chapter 10 (relatedness) Flashcards

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1
Q

process of fossilisation

A
  • animal/plant dies
  • the body is covered in sediment the soft tissues decomposed and the hard body structures become fossilised by permineralisation
  • the sedimentary layers accumulate and the resultant pressure forms sedimentary rock
  • the earth’s movement raise the layers of the rocks to the surface
  • the rock erodes exposing fossilised body structures.
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2
Q

increase the likelihood of fossilisation

A

areas of rapid sediment accumulation , constant cool temperatures, low oxygen availability, low light exposure

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3
Q

relative dating

A

a dating technique used to determine the relative ages of fossil by comparing its position to other fossils or rock in surrounding rock strata

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4
Q

absolute dating

A

a dating technique used to determine the absolute age of a fossil by measuring the relative amounts of radioisotopes to their products

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5
Q

index fossils

A
  • a group of widespread fossils which existed for a short period and have a known age
  • can be used to reference and easily determine the age of unknown fossils
  • best index fossils: physically distinctive, have a large population, existed in many geographical areas, lived within a known short period of time
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6
Q

transitional fossil

A

a fossil that shows traits that are common to both its ancestral group and its descendant group

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7
Q

mould fossil

A
  • fossil formed when a living thing decomposes underneath sediment
  • creating a cavity in the shape of the dead organism
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8
Q

cast fossil

A

fossil formed when a mould fossil is filled with sediment

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9
Q

trace fossil

A
  • fossil or structure indicating the presence of organisms
  • rather than the organisms themselves (e.g. nests, footprints, and burrows)
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10
Q

Radioisotope series

A
  • Carbon-14 - nitrogen-14
    5 730 years 1 000 - 50 000 years
    Organic materials
  • Uranium-235 - lead-207
    700 million years 1 million - 4.5 billion years
    (used together with U-238 - Pb-206 dating)
    Uranium-containing materials (shells, corals)
  • Uranium-238 - lead-206
    4.5 billion years 1 million - 4.5 billion years
    (used together with U-235 - Pb-207 dating)
    Uranium-containing materials (shells, corals)
  • Potassium-40 - argon-40
    1.3 billion years 100 000 + years
    Igneous (volcanic) rocks
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11
Q

Homologous structures

A
  • are physical evidence of divergent evolution
  • the evolutionary process where two or more populations of a single species accumulate enough genetic differences to be classified as different species.
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12
Q

Analogous structures

A

are structures that serve similar biological functions but are not derived from a common ancestor

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13
Q

Vestigial structures

A

are structures found within organisms that once served a purpose for an organism’s ancestors but due to changing selection pressures have lost their original function and are no longer required for survival.
(e.g human coccyx/tailbone)

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14
Q

Molecular homology

A

is the study of the similarities between organisms at a DNA and amino acid level

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