Week 6 - Microfossils Flashcards

1
Q

What are the main learning outcomes of microfossil studies?

A

Constructing age-depth models, calculating sedimentation rates, identifying breaks in sedimentation, and understanding biostratigraphy.

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2
Q

What defines a microfossil?

A

Any fossilized part of an organism (usually skeletal) ranging from <1 μm to >1 mm in size.

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3
Q

What are the two main types of microfossils based on cellular structure?

A

Single-celled (e.g., radiolarians, foraminifera) and multicellular (e.g., ostracods).

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4
Q

How do microfossils obtain energy?

A

They can be photosynthetic (e.g., diatoms, coccolithophores)

heterotrophic (e.g., foraminifera, radiolarians),

or a combination of both.

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5
Q

What are the different scales used to measure microfossils?

A

1000 μm (1 mm): Visible to the eye, microscope needed for details.

100 μm (0.1 mm): Invisible to the eye, requires a light microscope.

1 μm (1000 nm): Requires high magnification (light or electron microscopes).

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6
Q

What are the three main uses of microfossils in geology?

A

Biostratigraphy – Dating rocks by identifying fossil species.

Palaeoclimate/Palaeoenvironment – Reconstructing past climate and ocean conditions.

Evolutionary Studies – Understanding evolutionary history through fossil records.

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7
Q

What are the three main types of microfossils based on composition?

A

Calcareous (CaCO₃) – Foraminifera, calcareous nannofossils, ostracods, pteropods.

Siliceous (SiO₂) – Diatoms, radiolarians.

Organic-walled – Dinoflagellates, acritarchs, chitinozoa, pollen.

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8
Q

What are calcareous nannofossils primarily composed of?

A

Calcium carbonate (CaCO₃), usually in the form of calcite.

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9
Q

What is the main group of calcareous nannofossils?

A

Coccolithophores.

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10
Q

What is the size range of calcareous nannofossils?

A

~5 – 10 μm.

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11
Q

Where are calcareous nannofossils commonly found?

A

Marine environments; they make up chalk deposits like the White Cliffs of Dover.

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12
Q

What are foraminifera?

A

Single-celled protists with CaCO₃ shells, found in both planktonic and benthic environments.

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13
Q

What is the size range of foraminifera?

A

50 μm – 2 mm (usually).

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14
Q

What are the two main types of foraminifera?

A

Planktic foraminifera – Float in the ocean; delicate, thin shells.

Benthic foraminifera – Live on the sea floor; thicker shells.

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15
Q

How are foraminifera used in geology?

A

For biostratigraphy, ocean temperature reconstructions, and geochemical analysis.

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16
Q

What are ostracods?

A

Microscopic crustaceans with bivalved calcite carapaces.

17
Q

What is the size range of ostracods?

A

0.2 mm – 2 mm (up to 30 mm in rare cases).

18
Q

What are pteropods?

A

Planktonic molluscs with aragonite shells.

19
Q

What is the size ranges of pteropods?

A

0.2 mm – 5 mm (up to ~30 mm).

20
Q

What are diatoms?

A

Photosynthetic algae with opaline silica (SiO₂) skeletons.

21
Q

What is the size range of diatoms?

A

20 – 200 μm (up to 2 mm).

22
Q

What is the economic importance of diatoms?

A

They form diatomaceous earth, used in filters, toothpaste, paints, and insecticides.

23
Q

What are radiolarians?

A

Zooplankton with silica skeletons, floating at all ocean depths.

24
Q

What are the size ranges of Radiolarians?

A

100 – 300 μm.

25
Q

How are radiolarians used in geology?

A

Biostratigraphy, especially in deep-sea sediments with little CaCO₃.

26
Q

What are dinoflagellates?

A

Primitive eukaryotic plankton, some photosynthetic, some heterotrophic.

27
Q

What fossilized structures of dinoflagellates are found in the rock record?

A

Dinocysts (resting spores).

28
Q

What is the size range of dinoflagellates?

A

~50 – 300 μm.

29
Q

Why are dinoflagellates important in geology?

A

Used for biostratigraphy and climate reconstruction.

30
Q

What are acritarchs and chitinozoa?

A

Organic-walled microfossils of uncertain biological affinity.

31
Q

What is the size ranges of acritarchs and chitinozoa?

A

20 – 150 μm.

32
Q

What do LO and FO mean?

A

LO (Last Occurrence) – The highest occurrence of a species, marking extinction.
FO (First Occurrence) – The lowest occurrence, marking its evolutionary origin.

33
Q

How do scientists construct an age-depth model?

A

By plotting fossil occurrences against depth in a sediment core and assigning known ages.

34
Q

What is sedimentation rate, and how is it calculated?

A

The rate at which sediments accumulate, calculated using age-depth data (cm/kyr).