Stratigraphy and Geologic Time Flashcards

1
Q

Why document Earth history?

A

The past may be the key to the future: changes occur in cycles, patterns repeat
How has the Earth changed?- e.g.CO2 levels, climate, sea level, landmasses, biological evolution & extinctions, Wilson cycles
HOWEVER: Almost all of Earth’s history predates humans

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2
Q

How is Earth history documented?

A

The Rock Record

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3
Q

Sediments laid down in layers (strata) form a….

A

stratigraphy of events: a record of earth processes over geological time

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4
Q

what are the main concepts for reading the stratigraphic record?

A

1) Beds (strata, sedimentary units) – horizontal – bound by bedding planes
2) Multiple beds make up a stratigraphic ‘sequence’ - bound by erosional episodes due to fluctuations in sea-level, uplift
3) Strata contain fossilised flora and fauna
4) The rock record is incomplete at any one place (gaps in time)

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5
Q

what is biostratigraphy?

A

Fossils
Used in correlation of strata
Occur over a stratigraphic range
Organisms: also provide info on environment–some organisms tolerate very wide environmental conditions; others do not. e.g., different trilobite species: bottom dwellers vs. floaters vs. swimmers

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6
Q

what are the two ways to view geologic time?

A

(1) Relative time
- dating by sequence of events
- “older” vs. “younger”
- placed in order
(2) Absolute time
- numerical dating using radioactive decay in minerals

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7
Q

what are the principles of relative age dating?

A

1) Superposition
2) Original horizontality
3) Faunal (& floral) succession
4) Inclusions
5) Cross-cutting relations

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8
Q

what is the principle of superposition?

A

In an undisturbed stratigraphic sequence, the rocks at the top are youngest

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9
Q

what is the principle of original horizontality?

A

Sedimentary layers are deposited in horizontal units/beds

Inclined layering -> layers were tilted from initial horizontal orientation some time after deposition

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10
Q

what are unconformities?

A

large gaps of time between deposition of layers (strata)

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11
Q

what is the principle of faunal (& floral) succession?

A

Sedimentary layers contain fossilized flora & fauna
Organisms succeed each other vertically in a specific, reliable order -> fossil record
Rocks with similar fossils are (generally) of similar age e.g., Neanderthal bone (young) never found in same strata as a T-Rex (much older)

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12
Q

what are some useful index fossils?

A

dinosaurs

trilobites

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13
Q

what is the principle of inclusions?

A

Older rocks “included” in younger rocks – e.g., blocks eroded from country rock by intruding magma

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14
Q

what is the principle of cross-cutting relations?

A

Older rocks are “cross-cut” by younger rocks or features (e.g., dykes, faults, erosion surface)

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15
Q

what is radioactive decay?

A
Many atoms decay spontaneously
Decay produces energy (heat) & stable daughter products
Solved 2 problems:
(1) An ongoing source of heat for Earth
(2) Absolute dating of igneous rock
(discovered by Becquerel in 1896)
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16
Q

what is an isotope?

A

same number of protons different number of neutrons

17
Q

what is a radioactive half life?

A

Half the original atoms decay during one half life
Decay rates are exponential
Heat produced by decay decreases exponentially

18
Q

how old are earths oldest minerals? where are they found?

A

zircons
Jack Hills, Australia
4.4 billion years old

19
Q

why is olduvai gorge, Tanzania significant?

A

Important fossil site of early Homo species & stone tools

20
Q

who is Lucy? how long ago did she live?

A

she is our earliest known direct ancestor

“Lucy’s” Footprints (in volcanic ash) were dated by K/Ar dating of volcanic ash 1 m below fossil -> 3.2 million yrs

21
Q

why is C-14 dating no longer as effective?

A

nuclear weapons testing simulated atmospheric production of C-14 in unnatural quantities

22
Q

how old is the earth?

A

4.55 billion years

23
Q

what is the geologic time scale based on?

A

rock sequences in Europe correlated worldwide; includes use of fossils, radiometric data

24
Q

what do period divisions mark?

A

changes or loss in fauna