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Discover the diverse sedimentary archives found in marine environments, ranging from continental shelves to deep abyssal plains. Explore the unique characteristics of each zone, from the smooth continental shelf to the steep continental slope and the depths of the abyssal plain. Learn about the formation of deltas, barrier islands, lagoons, and tidal flats, each hosting a variety of sediments and marine organisms.
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SEDIMENTARY ARCHIVES Marine Environment
SEDIMENTARY ARCHIVES Marine Environment Continental Shelf Flat, smooth regions that fringe continents Few km to 300 km wide Low tide to 200 m depth Similar to continental deposits Shelf planed off by changes in sea level
SEDIMENTARY ARCHIVES Marine Environment Continental Shelf Most eroded continental material ends up here Primarily sand, silt, clay Carbonates develop where clastic influx is low In shallow marine biologic impact is great
SEDIMENTARY ARCHIVES Marine Environment
SEDIMENTARY ARCHIVES Marine Environment Steeper slope than shelf 300 to 3200 m deep Zone of erosion as material from shelf moves to abyssal plain Turbidity currents (Waterville Fm.) Mostly fine sand, silt, clay Continental Slope
SEDIMENTARY ARCHIVES Marine Environment Continental Slope Turbidity Currents
SEDIMENTARY ARCHIVES Marine Environment More gradual slope at base of continental slope Continental Rise
SEDIMENTARY ARCHIVES Marine Environment Depths >3200 m Only fine clay, volcanic ash and calcareous and siliceous oozes accumulate Carbonate compensation depth Oozes are skeletal remains Coarse-grains Slumps Ice-rafted debris Deep Marine – Abyssal Plain
SEDIMENTARY ARCHIVES Transitional Environments Represents the margin between the oceans and contintents (Shorelines and coasts) Clastic sediments
SEDIMENTARY ARCHIVES Transitional Environment Carbonate sediments
SEDIMENTARY ARCHIVES Transitional Environment Deltas Δ
SEDIMENTARY ARCHIVES Transitional Environment Mississippi River Delta Deltas Prograding Delta Deposition > Erosion Upward progression of fines to coarse Subsiding basin Contain organic matter Petroleum producing
SEDIMENTARY ARCHIVES Transitional Environment Deltas
SEDIMENTARY ARCHIVES Transitional Environment Deltas Deposition = Erosion Concentric enlargement of delta Niger River Delta
SEDIMENTARY ARCHIVES Transitional Environment Deltas Erosion > Deposition No visible delta Kennebec River
SEDIMENTARY ARCHIVES Transitional Environment Barrier Islands
SEDIMENTARY ARCHIVES Transitional Environment Usually sandy Organisms include bivalves, gastropods, echinoids, and crustaceans Barrier Islands
SEDIMENTARY ARCHIVES Transitional Environment Lagoon Shallow areas land- ward of barrier islands Can be protected inlets Sediments usually silty
SEDIMENTARY ARCHIVES Transitional Environment Lagoon
SEDIMENTARY ARCHIVES Transitional Environment Tidal Flats
SEDIMENTARY ARCHIVES Transitional Environment Tidal Flats Exposed and covered by tides Harsh environment Alternating wet and dry Generally fine-grained Diversity is low Includes bivalves, gastropods, crustaceans, worms, and cyanobacteria