Ichnology Flashcards

(51 cards)

1
Q

What are ichnofossils and how are they formed?

A

Trace fossils formed by the movement of organisms

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2
Q

What do ichnofossils show and what can they be used to determine?

A

They represent activity of soft-bodied organisms and can be used to determine current velocity, sedimentation rate, and strength of substrate.

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3
Q

Where are boring ichnofossils usually found?

A

High energy, rocky coastlines

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4
Q

Where are simple burrow ichnofossils usually found?

A

Sandy shores

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5
Q

Where are organisms that live and graze on the surface usually found?

A

Low energy offshore and deepwater environments

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6
Q

How are ichnofossils classified?

A

Ichnogenus, ichnospecies (Linnean binomials)

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7
Q

How can one organism produce different types of ichnofossils in its life?

A

Different activities and different substrates

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8
Q

What is the name for locomotion traces?

A

Repichnia

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9
Q

What is the name for resting traces?

A

Cubichnia

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10
Q

What is the name for dwelling traces?

A

Domichnia

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11
Q

What is the name for feeding burrows?

A

Fodinichnia

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12
Q

What is the name for grazing traces?

A

Pascichnia

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13
Q

Describe dwelling traces

A

Cylindrical tubes with minor branching

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14
Q

Name and describe the two different types of dwelling traces

A

Borings made into hard or semiarid substrate (rock). Burrows made into soft substrate (unconsolidated sand).

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15
Q

What can feeding burrows do and what can they show?

A

They can cross bedding surfaces and the complex patterns represent mining behaviour

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16
Q

What do repeating patterns in grazing traces show?

A

A systematic feeding strategy

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17
Q

FOSSIL ROOTS ARE NOT TRACE FOSSILS

A

Got that?

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18
Q

What are fossil roots diagnostic of?

A

The terrestrial depositional environment

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19
Q

Describe the morphology of fossil roots

A

Highly irregular and downward branching

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20
Q

What can bright colours in sedimentary rocks indicate?

A

Clays (broken down micas and feldspars) and organic material

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21
Q

Define diagenesis

A

The process of loose sediment becoming rock.

22
Q

What does diagenesis destroy?

23
Q

Describe the conditions of diagenesis

A

Begins at surface temperature and pressure and continues as T and P increases.

24
Q

Give the names for early and late diagenesis

A

Eodiagenetic and mesodiagenetic

25
What is bioturbation?
The disturbance of sedimentary structures by organisms
26
Give an example of bioturbation and what it results in
The consumption and excretion of sediment that can change the composition of some clays
27
Describe a eodiagenetic bioturbation
The mechanical and chemical activities of organisms buried near the surface sediment
28
What does the churning and homogenising of sediment result in?
The reduction of deposition barriers to flow in reservoirs
29
What causes mechanical compaction?
Overburden
30
What are two eodiagenetic processes that occur in mechanical compaction?
Grains are rotated to reduce volume and water is expelled upwards
31
Describe the formation of sandstone dykes
Water is explosively expelled upwards after a sudden, large compaction
32
Why types of grains can be highly compacted and why?
Silts and clays have platy morphology and can be compacted up to 90%.
33
What type of grain cannot be highly compacted and why?
Sand because it is mostly quartz, which is often round.
34
What mesodiagenetic process allows further compaction after the rotation of grains?
Mechanical fractioning of the grains
35
What type of process is pressure solution?
Mesodiagenetic
36
Describe the process of pressure solution
The material at the grain contacts (perpendicular to compaction) dissolves. This reprecipitates as cement at contacts that are perpendicular to compaction. Porosity is lost.
37
What causes dissolution?
Changes in temperature and pressure and/or composition of porewater
38
When is a mineral more stable?
In a solution
39
Where does dissolution without reprecipitation occur?
In systems that are subject prolonged pumping of exotic porewater with an abundant fresh supply
40
Describe the process of cementation
Chemical precipitates, forming new crystals in the mores of a sediment/rock, binding the grains together
41
What types of sources can the precipitate have during cementation?
Local or external
42
What are concretions?
Spherical masses of sediment that are more strongly cemented than the surrounding volume
43
What grain size do concretions have compared to the surrounding?
The same
44
What are concretions associated with?
Organic material that reacts with the surrounding chemistry
45
Give an example of a concretion produced by organic material
Iron found in organic matter that forms iron carbonate concretions
46
What is recrystallisation?
The reorientation of the same crystal lattices in mineral grains
47
What processes are involved in recrystallisation?
Solution and reprecipitation of the mineral phase already present
48
Where is the process of recrystallisation commonly seen?
Carbonate shells
49
What is mineral replacement?
Where a newly formed minerals replace preexisting ones in situ
50
How can the new minerals be different to the original mineral?
It can be a polymorph
51
How does mineral replacement affect pore space?
The new structure can have a different volume