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GEOL 325:  Stratigraphy & Sedimentary Basins University of South Carolina Spring 2005 Professor Chris Kendall EWS 304  kendall@sc.edu  777.2410 An Overview of Carbonates
Precipitated Sediments & Sedimentary Rocks An Epitaph to Limestones & Dolomites
Lecture Series Overview ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Sedimentary rocks are the product of the creation, transport, deposition, and diagenesis of detritus and solutes derived from pre-existing rocks.
Sedimentary rocks are the product of the creation, transport, deposition, and diagenesis of detritus and  solutes  derived from pre-existing rocks.
Sedimentary Rocks ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Lecture Outline ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Limestones Form - Where? ,[object Object],[object Object],[object Object],[object Object]
CO 2  - Temperature & Pressure Effect! ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Calcium Carbonate - Solubilty  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Controls on Carbonate Accumulation ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Limestones – Chemical or Bochemical ,[object Object],[object Object],[object Object],[object Object],Distinction between biochemical & physico-chemical blurred by ubiquitous cyanobacteria of biosphere!
 
 
 
Biological Carbon Pump  ,[object Object],[object Object],[object Object]
Carbonate Mineralogy ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
TROPICS TEMPERATE OCEANS
 
Basin Ramp Restricted Shelf Open Shelf
Basin Rim Restricted Shelf Open Shelf
Carbonate Components – The Key ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Carbonate Particles ,[object Object],[object Object],[object Object]
Lime Mud or Micrite
Lime Mud  or  Micrite
WHITING LIME MUD ACCUMULATES ON BANK, OFF BANK  & TIDAL FLATS
Three Creeks Tidal Flats
Lime Mud - Ordovician Kentucky
Carbonate Bio-physico-chemical Grains ,[object Object],[object Object],[object Object],[object Object]
 
 
 
Ooids
 
Aragonitic Ooids
After Scholle, 2003 Aragonitic Ooids
Calcitic &  Aragonitic Ooids Great  Salt Lake
Grapestones
Grapestones
Pellets
Pellets
 
 
 
 
After Scholle
Skeletal Particles - Mineralogy ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Drafted by Waite 99, after James 1984)
Foraminifera
After Scholle Foraminifera
Brachiopod
Brachiopods
Brachiopod
Bryozoan
Bryozoan
Trilobite Remains Ostracod Remains Calcispheres
Trilobite Carapice
Syntaxial  cement Crinoid
Red Calcareous Algae
 
Surface Water Organic Productivity  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Deep Water Carbonate Deposits ,[object Object],[object Object],[object Object],[object Object],[object Object]
Carbonate Compensation Depth - CCD ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
After James, 1984
 
After James, 1984
 
 
 
 
 
 
 
Carbonate Cement Fabrics  ,[object Object],[object Object],[object Object],[object Object],[object Object]
 
 
 
Isopachus Marine Cement
 
Meniscus Cement
 
 
 
 
 
 
 
 
 
 
 
 
Influx of  Magnesium Rich  Continental Ground  Waters Influx of  sea water Evaporation  of mixed  Waters 1. Aragonite 2. Gypsum 3. Anhydrite 4. Dolomite 5. Halite accumulate in this order
 
 
 
 
 
 
 
 
 
 
Stylolites ,[object Object],[object Object],[object Object],[object Object],A few grains are shown schematically to emphasize the change in scale from the previous figure ( after Bruce Railsback ) Two-dimensional cross-sectonal views of
Stylolites ,[object Object],[object Object],[object Object],[object Object],Intergranular contacts as seen in thin section
Stylolites After Bruce Railsback
Stylolites After Bruce Railsback
Lecture Conclusions ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
End of the Lecture Lets go for lunch!!!
Global Climate Cycles Global climatic cycles, referenced to geologic periods (yellow), megasequences (light purple), sea level cycles (blue), & volcanic output (dark purple).  (Redrawn & modified L. Waite, 2002 after Fischer, 1984)
Frakes et al. (1992) have alternating cold & warm states ("cool" & "warm" modes) at comparable time scales to Fischer (1984) cycles but propose older portion of Mesozoic greenhouse (Middle Jurassic to Early Cretaceous) has a cool climate, & presence of seasonal ice at higher latitudes (after L. Waite, 2002) Phanerozoic Global Climate History
Copied from Steven Wojtal of Oberlin College
CO2 - Temperature & Pressure Effect! ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Copied from Steven Wojtal of Oberlin College
Calcium Carbonate - Solubilty  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Copied from Steven Wojtal of Oberlin College
Copied from Suzanne O'Connell   Wesleyan College
Copied from Suzanne O'Connell   Wesleyan College
 
 
 
 
 
 
 

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