1. Marine Sedimentation

2. Streams
Rivers

3. Glaciers

4. Landslide
(Gravity)

5. Marine Sedimentation ?

6. Learning Objectives
1. Understand the origin and classification of marine sediments.
2. Use Hjulstrom’s diagram to explain the erosion, transportation, and deposition of sediments.
3. Explain the factors controlling origin and deposition of sediment on the continental shelf and in the deep ocean.
4. Calculate the rate of sedimentation in the deep sea.

7. Classification of marine sediments can be based upon size or origin.
Sediment in the Sea
4-1
Classification of marine sediments can be based upon size or origin.
Size classification divides sediment by grain size into gravel, sand, silt and clay.
Mud is a mixture of silt and clay.
Origin classification divides sediment into five categories: terrigenous sediments, biogenic sediments, authigenic sediments, volcanogenic sediments and cosmogenic sediments.

8. 4-1
Sediment in the Sea
Factors that control sedimentation include particle size and the turbulence of the depositional environment.
Terrigenous sediments strongly reflect their source and are transported to the sea by wind, rivers and glaciers.
Rate of erosion is important in determining nature of sediments.
Average grain size reflects the energy of the depositional environment.

9. Hjulstrom’s Diagram
Hjulstrom’s Diagram graphs the relationship between particle size and energy for erosion, transportation and deposition.

10. 4-2
Sedimentation in the Ocean
ocean environment can be divided into: the shelf (is shallow and near a terrigenous source) the deep ocean basin (is deep and far from a terrigenous source)

11. Shelf Versus Basin Depths

12. 4-2
Sedimentation in the Ocean
Shelf sedimentation is strongly controlled by tides, waves and currents, but their influence decreases with water depth.
Shoreline turbulence prevents small particles from settling and transports them seaward where they are deposited in deeper water.
Particle size decreases seaward for recent sediments.
Past fluctuations of sea level have stranded coarse sediment (relict sediment) across the shelf including most areas where only fine sediments are deposited today.

13. Model Prediction of Shelf Sediments

14. Influence of Past Sea Level

15. Relict Sediment

16. 4-2
Sedimentation in the Ocean
Worldwide distribution of recent shelf sediments by composition is strongly related to latitude and climate.
Calcareous biogenic sediments dominate tropical shelves.
River-supplied sands and muds dominate temperate shelves.
Glacial till and ice-rafted sediments dominate polar shelves.

17. Shelf Sedimentation Model

18. 4-2
Geologic controls of continental shelf sedimentation must be considered in terms of a time frame.
For a time frame up to 1000 years, waves, currents and tides control sedimentation.
For a time frame up to 1,000,000 years, sea level lowered by glaciation controlled sedimentation and caused rivers to deposit their sediments at the shelf edge and onto the upper continental slope.
For a time frame up to 100,000,000 years, plate tectonics has determined the type of margin that developed and controlled sedimentation.

20. Case study:
The Atlantic Passive Margin

21. Case study:
Pacific Destructive/Subduction Margin

22. Carbonate Shelves
If influx of terrigenous sediment is low and the water is warm, carbonate sediments and reefs will dominate.

23. Sedimentation in the Ocean
4-2
Sedimentation in the Ocean
Deep-sea Sedimentation has two main sources of sediment: external- terrigenous material from the land and internal-biogenic and authigenic from the sea.
Red Clays:
Kaolinite
Chlorite
Quartz
Feldspar
Sedimentation in the Deep Sea

24. Major pelagic sediments in the ocean are red clay and biogenic oozes.
4-2
Sedimentation in the Ocean
Major sedimentary processes in the deep sea include:, Bulk emplacement, Debris flows, Turbidity currents
Major pelagic sediments in the ocean are red clay and biogenic oozes.
Authigenic deposits are chemical and biochemical precipitates that form on the sea floor and include ferromanganese nodules and phosphorite (in general: metal rich sediments. Hydrothermal circulation is the controlling factor).

26. Ice Rafting

27. Biogenic Deposits
Silica
Carbonate

28. Figure 5-14

29. Figure 5-15

30. Figure 5-16

31. Figure 5-17

32. Authigenic Deposits
from precipitation of metal oxides

33. Distribution of sediments in the deep ocean
4-2
1) latitude 2) distance from landmasses 3) CCD (carbonate compensation depth)
Glacial marine sediments occur in the high latitudes.
Pelagic clays occur far from land and in the deepest water.
Calcareous oozes occur above the calcium carbonate composition depth.
The rate of sedimentation depends on the type of sediment in deep sea.

35. 4-2
Sedimentation in the Ocean
Deep-sea stratigraphy refers to the broad- scale layering of sediments that cover the basaltic crust. The stratigraphy of the deep sea is strongly influenced by sea-floor spreading.

36. 4-2
Sedimentation in the Ocean
The Atlantic basin contains a “two-layer-cake” stratigraphy–a thick basal layer of carbonate ooze overlain by a layer of mud.
Stratigraphy of the Atlantic Basin

37. 4-2
Sedimentation in the Ocean
The Pacific basin contains a “four-layer-cake” stratigraphy, because unlike the Atlantic its sea floor while spreading crosses the equator where the CCD is lower (5000m instead of m)

39. Stratigraphy and Model of Pacific Basin

40. 4-3
Collecting Marine Sediment
There are a number of sampling techniques for obtaining sediment from the ocean bottom.
Bottom dredges scrape the sediment and collect material in a wire or canvas bag.
Grab samplers take a “bite” out of the sediment covering the bottom.
Gravity and piston corers use a weight to drive a core barrel into a soft bottom. A piston corer takes a much longer core than a gravity corer because of the piston in the core barrel.

41. The Drying Up of the Mediterranean Sea
4-4
The Mediterranean basin is located where plates are colliding as Africa moves northward relative to Europe.
Anhydrite and stromatolites of Miocene age indicate that the Mediterranean sea “dried” out between 5 and 25 million years ago.
Two models have been suggested to account for this emptying of the Mediterranean Sea of its water.
The “Uplift” Model
The “Drying-Out” Model

42. Refilling the Mediterranean Sea
After drying out, seawater from the Atlantic Ocean cascaded down the face of the Gibraltar Sill, refilling it in about 100 years.