Carbonate environments

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Rudists• Dense stands of bizarre, organ-pipeshaped bivalves from the LateCretaceous• Baffle sediment, but no framework, sonot really reefs!• All died out suddenly in the K/Textinction.
Typical rudist buildup,Northern Sinai
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Carbonate environmentsEnvironments
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Carbonate environmentsvery differen
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Taphonomic feedback• Biogenic car
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• Usually dominant: range from hu
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Foramol association• Temperate wa
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Controls on associations
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Scleractinian Corals (Modern),Frame
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Homotrema Rubrum:Foraminifera• Mi
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Non-skeletal grains• Association
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Climate• Skeletal grains are depe
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Flux of calcium carbonate from surf
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Modern distribution ofcarbonates an
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Dunham’s classification
Page 31 and 32: Organisms and SedimentProducers
Page 33 and 34: Shallow Marine CarbonateSediments
Page 38 and 39: Fiji, High Tide
Page 40 and 41: More on ramps• Below FWB reworkin
Page 42 and 43: Epeiric Platform Facies• Tidal an
Page 44 and 45: Reef facies• High energy. Wave im
Page 46 and 47: Reef composition• Framework, cons
Page 48 and 49: Environments of Different growthfor
Page 50 and 51: Reef succession
Page 52 and 53: Modern Reef Environment
Page 54 and 55: Cementation by aragonite
Page 56 and 57: Later Burial (Dolomite dependanton
Page 58 and 59: Recognition of fossil reefs• Can
Page 60 and 61: Build-up classification
Page 62 and 63: Fossil reef structure• Core: mass
Page 64 and 65: Facies in the record
Page 66 and 67: Another interpretationof history of
Page 69 and 70: Lower-Middle CambrianArchaeocyaths
Page 71 and 72: Ordovician/Silurian build-ups• E.
Page 73 and 74: StromatactisTypical component - spa
Page 75 and 76: Gotland Stromatoporoid buildupsKupp
Page 77 and 78: Waulsortian mud mounds• Very hard
Page 79: Common in Ireland…MoundOverlyingb
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Carbonate environments

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