The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere):...

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Fossils – 99 percent of all species are extinct – Fossils give evidence of organisms existence – Most fossils are found in sedimentary rock and often destroyed ducts change in the earth’s crust

Transcript of The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere):...

Page 1: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
Page 2: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• The Earth’s age is estimated at about 4.6 billion years old

• Early History of Earth (atmosphere):–Was very hot, bombarded by meteorites

–Volcanic action with lava gases, water vapor, carbon dioxide and nitrogen

3.9 billion years Earth began to cool and first organisms appeared

Page 3: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Fossils–99 percent of all species are extinct

–Fossils give evidence of organisms existence

–Most fossils are found in sedimentary rock and often destroyed ducts change in the earth’s crust

Page 4: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Types of fossils

–Trace – markings left behind

–Casts – minerals fill in space left by organism

–Petrified – minerals penetrate and replace organism

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• Molds – empty space left in sedimentary rock

• Imprints – impression left in sedimentary rock

• Amber – preserves organisms intact

Page 6: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Age of Fossil • Hutton and Lyelle helped scientists recognize that Earth is millions of years old and that the processes that changes Earth in the past are the same processes that operate in the present

Relative dating – geologic law says oldest organism are on the bottom layer

Page 7: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Age of FossilsRadiometric dating – radioactive

isotopes break down into new substances–Half-life – decay rate of radioactive isotopes

– Ex: Potassium – 40 Argon – 40 1.3 million years

– Ex: Carbon – 14 Nitrogen – 40 5730 years

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PRECAMBRIAN

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Origin: the Early Ideas

• Spontaneous Generation (abiogenesis) – the idea that nonliving material can produce life

Page 12: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Experiments:• Fransico Redi –

controlled experiments that tested the spontaneous generation of maggots from decaying meat

• Spallanzani – showed that microorganisms would not grow in boiled and sealed gravy (similar to Redi – still did not receive credit)

Page 13: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

RediSpallanzani

Page 14: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

•Many scientists still thought that microorganisms were so numerous and widespread that they must still arise spontaneously from a vital force in air

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Spontaneous Generation disproved

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• Louis Pasteur – showed that microorganisms do not simply arise in broth, even in the presence of vital force

Page 17: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• Biogenesis – the idea that living organisms come from only other living organisms – now the cornerstone of biology

Page 18: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Origin: Modern Ideas

• Simple Organic Molecules Formed:–Alexander Oparin

(Russian) – hypothesized that life formed on early earth.

Page 19: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• Primordial soup – The sun’s energy, lighting, and heat triggered chemical reactions to produce small organic molecules (ex: amino acids) from substances present in the atmosphere; rain molecules into the oceans

Page 20: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• Miller and Urey (Americans) supported Oparin’s hypothesis by simulating the conditions of early earth (primitive earth)

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Formation of Protocells

• Sidney Fox showed how the first cells might have occurred as protocells (large, ordered structures enclosed by a membrane that could carry out some life activities) ex: growth, division

Page 22: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Formation of True cells–Thought to have been

mostly prokaryotes (w/o nucleus), anaerobic (w/o oxygen) and were heterotrophs (obtained food rather than making their own food)

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• The first autotrophs (The first autotrophs (make their own make their own foodfood) are thought to have evolved ) are thought to have evolved later and were probably similar to later and were probably similar to ArchaebacteriaArchaebacteria that live in that live in harsh harsh environmentsenvironments and make own food and make own food buy buy chemosynthesischemosynthesis rather than rather than photosynthesisphotosynthesis

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• Endosymbiont Theory – was proposed by Lynn Margulis; she proposed that eukaryotes evolved through a mutualistic relationship between ancient prokaryotes

• Evidence: mitochondria & chloroplast contain structures similar to prokaryotes & unlike DNA in eukaryotic nuclei; they also have ribosomes & reproduce independently of cells they are in.

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Endosymbiont Theory

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• Ideas of Evolution Ideas of Evolution – first published by – first published by Charles DarwinCharles Darwin and and now the basis of now the basis of the the Modern Modern Evolution TheoryEvolution Theory..

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• HMS Beagle an HMS Beagle an English Ship – at the English Ship – at the age of 21age of 21 Darwin Darwin took a job as a took a job as a naturalistnaturalist..

• It was a It was a 5 year5 year journey where journey where collected collected biologicalbiological specimens at every specimens at every portport

Page 29: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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• Galapagos Islands a group of small islands that was of great interest to Darwin.

• He made observations of many species of animals and plants that lead to the possibility that species can change over time

Page 31: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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• Next 22 yrs – Darwin worked to find an explanation for how species could change over time. He modified the ideas of Thomas Mathus (who was studying how human population was growing faster than Earth’s food supply).

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Darwin & 2Types of Selection:

• Artificial Selection: nature provides the variation but humans select those variations that they found useful

• Natural Selection: when organisms with certain variations survive, reproduce, and pass variations to the next generation “Survival of the Fittest.”

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3 Types of Natural Selection

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• Stabilizing: favors average individuals in a population;

• ex: spiders with average size are more likely to survive

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• Directional: favors one of the extreme variations of a trait; ex: woodpeckers with long becks feed on insect under bark

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• Disruptive: favors individuals with both extremes of trait ex: light colored and dark colored limpets blend in with light and dark rock

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2 Types of Adaptation:

• Structural Adaptations: Arise over time

• ex: teeth, claws, thorns–Mimicry – enables one species to

resemble another–Camouflage – enables species to

blend with their surrounding

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• The viceroy (right) and monarch butterflies look very similar but monarch is poisonous to predators

“Batesian Mimicry”

Page 41: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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• Physiological Adaptations: can develop rapidly; changes metabolic processes (DNA) ex: Bacterial Resistance to Penicillin – DIRECT EXAMPLE

Page 43: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• Fossils – provide a Fossils – provide a record record of of early lifeearly life and and evolutionary historyevolutionary history

Evidence for EvolutionEvidence for Evolution

Page 44: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Anatomy – structural adaptations

• Homologous Structures: similarities in arrangement (look alike, different functions)

• ex: forelimbs of animals

Page 45: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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• Analogous Structures: similarities in function (look different; same function)

• ex: wings of butterfly and bird

Page 47: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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• Vestigial Structures: body structures that have no function in present-day organism; probably used by ancestors.

• ex: appendix, snakes with legs

Page 49: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• Embryology – similarities in the earliest stages of growth and development

• ex: in birds, mammals, fish, reptiles it is difficult to distinguish embryos

Page 50: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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•Biochemistry – comparison of the DNA, amino acids sequences.

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Summary: Evidence for Evolution

1. Fossils2. Anatomy

3. Embryology4. Biochemistry

*All evidence only shows common ancestry

Page 53: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Mechanisms of Evolution

• Populations – consists of all the members of a species that live in that area;

• evolution occurs as a population’s genes change over time not individuals

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• Gene Pool – all the genes in a population

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• Allelic Frequency – percentage of any specific allele in a gene pool (Hardy Weinberg Principle = p2+2pq+q2=1)

Page 56: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Genetic Equilibrium – population’s genes remains the same (not

evolving)

Page 57: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Changes in Genetic Equilibrium:

1. Natural Selection: Survival of the Fittest – due to variations

2. Mutation: changes in DNA sequence; many are lethal

Page 58: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

3. Genetic Drift: alterations of alleles by chance events; usually in small isolated populations ex: Amish

4. Gene flow: movement of individuals in and out of a population

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Evolution of a species?? How??• Species – organism that look alike; can

interbreed to produce fertile offspring• Speciation – evolution of new species;

occurs when members of similar population no longer interbreed to produce fertile offspring

Page 60: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Causes of speciation

• Geographic Isolation (allopatry) – when two populations are separated by geographic barriers

• ex: river, mountains

Page 61: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• Behavioral Isolation – when two populations are capable of interbreeding but have differences in courtship rituals

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• Temporal (Reproductive) Isolation - when species reproduce at different times ex: orchids pollination on different days

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• Polyploidy – multiple sets of chromosomes

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Patterns of Evolution

• Divergent Evolution – where species that were once similar become different

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Adaptive Radiation - divergent evolution that occurs when a species evolves into an array of species to fit diverse habitats

ex: Galapagos finches

Page 66: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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Convergent Evolution – when distantly related organisms evolve similar traits due to similar habitats

ex: dolphin and shark

Page 68: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Patterns of Evolution

divergent convergent

Summary: Patterns of Evolution

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• In 1871, Charles Darwin proposed in his book “The Decent of Man” that there might be an evolutionary link among monkeys, apes, and humans.

Page 71: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

What is a primate?

• A group of mammals that include lemurs, monkeys, apes, & humans

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1. Opposable thumbs

2. Large brain

3. Binocular vision

4. Flexible joints

5. Adapted feet

6. arboreal

7. Round head, flat face

8. nails, claws

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PRIMATE ORIGIN

• Scientists use fossil evidence, anatomy, embryology and genetics to propose ideas about how modern primates evolved

Page 75: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

PrimatesProsimians•Live in tress•Mostly active at night•No larger than a house cat•Eat insects, seeds, fruits

Anthropoids•Large brain•Complex skeleton

New World Monkeys•Central & South America•Live in trees-arboreal•Can grab things with their tails (prehensile tail)

Old World monkeys•Africa & Asia•Live in trees or on ground•Some live in cold regions•Use tails for balance

Hominoids•Do not have tail•Use simple tools•Humans have largest brain capacity•Classified as apes or humans

Page 76: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.
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Human Ancestry

• Hominids are primates that can walk upright (bipedalism) & include gorillas, chimpanzees, & humans

Page 78: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

• Scientists propose that between 5 and 8 million years ago in Africa that hominids diverged into 2 lines:

1. African Apes – gorillas and chimpanzees

Page 79: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

2. Modern Humans-Evolution of Homo Sapiens

Australopithecus afarensis (1924)

Lucy

4 mya

Australopithecus africanus (1974)

3 mya

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Skills• Australopithecines climbed trees• They could also walk upright on the

ground• They have a foramen magnum opening in

the skull through which the spinal cord passes

• Possessed ape-like & human-like traits

Page 81: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Homo Habilis (1964)Leaky1.5-2 mya

Homo erectus

1.6 mya

Page 82: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Skills

• Homo habilis used simple tools• “Handy Man”• Homo Erectus used large tools• “Upright Man”; more human like

Page 83: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Archaic Homo Sapiens

Neanderthal

3500-100,000 yrs ago

Homo sapien

100,000 yrs ago

Cro-Magnon

33-40,000 yrs ago

Page 84: The Earth’s age is estimated at about 4.6 billion years old Early History of Earth (atmosphere): – Was very hot, bombarded by meteorites – Volcanic action.

Skills

• Neanderthals seem to have hatchet, culture, and spoken language

• Cro-Magnons were talented artists & tool makers

• Homo sapiens build cities and used technology

• Brain volume of 1,000 to 1,4000 cm3