Biogenic Sedimentary Structures Flashcards

1
Q

Trace fossil

A

Sedimentary structure formes due to the activity of organisms

Mostly macro organisms, but smallest scale effects of Bioturbation approach “grain size”

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What is Ichnology?

A

Study of traces and trace fossils

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Bioturbation

A

Reworking of sediment by organisms
Post-deposition disruption

The disturbance of sediments due to biological activity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Burrows vs Boring

A

Burrows are tunnels in soft/loose substrate

Borings (bioerosion) are holes/ openings in HARD/firm substrate

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Track vs Trails

A

Tracks are series of discrete impressions in the sediment

Trail is one continuous disturbance in the sediment (slimes)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Examples of Bioturbation

A
Boring
Burrows 
Track
Trail
Resting place
Feeding traces
Fecal pellets
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

What is a great example (organism) of grazing trace

A

Trilobites

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What dictates the type of Bioturbation happening in an environment?

A

The type of organism and the substrate the organism is moving across

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What is a borer

A

A borer means that the organism can dig through hard substrate. A worm, mollusk, insect, or insect larva that bores into wood, other plant material, or rock. Some snails and mollusks have tongues reinforced with magnetite

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

In terms of trace fossils, what kind of structures you can have?

A

Bioturbation structures (burrows,traces, trails, root penetration structures)

Biostratification structures (algal stromatolites, graded bedding of biogenic origin)

Bioerosion structures (borings scraping, biting)

Excrement ( coprolites, such as fecal pallets or fecal castings)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

What is the utility of trace fossils?

A

Important paleoecological indicators

Way up indicators!

Environmental interpretation/paleoclimate

Hydrocarbon recovery

Bioturbation can create porosity!! They alter what’s going on in the sedimentary layers altering the movement of fluids in the system

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

How trace fossils are named (taxonomy)?

A

According to the Binomial nomenclature used for organisms!!

Name is given to the shape of the trace ( not the animal/plant/thing that formed it)!!

Relatively rare that ichnofossils can be assigned to a known body fossil

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What are ICHNOFACIES?

!!!

A

Is an assemblage of trace fossils that provide an indication of the environment conditions that their formative organism inhibit.

Or a group of ichnofossils associated with:

Bathymetry
Energy conditions
Sediment regimes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Bathymetry

A

The measurement of depth of water in oceans, seas, or lakes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What kind of information can ICHNOFACIES give us?

A

How deep it is

How energetic was the conditions of the system

What is the sediment regime

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

What is ichnogenera?

A

Is the plural of ichnogenus, which is the name of the trace fossil

17
Q

What is the difference between ICHNOFACIES and ichnogenus?

A

Ichnofacies is an assemblage of ichnofossils associated with a particular environment (bathymetry, energy conditions, and sedimentation regimes)

Ichnogenus is the name of the ichnofossil. ( like Homo Sapiens).

18
Q

How important or how depth controls the type of ichnofossils with will find in the rock record?

With depth we have…

A
Less Biomass
Salinity (change with depth and also temperature)!
Light levels
Decreased O2 levels
Decreased Energy levels

But it is not a dead zone!

19
Q

Why there are not a lot of vertebrate tracks outside the shallow waters?
!!!

A

Because they tend to be swimming, so they don’t leave a lot of traces ( eg. fish)

20
Q

Why there are more burrows on relative shallow than in deep waters?

A

More Biomass! And because organisms can sit and wait for food

21
Q

Why there are more trails on deep/abyssal waters?

A

Because the organism has to find food. Scarce biomass on the deep abyssal zone

22
Q

What type of trace/ structure is created after the occurrence of mass movements/ turbidity flows and underwater landslides?

A

Scape structures

23
Q

Can you define a ICHNOFACIE baseon on trace?

A

NO. Tou have to look at different ichnofossils. E.g Zoophycus ichnogenus appears in 5 different ichnofacies. You name it based on the assemblage.

24
Q

What ICHNOFACIES represent? What tipe of information can you infer from them?
!!!

A
Different micro environments
Energy distribution 
Nutrient distribution 
Temperature 
Substrate expectations
25
Q

What is a facies?

A

A body of rock with a specific characteristic