PALEONTOLOGY & EVOLUTIONARY BIOLOGY (Ch. 18.1-18.3) Flashcards

1
Q

The most common type of fossil that shows the original shape of the fossil to the cellular detail

A

Permineralization and Replacement

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2
Q

These fossils show the surface shape but give no information on internal details

A

Natural Molds

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3
Q

These fossils form when unfilled space is infiltrated, filled, and harden into rock

A

Casts

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4
Q

These fossils show body shape and can tell us about behavior. there are three types of this type of fossil.

A

Trace fossils. Trackaways, Coprolites, Burrow or Den

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5
Q

These fossils are preserved in resin. These fossils give us the most complete picture of ancient life.

A

Amber and Freezing

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6
Q

How much of life on earth is extinct? What do fossils tell us?

A

99% is extinct. Fossils tell about extinct phenotypes, when groups of organisms appeared and diversified, and transitional features that help us understand evolution.

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7
Q

Any trace of an organism that lived in the past

A

Fossil

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8
Q

Why is the fossil record more complete in the Northern Hemisphere?

A

Historically, the Northern Hemisphere has been sampled more than the Southern Hemisphere (Historical Bias). Also, there is less vegetation allowing for easier access to fossils.

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9
Q

How do paleontologists find fossil localities? How do they know how old rocks are?

A

Using previous sites, or discovering new sites with geologic maps. Once fossils are found they use radiocarbon dating to see how old the rocks are from the site.

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10
Q

Common ways to prepare a fossil for a study

A

Thin sectioning, CT scanning, and Cellulose Acetate Peel Technique.

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11
Q

Tools used to prepare a fossil for a study

A

Lapidary ( a saw that grinds rock) and an Air Scribe that breaks rocks.

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12
Q

What three features of species do fossils need to rely on? Why do some depositional environments preserve more complete fossils than others?

A

Durability, burial, and lack of oxygen. This is because sediment will preserve the fossils well unlike other areas that are too arid and rapidly eroding like mountain ranges. Hard-structured fossils are preserved well in rivers deltas, beaches, floodplains, marshes, lakeshores, and lakeshores, and seafloors.

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