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UNIT IV Chapter 12 The History Of Life

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Page 1: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

UNIT IV

Chapter 12 The History

Of Life

Page 2: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

UNIT 4: EVOLUTIONChapter 12: The History of Life I. The Fossil Record (12.1) 

A. Fossils can form in several ways

Page 3: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

1. Permineralization- minerals carried by water are deposited around or replace the hard structure 

Petrified wood

Page 4: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Natural casts- form when flowing water removes all of original bones, leaving impression in sediment. Minerals fill in the mold 

Archaeopteryx

Page 5: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

3. Trace fossils- record activity of organism. Include nests, burrows, imprints of leaves, and footprints

Page 6: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

4. Amber-preserved fossils- organisms trapped in tree resin that hardens into amber 

Page 7: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

5. Preserved remains- form when entire organism becomes encased in material such as ice, volcanic ash, or immersed in bogs. 

Page 8: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

B. Most fossils form in sedimentary rock1. Most common fossils result from permineralization2. Best environments for fossilization include wetlands, bogs, rivers, lakebeds, and floodplains

Page 9: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

C. Only tiny percentage of living things become fossils 

Page 10: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

D. Radiometric dating provides an accurate estimate of fossil’s age  1. Relative Dating- estimate of date by comparing placement of fossils in rock layers. 

Page 11: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Radiometric dating- technique using natural decay rate of unstable isotopes

 

Page 12: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

a. Radiocarbon dating- Isotope of Carbon (14C) used with half-life of 5700 years

1). Organisms consume carbon by eating and breathing.

2). When organism dies, 14C begins to decay

3) Look at ratio of 14C to 12C

 

Page 13: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

b. Determining Earth’s Age

  1). Use decay of uranium to determine age (long half-life)

  2). Earth’s age about 4.5 billion years

 

Page 14: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

 II. The Geologic Time Scale (12.2)  A. Index fossils are another tool to determine

the age of rock layers.

Page 15: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

1. Index fossils- organisms that existed only during specific spans of time over large geographic area2. Estimate age of rock layers by fossils they contain

Page 16: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

B. The geologic time scale organizes Earth’s history  1. geologic time scale- representation of the

history of Earth

a. Organizes by major changes or events

b. Uses evidence from fossil and geologic records

Page 17: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Divided into three basic units of time

a. Eras- lasts tens to hundreds of millions of years.

1). Separated by periods of mass extinction

2). leads to periods of adaptive radiation of species

b. Periods- most common used units. Lasts tens of millions of years

c. Epochs-smallest units

 

Page 18: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

III. Origin of Life (12.3)A. Earth was very different billions of years ago

1. Earth was extremely hot first 700 million years

Page 19: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Atmosphere formed when cooled (no oxygen at first)

3. When cooled more, water vapor condensed and fell as rain.

4. Organic compounds formed from inorganic materials once water was present

Page 20: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

B. Several sets of hypotheses propose how life began on Earth  1. Organic Molecule Hypotheses

a. Miller-Urey experiment (1953)- demonstrated that organic compounds could be made by simulating conditions on early Earth

  

Page 21: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

b. Meteorite hypothesis- organic molecules may have arrived on Earth through meteorite or asteroid impacts 

Page 22: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Early Cell Structure Hypothesesa. Iron-sulfide bubbles hypothesis-

biological molecules formed in chimneys of hydrothermal vents  

Page 23: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

b. Lipid membrane hypothesis- evolution of lipid membranes crucial step for origin of life.

  1).Lipid molecules spontaneously form membrane-enclosed spheres.

2). These formed around organic molecules forming cell-like structures

Page 24: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

3. RNA as early genetic material

  a. hypothesis that RNA instead of DNA was original genetic material

  b. RNA can self-replicate

 

Page 25: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

IV. Early Single-Celled Organisms (12.4)A. Single-celled organisms changed Earth’s

surface by depositing minerals

Page 26: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

B. Changed atmosphere by giving off oxygen1. 3.5 billion years ago photosynthetic life evolved (cyanobacteria)2. Higher oxygen levels in atmosphere and

oceans allowed evolution of aerobic prokaryotes.

Page 27: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

C. Eukaryotic cells may have evolved through endosymbiosis

1. Endosymbiosis theory- one organisms lives within body of another, and both benefit from relationship

Page 28: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

 a. Early mitochondria and chloroplasts were once simple prokaryotic cells taken up by larger prokaryotes 1.5 billion years ago

b. Based theory on fact that mitochondria and chloroplasts have their own DNA and ribosomes

Page 29: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

D. The evolution of sexual reproduction led to increased diversity

  1. First prokaryotes and eukaryotes reproduced asexually

Page 30: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Sexual reproduction increases genetic variation which lets a population adapt quickly to new conditions

3. First step in evolution of multicellular life. 

Page 31: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

V. Radiation of Multicellular Life (12.5)A. One of most important transitions in history of life

1. First appeared during Paleozoic era (544 million years ago)

Page 32: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Huge diversity of animal species evolved

a. At first all life was found in ocean

 b. Eventually life moved onto land

c. Dead remains of organisms from this era changed into coal and petroleum

Page 33: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

3. Paleozoic Era ended with mass extinction

Page 34: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

B. Reptiles radiated during the Mesozoic era.1. Age of reptiles2. First mammals appeared3. Era ended with mass extinction caused by meteorite impact

Page 35: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways
Page 36: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

C. Mammals radiated during the Cenozoic era 

Page 37: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

VI. Primate Evolution (12.6)A. Humans share a common ancestor with other primates

  1. Primates- category of mammals withflexible hands and feet, forward looking eyes, and enlarged brains relative to body size.

Page 38: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2. Primate evolution- two main branches 

a. Prosimians- oldest living primate group 

Page 39: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

 b. Anthropoids- human-like primates

1). includes hominids-all species of human lineage)

Page 40: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

2). Bipedal- two legged or upright walking led to evolutionary success

Page 41: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

B. There are many fossils of extinct hominids1. Australopithecus afarensis (3 to 4

millions years ago in Africa) 

Page 42: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

 2. Homo habilis (2.4 to 1.5 million years ago) - “handy man”- used crude stone tools

Page 43: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

3. Homo Neanderthalensis (200,000 to 30,000 years ago)

Page 44: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

4. Homo sapiens- modern man

Page 45: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

C. Modern humans arose about 100,000 years ago1. Evidence points to origin in Ethiopia

100,000 years ago2. Human evolution was influenced by

culture- tools are key markers in human evolution

3. Increased skull and brain size gave humans a selective advantage

Australopithecusafarensis

Homo habilis Homo neanderthalensis

Homo sapiens

Page 46: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Chapter 12 The History

Of Life

Page 47: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

What proportion of all species that ever lived has become extinct?

a. less than 1 percent

b. approximate one-half

c. more than 99 percent

d. It is impossible to estimate.

Page 48: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

What proportion of all species that ever lived has become extinct?

a. less than 1 percent

b. approximate one-half

c. more than 99 percent

d. It is impossible to estimate.

Page 49: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Most fossils form in

a. peat bogs.

b. tar pits.

c. sedimentary rock.

d. the sap of ancient trees.

Page 50: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Most fossils form in

a. peat bogs.

b. tar pits.

c. sedimentary rock.

d. the sap of ancient trees.

Page 51: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The length of time required for half of the radioactive atoms in a sample to decay is its

a. half-life.

b. relative date.

c. radioactive date.

d. none of the above

Page 52: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The length of time required for half of the radioactive atoms in a sample to decay is its

a. half-life.

b. relative date.

c. radioactive date.

d. none of the above

Page 53: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

How would you date a sample of rock that you suspect as being one of the earliest on Earth?

a. Use a radioactive isotope with a short half-life.

b. Use a radioactive isotope with a long half-life.

c. Use an index fossil.

d. It is impossible to date very early rocks.

Page 54: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

How would you date a sample of rock that you suspect as being one of the earliest on Earth?

a. Use a radioactive isotope with a short half-life.

b. Use a radioactive isotope with a long half-life.

c. Use an index fossil.

d. It is impossible to date very early rocks.

Page 55: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The levels of division of the geologic time scale, from smallest to largest are

a. eras, periods, and epochs.

b. epochs, periods, and eras.

c. periods, eras, and epochs.

d. periods, epochs, and eras.

Page 56: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The levels of division of the geologic time scale, from smallest to largest are

a. eras, periods, and epochs.

b. epochs, periods, and eras.

c. periods, eras, and epochs.

d. periods, epochs, and eras.

Page 57: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The Mesozoic is often called the Age of

a. Invertebrates.

b. Vertebrates.

c. Dinosaurs.

d. Mammals.

Page 58: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The Mesozoic is often called the Age of

a. Invertebrates.

b. Vertebrates.

c. Dinosaurs.

d. Mammals.

Page 59: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Earth's most recent era is the

a. Paleozoic.

b. Mesozoic.

c. Cenozoic.

d. Precambrian.

Page 60: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Earth's most recent era is the

a. Paleozoic.

b. Mesozoic.

c. Cenozoic.

d. Precambrian.

Page 61: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Why did oceans not exist on Earth nearly 4 billion years ago?

a. No water was present.

b. Water remained a gas because Earth was very hot.

c. Water existed as ice because Earth was very cold.

d. none of the above

Page 62: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Why did oceans not exist on Earth nearly 4 billion years ago?

a. No water was present.

b. Water remained a gas because Earth was very hot.

c. Water existed as ice because Earth was very cold.

d. none of the above

Page 63: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Miller and Urey's experiments attempted to simulate the conditions

a. of Earth's early seas.

b. of Earth's early atmosphere.

c. of Earth before liquid water existed.

d. deep inside Earth.

Page 64: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Miller and Urey's experiments attempted to simulate the conditions

a. of Earth's early seas.

b. of Earth's early atmosphere.

c. of Earth before liquid water existed.

d. deep inside Earth.

Page 65: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A necessary condition for the evolution of life on Earth was

a. the existence of DNA.

b. free oxygen.

c. the formation of the ozone layer.

d. liquid water.

Page 66: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A necessary condition for the evolution of life on Earth was

a. the existence of DNA.

b. free oxygen.

c. the formation of the ozone layer.

d. liquid water.

Page 67: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

What do proteinoid microspheres have in common with cells?

a. They can store and release energy.

b. They contain DNA.

c. They contain RNA.

d. They are communities of organisms.

Page 68: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

What do proteinoid microspheres have in common with cells?

a. They can store and release energy.

b. They contain DNA.

c. They contain RNA.

d. They are communities of organisms.

Page 69: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The endosymbiont theory proposes that eukaryotic cells arose from

a. single prokaryotic cells.

b. multicellular prokaryotes.

c. communities of prokaryotes inside a larger cell.

d. communities of eukaryotes inside a larger cell.

Page 70: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The endosymbiont theory proposes that eukaryotic cells arose from

a. single prokaryotic cells.

b. multicellular prokaryotes.

c. communities of prokaryotes inside a larger cell.

d. communities of eukaryotes inside a larger cell.

Page 71: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

What was the response of various groups of early organisms when oxygen levels rose in the atmosphere?

a. extinction

b. a move into airless habitats

c. the evolution of metabolic pathways that used oxygen for respiration

d. all of the above

Page 72: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

What was the response of various groups of early organisms when oxygen levels rose in the atmosphere?

a. extinction

b. a move into airless habitats

c. the evolution of metabolic pathways that used oxygen for respiration

d. all of the above

Page 73: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The first organisms were

a. prokaryotes.

b. eukaryotes.

c. proteinoid microspheres.

d. microfossils

Page 74: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The first organisms were

a. prokaryotes.

b. eukaryotes.

c. proteinoid microspheres.

d. microfossils

Page 75: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A very large mass extinction occurred at the end of the

a. Precambrian.

b. Cambrian Period.

c. Paleozoic Era

d. Quaternary Period.

Page 76: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A very large mass extinction occurred at the end of the

a. Precambrian.

b. Cambrian Period.

c. Paleozoic Era

d. Quaternary Period.

Page 77: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The process by which two species evolve in response to each other, for example, a flower having a structure compatible with the body structure of its pollinator, is an example of

a. convergent evolution.

b. adaptive radiation.

c. coevolution.

d. punctuated equilibrium.

Page 78: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

The process by which two species evolve in response to each other, for example, a flower having a structure compatible with the body structure of its pollinator, is an example of

a. convergent evolution.

b. adaptive radiation.

c. coevolution.

d. punctuated equilibrium.

Page 79: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A mass extinction would encourage the rapid evolution of surviving species

a. by changing developmental genes.

b. by opening ecological niches.

c. because it killed all organisms that had coevolved.

d. because it spared all organisms that had evolved convergently.

Page 80: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A mass extinction would encourage the rapid evolution of surviving species

a. by changing developmental genes.

b. by opening ecological niches.

c. because it killed all organisms that had coevolved.

d. because it spared all organisms that had evolved convergently.

Page 81: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A single species that has evolved into several different forms that live in different ways has undergone

a. adaptive radiation.

b. coevolution.

c. punctuated equilibrium.

d. mass extinction.

Page 82: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

A single species that has evolved into several different forms that live in different ways has undergone

a. adaptive radiation.

b. coevolution.

c. punctuated equilibrium.

d. mass extinction.

Page 83: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Two patterns of macroevolution that involve very rapid response to environmental pressures are

a. convergent evolution and changes in developmental genes.

b. coevolution and convergent evolution.

c. adaptive radiation and changes in developmental genes.

d. punctuated equilibrium and mass extinction.

Page 84: UNIT IV Chapter 12 The History Of Life. UNIT 4: EVOLUTION Chapter 12: The History of Life I. The Fossil Record (12.1) A. Fossils can form in several ways

Two patterns of macroevolution that involve very rapid response to environmental pressures are

a. convergent evolution and changes in developmental genes.

b. coevolution and convergent evolution.

c. adaptive radiation and changes in developmental genes.

d. punctuated equilibrium and mass extinction.