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Extinction Outline

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Title: Topic 13 leftovers 15: Transitions and Extinctions Author: Eric Baack Last modified by: Anonymous User Created Date: 3/23/2006 12:52:31 AM – PowerPoint PPT presentation

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Title: Extinction Outline


1
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

2
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

3
Extinctions through time percent of families lost
End Permian
K/T boundary
background extinction
4
The Cretaceous-Triassic Extinction (K/T)
  • Initial evidence in favor of asteroid impact
  • Iridium anomaly

77 Ir 192.217
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?
5
If impact, what consequences (and what evidence
might be found?)
  • Evidence of impact?
  • Why would this cause extinctions?

6
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

7
Evidence for impact Ir anomaly
Hallam Fig 8.3
8
Evidence for impact tsunami deposits
Fastovksy and Weishampel Fig 18.6
9
How does an asteroid cause extinction?
  • Initial effects (first hour to day)
  • Middle-term effects
  • Long-term effects

10
Were the dinosaurs already dying out? (Or did an
asteroid kill off a dying group?)
  • Difficulties of answering!

11
No loss of diversity until boundary instaneous
death (at least by geological time)
Fastovksy and Weishampel Fig 18.12
12
Who survived? Who went extinct?
Percent of species extinct at K/T boundary
  • Marine Continental
  • 83 planktonic foraminifera 100 non-bird
    dinosaurs
  • 100 ammonites 100 pterosaurs
  • 93 marine reptiles 56 other reptiles
  • 65 corals 10 flowering plants
  • All animals gt 25 kg

Ammonite extinct
Nautiloid survived
13
One other great extinction the end of the
Permian
  • Cause?

14
Flood basalts
15
How would volcanic eruptions lead to mass
extinction?
16
How would volcanic eruptions lead to mass
extinction?
17
. . . yet?
  • methane (CH4) very potent greenhouse gas 23x
    as potent as carbon dioxide

18
Methane and Eocene
Eocene
Pliocene
65 mya
present
Paleocene
Pleistocene
Oligocene
  • 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?

19
Evidence of warming ? 18 O and ? 13 C
20
Possible Permian Scenario
21
Carbon and extinction?
22
The next mass extinction?
  • Habitat destruction
  • Global warming, ocean acidification

Increase in diversity after K/T extinction
23
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 doesnt heat up the earth.
  • Taylor, Paul W. (ed). 2004. Extinctions in the
    history of life. Cambridge University Press.

24
Study questions
  1. 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?

25
Study questions
6. Why are duplications of Hox genes thought to
be crucial for the development of bilaterally
symmetric animals?
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