Chapter 14 Table of Contents Section 1 Biogenesis

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Chapter 14 Table of Contents Section 1 Biogenesis History of Life Chapter 14 Table of Contents Section 1 Biogenesis Section 2 Earth’s History Section 3 The First Life-Forms

Section 1 Biogenesis Chapter 14 Objectives Compare the principle of biogenesis with the idea of spontaneous generation. Summarize the results of experiments by Redi and by Spallanzani that tested the hypothesis of spontaneous generation. Describe how Pasteur’s experiment disproved the hypothesis of spontaneous generation.

Chapter 14 Redi’s Experiment Section 1 Biogenesis Chapter 14 Redi’s Experiment Before the 1600s, it was generally thought that organisms could arise from nonliving material by spontaneous generation.

Redi’s Experiment, continued Section 1 Biogenesis Chapter 14 Redi’s Experiment, continued Redi showed in 1668 that rotting meat kept away from flies would not produce new flies. Maggots appeared only on meat that had been exposed to flies.

Spallanzani’s Experiment Section 1 Biogenesis Chapter 14 Spallanzani’s Experiment Spallanzani showed in the 1700s that microorganisms would not grow in broth when its container was heated and then sealed. He inferred that microorganisms do not arise spontaneously but, rather, are carried in the air.

Spallanzani’s Experiment Section 1 Biogenesis Chapter 14 Spallanzani’s Experiment

Chapter 14 Pasteur’s Experiment Section 1 Biogenesis Chapter 14 Pasteur’s Experiment Pasteur in the 1800s used a variation of Spallanzani’s design to prove that microorganisms are carried in the air and do not arise by spontaneous generation.

Section 1 Biogenesis Chapter 14 Pasteur’s Experiment

Section 2 Earth’s History Chapter 14 Objectives Outline the modern scientific understanding of the formation of Earth. Summarize the concept of half-life. Describe the production of organic compounds in the Miller-Urey apparatus. Summarize the possible importance of cell-like structures produced in the laboratory.

Chapter 14 The Formation of Earth Earth’s Age Section 2 Earth’s History Chapter 14 The Formation of Earth Earth’s Age Scientists think that Earth formed more than 4 billion years ago by the gravitational accumulation of dust and debris moving through space.

The Formation of Earth, continued Section 2 Earth’s History Chapter 14 The Formation of Earth, continued Radiometric Dating Isotopes are atoms with varying numbers of neutrons.

The Formation of Earth, continued Section 2 Earth’s History Chapter 14 The Formation of Earth, continued Radiometric Dating The ages of rocks and other materials can be determined by measuring the amount of radioactive decay that has occurred in radioactive isotopes found in samples of those materials. An isotope’s half-life is the time that one-half of a sample of the isotope takes to decay.

Section 2 Earth’s History Chapter 14 Radioactive Decay

Chapter 14 Radiometric Dating Section 2 Earth’s History Click below to watch the Visual Concept. Visual Concept

First Organic Compounds Section 2 Earth’s History Chapter 14 First Organic Compounds Synthesis of Organic Compounds The first simple organic compounds on early Earth may have formed under conditions of high energy and in an atmosphere very different from that of today’s Earth. Further chemical reactions may have converted simple organic compounds into the macromolecules important to life. These conditions have been experimentally modeled.

Miller-Urey Experiment Section 2 Earth’s History Chapter 14 Miller-Urey Experiment

First Organic Compounds, continued Section 2 Earth’s History Chapter 14 First Organic Compounds, continued Organic Compounds from Beyond Earth Meteorites may have brought organic compounds to Earth.

From Molecules to Cell-Like Structures Section 2 Earth’s History Chapter 14 From Molecules to Cell-Like Structures Cell-like structures, including microspheres and coacervates, form spontaneously in certain kinds of solutions. These structures could have been a step in the formation of modern cells but lack hereditary material.

From Molecules to Cell-Like Structures, continued Section 2 Earth’s History Chapter 14 From Molecules to Cell-Like Structures, continued Scientists continue to investigate many hypotheses about the origins of organic molecules and cells in Earth’s history.

Chapter 14 Objectives Section 3 The First Life-Forms Explain the importance of the chemistry of RNA in relation to the origin of life. List three inferred characteristics that describe the first forms of cellular life on Earth. Compare the two types of autotrophy used by early cells. Relate the development of photosynthesis to the development of aerobic respiration in early cells. Explain the theory of endosymbiosis.

Chapter 14 The Origin of Heredity Section 3 The First Life-Forms Chapter 14 The Origin of Heredity The first molecule that held hereditary information may have been RNA rather than DNA.

Chapter 14 The Roles of RNA Section 3 The First Life-Forms Chapter 14 The Roles of RNA In addition to serving as a template for protein assembly, some RNA molecules can act as self-replicating enzymes and are called ribozymes.

Chapter 14 The First Cells Section 3 The First Life-Forms Chapter 14 The First Cells The first cells that formed on Earth were probably heterotrophic prokaryotes.

The First Cells, continued Section 3 The First Life-Forms Chapter 14 The First Cells, continued Chemosynthesis The first autotrophic cells probably used chemosynthesis to make food. Chemosynthesis produces energy through the oxidation of inorganic substances, such as sulfur.

The First Cells, continued Section 3 The First Life-Forms Chapter 14 The First Cells, continued Photosynthesis and Aerobic Respiration Most modern autotrophic cells, such as cyanobacteria, use photosynthesis to make food. An important byproduct of photosynthesis is oxygen.

The First Cells, continued Section 3 The First Life-Forms Chapter 14 The First Cells, continued Photosynthesis and Aerobic Respiration Once oxygen began to accumulate on Earth, cells would need to bind oxygen to other compounds in order to prevent damage to cell enzymes. This binding function may have been a first step toward aerobic respiration in cells.

Chapter 14 The First Eukaryotes Section 3 The First Life-Forms Chapter 14 The First Eukaryotes Eukaryotic cells may have evolved from large prokaryotic cells that engulfed smaller prokaryotic cells. This is known as the theory of endosymbiosis. The engulfed prokaryotic cells may have become the ancestors of organelles such as mitochondria and chloroplasts.

Origin of Eukaryotic Cells Section 3 The First Life-Forms Chapter 14 Origin of Eukaryotic Cells Click below to watch the Visual Concept. Visual Concept