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CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張張張 張張張張 張張張 http://genomed.dlearn.kmu.edu.tw

CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

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Page 1: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE

Section A: Introduction to the History of Life

張學偉 助理教授 生物系

http://genomed.dlearn.kmu.edu.tw

Page 2: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

Fig. 26.1

chronology episodes

phylogenetic tree

Introduction

Page 3: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

Copyright © 2002 Pearson Education, Inc., publishing as Benjamin Cummings

Fig. 26.2

Page 4: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

organisms were microscopic and mostly unicellular.

1. Life on Earth originated between 3.5 and 4.0 billion years ago

• prokaryotes diverged into two main evolutionary branches, the bacteria and the archaea.

2. Prokaryotes dominated evolutionary history from 3.5 to 2.0 billion years ago

Page 5: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• Two rich sources for early prokaryote fossils are:

1. stromatolites (fossilized layered microbial mats)

2. sediments from ancient hydrothermal vent habitats.

Fig. 26.4

stromatolites

Page 6: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系
Page 7: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• early versions of photosynthesis did not split water and liberate oxygen.

3. Oxygen began accumulating in the atmosphere about 2.7 billion years ago

• Cyanobacteria, photosynthetic organisms that split water and produce O2 as a byproduct

• Water were saturated with O2 extra O2 reacted with dissolved iron to form the precipitate iron oxide. (banded iron with red color) [Fig 26.5]

all iron preciptate

oxygen began accumulating in the atmosphere (10% of current values)

Page 8: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

This “corrosive” O2 had an enormous impact on life, dooming many prokaryote groups.

terrestrial rocks with iron began oxidizing.

• Some species survived in habitats that remained anaerobic.

• Other species evolved mechanisms to use O2 in cellular respiration (aerobic).

Copyright © 2002 Pearson Education, Inc., publishing as Benjamin Cummings

Page 9: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• Eukaryotic cells are generally larger and more complex than prokaryotic cells.

• In part, this is due to “endosymbiotic prokaryotes” that evolved into mitochondria and chloroplasts.

4. Eukaryotic life began by 2.1 billion years ago

•The evolution of chloroplasts and mitochondrion, turned the accumulating O2 to metabolic advantage through cellular respiration.

Page 10: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• A great range of eukaryotic unicellular forms evolved into the diversity of present-day “protists.”

5. Multicellular eukaryotes evolved by 1.2 billion years ago

Fig. 26.6

Fossilzed algawith more than 2 types of cells

Page 11: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• snowball Earth hypothesis

ice age (750 to 570 million years ago) may be responsible for the limited diversity and distribution of multicellular eukaryotes until the very late Precambrian.

The first major diversification at the time of thawing of snowball Earth.

Page 12: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

= Cambrian radiation

(explosion) of animal

6. Animal diversity exploded during the early Cambrian period

• extent from their first fossil

Fig. 26.8See detail in chapter 32-34

Page 13: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

7. Plants, fungi, and animals colonized the land about 500 million years ago

• Plants colonized land in association with fungi. symbiotic association

• herbivorous (plant-eating) animals and their predators.

• The most widespread and diverse terrestrial animals are certain arthropods and certain vertebrates.

• Most orders of modern mammals, including primates, appeared 50-60 million years ago.

• Humans diverged from other primates only 5 million years ago

Page 14: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

Section B: The Origin of Life

CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE

• Hypothesis:

• 4.0 billion years ago the Earth’s crust began to solidify

• 3.5 billion years ago stromatolites appear the first organisms

Introduction

Page 15: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• Most scientists favor the hypothesis that life on Earth developed from nonliving materials, an idea called spontaneous generation.

1. The first cells may have originated by chemical evolution on a young Earth: an overview

Page 16: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

In 1862, Louis Pasteur conducted broth experiments that rejected the idea of spontaneous generation.

Fig. 26.9•Although there is no evidence that spontaneous generation occurs today, conditions on the early Earth were very different.

Page 17: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• the principle of biogenesis

All life today arises only by the reproduction of preexisting life.

• hypothesis is that chemical and physical processes in Earth’s primordial environment eventually produced simple cells.

four stages that can be tested in the laboratory:

(1) the abiotic synthesis of small organic molecules;

(2) joining these small molecules into polymers:

(3) origin of self-replicating molecules;

(4) packaging of these molecules into “protobionts.”

Page 18: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• In the 1920’s, A.I. Oparin and J.B.S. Haldane independently postulated

that conditions on the early Earth favored the synthesis of organic compounds from inorganic precursors.

• The reducing environment in the early atmosphere promoted the joining of simple molecules to form more complex ones.

2. Abiotic synthesis of organic molecules is a testable hypothesis

Page 19: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

In 1953, Stanley Miller and Harold Urey tested the Oparin-Haldane hypothesis

Fig. 26.10

•The atmosphere in the Miller-Urey model is more strongly reducing environment than is currently believed.

amino acids & organic molecules.

Page 20: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• The abiotic origin hypothesis predicts that monomers should link to form polymers without enzymes and other cellular equipment.

3. Laboratory simulations of early-Earth conditions have produced organic polymers

Page 21: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• Today, cells store their genetic information as DNA transcribe into RNA translate into enzymes and other proteins.

• Many researchers have proposed that the first hereditary material was RNA, not DNA.

• Because RNA can also function as an enzymes, it helps resolve the paradox of which came first, genes or enzymes.

4. RNA may have been the first genetic material

Page 22: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• Short polymers of ribonucleotides can be synthesized abiotically in the laboratory.

• base-pairing rules up to 10 bp

• If zinc is added, may reach 40 bp with less than 1% error.

Fig. 26.11

Page 23: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• In the 1980’s Thomas Cech discovered that RNA molecules are important catalysts in modern cells.

• Ribozymes

1. RNA catalysts that remove introns from RNA.

2. help catalyze synthesis of new RNA polymers.

In the pre-biotic world, RNA molecules may have been fully capable of ribozyme-catalyzed replication.

Page 24: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• RNA sequences can evolve in abiotic conditions.

• RNA molecules have both a genotype (nucleotide sequence) and a phenotype (three

dimensional shape) that interacts with surrounding molecules.

• some RNA sequences are more stable, replicate faster and with fewer errors.

• RNA-directed protein synthesis is one function of rRNA today in ribosomes.

Page 25: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• Living cells may have been preceded by protobionts, aggregates of abiotically produced molecules.

• Protobionts do not reproduce precisely, but they associate with life, metabolism, and excitability.

5. Protobionts can form byself-assembly

Page 26: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• In the laboratory, lipid droplets of abiotically produced liposomes

form a molecular bilayer, like bio-membrane. [growth]

Fig. 26.12a

Simplereproduction

Page 27: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

Fig. 26.12b

absorb

release

Simplemetabolism

Page 28: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

6. Natural section could refine protobionts containing hereditary information

Fig. 26.13

Page 29: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• The most successful protobionts would grow and split, distributing copies of their genes to offspring.

• Evolution refined primitive metabolism and inheritance.

• One refinement was the replacement of RNA as the repository of genetic information by DNA, a more stable molecule.

Page 30: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

7. Debates about the origin of life abounds

• It is proposed that ancestors of modern prokaryotes thrived in very hot conditions and may have lived on inorganic sulfur compounds that are common in deep-sea vent environments.

• Hypothesis: life is not restricted to Earth.

• The presence of ice on Europa, a moon of Jupiter

• Mars is cold, dry, and lifeless today.

Page 31: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

Copyright © 2002 Pearson Education, Inc., publishing as Benjamin Cummings

Section C: The Major Lineages of Life

1. The five kingdom system reflected increased knowledge of

life’s diversity

2. Arranging the diversity of life into the highest taxa is a work in

progress

CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE

Page 32: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

1. The five-kingdom system reflected increased knowledge of life’s diversity

In the early days of biology, all organisms were classified as either plants or animals. [Linnaeus]

Single-celled eukaryotic organisms such as algae and Paramecium plant kingdoms [photosynthetic]

Fungi and prokaryotes plants [fungi are sedentary and prokaryotes have cell walls.]

Page 33: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

In 1969, R.H Whittaker

The five-kingdom system prevailed in biology for over 20Yr.

Fig. 26.15

autotrophic decomposer

Different Nutrition

Most protists are unicellular.

However, some multicellular organisms were included in Protista because of their relationships to specific unicellular protists.

Page 34: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

• During the last 30Yr, cladistic analysis have been identifying problems with the five-kingdom system. two distinct lineages of prokaryotes.

2. Arranging the diversity of life into the highest taxa is a work in progress

• three-domain system:

Bacteria, Archaea, and Eukarya, as superkingdoms.

Page 35: CHAPTER 26 EARLY EARTH AND THE ORIGIN OF LIFE Section A: Introduction to the History of Life 張學偉 助理教授 生物系

Fig. 26.16

• Keep in mind that phylogenetic trees and taxonomic groupings are hypotheses that fit the best available data.

• Many microbiologists have divided the two prokaryotic domains into multiple kingdoms (based on cladistic analysis of molecular data.)