Marine Sediments Flashcards

1
Q

why marine sediments are interesting to oceanographers.

A

Reveals Earth’s history.
Provides clues to past geographic distributions of marine organisms, movements of the ocean floor, ocean circulation patterns climate changes on Earth and global extinction.

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2
Q

four primary types of marine sediment

A

Lithogenous
Biogenous
Hydrogenous
Cosmogenous

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3
Q

List the past conditions that scientists can infer by analyzing marine sediments.

A
Sea surface Temperature
Nutrient supply
abundance of marine life
atmospheric winds
ocean current patterns
volcanic eruptions
major extinction events 
changes in Earth’s climate
movement of tectonic plates
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4
Q

paleoceanography

A

The study of how the ocean, atmosphere, and land have interacted to produce changes in ocean chemistry, circulation, biology and climate.

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5
Q

lithogenous sediment

A

Derived from pre-existing rock material that originates on the continents of islands from erosion, volcanic eruptions, or blown dust. Also referred to as terrigenous sediment.

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6
Q

Characteristics of Lithogenous Sediment

A

dsaf

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7
Q

List the transportation mechanism that carry sediment to the ocean

A

Streams, wind, glaciers, and gravity.

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8
Q

List the submarine transportation mechanisms that carry sediment beyond the continental margin

A

Turbidity currents

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9
Q

In which marine region do the largest marine sedimentary deposits form

A

Around the margins of the continents.

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10
Q

why most lithogenous particles, including most sand (but not Hawai’i sand), are quartz

A

Quartz is a major component of most rocks and since it is resistant to abrasion it can be transported long distances.

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11
Q

the primary sediment transportation mechanism from the Sahara Desert to the ocean.

A

Prevailing winds

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12
Q

list the primary sediment sizes from coarse-grained to fine-grained.

A

Boulder, cobble, pebble, granule, sand, silt, clay

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13
Q

why lithogenous sediments tend to become finer with increasing distance from shore.

A

Because high-energy transporting media predominate close to shore and lower-energy conditions exist in the deep-ocean basins.

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14
Q

Define well-sorted sediment and poorly-sorted sediment.

A

Well-sorted sediment is sediment composed of particle that are primarily the same size whereas poorly-sorted sediment is sediment that is comprised of a variety of differently sized particles.

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15
Q

Define neritic deposits and pelagic deposits.

A

Neritic deposits are found on continental shelves and in shallow water near islands and are generally coarse grained; pelagic deposits are found in deep-ocean basins and are typically fine grained

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16
Q

Decribe the characteristics and formaton of glacial deposits.

A

Poorly-sorted deposits containing particles ranging from boulders to clays may be found in the high-latitude portions of the continental shelf.

17
Q

Describe the characteristics and formation of abyssal clays.

A

70% (by weight) fine, clay sized-particles, composed of particles transported great distances and deposited on the deep ocean floor, and are red-brown due to the oxidized iron it contains.

18
Q

biogenous sediment

A

The remains of hard parts of once-living organisms.

19
Q

Explain why most marine biogenous deposits are called oozes

A

Because marine biogenous deposits resemble fine-grained, mushy material, or ooze.

20
Q

List the two primary biogenous sediment compositions: name and chemical formula.

A

Calcium carbonate (CaCO3) and Silica (SiO2)

21
Q

List two microscopic, planktonic organisms with siliceous tests.

A

Diatoms and radiolarians

22
Q

List two microscopic, planktonic organisms with calcareous tests.

A

Foraminifers and coccolithophores

23
Q

Explain why diatoms and coccolithophores live near the ocean’s surface.

A

They need sunlight because they photosynthesize

24
Q

List the three factors that control the formation of biogenous oozes.

A

Production, destruction, and dilution

25
Q

Explain why biogenous deposits dominate the pelagic sea floor.

A

Because there is so little lithogenous sediment deposited at great distances from the continents that could dilute the biogenous material.

26
Q

List the three dominate siliceous oozes types.

A

Diatomaceous ooze, radiolarian ooze, and silicoflagellate ooze

27
Q

List the two dominate calcarous ooze types.

A

coccolith ooze, foraminifer ooze

28
Q

Explain why calcareous oozes are rarely form on the deep-sea floor.

A

The carbonic acid dissolves calcareous material by the cold waters CO2

29
Q

Define the calcite compensation depth (CCD)

A

The depth at which the amount of calcite produced by the organisms in the overlying water column is equal to the amount of calcite the water column can dissolve. no calcite deposition occurs below this depth

30
Q

Give the average CCD depth

A

4500 m

31
Q

Explain the relationship between upwelling and siliceous deposits.

A

siliceous deposits form below cool surface water regions and upwellings being deep, cld nutrient rich water to the surface.

32
Q

Define hydrogenous sediment

A

sediment that forms from precipitation from ocean water or ion exchange between sediment and ocean water

33
Q

Describe growth of a Mn nodules

A

requires extremely low rates of lithogenous nodules or biogenous input so that the nodes are not buried

34
Q

Give the average Mn nodule growth rate.

A

5mm per million of years