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Marine Sediments Types (Detailed)
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Marine Sediments Types (Detailed)
1.
Diatoms Photosynthetic algae Diatomaceous earth Radiolarians Protozoans Use external food © 2011 Pearson Education, Inc.
2.
Tests from diatoms and radiolarians generate siliceous ooze. © 2011 Pearson Education, Inc.
3.
Coccolithophores Also called nannoplankton Photosynthetic algae Coccoliths – individual plates from dead organism Rock chalk Lithified coccolith- rich ooze © 2011 Pearson Education, Inc.
4.
Foraminifera Protozoans Use external food Calcareous ooze © 2011 Pearson Education, Inc.
5.
Depends on three processes: Productivity Destruction Dilution © 2011 Pearson Education, Inc.
6.
Dominated by lithogenous sediment, may contain biogenous sediment Carbonate Deposits Carbonate minerals containing carbon trioxide (CO3 ) Marine carbonates primarily limestone – CaCO3 Most limestones contain fossil shells Suggests biogenous origin Ancient marine carbonates constitute 25% of all sedimentary rocks on Earth. © 2011 Pearson Education, Inc.
7.
Stromatolites Fine layers of carbonate Warm, shallow- ocean, high salinity Cyanobacteria © 2011 Pearson Education, Inc.
8.
© 2011 Pearson
Education, Inc.
9.
© 2011 Pearson
Education, Inc.
10.
Minerals precipitate directly from seawater Manganese nodules Phosphates Carbonates Metal sulfides Small proportion of marine sediments Distributed in diverse environments © 2011 Pearson Education, Inc.
11.
Fist-sized lumps of manganese, iron, an d other metals Very slow accumulation rates Grows ~1 centimeter over several million years Many commercial uses © 2011 Pearson Education, Inc.
12.
Phosphates Phosphorus-bearing Occur beneath areas in surface ocean of very high biological productivity Economically useful as fertilizer Carbonates Aragonite and calcite Oolites © 2011 Pearson Education, Inc.
13.
Metal sulfides Contain: Iron Nickel Copper Zinc Silver Other metals Associated with hydrothermal vents © 2011 Pearson Education, Inc.
14.
Evaporites Minerals that form when seawater evaporates Restricted open ocean circulation High evaporation rates Halite (common table salt) and gypsum © 2011 Pearson Education, Inc.
15.
Macroscopic meteor debris Microscopic iron- nickel and silicate spherules (small globular masses) Tektites Space dust Overall, insignifica nt proportion of marine sediments © 2011 Pearson Education, Inc.
16.
© 2011 Pearson
Education, Inc.
17.
Energy resources Petroleum Mainly from continental shelves Gas hydrates Sand and gravel (including tin, gold, and so on) Evaporative salts Phosphorite Manganese nodules and crusts © 2011 Pearson Education, Inc.
18.
© 2011 Pearson
Education, Inc.
19.
© 2011 Pearson
Education, Inc.
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