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Extinction Outline Fossils continued: radioisotope dating & calibration Cambrian explosion Patterns in the fossil record Extinction mass extinctions Cretaceous extinction Permian extinction Next week: human evolution, evolution of disease

Extinction Outline

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Extinction Outline. Fossils continued: radioisotope dating & calibration Cambrian explosion Patterns in the fossil record Extinction mass extinctions Cretaceous extinction Permian extinction Next week: human evolution, evolution of disease. The story so far. Earth forms - PowerPoint PPT Presentation

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Page 1: Extinction Outline

Extinction Outline

Fossils continued: radioisotope dating & calibrationCambrian explosionPatterns in the fossil record

Extinction mass extinctions Cretaceous extinction Permian extinction

Next week: human evolution, evolution of disease

Page 2: Extinction Outline

The story so far . . .

• Earth forms• First life soon thereafter (ideas, little good

evidence)• Multicellular organisms much later –

needed atmospheric oxygen?• Tremendous increase in animal diversity in

Cambrian• Fossils give us a biased, incomplete

picture of the history of life

Page 3: Extinction Outline

Extinctions through time: percent of families lost

End Permian

K/T boundary

background extinction

Page 4: Extinction Outline

The Cretaceous-Triassic Extinction (K/T)

Iridium: rare on earth, more common in comets and asteroids

Also, more common in magma

Or, from nearby supernova

Source: massive volcanic eruptions? Or impact?

Initial evidence in favor of asteroid impact

Iridium anomaly77

Ir192.217

Page 5: Extinction Outline

If impact, what consequences (and what evidence might be found?)

• Evidence of impact?

• Why would this cause extinctions?

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Evidence for impact

• Iridium anomaly found worldwide at K-T boundary

• Shocked quartz in Caribbean and North America

• Evidence for tsunami in North America

• Crater in Yucatan

• Cr isotopes found not volcanic

Page 7: Extinction Outline

Evidence for impact: Ir anomaly

Hallam Fig 8.3

Page 8: Extinction Outline

Evidence for impact: tsunami deposits

Fastovksy and Weishampel Fig 18.6

Page 9: Extinction Outline

How does an asteroid cause extinction?

• Initial effects (first hour to day):

• Middle-term effects

• Long-term effects

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Were the dinosaurs already dying out? (Or did an asteroid kill off a dying group?)

• Difficulties of answering!

Page 11: Extinction Outline

No loss of diversity until boundary: instaneous death (at least by geological time)

Fastovksy and Weishampel Fig 18.12

Page 12: Extinction Outline

Who survived? Who went extinct?

Marine Continental83% planktonic foraminifera 100% non-bird dinosaurs

100% ammonites 100% pterosaurs

93% marine reptiles 56% other reptiles

65% corals 10% flowering plants

All animals > 25 kg

Percent of species extinct at K/T boundary

Ammonite: extinct

Nautiloid: survived

Page 13: Extinction Outline

One other great extinction: the end of the Permian

Cause?

Page 14: Extinction Outline

Flood basalts

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How would volcanic eruptions lead to mass extinction?

Page 16: Extinction Outline

How would volcanic eruptions lead to mass extinction?

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. . . yet?

– methane (CH4): very potent greenhouse gas [23x as potent as carbon dioxide]

Page 18: Extinction Outline

Oligo

Methane and Eocene• Clathrates: frozen water surrounding

methane

• Estimate 500 – 2,500 gigatons (=1012 kg)

• If released, could lead to substantial global warming

• 55 mya: a thaw leading to methane release?

Paleocene

Eocene

Oligocene

Pliocene

Pleistocene

65 mya present

Page 19: Extinction Outline

Evidence of warming: 18 O and 13 C

Page 20: Extinction Outline

Possible Permian Scenario

Page 21: Extinction Outline

Carbon and extinction?

Page 22: Extinction Outline

The next mass extinction?

• Habitat destruction

• Global warming, ocean acidification

Increase in diversity after K/T extinction

Page 23: Extinction Outline

References

Fastovsky, David E. and Weishampel, David B. 2005. The evolution and extinction of the dinosaurs. Cambridge University Press.

Hallam, Tony. 2005. Catastrophes and lesser calamities: the causes of mass extinctions. Oxford University Press.

Kolbert, Elizabeth. 2006. The darkening sea: what carbon emissions are doing to the ocean. New Yorker November 20, 2006. Excellent article: something more to worry about even if carbon dioxides doesn’t heat up the earth.

Taylor, Paul W. (ed). 2004. Extinctions in the history of life. Cambridge University Press.

Page 24: Extinction Outline

Study questions1. If the last fossil is dated to 70 million years ago, can we

conclude that it went extinct at that time? Why or why not?

2. Figure 17.21 shows the pattern of extinctions for all organisms. How might the data presented here be misleading? (Think about the biases discussed in topic 13).

3. How would an asteroid impact lead to extinctions of marine organisms? Of terrestrial organisms?

4. How could global warming have led to a mass extinction at the end of the Permian?

5. Ammonites and nautiloids are both molluscs with chambered shells. Ammonites went extinct at the end of the Cretaceous while nautiloids survived. Ammonites produce free-swimming young that feed at the surface and grow rapidly while nautiloids produce a few large eggs that may sit for up to a year in the deep before growing slowly. How might these differences explain the nautiloids survival while the ammonistes went extinct?

Page 25: Extinction Outline

Study questions6. Why are duplications of Hox genes thought to be crucial for the

development of bilaterally symmetric animals?