Essentials of Oceanography Chap 4 Flashcards

1
Q

How do deep ocean basin sediments form

A

suspension settling leads to fine particles sinking to the bottom of the ocean

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2
Q

What is ocean basin sediment connection to sedimentary rock on land

A

A lot of the sedimentary rock on land was formed by suspension settling in ocean basins and later uplift.

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3
Q

What is north atlantic deep water circulation

A

North Atlantic Ocean, cold, relatively salty water sinks, which circulates through the global ocean, driving deep-ocean circulation and global
heat transport

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4
Q

what mineral is the main composer of lithogenous sediment

A

Quartz

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5
Q

2 types of marine deposits

A

neritic and pelagic

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6
Q

what are neritic deposits

A

Near coast deposits on continental shelves and in shallow waters. Usually coarse grained due to high energy.

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7
Q

What are pelagic deposits

A

Deep-Ocean basin deposits, fine sediments due to low energy.

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8
Q

Why are a lot of continental shelf deposits only composed of sediment from 3-7 thousand years ago

A

10,000 years ago, after the glaciers melted, river mouths were drowned and led to less sediment transported to the ocean as the sediment would be dropped at these drowned river mouths.

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9
Q

What are biogenous marine deposits

A

rock formed of the hard parts of marine organisms

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10
Q

What is biogenous ooze

A

fine grained, soft biogenous deposit

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11
Q

2 most common chemical compounds in biogenous ooze

A

Silica and calcium carbonate.

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12
Q

What are the organisms that form biogenous ooze

A

Algae(marine plants) and Protozoans( marine animals)

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13
Q

What organisms form silica in biogenous ooze

A

diatoms(algae) and radiolarians(protozoan)

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14
Q

What is diatomaceous earth

A

when diatom rich ooze lithifies, it forms into a white soft rock

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15
Q

What is siliceous ooze

A

ooze primarily formed of diatoms and radiolarians

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16
Q

2 organisms that form calcareous ooze

A

foraminifers(protozoan) and coccolithophores(algae)

17
Q

What does coccolith rich calcareous ooze often lithify into

18
Q

How large are coccoliths

A

extremely small

19
Q

Where does most carbonate and calcareous ooze deposits form

A

shallow waters

20
Q

What happens to most silica in the ocean

A

Dissolves in ocean water

21
Q

How does siliceous ooze form

A

areas of high biological activity of silica-secreting organisms. This is because if only a small amount of silica-secreting organisms sinks to the sea floor, it will constantly get dissolved.

22
Q

where does calcite dissolve in oceans

A

Deeper waters, as colder water contains more carbon dioxide. Furthermore, higher pressure speeds up the dissolution of calcite.

23
Q

What is the lysocline

A

depth at which the rate of dissolution of calcite begins to increase dramatically.

24
Q

Do calcite secreting organisms live in cold or warm water

A

warm water

25
Q

Do silica-secreting organisms live in cold or warm water

A

cold water.

26
Q

What structure do calcareous ooze like to form around

A

Mid-ocean ridges to do increased elevation on the crest and warm waters due to the mid-ocean ridge

27
Q

What mechanism leads to increase in silica-secreting organisms locally

A

upwelling, as cold, nutrient dense water rises.

28
Q

What is hydrogenous sediment

A

sediment derived from dissolved material precipitating from water

29
Q

when does precipitation occur

A

change in conditions, such as a change in temperature or pressure or the addition of chemically active fluids.

30
Q

What is cosmogenous sediment

A

extraterrestrial sediment

31
Q

2 main types of cosmogenous sediment

A

spherules and meteor debris

32
Q

How thick is the layer of sediment in mid-ocean ridges

A

thin. the older the sea floor, the thicker the layer of sediment