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FOSSIL RECORD EVIDENCE
Background: Students know fossils are the remains of organisms that lived long ago. The fossils can be dated to show their age.
Essential Question: Why is important to use other evidences of evolution and not just the fossil record ? (CIRCLE ans. )
Vocabulary: Highlight or underline the different time periods that show the evolution of life on earth.
Darwin’s Quote“Of this history (of the world)
we possess the last volume alone….
Of this volume
only here and there a short chapter
has been preserved;
and of each page,
only here and there a few lines.”
WHAT DID HE MEAN?
RELATE IT TO THE FOSSIL RECORD
B. Fossils are remains that can tell a story
1. the relationship between species
2. the climate of earth during specific times
3. behavior and physical characteristics
I. FOSSIL RECORDA. Shows evidence of Evolution over time
THE FOSSIL RECORD REVEALS THE DIVERSITY OFVARIOUS GROUPS OF ORGANISMS OVER GEOLOGIC
TIME
C. Shows Speciation1. Usually most abundant after mass extinctions
a. species have new places to liveb. less competition for food
The GOOD news: the species that manage to survive a mass
extinction become the "stock" for the new adaptive radiations that fill
the many gaps left by extinctions. Lucky for us one primate survived
the Cretacious extinctions......
D. Shows 5 Mass extinction
1. Usually caused by change in environment
a. cooler temperatures killed the dinosaurs
b. continent movement change habitat of marine animals
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Ordovician: 50% of animal families,
Devonian: 30% of animal families,
Permian: 90% of animal families, including over 95% of marine species; many trees, amphibians, most bryozoans and brachiopods, all trilobites.
Triassic: 35% of animal families, including many reptiles and marine mollusks.
Cretaceous: up to 80% of ruling reptiles (dinosaurs); many marine species including manyforaminiferans and mollusks.
Current extinction crisis causedby human activities.
Species and families experiencing mass extinction
Bar width represents relative number of living species
Extinction
Millions ofyears ago
PeriodEra
Pa
leo
zo
icM
eso
zo
icC
en
ozo
ic Quaternary
Tertiary
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Today
65
180
250
345
500Extinction
Extinction
Extinction
Extinction
Extinction
Extinction• Evolution has not always progressed in a straight-forward manner, or from simple to complex.
• The Burgess Shale fauna were complex and bizarre marine animals from 530 million years ago that vanished completely.
Extinction in the context of Evolution
• If the environment changes rapidly and• The species living in these environments do not already possess genes which enable survival in the face of such change and
• Random mutations do not accumulate quickly enough then
• All members of the unlucky species may die
E. Incomplete fossil record
1. Most organisms will decay or be eaten before becoming fossils
2. Organisms that live in area where there is no potential of being fossilized will never be represented.
3. Due to small sample size it is difficult to study biodiversity within in species.
630-542 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
II. Ediacara Evidence – 630 mya
A. The Ediacara animals were strange organisms from which animal life began
B. The evolution of the familiar animals, plant and fungi Kingdoms happened during this time.
www.peripatus.gen.nz/paleontology/Ediacara.html
542-515 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
III. Cambrian Explosion – 542-515 mya
A. Several fossil sites show the diversity of marine animal life
B. Dramatically exploded over a short time.
Claw of AnomalocarisBurgess Shale fossils
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IV. Land Visitors – 500 mya
500 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
© Simon Braddy
Eurypterid
A. Tracks in ancient coastal dunes show that some marine animals started to make temporary visits to the sea shore to feed or mate
B. Similar to crabs today
V. Permanent Residents -460-400 mya
460 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. Worms and primitive plants started to colonize the land
Liverworts similar to the first plants
Ancient worm burrows
420 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
B. Analysis of fossil poo shows that animals started to eat plants
Fossil millipedesFossil poo contains plants
VI. First Forests 380-370 mya
380-370 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. plants grew trunks, leaves and seeds for the first time
B. This allowed them to live away from water.
SeedsLarge leavesTree trunks
VII. Amphibians -380-365 mya
380-365 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
IchthyostegaPanderichthys
A. Certain fish evolved limbs and lungs for life on land
B. The first land-dwelling amphibians retainedmany fishy characteristics
VIII. Reptiles -315 mya
315 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. The evolution of laying eggs on land.
B. This allowed reptiles to move away from water
Hylonomus lyelli
Lay eggs on land
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Links Between Major Groups
Fishes
Coelacanth and Lung Fish
Early Amphibian
Lizard-Legs on the sides
Lizard Legs
under body
Early Mammal
Early Primate
IX. First Rainforests -320-290 mya
320-290 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. Coal layers in North America and Europe are the results of the first tropical rainforests.
B. Era of giant insects.
Coal ForestsFossil plant
X. The Great Dying -251 mya
251.4 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
Extinction intensity
A. 90% of life died in a massive wave of extinction B. the largest of the so-called “Big Five”
mass extinctions
% s
pecie
s e
xtinct
XI. Dinosaurs -220-65 mya
220-65 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. Shortly after the extinction, dinosaurs appeared.
B. dominated the land for the next 150 myrs!
Links
• Links have been found between:– Fish and Amphibians– Reptiles and Birds– Reptiles and Mammals
Dinosaur Foot
Modern BirdsFeet
XII. Birds -155 mya
155 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. Birds evolved from dinosaurs.B. The similarity between birds and dinosaurs has been recognized for 160 years.
Archaeopteryx
is one of the earliest knownbirds
Microraptor
is a small feathereddinosaur
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Missing Links
• Darwin predicted that intermediate species yet to be discovered (Missing Links), would have traits linking the major groups of organisms
• Since Darwin many of these “Missing links” have been found.
Modern Bird
Archaeopteryx
Dino
Archaeopteryx Fossil
XIII. Mammals -220 mya to present
220 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. Mammals evolved about thesame time as the dinosaurs, but lived in their shadow for a 150 million years
B. Many were small, nocturnalinsect-eating animals
1. This could have lead to being warmblooded.
Yanoconodon
Link between hoofed mammals
and Whales60 million years ago
Could walk like a sea lion
But also swam50 Million years ago
Spent little time on
land, small hind legs useless for walking
40 Million years ago
Modern Whales have front
flippers and small internal hind leg bones that do not
have a function
Whale Evolution
XIV. Deep Impact -65 mya
65 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
Shocked quartz
The Crater of Doom
miac.uqac.ca/MIAC/qtz-chic.jpgA. the Earth was hit by a 10 km meteorite B. wiping out the dinosaurs
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• Cretaceous Extinction: 65 million years ago.• Loss of the dinosaurs.• Good evidence that this event was caused by an
asteroid that hit in the Yucatan, causing a “nuclear winter”.
XV. Grass and Grazers -35 mya
35 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
A. climate became cooler and drier creating grasslands
B. grazing mammals became widespread
XVI. Humans -2 mya
2 million years agohttp://en.wikipedia.org/wiki/Geologic_time_scale
Cave art
Neanderthal
A. They pioneered the use of fire and tools to control their world
A. developed society and culture
XVII. Sixth Extinction -today
Todayhttp://en.wikipedia.org/wiki/Geologic_time_scale
A. humans activity has increased the rate of species extinction
B. Possibly in our sixth mass extinction