Lecture 4 Flashcards

1
Q

Facies

A

packages of sediments with a particular set of characteristics that formed in a particular depositional environment

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2
Q

Depositional system

A

an environment with a distinctive set of facies indicating different sedimentary environments

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3
Q

What is a biozone? How are they usually bounded and correlated? How are radiometric dates important?

A

Biozone: units of strata distinguished based on fossils, especially lowest and highest occurrences
Radiometric dating important to recognize diachronous biozones

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4
Q

What are the basic questions in determining the causes of biotic events? What is
meant by “correlation is not causation”, and how is that significant?

A

-Existence: How do we identify biotic events?
*Does the stratigraphic data support
a change in the ecosystem?

  • Cause: How do we determine the cause of biotic events?
    *Does the fossil record show the event at the same stratigraphic level as evidence of a potential cause?

-“Correlation is not causation” means that just because two variables are associated or occur together does not imply that one directly causes the other.

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5
Q

Explain how the incompleteness of the fossil record makes identifying biotic
events such as mass extinctions difficult (the Signor-Lipps effect)

A

because individual species may not be preserved uniformly across geological time.

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6
Q

How can confidence intervals be used to address the incompleteness of the fossil
record?

A

can be used to evaulate stratigraphic ranges, and therefore mass extinctions.

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7
Q

.How can unconformities be a problem?

A

can terminate the ranges of many taxa

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8
Q

How can the reworking of fossils cause problems?

A

may lead to inaccuracies in interpreting the age and evolutionary context of the fossils, as they may appear in a layer that does not correspond to their actual time of existence

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9
Q

What is a C13 excursion? What does it indicate, and why

A

rapid change in the isotopic composition of carbon-13 in geological records, often indicating significant shifts in the global carbon cycle.

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