Introduction and history Flashcards

0
Q

William Smith

A

Made the 1st true geological map

Noticed layers of sedimentary rocks in any given location have the same fossil sequence

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1
Q

Fossil

A

Any nonliving biologically generated trace or material that paleontologists study as part of the record of life

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2
Q

Robert Hooke

A

Microscopic examination of fossil and modern wood and shells showed that they were the same

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3
Q

Nicolaus Steno

A

Decided “tongue stones” were really fossilized shark teeth
Argued that if fossils grew in place we should find half fossils
Said that a solid object will cause solids around it to form to its shape so fossils must have been there before rocks

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4
Q

1720 Beringer Hoax

A

Competitors gave him fake fossils, which he published a book about.

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5
Q

In the 16th century how did people believe fossils were made

A

From the solidification of a fluid

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6
Q

What does a paleontologist do?

A

Collects fossils from the field
Compare with previously described fossils and living organisms
Describe them if not previously known
Document their occurrence in a particular time/place/environment

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7
Q

Neo-Platonist

A

One of the schools of thinking about fossils. Thought fossils grew under celestial influence and emphasized the unity of nature.

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8
Q

Aristotelian

A

Believed fossils formed from “seeds” that washed into the ground.

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9
Q

Soft parts are made of which elements

A

CHNOPS

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10
Q

Redford ratio of N:P

A

16:1

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11
Q

Diagenesis

A

Processes that take place after burial

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12
Q

Taphonomy

A

Study of the process of fossilization

Represents the passage of biological info from the biosphere to the lithosphere

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13
Q

George’s Cuvier

A

An anatomist.
Noticed the oldest fossils were below younger ones
Established that fossils record a history of life.
Established the reality of extinction.

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14
Q

Lagerstatten

A

Unusual preservation. A fossil mother lode.

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15
Q

Time Averaging

A

How much time does a fossil collection represent.
Organisms found together may not have lived together.
Sedimentary processes may mix together fossils of different ages

16
Q

Taphofacies

A

Bodied of sedimentary rock characterized by particular combinations of preserved features of the contained fossils.
Help us to reconstructing environments.

17
Q

Stagnation deposits

A

A type of conservation lagerstatten caused by low oxygen which stops scavenging.

18
Q

Obrution deposits

A

Lagerstatten conservation deposits. Caused by rapid burial maybe a worm or a huge sediment deposit.

19
Q

Paleobiology

A

Looks at fossils as the remains of living organisms. A documentation of life of the past.

20
Q

How organisms preserve Ina marine environment depends on…

A

Water energy (waves/currents), rates of sedimentation, oxygen.

21
Q

The “external metaphors” of paleontology

A

Does the history of life have an arrow, what is the motor of organic change, is the history of life gradual or episodic, what is the tempo.

22
Q

How do internal and external molds form?

A

Spaces are filled by sediment and then the minerals are dissolved leaving impressions on the sediment.

23
Q

How do concretes form?

A

Precipitation of minerals around decaying organisms (soft tissue impressions are preserved)

24
Q

Permineralization

A

Filling void spaces with minerals (petrified)

25
Q

Biostratinomy

A

Begins with the death of an organism and ends with it’s burial. (Scavenging, bacterial decomposition, etc.)

26
Q

Necrology

A

The study of death processes. How dead organisms or dead pieces of organisms are produced.