Chapter 8.4 Evidence for the Theory of Evolution: The Fossil Record Flashcards

1
Q

Define paleontology

A

The study of fossils

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2
Q

What can fossils tell us?

A

Shows clear change over time from simple to very complex organisms which is evidence for evolution

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3
Q

What conditions are necessary for fossilisation to begin?

A

Organic matter must be quickly buried in sediments in an oxygen-poor environment to prevent decomposition

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4
Q

How does sediment help preserve plant and animal remains?

A

It protects remains from oxygen and scavengers, slowing decay and allowing fossilisation

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5
Q

What is mineralisation in fossilisation?

A

It’s when minerals from sediment replace natural bone or shell, making the remains harder and more likely to fossilise

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6
Q

What type of sedimentary materials help form fossils?

A

-Mud
-Slit
-Sand
-Clay
which are all often carried and deposited by rivers and streams

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7
Q

In what type of rock are fossils most commonly found?

A

Sedimentary rock

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8
Q

Why aren’t fossils found in volcanic rock?

A

Molten lava is about 1000°C, which burns any organic material

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9
Q

Can fossils be found in volcanic ash?

A

Yes if the ash is part of sedimentary layers that eroded and buried the organism

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10
Q

Why are fossils rare in metamorphic rock?

A

Because the heat and pressure usually destroy organic remains

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11
Q

What kinds of remains are most commonly fossilised?

A

Hard parts like bones and shells, but delicate tissues can occasionally be preserved

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12
Q

How are impressions or films of thin tissues formed in rocks?

A

When tissues like leaves or mussels leave a mark or thin film in sedimentary rock

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13
Q

What other conditions, apart from mineralisation, can lead to fossilisation?

A

Freezing or dehydration

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14
Q

How are plants fossilised?

A

Some tissues is replaced with dissolved salts, a process called petrification

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15
Q

What is pretrification?

A

Replacement of original plant tissue with rock-forming mineral

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16
Q

Define the principle of superposition

A

The principle states that the oldest rock layer is found in the deepest position, and each consecutive layer above it is relatively younger; it indicates the relative ages of the rock layers and the fossils within them.

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17
Q

What does the position of a fossil in rock layers indicate about its age?

A

Fossils found in lower rock layers are older than those near the surface, unless folding has occured.

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18
Q

Define stratum (plural strata)

A

The layers of rock in an area (profile); strata occur in order, with the oldest layer at the bottom

19
Q

Define absolute dating

A

The process of determining the age of rocks and the fossils they contain based on the physical or chemical properties of, materials in the rock

20
Q

Define gradualism

A

A theoretical model of evolution that proposes there has been a steady, slow divergence of lineages, irrespective of gaps in the fossil organisms

21
Q

Define punctuated equilibrium

A

A theory of evolution that proposes new organisms evolve quickly after a long period of no change, rather than evolving by gradual change

22
Q

What two techniques are used to estimate the dates of fossils?

A

Comparative dating and absolute dating

23
Q

Define comparative dating

A

The process of determining the age of rocks and their contained fossils relative to one another, allowing an estimation of ‘oldest to youngest’, without assigning an actual age.

24
Q

What are the three types of absolute dating?

A

-Radiometric dating (most common)
-Electron spin resonance
-Luminescence

25
Define radiometric dating
Uses the known rates of decay of naturally occurring radioactive isotopes present in a rock or fossil to obtain an absolute date for its age
26
What are the main steps involved in the process of fossilisation
1) Death of organism 2) Rapid burial: The remains are quickly buried by sediment (mud, sand, slit) protecting them from scavengers and slowing decomposing 3) Lack of oxygen 4) Sediment accumulation: Over time more sediment layers build up and compress the lower layers, forming a sedimentary rock 5) Mineralisation: Minerals from surrounding sediments seep into the remains. These minerals replace the organic material, hardening the structure into the rock. 6) Uplift and erosion: After million of years, geological forces may lift the rock layers. Erosion from wind or water can eventually expose the fossil at the surface
27
Most of our knowledge of the evolution of sharks is based on the remains of fossilised shark teeth. Suggest why other fossilised body parts of sharks haven't been found in abundance.
-Because sharks have skeletons made of cartilage, not bone. -Cartilage is softer and less dense than bone so it decays much faster and doesn't fossilise easily. -Teeth on the other hand are made of hard mineralised tissues which means they are much more durable and have a higher chance of fossilising. -That's why teeth are commonly found, while the rest of the body is rarely preserved
28
What are some alternative ways (other than fossils) to determine how closely related present-day animals are to each other?
-DNA/molecular comparisons -Comparative anatomy -Embryology -Biogeography -Behavioural and physiological traits
29
Why is tracing the evolution of jellyfish through fossils difficult?
1) They are soft-bodied animals: Jellyfish don't have bones or shells, so they rarely leave behind fossils evidence 2) Rapid decay: Their bodies break down quickly, often before they can be buried in sediment 3) Unfavourable environment: They usually live and die in the open ocean, not in areas where fossilisation is likely 4) Poor fossil quality: When fossils do form, they're often faint or incomplete, making it hard to identify evolutionary traits
30
What do isotopes of the same element have in common and what differs?
They have the same number of protons (same atomic number) but different numbers of neutrons (different atomic mass).
31
What are the three natural isotopes of carbon?
-Carbon-12 -Carbon-13 -Carbon-14.
32
How many protons and neutrons does carbon-12 have?
6 protons and 6 neutrons.
33
How many protons and neutrons does carbon-14 have?
6 protons and 8 neutrons.
34
What makes some isotopes radioactive?
They have unstable nuclei that emit energy as alpha, beta, or gamma rays.
35
What is the half-life of an isotope?
The time it takes for half of the radioactive nuclei in a sample to decay.
36
Into what does carbon-14 decay?
Nitrogen-14.
37
What is the half-life of carbon-14?
5730 years.
38
What does carbon dating compare to estimate age?
The percentage of carbon-14 remaining in a sample compared to atmospheric carbon-14.
39
Why is the result of carbon dating often given as ±x years?
Because atmospheric carbon-14 levels vary over time, as shown by tree ring data.
40
What is the maximum reliable age range for carbon-14 dating?
Up to about 12,000 years.
41
Why is carbon-14 dating unreliable for samples older than 12,000 years?
The carbon-14 levels become too low to measure accurately.
42
What radioactive isotope is often used for dating older samples?
Potassium-40, which decays into argon.
43
Why is carbon-14 not usually used to date fossils, and how can their age still be estimated?
Carbon-14 is not usually used because fossils are often mineralised with their original carbon-containing tissues replaced or altered, and fossilisation generally takes longer than the 12,000-year limit of carbon-14 dating. Instead, scientists determine the radioactive isotopes present in the sample to estimate the fossil's age.
44
How can the age of a fossil still be estimated if carbon-14 dating isn’t suitable?
By determining the radioactive isotopes present in the sample and calculating based on their decay.