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Chapter 25. The History of Life on Earth. 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

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chapter 25

Chapter 25

The History of Life on Earth

overview lost worlds
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
slide4

Fig 25-UN1

Cryolophosaurus

concept 25 1 conditions on early earth made the origin of life possible
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

synthesis of organic compounds on early earth
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)
slide7
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
slide8
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

abiotic synthesis of macromolecules
Abiotic Synthesis of Macromolecules
  • Small organic molecules polymerize when they are concentrated on hot sand, clay, or rock
protobionts
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
slide13
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
slide14

Fig. 25-3

20 µm

Glucose-phosphate

Glucose-phosphate

Phosphatase

Starch

Amylase

Phosphate

Maltose

(a) Simple reproduction by

liposomes

Maltose

(b) Simple metabolism

slide15

Fig. 25-3a

20 µm

(a) Simple reproduction by

liposomes

slide16

Fig. 25-3b

Glucose-phosphate

Glucose-phosphate

Phosphatase

Starch

Amylase

Phosphate

Maltose

Maltose

(b) Simple metabolism

self replicating rna and the dawn of natural selection
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
slide18
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”
concept 25 2 the fossil record documents the history of life
Concept 25.2: The fossil record documents the history of life
  • The fossil record reveals changes in the history of life on earth
the fossil record
The Fossil Record
  • Sedimentary rocks are deposited into layers called strata and are the richest source of fossils

Video: Grand Canyon

slide21

Fig. 25-4

Rhomaleosaurus victor,

a plesiosaur

Present

Dimetrodon

100 million years ago

Casts of

ammonites

175

200

270

300

Hallucigenia

4.5 cm

375

Coccosteus cuspidatus

400

1 cm

Dickinsonia

costata

500

525

2.5 cm

565

Stromatolites

Tappania, a

unicellular

eukaryote

600

3,500 1,500

Fossilized

stromatolite

slide22

Fig. 25-4-1

Hallucigenia

1 cm

Dickinsonia

costata

500

525

2.5 cm

4.5 cm

565

Stromatolites

Tappania, a

unicellular

eukaryote

600

3,500 1,500

Fossilized

stromatolite

slide23

Fig. 25-4a-2

Rhomaleosaurus victor,

a plesiosaur

Present

100 million years ago

Dimetrodon

Casts of

ammonites

175

200

270

300

4.5 cm

375

Coccosteus cuspidatus

400

slide24

Fig. 25-4b

Rhomaleosaurus victor, a plesiosaur

slide25

Fig. 25-4c

Dimetrodon

slide26

Fig. 25-4d

Casts of ammonites

slide27

Fig. 25-4e

4.5 cm

Coccosteuscuspidatus

slide28

Fig. 25-4f

1 cm

Hallucigenia

slide29

Fig. 25-4g

2.5 cm

Dickinsonia costata

slide30

Fig. 25-4h

Tappania, a unicellular eukaryote

slide31

Fig. 25-4i

Stromatolites

slide32

Fig. 25-4j

Fossilized stromatolite

slide33
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

The Geologic Record

how rocks and fossils are dated
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
slide35

Fig. 25-5

Accumulating

“daughter”

isotope

Fraction of parent isotope remaining

1/2

Remaining

“parent”

isotope

1/4

1/8

1/16

4

3

2

1

Time (half-lives)

slide36
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
slide37
The magnetism of rocks can provide dating information
  • Reversals of the magnetic poles leave their record on rocks throughout the world
the origin of new groups of organisms
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
slide39

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

Very late cynodonts

Temporal

fenestra

Earlier cynodonts

Therapsids

Later cynodont (220 mya)

Mammals

Very late cynodont (195 mya)

slide40

Fig. 25-6-1

Synapsid (300 mya)

Temporal

fenestra

Key

Articular

Quadrate

Therapsid (280 mya)

Dentary

Squamosal

Temporal

fenestra

slide41

Fig. 25-6-2

Early cynodont (260 mya)

Key

Articular

Temporal

fenestra

Quadrate

Dentary

Squamosal

Later cynodont (220 mya)

Very late cynodont (195 mya)

slide42
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
slide46
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
slide47

Fig. 25-7

Ceno-

zoic

Meso-

zoic

Humans

Paleozoic

Colonization

of land

Animals

Origin of solar

system and

Earth

4

1

Proterozoic

Archaean

Prokaryotes

years ago

Billions of

3

2

Multicellular

eukaryotes

Single-celled

eukaryotes

Atmospheric

oxygen

the first single celled organisms
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
slide49

Fig 25-UN2

1

4

Billions of

years ago

2

3

Prokaryotes

photosynthesis and the oxygen revolution
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
slide51
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
slide52

Fig 25-UN3

1

4

Billions of

years ago

2

3

Atmospheric

oxygen

the first eukaryotes
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
slide55

Fig 25-UN4

1

4

Billions of

years ago

3

2

Single-

celled

eukaryotes

slide56
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
slide57

Fig. 25-9-1

Cytoplasm

Plasma membrane

DNA

Ancestral

prokaryote

Endoplasmic reticulum

Nucleus

Nuclear envelope

slide58

Fig. 25-9-2

Aerobic

heterotrophic

prokaryote

Mitochondrion

Ancestral

heterotrophic

eukaryote

slide59

Fig. 25-9-3

Photosynthetic

prokaryote

Mitochondrion

Plastid

Ancestral photosynthetic

eukaryote

slide60

Fig. 25-9-4

Cytoplasm

Plasma membrane

DNA

Ancestral

prokaryote

Endoplasmic reticulum

Nucleus

Nuclear envelope

Aerobic

heterotrophic

prokaryote

Photosynthetic

prokaryote

Mitochondrion

Mitochondrion

Ancestral

heterotrophic

eukaryote

Plastid

Ancestral photosynthetic

eukaryote

slide61
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
the origin of multicellularity
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
the earliest multicellular eukaryotes
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
slide64
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
slide65

Fig 25-UN5

1

4

Billions of

years ago

2

3

Multicellular

eukaryotes

the cambrian explosion
The Cambrian Explosion
  • The Cambrian explosion refers to the sudden appearance of fossils resembling modern phyla in the Cambrian period (535 to 525 million years ago)
  • The Cambrian explosion provides the first evidence of predator-prey interactions
slide67

Fig 25-UN6

Animals

1

4

Billions of

years ago

3

2

slide68

Fig. 25-10

500

Sponges

Cnidarians

Molluscs

Annelids

Chordates

Arthropods

Brachiopods

Echinoderms

Early

Paleozoic

era

(Cambrian

period)

Millions of years ago

542

Late

Proterozoic

eon

slide69
DNA analyses suggest that many animal phyla diverged before the Cambrian explosion, perhaps as early as 700 million to 1 billion years ago
  • Fossils in China provide evidence of modern animal phyla tens of millions of years before the Cambrian explosion
  • The Chinese fossils suggest that “the Cambrian explosion had a long fuse”
slide70

Fig. 25-11

(a) Two-cell stage

(b) Later stage

200 µm

150 µm

the colonization of land
The Colonization of Land
  • Fungi, plants, and animals began to colonize land about 500 million years ago
  • Plants and fungi likely colonized land together by 420 million years ago
  • Arthropods and tetrapods are the most widespread and diverse land animals
  • Tetrapods evolved from lobe-finned fishes around 365 million years ago
slide72

Fig 25-UN7

Colonization of land

1

4

Billions of

years ago

3

2

slide73
Concept 25.4: The rise and fall of dominant groups reflect continental drift, mass extinctions, and adaptive radiations
  • The history of life on Earth has seen the rise and fall of many groups of organisms

Video: Volcanic Eruption

Video: Lava Flow

continental drift
Continental Drift
  • At three points in time, the land masses of Earth have formed a supercontinent: 1.1 billion, 600 million, and 250 million years ago
  • Earth’s continents move slowly over the underlying hot mantle through the process of continental drift
  • Oceanic and continental plates can collide, separate, or slide past each other
  • Interactions between plates cause the formation of mountains and islands, and earthquakes
slide75

Fig. 25-12

North

American

Plate

Eurasian Plate

Crust

Caribbean

Plate

Philippine

Plate

Juan de Fuca

Plate

Arabian

Plate

Indian

Plate

Cocos Plate

Mantle

South

American

Plate

Pacific

Plate

Nazca

Plate

African

Plate

Outer

core

Australian

Plate

Inner

core

Antarctic

Plate

Scotia Plate

(b) Major continental plates

(a) Cutaway view of Earth

slide76

Fig. 25-12a

Crust

Mantle

Outer

core

Inner

core

(a) Cutaway view of Earth

slide77

Fig. 25-12b

North

American

Plate

Eurasian Plate

Caribbean

Plate

Philippine

Plate

Juan de Fuca

Plate

Arabian

Plate

Indian

Plate

Cocos Plate

South

American

Plate

Pacific

Plate

Nazca

Plate

African

Plate

Australian

Plate

Antarctic

Plate

Scotia Plate

(b) Major continental plates

consequences of continental drift
Consequences of Continental Drift
  • Formation of the supercontinent Pangaea about 250 million years ago had many effects
    • A reduction in shallow water habitat
    • A colder and drier climate inland
    • Changes in climate as continents moved toward and away from the poles
    • Changes in ocean circulation patterns leading to global cooling
slide79

Fig. 25-13

Present

Cenozoic

Eurasia

North America

Africa

65.5

India

South

America

Madagascar

Australia

Antarctica

Laurasia

135

Mesozoic

Gondwana

Millions of years ago

Pangaea

251

Paleozoic

slide80

Fig. 25-13a

Present

Cenozoic

North America

Eurasia

Millions of years ago

Africa

65.5

India

South

America

Madagascar

Australia

Antarctica

slide81

Fig. 25-13b

Laurasia

135

Gondwana

Mesozoic

Millions of years ago

251

Pangaea

Paleozoic

slide82
The break-up of Pangaea lead to allopatric speciation
  • The current distribution of fossils reflects the movement of continental drift
  • For example, the similarity of fossils in parts of South America and Africa is consistent with the idea that these continents were formerly attached
mass extinctions
Mass Extinctions
  • The fossil record shows that most species that have ever lived are now extinct
  • At times, the rate of extinction has increased dramatically and caused a mass extinction
the big five mass extinction events
The “Big Five” Mass Extinction Events
  • In each of the five mass extinction events, more than 50% of Earth’s species became extinct
slide85

Fig. 25-14

800

20

700

600

15

500

Number of families:

400

Total extinction rate

(families per million years):

10

300

200

5

100

0

0

Mesozoic

Paleozoic

Cenozoic

Era

Period

E

C

Tr

C

O

S

D

P

J

P

N

200

145

65.5

0

542

488

444

416

359

299

251

Time (millions of years ago)

slide86
The Permian extinction defines the boundary between the Paleozoic and Mesozoic eras
  • This mass extinction occurred in less than 5 million years and caused the extinction of about 96% of marine animal species
  • This event might have been caused by volcanism, which lead to global warming, and a decrease in oceanic oxygen
slide87
The Cretaceous mass extinction 65.5 million years ago separates the Mesozoic from the Cenozoic
  • Organisms that went extinct include about half of all marine species and many terrestrial plants and animals, including most dinosaurs
slide88

Fig. 25-15

NORTH

AMERICA

Chicxulub

crater

Yucatán

Peninsula

slide89
The presence of iridium in sedimentary rocks suggests a meteorite impact about 65 million years ago
  • The Chicxulub crater off the coast of Mexico is evidence of a meteorite that dates to the same time
is a sixth mass extinction under way
Is a Sixth Mass Extinction Under Way?
  • Scientists estimate that the current rate of extinction is 100 to 1,000 times the typical background rate
  • Data suggest that a sixth human-caused mass extinction is likely to occur unless dramatic action is taken
consequences of mass extinctions
Consequences of Mass Extinctions
  • Mass extinction can alter ecological communities and the niches available to organisms
  • It can take from 5 to 100 million years for diversity to recover following a mass extinction
  • Mass extinction can pave the way for adaptive radiations
slide92

Fig. 25-16

50

40

30

Predator genera

(percentage of marine genera)

20

10

0

Cenozoic

Paleozoic

Mesozoic

Era

Period

P

D

C

P

C

N

E

O

J

S

Tr

200

145

359

65.5

0

488

444

542

416

299

251

Time (millions of years ago)

adaptive radiations
Adaptive Radiations
  • Adaptive radiation is the evolution of diversely adapted species from a common ancestor upon introduction to new environmental opportunities
worldwide adaptive radiations
Worldwide Adaptive Radiations
  • Mammals underwent an adaptive radiation after the extinction of terrestrial dinosaurs
  • The disappearance of dinosaurs (except birds) allowed for the expansion of mammals in diversity and size
  • Other notable radiations include photosynthetic prokaryotes, large predators in the Cambrian, land plants, insects, and tetrapods
slide95

Fig. 25-17

Ancestral

mammal

Monotremes

(5 species)

ANCESTRAL

CYNODONT

Marsupials

(324 species)

Eutherians

(placental

mammals;

5,010 species)

50

200

250

100

150

0

Millions of years ago

regional adaptive radiations
Regional Adaptive Radiations
  • Adaptive radiations can occur when organisms colonize new environments with little competition
  • The Hawaiian Islands are one of the world’s great showcases of adaptive radiation
slide97

Fig. 25-18

Close North American relative,

the tarweed Carlquistia muirii

1.3

million

years

MOLOKAI

KAUAI

5.1

million

years

Dubautia laxa

MAUI

OAHU

3.7

million

years

Argyroxiphiumsandwicense

LANAI

HAWAII

0.4

million

years

Dubautia waialealae

Dubautia scabra

Dubautia linearis

slide98

Fig. 25-18a

1.3

million

years

KAUAI

5.1

million

years

MOLOKAI

MAUI

OAHU

3.7

million

years

LANAI

HAWAII

0.4

million

years

slide99

Fig. 25-18b

Close North American relative,

the tarweed Carlquistia muirii

slide100

Fig. 25-18c

Dubautia waialealae

slide101

Fig. 25-18d

Dubautia laxa

slide102

Fig. 25-18e

Dubautia scabra

slide103

Fig. 25-18f

Argyroxiphium sandwicense

slide104

Fig. 25-18g

Dubautia linearis

slide105
Concept 25.5: Major changes in body form can result from changes in the sequences and regulation of developmental genes
  • Studying genetic mechanisms of change can provide insight into large-scale evolutionary change
evolutionary effects of development genes
Evolutionary Effects of Development Genes
  • Genes that program development control the rate, timing, and spatial pattern of changes in an organism’s form as it develops into an adult
changes in rate and timing
Changes in Rate and Timing
  • Heterochrony is an evolutionary change in the rate or timing of developmental events
  • It can have a significant impact on body shape
  • The contrasting shapes of human and chimpanzee skulls are the result of small changes in relative growth rates

Allometric Growth

slide108

Fig. 25-19

15

Newborn

5

Adult

2

Age (years)

(a) Differential growth rates in a human

Chimpanzee adult

Chimpanzee fetus

Human adult

Human fetus

(b) Comparison of chimpanzee and human skull growth

slide109

Fig. 25-19a

Newborn

2

15

Adult

5

Age (years)

(a) Differential growth rates in a human

slide110

Fig. 25-19b

Chimpanzee fetus

Chimpanzee adult

Human adult

Human fetus

(b) Comparison of chimpanzee and human skull growth

slide111
Heterochrony can alter the timing of reproductive development relative to the development of nonreproductive organs
  • In paedomorphosis, the rate of reproductive development accelerates compared with somatic development
  • The sexually mature species may retain body features that were juvenile structures in an ancestral species
changes in spatial pattern
Changes in Spatial Pattern
  • Substantial evolutionary change can also result from alterations in genes that control the placement and organization of body parts
  • Homeotic genes determine such basic features as where wings and legs will develop on a bird or how a flower’s parts are arranged
slide114
Hox genes are a class of homeotic genes that provide positional information during development
  • If Hox genes are expressed in the wrong location, body parts can be produced in the wrong location
  • For example, in crustaceans, a swimming appendage can be produced instead of a feeding appendage
slide115
Evolution of vertebrates from invertebrate animals was associated with alterations in Hox genes
  • Two duplications of Hox genes have occurred in the vertebrate lineage
  • These duplications may have been important in the evolution of new vertebrate characteristics
slide116

Fig. 25-21

Hypothetical vertebrate

ancestor (invertebrate)

with a single Hox cluster

First Hox

duplication

Hypothetical early

vertebrates (jawless)

with two Hox clusters

Second Hox

duplication

Vertebrates (with jaws)

with four Hox clusters

the evolution of development
The Evolution of Development
  • The tremendous increase in diversity during the Cambrian explosion is a puzzle
  • Developmental genes may play an especially important role
  • Changes in developmental genes can result in new morphological forms
changes in genes
Changes in Genes
  • New morphological forms likely come from gene duplication events that produce new developmental genes
  • A possible mechanism for the evolution of six-legged insects from a many-legged crustacean ancestor has been demonstrated in lab experiments
  • Specific changes in the Ubx gene have been identified that can “turn off” leg development
slide119

Fig. 25-22

Hox gene 6

Hox gene 7

Hox gene 8

Ubx

About 400 mya

Artemia

Drosophila

changes in gene regulation
Changes in Gene Regulation
  • Changes in the form of organisms may be caused more often by changes in the regulation of developmental genes instead of changes in their sequence
  • For example three-spine sticklebacks in lakes have fewer spines than their marine relatives
  • The gene sequence remains the same, but the regulation of gene expression is different in the two groups of fish
slide121

Fig. 25-23

RESULTS

Test of Hypothesis A:

Differences in the coding

sequence of the Pitx1 gene?

Result:

No

The 283 amino acids of the Pitx1 protein

are identical.

Test of Hypothesis B:

Differences in the regulation

of expression of Pitx1 ?

Pitx1 is expressed in the ventral spine

and mouth regions of developing marine

sticklebacks but only in the mouth region

of developing lake stickbacks.

Result:

Yes

Lake stickleback embryo

Marine stickleback embryo

Close-up

of mouth

Close-up of ventral surface

slide122

Fig. 25-23a

Marine stickleback embryo

Lake stickleback embryo

Close-up

of mouth

Close-up of ventral surface

concept 25 6 evolution is not goal oriented
Concept 25.6: Evolution is not goal oriented
  • Evolution is like tinkering—it is a process in which new forms arise by the slight modification of existing forms
evolutionary novelties
Evolutionary Novelties
  • Most novel biological structures evolve in many stages from previously existing structures
  • Complex eyes have evolved from simple photosensitive cells independently many times
  • Exaptations are structures that evolve in one context but become co-opted for a different function
  • Natural selection can only improve a structure in the context of its current utility
slide125

Fig. 25-24

Pigmented

cells

Pigmented cells

(photoreceptors)

Epithelium

Nerve fibers

Nerve fibers

(b) Eyecup

(a) Patch of pigmented cells

Fluid-filled cavity

Cellular

mass

(lens)

Cornea

Epithelium

Optic

nerve

Pigmented

layer (retina)

Optic nerve

(c) Pinhole camera-type eye

(d) Eye with primitive lens

Cornea

Lens

Retina

Optic nerve

(e) Complex camera-type eye

evolutionary trends
Evolutionary Trends
  • Extracting a single evolutionary progression from the fossil record can be misleading
  • Apparent trends should be examined in a broader context
slide127

Fig. 25-25

Recent

(11,500 ya)

Equus

Hippidion and other genera

Pleistocene

(1.8 mya)

Nannippus

Pliohippus

Pliocene

(5.3 mya)

Neohipparion

Hipparion

Megahippus

Sinohippus

Callippus

Archaeohippus

Merychippus

Miocene

(23 mya)

Hypohippus

Anchitherium

Parahippus

Miohippus

Oligocene

(33.9 mya)

Mesohippus

Paleotherium

Epihippus

Propalaeotherium

Eocene

(55.8 mya)

Pachynolophus

Orohippus

Key

Grazers

Hyracotherium

Browsers

slide128

Fig. 25-25a

Miohippus

Oligocene

(33.9 mya)

Mesohippus

Paleotherium

Epihippus

Propalaeotherium

Eocene

(55.8 mya)

Orohippus

Pachynolophus

Key

Grazers

Hyracotherium

Browsers

slide129

Fig. 25-25b

Recent

(11,500 ya)

Equus

Hippidion and other genera

Pleistocene

(1.8 mya)

Nannippus

Pliohippus

Pliocene

(5.3 mya)

Neohipparion

Hipparion

Megahippus

Sinohippus

Callippus

Archaeohippus

Merychippus

Miocene

(23 mya)

Hypohippus

Anchitherium

Parahippus

slide130
According to the species selection model, trends may result when species with certain characteristics endure longer and speciate more often than those with other characteristics
  • The appearance of an evolutionary trend does not imply that there is some intrinsic drive toward a particular phenotype
slide131

Fig 25-UN8

1.2 bya:

First multicellular eukaryotes

535–525 mya:

Cambrian explosion

(great increase

in diversity of

animal forms)

500 mya:

Colonization

of land by

fungi, plants

and animals

2.1 bya:

First eukaryotes (single-celled)

3.5 billion years ago (bya):

First prokaryotes (single-celled)

500

1,000

1,500

4,000

3,000

3,500

2,500

2,000

Present

Millions of years ago (mya)

slide132

Fig 25-UN9

Ceno-

zoic

Meso-

zoic

Paleozoic

Origin of solar system

and Earth

4

1

Proterozoic

Archaean

years ago

Billions of

2

3

slide133

Fig 25-UN10

Flies and

fleas

Caddisflies

Moths and

butterflies

Herbivory

slide134

Fig 25-UN11

Ceno-

zoic

Meso-

zoic

Paleozoic

Origin of solar system

and Earth

4

1

Proterozoic

Archaean

years ago

Billions of

2

3

you should now be able to
You should now be able to:
  • Define radiometric dating, serial endosymbiosis, Pangaea, snowball Earth, exaptation, heterochrony, and paedomorphosis
  • Describe the contributions made by Oparin, Haldane, Miller, and Urey toward understanding the origin of organic molecules
  • Explain why RNA, not DNA, was likely the first genetic material
slide136
Describe and suggest evidence for the major events in the history of life on Earth from Earth’s origin to 2 billion years ago
  • Briefly describe the Cambrian explosion
  • Explain how continental drift led to Australia’s unique flora and fauna
  • Describe the mass extinctions that ended the Permian and Cretaceous periods
  • Explain the function of Hox genes