Chapter 16. From the 1600s on, geologists began mapping layers of rocks at sites where there were...

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Chapter 16

Transcript of Chapter 16. From the 1600s on, geologists began mapping layers of rocks at sites where there were...

Page 1: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Chapter 16

Page 2: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.

They found similar layers around the world and decided that sand and sediments had deposited at different times to form the layers.

Page 3: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.
Page 4: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Within certain layers were distinctive fossils.

Some deeper layers had simple marine organisms, where, other layers had organisms similar to those found at the time.

Page 5: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

They decided that maybe all organisms had not left one central location, but had originated in more than one place.

If the body structure was different in different areas, then perhaps they had evolved, or modified over time.

Page 6: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Georges Cuvier was one of the leaders in the naturalist field at this time.

He founded the belief of catastrophism

Page 7: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

At the time of creation, the world was populated with all species, but some great catastrophy had destroyed some of the species, and the survivors had repopulated the world.

Other catastrophies through time had wiped out other species, thus leading to the species in existence.

Page 8: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Environmental pressure and internal needs bring about a permanent change in body form and function.

This gradual improvement should lead to perfection in time.

Page 9: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

For example the giraffe: short neck giraffes needed to reach leaves higher in trees, so they stretched their neck to reach them.

This stretched neck was passed on to offspring, who in turn, stretched their own necks and passed on that neck to their offspring.

Page 10: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.
Page 11: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

A clergyman and economist, documented human survival and the influences of famine, disease, and war.

Humans would run out of food, living space, and other resources because they reproduce too much.

When this happens, they compete for the remaining resources

Page 12: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Charles Lyell

Lyell traveled through Europe to find more evidence that gradual changes, the same we can see happening today, had produced the features of the Earth's surface.

He found evidence for many rises and falls of sea level, and of giant volcanoes built on top of far older rocks.

Processes such as earthquakes and eruptions, which had been witnessed by humans, were enough to produce mountain ranges.

Valleys were the work of the slow grinding force of wind and water.

Page 13: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Uniform Processes of Change

Lyell's version of geology came to be known as uniformitarianism, that the processes that alter the Earth are uniform through time.

Lyell could never have grasped the mechanism — plate tectonics — that makes this kind of geological change happen.

Page 14: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Lyell had an equally profound effect on our understanding of life's history.

He influenced Darwin so that Darwin envisioned evolution as a sort of biological uniformitarianism.

Evolution took place from one generation to the next before our very eyes, he argued, but it worked too slowly for us to perceive.

Page 15: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

In 1831, he boards the HMS Beagle as the ship’s naturalist.

It sailed to South America to map the coastline and crossed the Atlantic.

Darwin collected much information during the stops at the islands in between.

When he returned in 1836, Darwin began discussing his ideas with other scientists.

Page 16: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Darwin wondered if he could apply Malthus’ idea to other animals.

He assumed the environment would restrict the number of individuals, and then what would decide who would live, and who would die.

He then realized that one individual’s traits could determine its survival.

Page 17: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

He realized that the Galapagos Island finches were representative of this idea.

Thirteen species of finch inhabited the islands.

Each species had a variation in traits that made it suitable to the environment in which it lived.

Page 18: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.
Page 19: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

In 1859, he published On the Origin of Species.

He discussed how artificial selection could be used to quickly mold species, and how natural selection could do the same thing in a longer time.

Page 20: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Population is a group of the same species occupying a given area.

Certain features characterize a species: morphology (a unique body plan), physiology (the cells operate in the same way), behavior (the organisms respond in the same basic way to stimulus), and they reproduce with members of their own species.

Page 21: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

There are other small variations within the population, but they are basically the same.

Variations (polymorphism) include differences in color and size.

Page 22: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Within a population is a gene pool – all of the genes within the population.

Each gene within the pool exists in two or more slightly different forms (alleles).

Individuals inherit different combinations of alleles leading to different phenotypes.

Page 23: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Which alleles are passed on depends on five things:

a. Gene mutations – produce new alleles

b. Crossing over at meiosis I – produces new allele combinations

c. Independent assortment at meiosis I – randomly puts mixes of parental alleles into egg or sperm

Page 24: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

d. fertilization – combines two parentse. change in chromosome number or

structure – can lead to loss, duplication or relocation of genes

Page 25: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

All five criteria are rarely in play at one time.

Mutations are infrequent, but they are inevitable.

These changes lead to microevolution – small-scale changes in allele frequency as brought about by mutation, genetic drift, gene flow, and natural selection.

Page 26: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Darwin explained natural selection after associating inheritance of certain features and the environment.

He made four observations to explain his ideas:

Page 27: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

1. All populations can increase in number over generations

2. No population can increase indefinitely – it will run out of resources

Inference: Individuals will end up competing for resources

Page 28: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

3. All individuals have the same genes, which specify the assortment of traits

4. Most genes occur in alleles which give rise to different phenotypes

Page 29: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Inference: Some phenotypes are better for resource competitions and therefore help them to survive and reproduce.

These alleles increase and the genetic change leads to fitness - an increase in adaptation to the environment

Page 30: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Conclusion: Natural selection is the difference in survival and reproduction among individuals that differ in heritable traits.

Adaptation is one outcome of the microevolutionary process.

Page 31: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Allele frequency shifts in a consistent direction.

This shift occurs in response to changes in the environment.

A trait at one end of the range becomes dominant over the midrange traits.

Page 32: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Favoring of the intermediate form of a trait.

This mode counteracts gene flow, mutations and genetic drift to keep the common phenotype.

Page 33: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Forms at both extremes are favored over the intermediate form.

Page 34: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.
Page 35: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Individuals of a species may move about.

Alleles from those individuals are lost when they leave the population.

Physical flow of genes (gene flow) tries to counteract the loss and genetic differences.

It helps keep populations genetically similar.

Page 36: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.
Page 37: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Random changes in allele frequency brought about by chance alone.

Page 38: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Only one kind of allele remains in the population and all individuals are homozygous for it.

It happens in all populations eventually, but quickly in small populations.

Page 39: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Severe reduction in population size brought about by a catastrophy such as disease, habitat loss, hunting, or natural disaster.

Page 40: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

Nonrandom mating among closely related individuals.

Human populations discourage such things.

In animal populations, it has lead to rare inheritable diseases that can cause painful death in the animals.

Page 41: Chapter 16.  From the 1600s on, geologists began mapping layers of rocks at sites where there were deep cuts in the earth.  They found similar layers.

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http://www.evoled.org/images/modes.gif http://evolution.berkeley.edu/evosite/evo101/

images/geneflow_beetles.gif http://fig.cox.miami.edu/~cmallery/150/evol/

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