Ch. 16 Fossil Evidence for Evolution Flashcards

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1
Q

define fossil

A

any preserved trace left by an organism that lived a long time ago

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2
Q

What can fossils be

A

o Footprints, burrows, faeces, or impressions of all or part of an animal or a plant
o Bones, teeth, shell

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3
Q

Why are rocks important fossils

A

o Other material associated with bones, i.e. rocks in which they were found and fossils of other plants and animals allows to develop a picture of life in the past
♣ i.e. what organism ate, what other organisms existed at the time, and what the climate was like

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4
Q

when can an organism be fossilised (what buries it)

A

o buried by drifting sand, mud deposited by rivers, volcanic ash, or other members of the species

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5
Q

why does burying rapidly increase chance of fossilations

A
  • If buried rapidly, conditions may not be suitable for activity of decay organisms and decomposition may be delayed
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6
Q

what condition of soils will not allow fossilisation and why

A

wet, acidic soils (minerals in bone dissolves)

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7
Q

what are the three best soil conditions for fossils

A

♣ No oxygen (in case of peat, complete preservation of the soft tissues and bones of animal may occur)

♣ Alkaline soils (minerals not dissolved)

♣ New materials (often lime or iron oxide) deposited in pores of bone, replacing the organic matter // turning into rock (petrified) but the details of structure are still preserved

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8
Q

Where are human fossils often found

A
  • edges of ancient lakes and river systems, caves, volcanically active areas
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9
Q

why are humans fossils found near lakes, caves and volcanic areas

A

o Lakes and rivers= build up sediments when flooding occurs or when water flow slows rapidly
o Many caves= limestone (CaCO3) // may be deposited covering bodies
o Unusual to be preserved near volcanic areas (heat from the volcanic material destroys the organisms), but ash can fall preserving fossils of many human ancestors

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10
Q

what makes surface discoveries possible and what do they indicate

A

erosion

- Surface discoveries (fossil fragments, evidence of human occupation) indicate places

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11
Q

where are fossils usually found

A

excavation sites

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12
Q

define artefacts and examples

A

>

Artefacts: objects deliberately made by humans

o E.g. stone tools, beads, carvings, charcoal from cooking fires and cave paintings

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13
Q

define dating

A

>

determining the age of excavated artifacts or fossils
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14
Q

what are the two methods of fossil dating

A

o Absolute dates: actual age of the specimen in years

o Relative dates: whether one sample is older or younger than another

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15
Q

what are three types of absolute dating, material used and tie limitations

A

o Potassium argon dating (volcanic deposits used, 100 000- 200 000)
o Radiocarbon dating (carbon compounds used, 60 000)
o Dendrochronology (wood used, 9 000)

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16
Q

what is potassium argon dating based on

A
  • Based on decay of radioactive potassium to form calcium and argon
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17
Q

what are the two limitations of K Ar dating

A

o Not all rocks suitable: Some suitable rock of same as age as fossil must be available This occurs, for example, when rocks produced in volcanic eruptions bury bones
o Only date rocks older than 100 000 to 200 000 years
♣ Earlier than 100 000 = only 0.0053% of potassium would have decayed // limits of detection devices

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18
Q

what does K 40 decay to

A
  • Potassium-40= radioactive + decays to form calcium-40 and argon-40
19
Q

how is K Ar dating to calculate age

A
  • Decay takes place at an extremely slow but constant rate

o Determining amounts of potassium-40 and argon-40 in a rock sample enables age of rock to be calculated

20
Q

what is radiocarbon dating based on

A

Based on decay of radioactive isotope of carbon (carbon-14) to nitrogen

21
Q

explain c14 in atmosphere and how enters animals

A
  • Carbon-14 produced in upper atmosphere by action of cosmic radiation on nitrogen at about the same rate at which it decays
  • In atmosphere= ratio of 1: million million (1012) carbon-14 carbon-12
  • During photosynthesis when plant use atmospheric carbon dioxide, on atom in every million atoms is carbon 14 (incorporated into tissue)
  • Should animal eat plant= the carbon-14 becomes part of animals tissues
22
Q

how is radiocarbon measured to date

A
  • With death C14 intake ceases, but C14 in tissues decays at a fixed rate
  • By measuring amount of radiation liberated by a sample, ratio of C14 to C12 can be estimated and // age of sample can be calculated
23
Q

what is the half life of carbon 14

A

5730

24
Q

what are the four limitations of radio carbon dating

A
  • must be organic material
  • must be at least 3 grams
  • can’t date back longer than 60 000 years
  • amount of c14 in atmosphere varies
25
Q

explain the limitation of carbon needing to be at least 3 grams and how is this avoided

A

o Normally requires at least three grams of organic material so that rate of radioactive decay of C14 in a sample can be measured,
♣ Unless using Accelerator Mass spectrometry (AMS) where sample 100 micrograms can be used
♣ Involves breaking sample up into its constituent atoms so that the number of atoms of each isotope of carbon can be counted
♣ Date cave paintings accurately from tiny samples of pigments

26
Q

explain limitation of variation of c14 in atmosphere

A

o Amount of C14 in atmosphere varies
♣ Thought to be constant
♣ // radiocarbon dates must be treated with certain degree of caution
♣ Corrections in fluctuations in C14 content of atmosphere are however now possible past 9000 years by reference to tree-ring dating

27
Q

what does each ring in a tree represent

A

each concentric ring represents one year’s growth and the rings differ in width according to how favorable the growing season was

28
Q

what are marker rings

A
  • Certain rings produced in years of exceptional weather can be used as marker rings
    o Correlate marker rings with living trees and timber taken from ancient structures
29
Q

explain use of dendrochronology to date fossils

A
  • Living trees dated by drilling small core out of trunk and counting rings
    o May be noted for example, particularly wide ring, indicating favorable growth year, occurs in middle of the trunk
    o This wide marker may be found near the outside of a piece of tree used in an ancient structure
    o By such correlation of marker rings, dates for the building of structures can be determined
30
Q

what are the limitations of dendro

A

o Timber not preserved for more than 9000 years

31
Q

what does relative dating enable

A
  • Enables a sequence of events to be established
32
Q

what is stratigraphy

A
  • Study of layer, or strata
33
Q

what are the three parts to stratigraphy

A
  1. principal of superposition
  2. correlation of rock strata
  3. index fossils
34
Q

explain principal of superposition

A
  • assumes that in layers of sedimentary rock the layers at the top are younger than material found lower
    o Applied with caution because distortions of Earth’s crust do occur and a sequence of rock layers may be turned upside down
  • Fossils can also be buried by animals, or early humans, sometime after deposition of sediment // specimen may be younger than some layers above it
35
Q

explain correlation of rock strata

A
  • Matching layers of rock from different areas
  • Done by examining rock itself and also by studying fossils it contains
  • Rocks that contain same fossils may be assumed to be the same age
36
Q

explain index fossils

A
  • Certain fossils= great value in correlation as they are widely distributed and were present for only a limited amount of time, making more precise
    o = index fossils
37
Q

how is fossilised pollen grains used

A
  • Example: fossilized pollen grains
    o Can be used as index fossil
    o If not used that way= presence of preserved pollen grains in soil or rock sample can enable construction of type and amount of vegetation existing at the time the deposit is laid
    ♣ > idea of climatic conditions prevailing at time can be worked out
    ♣ this data= confirms or refutes relative dates arrived at by other methods
38
Q

what is the breakdown of the geological time scale

A

o Consist of eras > subdivided into periods > further divided into epochs

39
Q

what era are humans

A
-	cainozoic era
o	Primates (group where humans belong) first evolved at beginning of this era
40
Q

what are the 4 problems with the fossil record

A
  1. organisms not preserved
  2. small proportion discovered
  3. problematic dating
  4. controversial reconstruction
41
Q

explain the problem of organisms not preserved

A
  • Conditions for fossilization do not always occur or occur at irregular periods of time // organisms not being preserved
  • For fossils to form= four conditions
    > Quick burial
    > Presence of hard body parts
    > Absence of decay organisms
    > Long periods of stability (left undisturbed)
  • Fossilization // chance occurrence + many gaps un record often due to organisms not being preserved
42
Q

explain the problem of small proportion discovered

A
  • Some buried too deep or inaccessible, destroyed by human activity (agriculture or industry)
43
Q

explain the problem of problematic dating

A

conditions and certain materials required for different methods as well as time limitations

44
Q

explain the problem of controversial reconstruction

A
  • Unusual to find fossil of entire organism or whole skeleton > particular true for human ancestors
  • Usually few fragments of bone formed // reconstruction of what what organisms may have looked like is formed
  • Other scientists may disagree of shape // controversy
  • Only resolution find more fossils (but as shown chances are slim)