Ch 13 evolution Evidence of change Flashcards

1
Q

who was Charles Darwin

A
  • Charles Darwin (1809-1892) contributed more to our understanding of evolution than any other scientist
  • During his 5 year long voyage on the HMS Beagle Darwin spent many hours collecting, cataloging and studying organisms
  • The vast diversity of life he saw lead him go question the origin of species
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2
Q

what are adaptations

A

Darwin thought that certain inherited traits would be better for the organisms survival
these would be called adaptations

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3
Q

what are structural adaptations

A

structural adaptations were physical traits

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4
Q

what are behavioural adaptations

A

Behavioural adaptations affect how the organisms acts

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5
Q

what are biochemical adaptations

A

Biochemical adaptations allow the organisms to do things like produce venom, and maintain homeostasis

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6
Q

what is fitness in an evolutionary sense

A
  • Darwin thought the traits that allowed the organism to survive and reproduce would give the organism a fitness towards it’s environment
  • creatures more fit to their environment were more likely to reproduce and pass on their traits
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7
Q

what is Darwins theory of common descent and speciation

A
  • Darwin theorized that as species changed over time they become more and more distinct, and can form new species
  • he though that all organism had evolved from others, and by tracing back evolution everything was related to a single universal common ancestor
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8
Q

which scientists helped prove the magnitude of geological time

A
  • For the process of Evolution to produce the variety we see today an immense range of time is required to exist in earths past
  • James Hutton observed the process that shaped the earth occurred very slowly and thought that therefor the earth must be very old to posses mountain, valleys, and other features
  • Charles Lyell agreed and further evidence led them to argue the age of the earth and geological change
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9
Q

what are fossils

A
  • Fossils are preserved remains of dead organisms found in sedimentary rock
  • they form rarely so the fossil record is necessarily incomplete, and estimated 0.01% of organism are seen in the fossil record
  • Fossils show change in organism and even climate
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10
Q

what process leads to fossil formation and discovery

A
  • Dead Organisms can eventually get buried in sediment, the sediment turns to rock, and eventually the organic material can be replaced with mineral compounds, petrifying it, and in even rarer cases soft material are preserved
  • Fossils can eventually reach the surface and they might be discovered by scientists, who might then reconstruct the organism, or otherwise use the fossil to learn about the long dead organism
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11
Q

what are palaeontologists

A

Palaeontologists are scientists that study the fossil record to see how organisms and environments have changed as well as to make a history of life.

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12
Q

what is relative dating

A

relative dating compares layers of rock to set the age of some deposits relative to others, but this is not process of give us the actual age.

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13
Q

what is radioactive dating

A
  • Radioactive elements breakdown into new ones at a steady rate, each isotope has a half-life (the time for 1/2 of any sample of the atoms to decay) After 1HL you have 1/2, after 2HF you have 1/4, after 3HF you have 1/8, etc
  • Knowing the half life of a particular isotope, using measurements we can calculate how many half-lines have passed and therefor the age of the sample
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14
Q

what are the four eons of earth’s history

A

Eon 1: The Hadean: 4.6-4 bya

Eon 2: The Archean: 4-2.5 bya

Eon 3: The Proterozoic: 2.5 bya-541 mya

Eon 4: The Phanerozoic: 541 mya-present

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15
Q

what are the three eras of the Phanerozoic

A

Era 1: The Palaeozoic: 541-252 mya

Era 2: The Mesozoic: 252-66 mya

Era 3: the Cenozoic: 66 mya - Present

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16
Q

what are the 6 periods of the paleozoic

A

Periode 1: The Cambrian: 541-485.4 mya

Periode 2: The Ordovician: 485.4-443.8 mya

Periode 3: The Silurian: 443.8-419.2 mya

Periode 4: The Devonian: 419.2-358.9 mya

Periode 5: The Carboniferous: 358.9-299 mya

Periode 6: The Permian: 299-252 mya

17
Q

what are the two epochs of the Carboniferous

A

Epoch 1: The Mississippian: 358.9-323.2 mya

Epoch 2: The Pennsylvanian: 323.2-299 mya

18
Q

what are the three periods of the mesozoic

A

Periode 1: The Triassic: 252-200 mya

Periode 2: The Jurassic: 200-145 mya

Periode 3: The Cretaceous: 145-66 mya

19
Q

what are the three periods of the Cenozoic

A

Periode 1: Paleogene: 66-23.03 mya

Periode 2: Neogene: 23.03-2.58 mya

periods 3: Quaternary: 2.58 mya - Present

20
Q

what are the three epochs of the Paleogene

A

Epoch 1: Paleocene: 66-55.8 mya

Epoch 2: Eocene: 55.8-33.9 mya

Epoch 3: Oligocene: 33.9-23.03 mya

21
Q

what are the two epochs of the Neogene

A

Epoch 1: Miocene: 23.03-5.33 mya

Epoch 2: Pliocene: 5.33-2.58 mya

22
Q

What are the two periods of the Quaternary

A

Epoch 1: Pleistocene: 2.58 mya - 11,650 ya

Epoch 2: Holocen: 11,650 ya - Present

23
Q

what developmental evidence do we have for evolution

A
  • the early embryos of many organism look very similar
  • all vertebrates use the same gene group for the basic body plan (called the HOX cluster)
  • As the embryo develops new and different genes change the organism to its species specific form
24
Q

what are homologous structure

A
  • structures in closely related organism, though suited to different functions, frequently have the same basic components
  • Ex: all mammal limbs have the same basic parts
  • Homologous structures show how structures were repurposed to new functions
25
Q

what are vestigial structures

A
  • Vestigial Structures are structures used by an organism’s ancestors, but now have a limited or no function
  • They are not necessary for survival and may eventually be lost in the organisms descendents
  • ex wisdom teeth in humans
26
Q

what biochemical evidence do we have for evolution

A
  • most biochemical molecules are shared between most organisms
  • ex: DNA RNA ATP, proteins
  • these homologies show how organism evolved from a common ancestor