the fossil record
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The Fossil Record. Chapter 5. objectives. SPI 0807.5.5 Compare fossils found in sedimentary rock to determine their relative age. I can: Compare fossils found in sedimentary rock to determine their relative age. Identify types of fossils. - PowerPoint PPT PresentationTRANSCRIPT
THE FOSSIL RECORD
Chapter 5
OBJECTIVES SPI 0807.5.5 Compare fossils found in
sedimentary rock to determine their relative age.
I can: Compare fossils found in sedimentary
rock to determine their relative age. Identify types of fossils. Explain how fossils are used to interpret
the past. Explain the geologic time scale.
GEOLOGIC HISTORY1. Uniformitarianism: geologic change
happen through slow gradual processes.
Most geologic change
2. Catastrophism: geologic change occurs suddenly by catastrophes.
Asteroid, comets, earthquakes, volcanoes
I can explain how fossils are used to interpret the past.
RELATIVE AGE (#77) Examines the position within rock layers
to estimate the age of an object.Look for key words such as before, after,
older, youngerExamples:
Before the dinosaurs existed Older than my brother After the extinction of the dinosaurs
Bottom layers: oldest Top layers: youngest
I can compare fossils found in sedimentary rock to determine their relative age.
ABSOLUTE AGE Precisely measures the age of fossils or
rocks in years.Examples:
5780 years ago Born in 1900 At the beginning of the Triassic period
I can compare fossils found in sedimentary rock to determine their relative age.
TYPES OF FOSSILS Fossil (#36): Remains
or physical evidence of an organism preserved by geologic processes.
1. Fossils in rock: formed when organism dies and quickly covered by sediment.
Hard parts of the organism are preserved
Soft parts decayI can identify types of fossils.
TYPES OF FOSSILS2. Fossils in
amber: entire organisms preserved inside hardened tree sap.
Insect gets caught in sticky sap, and then hardens.
Some of the best fossils.
I can identify types of fossils.
TYPES OF FOSSILS3. Petrification:
minerals replace the organism’s tissues.
I can identify types of fossils.
TYPES OF FOSSILS4. Fossils in asphalt
Thick, sticky pools trap and preserve organisms.
The La Brea asphalt deposits in Los Angeles, California have preserved organisms for at least 38,000 years.
I can identify types of fossils.
TYPES OF FOSSILS5. Frozen Fossils
In 1999, scientists removed a 20,000-year-old woolly mammoth that was frozen in the Siberian tundra.
These mammoths became extinct about 10,000 years ago.
Because cold temperatures slow down decay, the mammoth was almost perfectly preserved.
I can identify types of fossils.
TYPES OF TRACE FOSSILSTrace fossils: naturally preserved evidence of animal activity.
Tracks Reveal size and
speed of an animal. Burrows
Preserved shelters. Coprolite
Preserved animal dung.I can identify types of
fossils.
TYPES OF TRACE FOSSILS Molds: a cavity
in rock where an organism was buriedSunk in/hole
Cast: created when sediment fills a mold and becomes rock.Raised up
I can identify types of fossils.
INDEX FOSSILS Index fossils
(#44): fossils of organisms that lived for a relatively short, well-defined geologic time span.
AmmonitesMarine mollusks
similar to modern squid.
Lived b/t 230 million and 208 million years ago
I can identify types of fossils.
INDEX FOSSILS Trilobites
Closest living relative is the horseshoe crab
Lived about 400 million years ago
When scientists find fossils of trilobites anywhere on Earth, they assume the rock layers are also approximately 400 million years oldI can identify types of
fossils.
USING FOSSILS TO INTERPRET THE PAST Gives a rough sketch of the history of
life on Earth. Organisms with hard body parts have
left more fossils. Organisms that lived in areas that
favored fossilization have left more fossils.
I can explain how fossils are used to interpret the past.
USING FOSSILS TO INTERPRET THE PAST Show a history of environmental
change.Marine fossils found on mountaintops in
Canada means that these mountains formed at the bottom of the ocean.
Detect the presence of ancient seasReconstruct ancient coastlinesReconstruct past climates
Determine relationships and similarities between fossils
I can explain how fossils are used to interpret the past.
GEOLOGIC TIME Earth is about
4.6 billion years old.
The Grand CanyonColorado River
has cut/eroded away nearly 2 km deep in some places.
Represent almost half, nearly 2 billion years, of Earth’s history.
I can explain the geologic time scale.
GEOLOGIC TIME SCALE Geologists divided Earth’s history into a
scale with distinct sections of time.1. Eons: largest division of geologic time
Four eons: Hadean, Archean, Proterozoic, Phanerozoic
2. Eras: 2nd largest division of geologic time3. Periods: 3rd largest division of geologic
time4. Epochs: 4th largest division of geologic
timeI can explain the geologic time scale.
I can explain the geologic time scale.
PHANEROZOIC ERA1. Paleozoic Era (Old Life)
Marine life flourished, few land animals Land plants appeared By the end of the era, amphibians and reptiles
lived on the land. Ended with the largest mass extinction(#33) in
history 90% of all species became extinct
I can explain the geologic time scale.
MESOZOIC ERA2. Mesozoic Era (Age of Reptiles)
Dinosaurs dominated the landSmall mammalsBirdsEnded with a mass extinction15-20% of all species became extinctPossibly caused by global climate change
I can explain the geologic time scale.
CENOZOIC ERA3. Cenozoic era (Age
of Mammals) Mammals flourished Adaptations may
have helped them survive the extinction of the dinosaurs caused by environmental changes.
Regulate internal body temperature
Develop young inside the mother
I can explain the geologic time scale.