Chapter 10 Flashcards

1
Q

Fossil Record

A

Information derived from fossils that help map out the history of life on Earth - Geologic time frame.

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2
Q

Fossil

A

Preserved body, impressions or traces of a dead organism.

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3
Q

Process of fossilisation

A
  1. Remanents of organisms covered by sediment, therefore not exposed to oxygen, microorganisms + other disturbances.
  2. Over sediment layers build + compact until pressure cements together to form sediments.
  3. Fossilised remains can take many forms including permineralised, mould or cast fossil.
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4
Q

Conditions that increase the chance of fossilisation

A
  • Physical protection from scavengers + decomposers.
  • Areas of rapid sediment accumulation.
  • Constant cool temperatures.
  • Low oxygen.
  • Low light exposure.
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5
Q

Using the fossil record - relative dating

A

Uses the law of fossil succession to assign a relative age in relation to other fossils and rock strata.
- Use transitional fossils.

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6
Q

Transitional fossils

A

Assist in relative dating.
- Shows traits common to both ancestral and descendant groups. - Shows the evolutionary changes.
Is useful when the descendant group is physically distant from the ancestral species.

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7
Q

Using the fossil record - absolute dating

A

Known half-lives or different radioisotopes can be used to measure the absolute (estimated) age of a fossil.

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8
Q

Radioactive isotopes

A

Radioactive atom of a specific element that breaks down into a predictable + stable product.

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9
Q

Absolute dating is based on:

A
  1. Radioisotopes.
  2. Breakdown of these atoms is constant + can be modelled.
  3. Half-life; amount of time before half of the mass of the radioisotope is broken down into predictable + stable products. 14C –> 14N.
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10
Q

Radiocarbon dating

A

Form of absolute dating that determines the age of a fossil by measuring properties or radiocarbon (a radioactive isotope of carbon).

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11
Q

General principles of radiocarbon dating.

A
  1. Living things exist as a ratio between 12C (isotope; stable) and 14C (radioactive isotope).
  2. Death of an organism –> 14C decays and breaks down into 14N(stable). 12C remains the same.
  3. 14C is used to measure how long ago a fossil died. Comparing the ratio to the ratio in the atmosphere.
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12
Q

Homologous structures

A

Features found in different species that may look and function very differently from one another but derived from the same ancestor.

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13
Q

Analogous structures

A

Features present in 2 or more species with the same function, but don’t originate from a common ancestor.

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14
Q

Vestigial structures

A

Features that have lost all or most of their usefulness as a result of revolution.
eg. Human coccyx (tail bone) was used to balance in trees –> modern humans now use inner ears to help balance on the ground.

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15
Q

Aminoacid sequence similarity

A

Compare amino acid sequences to determine how related different organisms are.
- Haemoglobin
- Cytochrome c.

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16
Q

Molecular homology

A

Study of the similarities between organisms at DNA + amino acid level.

17
Q

Haemoglobin

A

4 polypeptide chains; 146 amino acids.
Assesses the number of amino acid differences between chains of different organisms regarding the degree of relatedness.

18
Q

Cytochrome C

A

Enzyme in mitochondria - 104 amino acids in mitochondrial DNA.

19
Q

DNA sequence similarity

A

Determines relatedness.
High similarity = closer relatedness.

20
Q

Mitochondrial DNA

A

Maternally inherited.
ADVANTAGES:
- The mutation rate of mtDNA is much higher.
- No recombination during mitosis.

21
Q

Limitation of analysing amino acid sequences

A

Closely related species share similar sequences for certain proteins.

22
Q

Phylogenetic trees

A

Shows the evolutionary relationships between different species.
- timeline of lineages.
- relatedness between taxa.
- shared characteristics of different taxa.

23
Q

Phylogenetic tree construction

A
  1. Figure out the largest shared trait.
  2. Trait shared by the second largest number of animals.
  3. Branch animals that share traits - directly.
24
Q

Structure of phylogenetic trees

A

Root –> the line at the origin.
Branch –> Each line of the tree.
Node –> Point where branches split.
Leaf –> End of the branch; the animal.