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Chapter 15: Macroevolution Origin of life Big Bang Early Earth molton atmosphere 1st this with water vapor and volcanic gasses as earth cooled, H 2 O QuickTime™ and a decompressor are needed to see this picture. QuickTime™ and a decompressor are needed to see this picture.

Chapter 15: Macroevolution

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Chapter 15: Macroevolution. Origin of life Big Bang Early Earth molton atmosphere 1st this with water vapor and volcanic gasses as earth cooled, H 2 O condensed, N 2 escaped. First fossils 3.5 billion years ago stromatolite - PowerPoint PPT Presentation

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Page 1: Chapter 15:  Macroevolution

Chapter 15: Macroevolution

Origin of life

Big Bang

Early Earth

molton

atmosphere

1st this with water vapor and volcanic gasses

as earth cooled, H2O condensed, N2 escaped

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Page 2: Chapter 15:  Macroevolution

First fossils

3.5 billion years ago

stromatolite

can not be first life because they photosynthesized

Life is therefore older than 3.9 billion years

Page 3: Chapter 15:  Macroevolution

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How did life begin?

Current hypothesis

1. Abiotic synthesis of organic molecules

2. Small molecules join to form macromolecules

3. Macromolecules get packaged in membrane

4. Origin of self replicating molecule

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Evidence

Miller-Urey experiment

1923

tested hypothesis of JBS Haldane and AI Oparin

H2O, H2, CH4, NH3, + sparks = aas

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Page 7: Chapter 15:  Macroevolution

The path to life…

Polymers

produced by dehydration reactions and without enzymes

Protobionts

formed spontaneously in lab

Page 8: Chapter 15:  Macroevolution
Page 9: Chapter 15:  Macroevolution

RNA World

Chicken vs Egg:

DNA-----RNA-----Protein

How did it evolve?

RNA that could self replicate (w/out ribosomes or proteins)

Ribozymes

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Once self replication exists, natural selection can begin

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Significant Events

Origin of single celled organisms

Origin of multi-celled organisms

Colonization of land

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Single Celled Organisms

Prokaryotes

Earth’s sole inhabitants from 3.5 to 3 bya

Transformed the atmosphere

O2 causeddecline in anaerobesincrease in aerobic prokaryotes

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Single Celled Organisms

Eukaryote

oldest fossil 2.1 bya

photosynthetic and/or respiratory prokaryotes living in larger cell

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Multi-Celled Eukaryotes

Oldest fossils 1.2 bya

Molecular clock suggests 1.5 bya

More diverse fossils 600 mya

Cambrian Explosion 535 to 525 mya

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Colonization of land by multi-celled eukarotes

500 mya

Plants and fungi colonized together

Arthropods and Tetrapods are the most widespread and diverse

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Human lineage diverged 6 to 7 mya

Homo sapiens diverged 195,000 ya

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How do we know?

Actual ages of rocks and fossilsradiometric dating

Fossil record documents history of life

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Radiometric Dating

Isotopes - use half life to determine age

C12/C14 good for young fossils (<25,000 years)

Other isotopes better for older fossils

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Fossil Record

Fossils appear in strata

Earth’s history divided into 3 Eons

Archaeon

Protozeroic

Phanerzoic

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Phanerzoic eon divided into 3 eras

Paleozoic

Mesozoic

Cenozoic

Boundaries of eras = mass extinctions

Lesser extinctions often mark boundaries of periods

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Page 23: Chapter 15:  Macroevolution

Cambrian Explosion

Suddenly all modern animal phyla appear

Why the sudden appearance?

1. Lots of empty niches

Or 2. Sudden appearance of hard body parts = good fossils

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Mechanisms of Macro Evolution

Continental Drift

Mass Extinctions

Adaptive Radiations

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Continental Drift

Proposed in 1916, accepted in 1960s

Since origin of eukaryotes, all continents have come together 3 times

1.1 bya

600 mya

250 mya

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Thin crust on hot mantle

Some places moving apartNorth America and Europe

Others moving together“Ring of Fire”

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Page 29: Chapter 15:  Macroevolution

Pangea

250 million years ago

Brought species together that had evolved separately

Inland seas drained

Interior of continenet probably extreme

Caused big biological shake up

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Break-up of Pangea

180 million years ago (mesozoic)

135 mya First split into north and south

65 mya modern continents take shapeend of mesozoic, beginning of cenozoic

55 mya India ran into Eurasia = Himalayas

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This pattern of continents merging and breaking up solves a lot of

puzzles

Marsupials vs eutharians

lungfishes

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Page 33: Chapter 15:  Macroevolution

Mass Extinctions

5 over past 500 million years

50% or more of earth’s species went extinct in each event

End of Permian and Cretaceous get most attention

End of Permian took 96% of marine animals

End of Cretaceous took >50% of marine species and dinosaurs

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Causes of mass extinctions

Permian

enormous volcanic eruptions in present day Serbia

lava, ash, CO2 increased T

slowed mixing of ocean between pole and equator = decrease in O2 in water

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Causes of mass extinctions

Cretaceous

Asteroid

iridium signature

65 my old crater off yucatan, 180 km in diameter

Page 36: Chapter 15:  Macroevolution
Page 37: Chapter 15:  Macroevolution

Consequences of mass extinctions

Loss of whole ecosystems

Changes course of evolution

Recovery takes 5 to 10 million years or longer (100 my after permian)

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Is the 6th mass extinction underway?

> 1000 species have gone extinct in the last 400 years

100 to 1000 times normal rate

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Adaptive Radiations

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Evo-devo

Evolutionary changes caused by:

Changes in timing or rate of devolpment

Changes in spatial patterning

New genes/changes in genes

Changes in regulation

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Page 42: Chapter 15:  Macroevolution
Page 43: Chapter 15:  Macroevolution

How novelties can arrise

Gradual change

e.g. eyes

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Exaption

adapted for one purpose,

adopted for another

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Evolution is not goal oriented!

Trends don’t mean there is a goal.

Evolution is the result of existing organisms’ genetic diversity and the CURRENT

environment.

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Phylogenies

The evolutionary history of a species or group of species.

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Phylogenies

Inferred from

fossil record

morphological homologies

molecular homologies

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Analogous vs homologous structures

Convergent evolution can be misleading.

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Ocotillo found in SW US Alluaudia found in Madagascar

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Systematics

Focuses on classifying organisms and determines their evolutionary origin

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Taxonomists name things

Genus species

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Linneaus’s system still used:

SpeciesGenusFamilyOrderClass

PhylumKingdomDomains

africanaLoxodonta

ElephantidaeProboscideaMammaliaChordataAnimalia

Eukaryote

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Problems with the system…

It is all subjective and ultimately, arbitrary.

Phylocode

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Since Darwin, systematics

has expanded to reflect

evolutionary relationships in phylogenetic

trees.

Page 54: Chapter 15:  Macroevolution

Constructing Trees

Cladistics

evolution proceeds when a new heritable trait developes

Shared derived characteristics

Shared ancestral characteristics

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Ingroup compared to outgroup

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Parsimony

the simplest hypothesis is most likely to be the correct one.

construct trees with fewest changes

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Trees as hypotheses

Best tree is only most likely

Always changing with new information

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Trees allow us to make and test predictions

The more we know the more accurately we can make and test predictions.

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Page 60: Chapter 15:  Macroevolution

Molecular Systematics

Comparing nucleic acids or other molecules to infer relatedness

Booming field - tons of new data

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Molecular Systematics

Can compare recent and ancient divergences

rDNA for ancient

mtDNA for recent

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Genome Evolution

Humans have 99% homology to mice

50% homology to yeast

Many shared biochemical and developemental pathways

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Overwhelming support for Darwin’s concept of

“decent with modification”

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Gene duplication

We can trace evolution of gene families

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The number of genes does not increase at the same rate as

organismal complexity.

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Molecular Clock

Some genomic regions appear to accumulate change at a constant rate.

Calibrated by graphing nucleotide changes vs date of branch

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Molecular systematics is helping link all life.

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A highly resolved Tree Of Life, based on completely sequenced genomes [1].

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