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12.1 The Fossil Record
KEY CONCEPT
Specific environmental conditions are necessary in
order for fossils to form.
12.1 The Fossil Record
Fossils can form in several ways.
• Permineralization occurs when minerals carried by water
are deposited around a hard structure.
12.1 The Fossil Record
• A natural cast forms when flowing water removes all of the
original tissue, leaving an impression.
12.1 The Fossil Record
• Trace fossils record the activity of an organism.
12.1 The Fossil Record
• Amber-preserved fossils are organisms that become
trapped in tree resin that hardens after the tree is buried.
12.1 The Fossil Record
• Preserved remains form when an entire organism becomes
encased in material such as ice.
12.1 The Fossil Record
• Specific conditions are needed for fossilization.
• Only a tiny percentage of living things became fossils.
12.1 The Fossil Record
Radiometric dating provides an accurate way to estimate
the age of fossils.
• Relative dating estimates the time during which an
organism lived.
– It compares the placement
of fossils in layers of rock.
– Scientists infer the order in
which species existed.
12.1 The Fossil Record
• Radiometric dating uses decay of unstable isotopes.
– Isotopes are atoms of an element that differ in their
number of neutrons.
neutrons
protrons
12.1 The Fossil Record
• Radiometric dating uses decay of unstable isotopes.
– Isotopes are atoms of an element that differ in their
number of neutrons.
– A half-life is the amount of time it takes for half of the
isotope to decay.
12.3
of Life Record
12.1- Origin
The Fossil
KEY CONCEPT
The origin of life on Earth remains a puzzle.
12.3
of Life Record
12.1- Origin
The Fossil
Earth was very different billions of years ago.
• There have been many hypotheses of Earth’s origins.
• The most widely accepted hypothesis of Earth’s origins is
the nebula hypothesis.
• The cloud and dust
condensed forming our
solar system. (4.6 bya)
12.3
of Life Record
12.1- Origin
The Fossil
Several sets of hypotheses propose how life began on
Earth.
• There are two organic molecule hypotheses.
– Miller-Urey experiment (in put of energy from lightening)
electrodes
“atmosphere”
water
“ocean”
heat source
amino acids
– meteorite hypothesis (brought organic compounds)
12.3
of Life Record
12.1- Origin
The Fossil
• There are different hypotheses of early cell structure.
– iron-sulfide bubbles hypothesis
12.3
of Life Record
12.1- Origin
The Fossil
• There are different hypotheses of early cell structure.
– lipid membrane hypothesis, lipids spontaneously made a
cell membrane
12.3
of Life Record
12.1- Origin
The Fossil
• A hypothesis proposes that RNA was the first genetic
material.
– Ribozymes are RNA
molecules that catalyze
their own replication.
– DNA needs enzymes to
replicate itself.
12.4
Organisms
12.1- Early
The Single-Celled
Fossil Record
KEY CONCEPT
Single-celled organisms existed 3.8 billion years ago.
12.4
Organisms
12.1- Early
The Single-Celled
Fossil Record
Microbes have changed the physical and chemical
composition of Earth.
• The oldest known fossils are a group of marine
cyanobacteria.
– prokaryotic cells
– added oxygen to
atmosphere
– deposited minerals
12.4
Organisms
12.1- Early
The Single-Celled
Fossil Record
• Fossil stromatolites provide evidence of early colonies of
life. (contain cyanobacteria)
12.4
Organisms
12.1- Early
The Single-Celled
Fossil Record
Eukaryotic cells may have evolved through
endosymbiosis.
• Endosymbiosis is a relationship in which one organism lives
within the body of another.
• Mitochondria and chloroplasts may have developed through
endosymbiosis.
12.6
Evolution
12.1- Primate
The Fossil
Record
KEY CONCEPT
Humans appeared late in Earth’s history.
12.6
Evolution
12.1- Primate
The Fossil
Record
Humans share a common ancestor with other primates.
• Primates are mammals with flexible hands and feet,
forward-looking eyes and enlarged brains.
12.6
Evolution
12.1- Primate
The Fossil
Record
• Primates evolved into prosimians and anthropoids.
– Prosimians are the oldest living primates.
– They are mostly small and nocturnal.
12.6
Evolution
12.1- Primate
The Fossil
Record
– Anthropoids are humanlike primates.
– They are subdivided into the New World monkeys, Old
World monkeys, and hominoids.
– Homonoids are
divided into
hominids, great
apes, and lesser
apes.
– Hominids include
living and extinct
humans.
12.6
Evolution
12.1- Primate
The Fossil
Record
Hominids Characteristics:
• Bipedal means walking on two legs.
– foraging
– carrying infants and food
– using tools
• Walking upright has
important adaptive
advantages.
12.6
Evolution
12.1- Primate
The Fossil
Record
There are many fossils of extinct hominids.
• Most hominids are either the genus Australopithecus or
Homo.
• Australopithecines were a successful genus.
• The Homo genus first evolved 2.4 million years ago.
12.6
Evolution
12.1- Primate
The Fossil
Record
Modern humans arose about 200,000 years ago.
• Homo sapiens fossils date to 200,000 years ago.
• Human evolution is influenced by a tool-based culture.
• There is a trend toward increased brain size in hominids.
Australopithecus
afarensis
Homo habilis
Homo
neanderthalensis
Homo sapiens