Carbonate margins and reefs Flashcards

1
Q

Define carbonate build-ups

A

Laterally-restricted structures that have usually undergone organically-mediated growth

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2
Q

What are the two subdivision of carbonate build ups?

A

Organic (skeletal) reefs
Reef (mud) mounds

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3
Q

Describe organic (skeletal) reefs

A

Built by organisms with a rigid calcareous frame
Matrix or skeleton supported
Deposited in warm/cold water
Able to withstand high energy wind/wave action

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4
Q

Describe reef (mud) mounds

A

Inorganically and/or biogenically constructed
Lack rigid skeletal framework and unable to withstand high energy wind/wave action

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5
Q

Describe the structure of mud mounds

A

Mud (micrite)-dominated
Stability provided by matrix
Limited cementation
Low topographic relief

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6
Q

When were mud mounds common and why?

A

Palaeozoic
Skeletal frame builders were absent or in deeper water

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7
Q

Give examples of organic components in mud mounds

A

Bivalves, corals, sponges, bryozo, microbrobes

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8
Q

Where do reefs preferentially develop?

A

On topographic highs
e.g. older reefs, karst, volcanic features

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9
Q

Describe the constructive processes of reefs

A

Biological processes though direct growth, baffling, or binding

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10
Q

Describe destructive processes of reefs

A

Wave damage and biological destruction

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11
Q

Describe cementation of reefs

A

Early cementation from sea water

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12
Q

Describe sedimentation of reefs

A

Accumulation of biogenic matter and reef-derived detritus

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13
Q

What is the most contributing type of organism in frame built carbonates?

A

Frame-builders
Corals

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14
Q

What is the most contributing type of organism in mud mounds?

A

Precipitators
Microbial mats

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15
Q

What are the four stages of the Oxfordian reef ecological succession?

A

Pioneer, colonisation, diversification, domination

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16
Q

What conditions are required for delicate, branching growth forms?

A

Low wave energy and high sedimentation

17
Q

What conditions are required for globular and columnar growth forms?

A

Moderate wave energy and high sedimentation

18
Q

What conditions are required for encrusting growth forms?

A

Intense wave energy and low sedimentation

19
Q

What facies are seen on the back reef?

A

Bafflestone, floatstone

20
Q

What facies are seen on the reef flat?

A

Rudstone, grainstone

21
Q

What facies are seen on the reef crest?

A

Bindstone

22
Q

What facies are seen on the reef front?

A

Framstone, bindstone, bafflestone

23
Q

What facies are seen on the fore reef?

A

Grainstone, rudstone

24
Q

What types of growth forms are seen on the reef front? In order as you go down the front

A

Encrusting, massive, branching, plate-like

25
Q

Describe the reef front

A

Highest point on the reef to the seaward depth where little/no frame-building (up to 100m)

26
Q

Describe the reef crest

A

The highest, most exposed part of the reef
Very high energy (bioerosion and skeletal breakage is high)

27
Q

Describe the organisms at the reef crest

A

Dominated by encrusting organisms
e.g. red algae, usually coating dead coral/coral debris
May be encrusted by forams, gastropods

28
Q

Why is there low preservation potential at the reef front?

A

Bioerosion and early diagenesis

29
Q

Describe the structures on the reef front

A

In the higher energy zones, spur and groove structures form oblique to the shoreline

30
Q

Describe sedimentation at the fore reef slope

A

Positioned seaward of the reef front, transition to basin
Sedimentation dominated by gravity flow and deposition of pelagic sediments

31
Q

Describe the reef flat

A

Sand apron
Reworked reef debris and carbonate sand
Colonisation by sea grass and algal mats
Some coral growth

32
Q

What has caused the change in the composition of skeletal components of carbonates through time?

A

Evolution, extinction events, ocean chemistry, continental configuration