Lesson 9: Stratigraphy and Geologic Time Flashcards

1
Q

The tendency for rock layers to be

chronologically stacked is called the

A

Principle of Superposition.

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2
Q

Stratigraphy is the

A

science of using the arrangement and composition of rock layers to interpret geological history.

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3
Q

A large
uninterrupted sequence of rock that is made of
multiple layers that all share similar properties
(such as mineral composition and average
sediment grain size) and that all formed under
similar conditions is termed a

A

formation.

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4
Q

When
a sequence of rock changes from one formation
to another, it indicates that a large scale change
occurred in

A

the environment where the rocks

were being deposited

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5
Q

To age rocks in absolute terms, a

technique called __ is used.

A

radiometric dating

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6
Q

An isotope is a

A

variant of a chemical
element that has an unusual number of
neutrons

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7
Q

When a new rock forms, it has a ratio of

A

isotopes and decay products that matches that

of the environment.

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8
Q

. If sedimentary rocks that contain
fossils are found between two horizontally
deposited layers of igneous rocks, then dating
the igneous rocks above the sedimentary layer
will tell us

A

what age the fossils must be older
than, and dating the igneous rocks below the
sedimentary layer will tell us what age the
fossils must be younger than

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9
Q

The geologic time scale is a

A

standardized series of
chronological divisions that parses the Earth’s
history into discrete named units.

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10
Q

The largest

units in the time scale are __, followed by __, __, and __.

A

Eons, Eras, Periods, and Epochs

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11
Q

THE HADEAN EON

A

4.6 TO 4 BILLION YEARS AGO

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12
Q

THE ARCHEAN EON

A

4 TO 2.5 BILLION YEARS AGO The oldest known fossils come from the THE ARCHEAN EON (cyanobacteria age)

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13
Q

The Paleozoic Era

A

541 to 252 million years ago. At the start of the Paleozoic, animal life was restricted to primitive invertebrates living in the oceans, but, by its close, great forests covered
the land and teamed with reptiles, amphibians,
and insects

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14
Q

THE PROTEROZOIC EON

A

2.5 BILLION TO 541 MILLION YEARS AGO. At approximately 1.7 billion years ago, the first
multicellular organisms evolved.

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15
Q

Within the Proterozoic, the time span

from

A

630 to 542 million years ago is known as
the Ediacaran Period. During the Ediacaran,
large forms of life with some harder parts
evolved, including the first animal life.

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16
Q

THE PHANEROZOIC EON

A

541 TO 0 MILLION YEARS AGO The Phanerozoic Eon is subdivided into three
eras, which are themselves subdivided into
numerous periods. It is during the Phanerozoic
that animal life rapidly evolved into a multitude
of diverse forms, including dinosaurs.

17
Q

The Cambrian Period

A

541 to 485 million years

ago

18
Q

The beginning of the Cambrian marks such a
dramatic diversification of aquatic animal life
that it is often referred to as

A

The Cambrian Explosion

19
Q

The Ordovician Period

A

485 to 443 million years ago Global sea levels were high. Life in the oceans continued to diversify, with fish increasingly becoming the dominant large aquatic animals.

20
Q

The Silurian Period

A

443 to 419 million years ago Until this point, fish had not yet evolved jaws. With the evolution of jaws came the evolution of large predatory fish. Primitive plant life
began to flourish on land.

21
Q

The Devonian Period

A

419 to 359 million years ago The first forests appeared on land. Huge jawed fishes, like Dunkleosteus, evolved in the seas, and the first true sharks appeared. Lobe-finned
‘fishapods’, like Tiktaalik, ventured onto land,
and give rise to the tetrapods.

22
Q

The Carboniferous Period

A

359 to 299 million
years ago
Amphibians were widespread in the abundant
swamps, and reptiles, the first amniotes,
evolved. Much of the coal that is mined today
formed from the rotting plants of Carboniferous
swamps.

23
Q

The Permian Period

A

– 299 to 252
The continents collided together and formed a
single super continent called Pangaea.

24
Q

The Mesozoic Era

A

252 to 66 million years ago
The Mesozoic is often referred to as the Age of
Dinosaurs

25
Q

The Cenozoic Era

A

– 66 to 0 million years ago
The Cenozoic is often referred to as the Age of
Mammals.

26
Q

The Paleogene Period

A

66 to 23 million years
ago
Global temperatures began to cool. Mammals
diversified into a variety of new forms, including
primates, bats, and whales. Birds also
diversified.

27
Q

The Neogene Period

A

23 to 2.6 million years
ago
Global temperatures continued to cool. The first
hominids evolved in Africa.

28
Q

The Quaternary Period

A

2.6 to 0 million years
ago
The earth experienced several large glaciation
events, or “ice ages”. The first anatomically
modern humans evolved. Human civilization
spread.

29
Q

The Triassic Period

A

252 to 201 million years
ago
During the first ten million years of the Triassic,
life gradually recovered from the mass
extinction that occurred at the end of the
Permian.

30
Q

The Jurassic Period

A

– 201 to 145 million years
ago
Dinosaurs diversified. This was the peak of
sauropod diversity, and they were the dominant
terrestrial herbivores. The supercontinent Pangaea
began to break apart

31
Q

The Early Cretaceous Period

A

146 to 100
million years ago
Dinosaurs continue to diversify and the first
flowering plants evolved.

32
Q

The Late Cretaceous Period -

A
  • 100 to 65 million years ago
    Often considered the apex of non-avian
    dinosaur diversity, many of the most famous
    dinosaurs come from this period of time