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Evolution and Fossils

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Page 1: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Evolution and Fossils

Page 2: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Fossils:

• Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago.

Page 3: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Age of rocks can tell us the age of fossils

Page 4: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Fossils are remains of ancient life

Page 5: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

3 major points on evolution through the

use of the fossil record:•Earth is about 4.5 billion years old

•Organisms have inhabited Earth for most of its history

•All organisms living today evolved from earlier, simpler life forms

Page 6: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

• Most fossils form when organisms and traces of organism are rapidly buried in fine sediments deposited by water, wind or volcanic eruptions

• Paleontologists: scientists who studies fossils.

Page 7: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Becoming A Fossil• Scientists have

described about 250,000 different fossil species– Yet that is a small fraction of

those that lived in the past!

• Evolution can be seen in the fossil record.– Fossilized species found in

older rocks are different from those found in newer rocks

Page 8: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Fossil formation• The oldest fossils are

remains of marine organisms that populated the planet's oceans.

• When they died, the plants and animals were buried by mud, sand, or silt on the sea floor.

• Land animals and plants usually decomposed or were eaten, and mainly the hard parts -- teeth, bones, shells, or wood -- were preserved.

Page 9: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Fossils can be formed in several ways

• Buried bone and shell contain tiny air spaces into which water can seep, depositing minerals.

• Reinforced by these mineral deposits, bone and shell can survive for millions of years.

• Even if the bone or shell dissolves, the mineral deposits in the shape of the body structure remain.

Page 10: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Quick Recap:

• Arrange fossils in sequence from oldest to youngest to see patterns of evolution

• Fossils are classified according to the way they are found

Page 11: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Fossils are found in layers of rock

Page 12: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

• The oldest rock layers (and therefore the oldest fossils) are always on the bottom

• The youngest are on top.

• This is referred to as superposition (super = above)

Page 13: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Oldest to the bottom:

Page 14: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago
Page 15: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Becoming a Fossil

http://www.ucmp.berkeley.edu/education/explorations/tours/fossil/9to12/intro.html

Page 16: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Organisms die and are buried by sediment

Page 17: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

• Their weight causes the lower layers to harden into sedimentary rock, trapping the organism or trace inside.

Page 18: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Not all fossils are formed by sediment

Found in Tar Pit

Found in Amber

Page 19: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

• http://www.pbs.org/wgbh/evolution/library/04/3/l_043_01.html

• Casts: a mold of an organism is created and then filled by minerals making an exact copy

• Molds: AN organism decays leaving an empty space in the rock that is the exact shape of the organism

• Imprints: Thin objects such as leaves or feathers fall into mud and then mud hardens

Page 20: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

• Trace Fossils: Evidence of animal activity (footprints, trails, etc.)

• Petrified fossils: the hard part of the organism is replaced with minerals and the minerals harden making an exact stone copy.

• Amber-preserved: Rare, but when found whole organism is preserved.

Page 21: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

• Interpretation of fossils poses another set of challenges

• Their age can only be estimated by radiometric dating of rocks they were found near or within

Page 22: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Relative dating:

•fossils on the bottom are the oldest, and the ones on the top are the youngest

– Only tells if one fossil is older than another

Relative dating:

•fossils on the bottom are the oldest, and the ones on the top are the youngest

– Only tells if one fossil is older than another

Radiometeric dating:

•radioactive isotopes are used to determine age of fossil

Radiometeric dating:

•radioactive isotopes are used to determine age of fossil

Page 23: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Fossils can show us how ecosystems change• Nevada’s Silver Peak Mountain Range

Page 24: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

Fossil of a marine animal found in the rocks of the desert

Page 25: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

• Archaeocyathids were a group of sponges that lived about 500 million years ago, and are now extinct.

• They built huge reefs (similar to coral reefs we see today) and were extremely important members of their ecosystems

Page 26: Evolution and Fossils. Fossils: Fossil: the preserved or mineralized remain or imprint of an organism that lived long ago

What could explain finding fossils of sponges in the Nevada desert?