Lecture 2 - the nature of the fossil record Flashcards

1
Q

to become a useful fossil an organism must:

A

1 - die and avoid destruction by biological and physical processes
2 - be transported into an environment where it is incorporated into a sediment - then fossilised by taphonomy
3 - that sediment must then avoid destruction by diagenetic, metamorphic or erosive processes
4 - fossil must become exposed at the surface and discovered by someone who will study it

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2
Q

why is the fossil record incomplete?

A

1 - sediment only accumulates over a very small area of the earth at any given time
2 - only a tiny fraction of the organisms that ever live will be fossilised
3 - most fossils will be destroyed with the rock that contains them
4 - only a tiny fraction of fossils ever formed will be collected and studied

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3
Q

why is the fossil record biased?

A

1 - certain organisms/ parts of organisms are preferentially preserved
2 - certain environments preferentially preserve sediment and hence fossils
3 - older rocks are more likely to be destroyed
4 - collector bias e.g. from different parts of the world

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4
Q

organisms that leave a fossil record are:

A

bacteria - sheath and structures built by bacteria
protists - those that form exo- and endoskeletons
plants - woody tissues (lignin), cuticles and spores preserve well
fungi - chitinous spores and hyphae preserve well
animals - those with recalcitrant exo- and endoskeletons

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5
Q

oceanic crust covers what percentage of the planet?

A

70%

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6
Q

why does most sediment occur on continental crust?

A

oceanic crust is constantly created / destroyed therefore sediment doesn’t build up

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7
Q

what are large-scale bias’ related to the earth-system?

A
  1. sea level changes - due to long term climate trends and continental configuration
  2. continental configuration - more / less shelf
  3. atmospheric composition - e.g. oxygen level
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8
Q

how do we successfully interpret the fossil record?

A
  • plot the spatial and temporal distribution of fossils therefore allowing us to work out the plate positions at that time
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9
Q

when interpreting the fossil record we can also consider:

A
  • ghost ranges - sharing of common ancestors

- probabilities of range extensions

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10
Q

when interpreting the fossil record we can analyse

A
  • volume of rock deposited per time slice

- exposed area of rock per time slice

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11
Q

Dinosaur time span?

A
  • first appeared in the Triassic period
  • late Jurassic more familiar, larger dinosaurs evolve
  • early late Cretaceous period, birds appear
  • late Cretaceous period mass extinction
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