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Warming of Ocean and Thermal Expansion. Storage of Water as Ice in Glaciers. Changes in the Rate of Sea-floor Spreading (More hot expanded young ocean crust at MOR’s). Collision Orogeny (Reduction of area of continental crust). Sediment Transfer into Oceans (Reduces volume of ocean basins).
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Changes in the Rate of Sea-floor Spreading (More hot expanded young ocean crust at MOR’s)
Collision Orogeny (Reduction of area of continental crust)
Sediment Transfer into Oceans (Reduces volume of ocean basins)
Pangaea ~250 mya Pannotia ~550 mya
Changes in the Rate of Sea-floor Spreading Collision Orogeny Sediment Transfer into Oceans
Collision Orogeny (Reduction of area of continental crust)
Pangaea Pannotia
Changes in the Rate of Sea-floor Spreading Collision Orogeny Sediment Transfer into Oceans
Changes in the Rate of Sea-floor Spreading Sediment Transfer into Oceans
Rapid Sea Floor Spreading Sediment Transfer into Oceans Pangaea Rapid Sea Floor Spreading Sediment Transfer into Oceans Pannotia
Rapid Sea Floor Spreading Sediment Transfer into Oceans Pangaea Rapid Sea Floor Spreading Sediment Transfer into Oceans Pannotia
Changes in the Rate of Sea-floor Spreading Collision Orogeny
Slower Sea Floor Spreading Orogeny Orogeny Rapid Sea Floor Spreading Sediment Transfer into Oceans Pangaea Orogeny Orogeny Slower Sea Floor Spreading Orogeny Orogeny Rapid Sea Floor Spreading Sediment Transfer into Oceans Pannotia
Slower Sea Floor Spreading Orogeny Orogeny Rapid Sea Floor Spreading Sediment Transfer into Oceans Pangaea Orogeny Orogeny Slower Sea Floor Spreading Orogeny Orogeny Rapid Sea Floor Spreading Sediment Transfer into Oceans Pannotia
Sediment Transfer into Oceans (Reduces volume of ocean basins)