Lecture 14 - Deep Sea Sediments part 2 Flashcards

1
Q

What are calcerious oozes formed of?

A

Calcium carbonate

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2
Q

What makes this calcium carbonate

A

Coccolithophers ( algea, nanofossils, photic zone)
Foraminferua (unicelluar zoo plankton )
Pteropods (panktotic gastropods, surface waters)

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3
Q

Properties of calcerious ooze

A

More souble in cold waters, high pressure, acidic water

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4
Q

what controls the distribution of calcerious oozes

A

The same as before, plankton live in surface, then die and sink. Bacteria oxidse organic matter relaesing co2

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5
Q

What is needed for carcluim carbonate preseration

A

It occours in warmed shallower waters

atlanitc ocean more than pacific

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6
Q

Explain the calcite compesation depth

A

This is the depth at which no calcite can be preserved in ocean sediments. Above the CCD the rain rater is greater than the dissoultion and below its reverse

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7
Q

What is the Climap project?

A

looks at how diferent was the eath during the last glcial maximum

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8
Q

What was different back then

A

High lat ice sheets to do not directly effect the tropical temps, lower tropic temps as a result of CO2.

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9
Q

What did the climap project use?

A

it use calcite deposits in sedimentary records to calculate the temp and depth of the sea water

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10
Q

what is the MARGO protect

A

Combined lots of different work with modern geochemical techniques

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11
Q

What are terrigenous sediments

A

Weathing and erosion of land ares whichh is gravels and sands etc, sediments are transported to the ocean by rivers and deposited on the shelves and slopes

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12
Q

What is ice rafted debris

A

Sediment is transported by ice berg and is dropped when the ice berg melts, therefore they are subject to sediment source and ocean currents

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13
Q

During ice house worlds what is depleted in sea waterq

A

Oxygen - 16

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14
Q

In green house world what is seawater enriched in?

A

oxygen - 16

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15
Q

What can these oxygen isotopes tell us

A

THey can be used to study the earths climate histrory

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