk - Caused by Storm Events? (Abstract) -- The role of Storm Processes in Generating Shell Beds in Paleozoic Shelf Environments -- Rhythmic Bedding and Shell Bed Formation in the Upper Jurassic of East Greenland -- Shell Beds in the Lower Lias of South Germany — Facies and Origin -- Storm Sedimentation in the Carboniferous Limestones Near Weston-Super-Mare (Dinantian, SW-England) -- Event-Stratification in Nummulite Accumulations and in Shell Beds from the Eocene of Egypt -- The “Bank der kleinen Terebrateln” (Upper Muschelkalk, Triassic) Near Schwäbisch Hall (SW-Germany) — a Tempestite Condensation Horizon -- Glauconitic Condensation Through High-Energy Events in the Albian Near Clars (Escragnolles, Var, SE-France) -- Muschelkalk/Keuper Bone-Beds (Middle Triassic, SW-Germany) — Storm Condensation in a Regressive Cycle -- Condensed Griotte Facies and Cephalopod Accumulations in the Upper Devonian of the Eastern Anti-Atlas, Morocco -- Distinctive Features of Sandy Tempestites -- Multidirectional Paleocurrents as Indicators of Shelf Storm Beds -- Scour and Fill: The Significance of Event Separation -- Storm-surge Sandstones and the Deposition of Interbedded Limestone: Late Precambrian, Southern Norway -- Flat Pebble Conglomerates, Storm Deposits, and the Cambrian Bottom Fauna -- IIB. Event Stratification — Other Event Deposits -- Jurassic Bedded Cherts from the North Apennines, Italy: Dyscyclic Sedimentation in the Deep Pelagic Realm -- Quartz-sandy Allodapic Limestones as a Result of Lime Mud-Raising Clastic Turbidites -- Belemnites as Current Indicators in Shallow Marine Turbidites of the Santonian Bavnodde Grønsand, Bornholm (Denmark) -- Habits of Zircon as a Tool for Precise Tephrostratigraphic Correlation -- III. Cyclicity and Event Stratification in Black Shales -- Cyclic and Dyscyclic Black Shale Formation -- Cyclicity and the Storage of Organic Matter in Middle Cretaceous Pelagic Sediments -- Types of Stratification in the Kupferschiefer -- Environmental Changes During Oil Shale Deposition as Deduced from Stable Isotope Ratios -- The Community Structure of “Shell Islands” on Oxygen Depleted Substrates in Mesozoic Dark Shales and Laminated Carbonates (Abstract) -- Ammonite Shells as Habitats — Floats or Benthic Islands? (Abstract) -- Palynology of Upper Liassic Bituminous Shales (Abstract) -- The Bituminous Lower Toarcian at the Truc de Balduc Near Mende (Département de la Lozère, S-France) -- Bedding Types of the Toarcian Black Shales in NW-Greece -- Stratinomy of the Lower Kimmeridge Clay (Dorset, England) (Abstract) -- The Formation of the Bituminous Layers of the Middle Triassic of Ticino (Switzerland) (Abstract) -- Summary -- Paleogeographic Significance of Tempestites and Periodites.