Lecture 11 Shallow water carbonates Part 2 Flashcards

1
Q

Fossils are abundent inlimestone, what are the three key points about them

A

Diversity, Morpology and evolution

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2
Q

What do high diversity fossil content indicate?

A

Stable conditions

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3
Q

What does low diversity fossil content indicate

A

Intial colonization or

Unpredictable stressful environment (temp, salinity, light levels)

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4
Q

What does fosil morpohogy show?

A

it gives an idication of where the fossil lived (ed marine and non marine sepcies, this shell of deep water vs thick shell of tidal) Trace burrows, body size (related to temp - climate indicator) Coral morpoholgy - where did they form on the reef

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5
Q

why is coral morphology useful

A

Use for reconstructing the reef type and hence overall morpoholgy for a trap for oil

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6
Q

what are framwork builders?

A

THese construct the structures of framework reefs, in the past these inlcudded stromatolites and cyanobactieral.

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7
Q

Case study in the UK

A

Carboniferious Limestone in UK

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8
Q

What is this case study

A

A wallconstructed of reef buildnig organisms, including a fore-reef, back reef, and a wall. Structure is similar to modern day examples but the bioenigeneers were not

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9
Q

How were these reefs built?

A

Largely built by algea, with some coral
Little detrail sediment
Diverse fossil assembalages

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10
Q

What are the properties of a palaeoenviroment

A

Shallow water
Clear well lit water
Warm stable climate with nutrient supply

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11
Q

What are the major two minerals of calcium carbonate

A

Aragonite (more compact dense)

Calcite (more open, less soluble in water)

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12
Q

relationship between the two

A

fossils or orgaisms that were orginally aragonite are often preserved as calcite

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13
Q

What are the two chemical controls

A

Carbon doixide levels

Seawater Mg/Ca ratio (most important)

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14
Q

What do calcite seas show

A
High seafllor spreading rates
high pCO2
High sea level
warm 
low sewater mg/ca ration
GREENHOUSE
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15
Q

What do aragnoite seas show

A
Slow seafloor spreading
low pCO2
Low sea levels
Cold
High seawater mg/ca ratio
ICEHOUSE
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16
Q

There is more stuff on this lecture

A

Which i am not going to be able to remember anyways