History Of Earth Flashcards

1
Q

is a scale used by geologists
to understand and describe
the history of the Earth

A

Geologic time scale

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2
Q

4 era

A

Precambrian
Paleozoic
Mesozoic
Cenozoic

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3
Q

primitive life-forms existed
approximately 3.5 billion
years ago

the first multicellular
organisms evolved, and
sexual division developed

A

Precambrian

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4
Q

Called as ancient life; marine invertebrates and primitive fishes.

Plant and animal life
flourished. Amphibians left
the oceans to live on land,
reptiles evolved as fully
terrestrial life-forms, and
insect life began.

A

Paleozoic

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5
Q

Called as middle life

this era is
best known as the time of
the dinosaurs.

A

Mesozoic

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6
Q

is internationally accepted as the
youngest of the three
subdivisions of the fossiliferous
part of Earth history.

the interval of time during
which the continents
assumed their modern
configuration and
geographic positions and
during which Earth’s flora
and fauna evolved toward
those of the present.

A

Cenozoic

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7
Q

Oldest time in Paleozoic; widespread seas several scattered landmasses; no land plants or animals; age of trilobites

A

Cambrian

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8
Q

Rapid seafloor spreading; intense diversification of Maribel animal life;rise of fish

A

Ordovician

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9
Q

Global sea level is higher; rose dramatically; extensive glaciers ice age melted

A

Silurian

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10
Q

Age of fishes; ammonites appear early; first four legged amphibians

A

Devonian

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11
Q

Mississippian and Pennsylvania; longest period in Paleozoic; refers coal-bearing strata

A

Carboniferous

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12
Q

Hot and dry condition caused crisis; terrestrial plants broadly diversified; insects evolved they followed plants

A

Permian

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13
Q

Major landmasses supercontinent Pangea; terrestrial climate warm; reptiles increased; first dinosaur

A

Triassic

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14
Q

Pangea split apart; rock strata laid down yield gold, coal, petroleum; animals and plants recovered largest mass extinction

A

Jurassic

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15
Q

Latin for chalk; warmer more humid; very active volcanism; unusual high rates of ss

A

Cretaceous

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16
Q

Not only in mammals but also the flowering plants; insects; birds; corals….

A

Tertiary

17
Q

Rocks and sediments

A

Quaternary

18
Q

remnant, impression, or trace of
an animal or plant of a past
geologic age that has been
preserved in Earth’s crust

A

Fossil

19
Q

Small organism or part
trapped in amber, hardened
plant sap

A

Unaltered preservation

20
Q

The organic contents of bone
and wood are replaced with
silica, calcite or pyrite,
forming a rock-like fossil

A

Permineralization/petrification

21
Q

hard parts are dissolved and
replaced by other minerals,
like calcite, silica, pyrite, or
iron

A

Replacement

22
Q

The other elements are
removed and only the carbon
remained

A

Carbonization

23
Q

Hard parts are converted to
more stable minerals or small
crystals turn into larger
crystals

A

Recrystalization

24
Q

Molds and casts are formed
after most of the organism
have been destroyed or
dissolved

A

Authigenic preservation

25
Q

Knowing the age of a fossil can
help a scientist establish its
position in the geologic time
scale and find its relationship
with the other fossils.

A

Dating fossils

26
Q

study of layer
of rocks; not exact date; depends on position; uppermost younger; lowermost oldest

A

Relative dating

27
Q

actual age of
the fossil through radiometric
dating, using radioactive
isotopes carbon-14 and
potassium-40

A

Absolute dating