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Evolution I. Evolution I.

Evolution I 2007

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Page 1: Evolution I 2007

Evolution I.Evolution I.

Page 2: Evolution I 2007

EVOLUTION• gradual unfolding of new varieties of life from

previous forms over long periods of time (Darwin)

• from the genetic perspective : a change in allele frequency from one generation to the next

• TWO KINDS OF EVOLUTION– microevolution – short term effects occuring over

just a few generations– macroevolution – long-term effects through fossil

history, large changes produced only after many generations

Page 3: Evolution I 2007

Evolutional theories

Page 4: Evolution I 2007

JEAN BAPTISTE LAMARCK (1744 – 1829)

• Popularised the idea of evolution

• First scientific evolution theory

• Basic concepts of the Lamarck’s theory:– emphasis on the dynamic interaction of organic

forms with the environment

– environment affects and induce change in organic forms

– acquired characteristic is passed through heredity to the next generations

Page 5: Evolution I 2007

GEORGES CUVIER(1769 – 1832)

• the „father“ of zoology, palaeontology, and comparative anatomy

• criticised Lamarck’s views on evolution• proposed theory of catastrophism:

– series of violent and sudden catastrophes– all of creatures were destroyed during the

catastrophe– after things settled down, areas were restocked

with new organisms different from those previously living there)

Page 6: Evolution I 2007

CHARLES DARWIN(1809 – 1882)

• 1828 – 1831 theology studies (Christ’s College, Cambridge)

• (Reverend John Stevens Henslow – lectures in botany)

• 1831 – 1836 naturalist on a scientific expedition around the globe (H.M.S. Beagle) – recommended by Professor Henslow

• 1842 – short summary of Darwin’s views on natural selection

• 1859 – Darwin completed and published his work “On the Origin of Species by means of Natural Selection, or the Preservation of Favoured Races in the Struggle for Life”

Page 7: Evolution I 2007

Charles Darwin

stopover at the Galápagos Islands – Darwin described 13 species of finches resembled one another in the structure of their beaks, body

forms, and plumage

Page 8: Evolution I 2007

Darwin´s finches

Page 9: Evolution I 2007

DARWIN’S CONCEPT OF EVOLUTION

• All species are capable of producing offspring faster than the food supply increases.

• All living things show variation; no two individuals of a species are exactly alike.

• Because there are more individuals than can possibly survive, there is a fierce struggle for existence and those with a favourable variation in characteristics are necessary for survival will possess an advantage over others.

• These favourable variations are inherited and passed on to the next variation.

• Over long periods of geologic time, these successful variations produce great differences that result in new species.

• The background of the process is natural selection.

Page 10: Evolution I 2007

The fate of the Darwin's theory

Page 11: Evolution I 2007

Alfred Russel Wallace

(1823 – 1913)

• 1855 –published an article concerning the succession of species and their mutability

Page 12: Evolution I 2007

NEODARWINISM - THE MODERN SYNTHESIS

• Evolution is defined as a two stage

process:

– Production and redistribution of variation

(inherited differences between individuals)

– Natural selection acts on this variation

(inherited differences, or variation, among

individuals differentially affect their ability

to reproduce successfully

Page 13: Evolution I 2007

RECENT CHALLENGES TO THE MODERN SYNTHESIS

• neutral mutations– Much of variation in natural population is due to neutral

mutations and chance factors (i.e. genetic drift).

– Neutral mutations are not controlled by natural selection.

– “Natural selection is the editor, rather than composer of genetic message” (King and Jukes 1969)

• gradualism X punctuationalism– gradualism – evolution changes accumulate gradually in

evolving lineages

– punctuationalism (punctuated equilibrium) – evolution is nongradual process, evolutionary rates are not constant, the evolution is a process of long stasis and sudden quick spurts

Page 14: Evolution I 2007

MECHANISMS OF EVOLUTION

• Factors that produce and redistribute variation– mutation– migration– genetic drift– recombination

• Natural selection– differential net reproductive success– Some of genetic variations among

individual within a population may influence reproductive success. Therefore some individuals contribute more offspring to succeeding generations.

Page 15: Evolution I 2007

Theodosius Dobzhansky (1900 – 1975)

"Nothing in

biology makes

sense except in

the light of

evolution."

Page 16: Evolution I 2007

http://www.pbs.org/wgbh/evolution/index.html

Public Broadcasting Service

– www section about evolution

Page 17: Evolution I 2007

EARLY EVOLUTIONARY HISTORY

• The origin of Earth

– 4,5 – 4,6 thousands million years ago

• The oldest fossils were found in

3,8 thousands million years old

sedimentary rocks from Greenland (the

oldest terrestrial rocks).

Page 18: Evolution I 2007

Prebiotic evolution

Page 19: Evolution I 2007

What happened during the prebiotic evolution?

Urey-Miller experiment

Page 20: Evolution I 2007

The Urey - Miller experiment

Page 21: Evolution I 2007

The theory of RNA world

nucleotides

RNAaminoacids,

proteins

DNA

Page 22: Evolution I 2007

GEOLOGIC PERIODS

Origin of life

PREKAMBRIANARCHAEAN

PROTEROZOIC

PALEOZOIC

MESOZOIC

CENOZOIC ERATERTIARY

QUARTERNARY

Recent

Page 23: Evolution I 2007

Geologic periods

Page 24: Evolution I 2007

The Precambrian's lower limit is not defined, but ended about 542 (570?) million years ago.

The Precambrian encompasses about 90% of Earth's history.

Page 25: Evolution I 2007

EARLY EVOLUTIONARY HISTORY II.

• Earliest known structurally preserved organisms are stromatolites found near the North Pole, Australia.

• They have been dated at 3,5 thousands million years.

Page 26: Evolution I 2007

Ediacara Hills - Australia

Tribrachidium

CharniodiscusMawsonites

Dickinsonia

Fossils of precambrian soft-bodied organisms

Page 27: Evolution I 2007

Ediacaran (Vendian) organisms – possible reconstruction

Page 28: Evolution I 2007

Riddle of Ediacara

Page 29: Evolution I 2007

Cambrian – beginning of Paleozoic

Page 30: Evolution I 2007

Pikaia – a fossil of the first chordate

Page 31: Evolution I 2007

Pikaia – reconstruction

Page 32: Evolution I 2007

Cambrian explosion(cambrian radiation)

Page 33: Evolution I 2007

At the end of Paleozoic first land vertebrates appeared

reptile Dimetrodon

Page 34: Evolution I 2007

Mass extinction at the end of Permian

90% of species extinct

Page 35: Evolution I 2007

http://www.pbs.org/wgbh/evolution/change/deeptime/index.html

Evolution of life

Page 36: Evolution I 2007

http://www.pbs.org/wgbh/evolution/extinction/dinosaurs/index.html

What happened before 65 millions

of years?K/T border (= cretaceous / tertiary) – extinction

of dinosaurs and a lot of other species (approximately 75 % of species)