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Questions and Answers
What is the calcium carbonate compensation depth?
What is the calcium carbonate compensation depth?
- The depth at which sediment contains high levels of calcium carbonate.
- The deepest part of the ocean.
- The depth below which all sediments are siliceous.
- The depth at which the rate of accumulation of calcareous sediments equals the rate of dissolution of those sediments. (correct)
What is biogenous sediment?
What is biogenous sediment?
Sediment of biological origin.
What is calcareous ooze primarily composed of?
What is calcareous ooze primarily composed of?
Hard remains of organisms containing calcium carbonate.
What is the size of clay sediment particles?
What is the size of clay sediment particles?
What are coccolithophores?
What are coccolithophores?
What type of sediment is cosmogenous sediment?
What type of sediment is cosmogenous sediment?
What are diatoms?
What are diatoms?
What is a foraminiferan?
What is a foraminiferan?
What is lithification?
What is lithification?
What are microtektites?
What are microtektites?
What is neritic sediment?
What is neritic sediment?
What is a nodule in oceanography?
What is a nodule in oceanography?
What defines ooze in ocean sediment?
What defines ooze in ocean sediment?
What are pelagic sediments?
What are pelagic sediments?
What is a piston corer?
What is a piston corer?
What is a radiolarian?
What is a radiolarian?
What size are sand sediment particles?
What size are sand sediment particles?
What are sediments?
What are sediments?
What is siliceous ooze composed of?
What is siliceous ooze composed of?
What is the size range of silt particles?
What is the size range of silt particles?
What is terrigenous sediment?
What is terrigenous sediment?
What is a turbidite?
What is a turbidite?
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Study Notes
Key Terms in Oceanography
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Calcium Carbonate Compensation Depth (CCD): Depth where accumulation of calcareous sediments balances dissolution; below this, sediments lack calcium carbonate.
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Biogenous Sediment: Sediments originating from biological sources, which can include calcareous or siliceous residues from organisms.
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Calcareous Ooze: A type of ooze primarily made up of calcium carbonate from the remains of marine organisms.
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Clay: The smallest sediment particle, measuring less than 0.004 millimeters in diameter.
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Coccolithophore: Tiny planktonic algae that produce calcium carbonate discs, contributing to biogenous sediments.
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Cosmogenous Sediment: Sediments that originate from extraterrestrial sources, such as meteorites.
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Diatom: Dominant single-celled phytoplankton with silica-based valves; contributes significantly to biogenous sediments.
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Foraminiferan: Planktonic, amoeba-like organisms with calcareous shells, playing a role in biogenous sediment formation.
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Lithification: Process in which sediments transform into sedimentary rock via pressure or mineral cementation.
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Microtektites: Small, glassy particles of cosmic origin found in cosmogenous sediments.
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Neritic Sediment: Deposits mainly found on continental shelves, primarily composed of terrigenous (land-derived) materials.
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Nodule: A compact mass of hydrogenous sediment, commonly made of manganese or phosphorite.
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Ooze: A sediment that consists of at least 30% biological material.
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Pelagic Sediment: Sediments found on the ocean floor, from the slope, rise, and deep-sea regions, sourced from oceanic processes.
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Piston Corer: Equipment used for seabed sampling that penetrates up to 25 meters of sediment to collect intact samples.
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Radiolarian: Planktonic organisms with siliceous shells contributing to biogenous sediment.
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Sand: Sediment particles ranging from 0.062 to 2 millimeters in diameter.
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Sediment: Accumulated particles of organic or inorganic materials in a loose, unconsolidated state.
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Siliceous Ooze: Ooze primarily composed of silica-based remains from organisms.
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Silt: Sediment particles with diameters between 0.004 and 0.062 millimeters.
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Terrigenous Sediment: Sediments originating from land, transported to oceans by natural processes like wind and water flow.
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Turbidite: Sediment deposited by turbidity currents, characterized by alternating layers of coarse and fine materials.
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