HISTORY OF LIFE ON EARTH Physical conditions - last 4 billion years major changes: oxygen in...

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HISTORY OF LIFE ON EARTH sical conditions - last 4 billion year or changes: oxygen in atmosphere climate change ocean currents sea level changes continent movement volcanism meteorites

Transcript of HISTORY OF LIFE ON EARTH Physical conditions - last 4 billion years major changes: oxygen in...

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HISTORY OF LIFE ON EARTH

Physical conditions - last 4 billion years major changes:

•oxygen in atmosphere•climate change•ocean currents•sea level changes•continent movement•volcanism•meteorites

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How do we know ages?Relative ages of rock layers (sedimentary):

their relative positions their embedded fossils

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How do we know ages?

Absolute ages: radioisotopes

carbon 14 - half life of 5,700 y.less than 50,000 years

potassium 40 - half life of 1.3 b.y.the most ancient events

http://id-archserve.ucsb.edu/Anth3/Courseware/Chronology/09_Potassium_Argon_Dating.html

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AGE DIVISIONS

Earth’s geological history is divided into eras (eg. Cenozoic) and periods (eg. Cretaceous). boundaries between units based on differences between their fossil biotas

Cenozoic: 65 m.y.a. to presentMesozoic: ~250-65 m.y.a.Paleozoic: ~550-250 m.y.a.Precambrian: ~550 m.y.a. to 4.5 b.y.a.

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Crust movement

Continental drift: Throughout Earth’s history the continents have shifted, sometimes separating, at other times colliding.

Powered by radioactive decay within the Earth!

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Climate change (temperature)

volcanism sea level changesocean currentscarbon dioxide levels......dramatic effects on the evolution of life

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Sea levelchanges...up to 200 metersdifference

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Meteorite collisions also have changed conditions on Earth.

cause of abrupt mass extinction at the end of the Cretaceous period (65 m.y.a)

-- iridium-- Yucatan crater (180 km diameter)

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Crater - in Yucutan Mexico

Meterorite or asteroid 10 miles in diameter

70% of living species wiped out

Debris blown into air caused dramatic cooling- nuclear winter

Global firestorm from methane gas released from ocean

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The Fossil Record

Importance: Much of what we know about the history of life on Earth comes from the study of fossils.

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The Fossil Record

Reveals broad patterns in the evolution of life.

Fossils show that many evolutionary changes are gradual.

Incomplete but getting better...

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The Fossil Record

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The Fossil Record

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The Fossil Record

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Life in the Remote Past

The fossil record for Precambrian times is fragmentary, but fossils from Australia show that many animals that evolved disappeared forever.

Ediacara Hills

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Life in the Remote Past

Diversity exploded during the Cambrian period. The Cambrian Explosion. Why?

All modern phyla present ... and more

chinese fossil beds +

Burgess Shales

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Life in the Remote Past

Hallucigenia

A phylum body plan that disappeared?

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Rates of Evolutionary Change

Gradualism

Punctuated equilibrium

None? Coelacanth

... more later – molecular

clock

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Rates of Evolutionary Change

Mass extinctions (5 so far)

99% spp. have become extinct, some during mass extinctions

major changes in flora and fauna

subsequent radiations after extinctions eg. Cenozoic radiations of modern mammals

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Patterns of Evolutionary Change

Cambrian - all major Animal body plans (phyla) have evolved!

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The Future of Evolution

The forces of evolution continue to operate today

eg. in humans: West Nile Virus, sexually transmitted diseases....

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The Future of Evolution

Human intervention now plays an unprecedented role in the history of life.

Biodiversity crisis - the sixth great extinction