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The History of Life on Earth
Chapter 25 The History of Life on Earth
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Overview: Lost Worlds Past organisms were very different from those now alive The fossil record shows macroevolutionary changes over large time scales including The emergence of terrestrial vertebrates The origin of photosynthesis Long-term impacts of mass extinctions
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Fig. 25-1 Figure 25.1 What does fossil evidence say about where these dinosaurs lived?
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Fig 25-UN1 Cryolophosaurus
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Concept 25.1: Conditions on early Earth made the origin of life possible
Chemical and physical processes on early Earth may have produced very simple cells through a sequence of stages: 1. Abiotic synthesis of small organic molecules 2. Joining of these small molecules into macromolecules 3. Packaging of molecules into “protobionts” 4. Origin of self-replicating molecules
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Synthesis of Organic Compounds on Early Earth
Earth formed about 4.6 billion years ago, along with the rest of the solar system Earth’s early atmosphere likely contained water vapor and chemicals released by volcanic eruptions (nitrogen, nitrogen oxides, carbon dioxide, methane, ammonia, hydrogen, hydrogen sulfide)
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A. I. Oparin and J. B. S. Haldane hypothesized that the early atmosphere was a reducing environment
Stanley Miller and Harold Urey conducted lab experiments that showed that the abiotic synthesis of organic molecules in a reducing atmosphere is possible
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Video: Hydrothermal Vent
However, the evidence is not yet convincing that the early atmosphere was in fact reducing Instead of forming in the atmosphere, the first organic compounds may have been synthesized near submerged volcanoes and deep-sea vents Video: Tubeworms Video: Hydrothermal Vent
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Fig. 25-2 Figure 25.2 A window to early life?
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Amino acids have also been found in meteorites
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Abiotic Synthesis of Macromolecules
Small organic molecules polymerize when they are concentrated on hot sand, clay, or rock
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Protobionts Replication and metabolism are key properties of life
Protobionts are aggregates of abiotically produced molecules surrounded by a membrane or membrane-like structure Protobionts exhibit simple reproduction and metabolism and maintain an internal chemical environment
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Experiments demonstrate that protobionts could have formed spontaneously from abiotically produced organic compounds For example, small membrane-bounded droplets called liposomes can form when lipids or other organic molecules are added to water
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(a) Simple reproduction by liposomes Maltose (b) Simple metabolism
Fig. 25-3 20 µm Glucose-phosphate Glucose-phosphate Phosphatase Starch Amylase Phosphate Maltose Figure 25.3 Laboratory versions of protobionts (a) Simple reproduction by liposomes Maltose (b) Simple metabolism
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(a) Simple reproduction by liposomes
Fig. 25-3a 20 µm Figure 25.3 Laboratory versions of protobionts (a) Simple reproduction by liposomes
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Glucose-phosphate Glucose-phosphate Phosphatase Starch Amylase
Fig. 25-3b Glucose-phosphate Glucose-phosphate Phosphatase Starch Amylase Phosphate Figure 25.3 Laboratory versions of protobionts Maltose Maltose (b) Simple metabolism
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Self-Replicating RNA and the Dawn of Natural Selection
The first genetic material was probably RNA, not DNA RNA molecules called ribozymes have been found to catalyze many different reactions For example, ribozymes can make complementary copies of short stretches of their own sequence or other short pieces of RNA
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Early protobionts with self-replicating, catalytic RNA would have been more effective at using resources and would have increased in number through natural selection The early genetic material might have formed an “RNA world”
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Concept 25.2: The fossil record documents the history of life
The fossil record reveals changes in the history of life on earth
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The Fossil Record Sedimentary rocks are deposited into layers called strata and are the richest source of fossils Video: Grand Canyon
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Figure 25.4 Documenting the history of life
Present Rhomaleosaurus victor, a plesiosaur Dimetrodon 100 million years ago Casts of ammonites 175 200 270 300 4.5 cm Hallucigenia 375 Coccosteus cuspidatus 400 1 cm Figure 25.4 Documenting the history of life Dickinsonia costata 500 525 2.5 cm 565 Stromatolites 600 Tappania, a unicellular eukaryote Fossilized stromatolite 3,500 1,500
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Hallucigenia Dickinsonia costata 500 525 565 Stromatolites Tappania, a
Fig Hallucigenia 1 cm Dickinsonia costata 500 525 2.5 cm 4.5 cm 565 Stromatolites Figure 25.4 Documenting the history of life 600 Tappania, a unicellular eukaryote Fossilized stromatolite 3,500 1,500
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Rhomaleosaurus victor, a plesiosaur
Fig. 25-4a-2 Present Rhomaleosaurus victor, a plesiosaur Dimetrodon 100 million years ago Casts of ammonites 175 200 Figure 25.4 Documenting the history of life 270 300 4.5 cm 375 Coccosteus cuspidatus 400
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Rhomaleosaurus victor, a plesiosaur
Fig. 25-4b Figure 25.4 Documenting the history of life Rhomaleosaurus victor, a plesiosaur
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Fig. 25-4c Figure 25.4 Documenting the history of life Dimetrodon
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Casts of ammonites Fig. 25-4d
Figure 25.4 Documenting the history of life Casts of ammonites
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Coccosteus cuspidatus
Fig. 25-4e Figure 25.4 Documenting the history of life 4.5 cm Coccosteus cuspidatus
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Fig. 25-4f Figure 25.4 Documenting the history of life 1 cm Hallucigenia
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2.5 cm Dickinsonia costata Fig. 25-4g
Figure 25.4 Documenting the history of life Dickinsonia costata 2.5 cm
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Tappania, a unicellular eukaryote
Fig. 25-4h Figure 25.4 Documenting the history of life Tappania, a unicellular eukaryote
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Fig. 25-4i Figure 25.4 Documenting the history of life Stromatolites
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Fossilized stromatolite
Fig. 25-4j Figure 25.4 Documenting the history of life Fossilized stromatolite
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Animation: The Geologic Record
Few individuals have fossilized, and even fewer have been discovered The fossil record is biased in favor of species that Existed for a long time Were abundant and widespread Had hard parts Animation: The Geologic Record
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How Rocks and Fossils Are Dated
Sedimentary strata reveal the relative ages of fossils The absolute ages of fossils can be determined by radiometric dating A “parent” isotope decays to a “daughter” isotope at a constant rate Each isotope has a known half-life, the time required for half the parent isotope to decay
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1/2 1/4 1/8 1/16 Accumulating “daughter” isotope
Fig. 25-5 Accumulating “daughter” isotope Fraction of parent isotope remaining 1/2 Remaining “parent” isotope 1/4 Figure 25.5 Radiometric dating 1/8 1/16 1 2 3 4 Time (half-lives)
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Radiocarbon dating can be used to date fossils up to 75,000 years old
For older fossils, some isotopes can be used to date sedimentary rock layers above and below the fossil
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The magnetism of rocks can provide dating information
Reversals of the magnetic poles leave their record on rocks throughout the world
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The Origin of New Groups of Organisms
Mammals belong to the group of animals called tetrapods The evolution of unique mammalian features through gradual modifications can be traced from ancestral synapsids through the present
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Fig. 25-6 Synapsid (300 mya) Temporal fenestra Key Articular Dentary Quadrate Squamosal Therapsid (280 mya) Reptiles (including dinosaurs and birds) Temporal fenestra EARLY TETRAPODS Dimetrodon Early cynodont (260 mya) Synapsids Temporal fenestra Very late cynodonts Earlier cynodonts Therapsids Figure 25.6 The origin of mammals Later cynodont (220 mya) Mammals Very late cynodont (195 mya)
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Synapsid (300 mya) Temporal fenestra Key Articular Quadrate
Fig Synapsid (300 mya) Temporal fenestra Key Articular Quadrate Therapsid (280 mya) Dentary Squamosal Figure 25.6 The origin of mammals Temporal fenestra
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Very late cynodont (195 mya)
Fig Early cynodont (260 mya) Key Articular Temporal fenestra Quadrate Dentary Squamosal Later cynodont (220 mya) Figure 25.6 The origin of mammals Very late cynodont (195 mya)
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Concept 25.3: Key events in life’s history include the origins of single-celled and multicelled organisms and the colonization of land The geologic record is divided into the Archaean, the Proterozoic, and the Phanerozoic eons
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Table 25-1 Table 25.1
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Table 25-1a Table 25.1
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Table 25-1b Table 25.1
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The Phanerozoic encompasses multicellular eukaryotic life
The Phanerozoic is divided into three eras: the Paleozoic, Mesozoic, and Cenozoic Major boundaries between geological divisions correspond to extinction events in the fossil record
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Ceno- zoic Meso- zoic Humans Paleozoic Colonization of land Animals
Fig. 25-7 Ceno- zoic Meso- zoic Humans Paleozoic Colonization of land Animals Origin of solar system and Earth 1 4 Proterozoic Archaean Prokaryotes Figure 25.7 Clock analogy for some key events in Earth’s history Billions of years ago 2 3 Multicellular eukaryotes Single-celled eukaryotes Atmospheric oxygen
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The First Single-Celled Organisms
The oldest known fossils are stromatolites, rock-like structures composed of many layers of bacteria and sediment Stromatolites date back 3.5 billion years ago Prokaryotes were Earth’s sole inhabitants from 3.5 to about 2.1 billion years ago
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Fig 25-UN2 1 4 Billions of years ago 2 3 Prokaryotes
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Photosynthesis and the Oxygen Revolution
Most atmospheric oxygen (O2) is of biological origin O2 produced by oxygenic photosynthesis reacted with dissolved iron and precipitated out to form banded iron formations The source of O2 was likely bacteria similar to modern cyanobacteria
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This “oxygen revolution” from 2.7 to 2.2 billion years ago
By about 2.7 billion years ago, O2 began accumulating in the atmosphere and rusting iron-rich terrestrial rocks This “oxygen revolution” from 2.7 to 2.2 billion years ago Posed a challenge for life Provided opportunity to gain energy from light Allowed organisms to exploit new ecosystems
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Fig 25-UN3 1 4 Billions of years ago 2 3 Atmospheric oxygen
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Fig. 25-8 Figure 25.8 Banded iron formations: evidence of oxygenic photosynthesis For the Discovery Video Early Life, go to Animation and Video Files.
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The First Eukaryotes The oldest fossils of eukaryotic cells date back 2.1 billion years The hypothesis of endosymbiosis proposes that mitochondria and plastids (chloroplasts and related organelles) were formerly small prokaryotes living within larger host cells An endosymbiont is a cell that lives within a host cell
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Fig 25-UN4 1 4 Billions of years ago 2 3 Single- celled eukaryotes
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The prokaryotic ancestors of mitochondria and plastids probably gained entry to the host cell as undigested prey or internal parasites In the process of becoming more interdependent, the host and endosymbionts would have become a single organism Serial endosymbiosis supposes that mitochondria evolved before plastids through a sequence of endosymbiotic events
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Endoplasmic reticulum Nucleus
Fig Cytoplasm Plasma membrane DNA Ancestral prokaryote Endoplasmic reticulum Nucleus Figure 25.9 A model of the origin of eukaryotes through serial endosymbiosis Nuclear envelope
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Aerobic heterotrophic prokaryote Mitochondrion Ancestral heterotrophic
Fig Aerobic heterotrophic prokaryote Mitochondrion Ancestral heterotrophic eukaryote Figure 25.9 A model of the origin of eukaryotes through serial endosymbiosis
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Ancestral photosynthetic eukaryote
Fig Photosynthetic prokaryote Mitochondrion Plastid Figure 25.9 A model of the origin of eukaryotes through serial endosymbiosis Ancestral photosynthetic eukaryote
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Endoplasmic reticulum Nucleus
Fig Cytoplasm Plasma membrane DNA Ancestral prokaryote Endoplasmic reticulum Nucleus Nuclear envelope Aerobic heterotrophic prokaryote Photosynthetic prokaryote Mitochondrion Figure 25.9 A model of the origin of eukaryotes through serial endosymbiosis Mitochondrion Ancestral heterotrophic eukaryote Plastid Ancestral photosynthetic eukaryote
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Key evidence supporting an endosymbiotic origin of mitochondria and plastids:
Similarities in inner membrane structures and functions Division is similar in these organelles and some prokaryotes These organelles transcribe and translate their own DNA Their ribosomes are more similar to prokaryotic than eukaryotic ribosomes
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The Origin of Multicellularity
The evolution of eukaryotic cells allowed for a greater range of unicellular forms A second wave of diversification occurred when multicellularity evolved and gave rise to algae, plants, fungi, and animals
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The Earliest Multicellular Eukaryotes
Comparisons of DNA sequences date the common ancestor of multicellular eukaryotes to 1.5 billion years ago The oldest known fossils of multicellular eukaryotes are of small algae that lived about 1.2 billion years ago
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The “snowball Earth” hypothesis suggests that periods of extreme glaciation confined life to the equatorial region or deep-sea vents from 750 to 580 million years ago The Ediacaran biota were an assemblage of larger and more diverse soft-bodied organisms that lived from 565 to 535 million years ago
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Fig 25-UN5 1 4 Billions of years ago 2 3 Multicellular eukaryotes
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