Carbonate margins and reefs Flashcards

(32 cards)

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?

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
Describe the reef front
Highest point on the reef to the seaward depth where little/no frame-building (up to 100m)
26
Describe the reef crest
The highest, most exposed part of the reef Very high energy (bioerosion and skeletal breakage is high)
27
Describe the organisms at the reef crest
Dominated by encrusting organisms e.g. red algae, usually coating dead coral/coral debris May be encrusted by forams, gastropods
28
Why is there low preservation potential at the reef front?
Bioerosion and early diagenesis
29
Describe the structures on the reef front
In the higher energy zones, spur and groove structures form oblique to the shoreline
30
Describe sedimentation at the fore reef slope
Positioned seaward of the reef front, transition to basin Sedimentation dominated by gravity flow and deposition of pelagic sediments
31
Describe the reef flat
Sand apron Reworked reef debris and carbonate sand Colonisation by sea grass and algal mats Some coral growth
32
What has caused the change in the composition of skeletal components of carbonates through time?
Evolution, extinction events, ocean chemistry, continental configuration