Chapter 13 Biodiversity Through Earth History

1. Chapter 13 Biodiversity Through Earth History

2. The Fossil Record of Biodiversity • Underlying assumption is that the process of evolution is occurring • evolution: creation of new species • random mutation: genetic changes • natural selection: environmental pressures favor certain characteristics • adaptation: favored characteristics prevail • extinction: death of all members of a species

3. The Fossil Record of Biodiversity The text starts off with two ideas about how the number of species changes over time that do not seem to pan out One view is that, perhaps, diversity is a dynamic process: logistic growth – “S-shaped” growth observed for populations, common model used in population dynamics rate of change in number = origination - extinction of species on earth rate rate This does not seem to be the case.

4. The Fossil Record of Biodiversity These observations do not appear to be logistic, but do they indicate exponential growth in # of species? Problem with this: # of species may simply be a function of the amount of sediment available. Does not appear to be either logistic or exponential

5. The Fossil Record of Biodiversity The taxonomic tree for homo sapiens

6. The Fossil Record of Biodiversity Data on the number of new appearances of marine invertebrates of a given age (namely, as they appeared) by phyla-classes-orders taxonomic levels. Compare to previous data - no exponential growth is observed when looking at the evidence this way

7. The Fossil Record of Biodiversity Marine invertebrate fossils indicating diversity through geological time At least five major extinctions over the past 500 m. y. Largest mass extinction at end of Permian, 251 mya. Best researched extinction (dinosaurs) is the Cretaceous-Tertiary (K-T), 65 mya. Fossil record indicates high taxonomic levels are less affected, and that lower taxonomic levels recover rapidly from mass extinctions Mass extinctions cause great losses but stimulate origination. 65 my 440 my 360 my 251 my 206 my

8. Extinction of dinosaurs, many other marine and terrestrial species (both animal and plant) • Iridium: normally deposited at a slow, known, rate from extraterrestrial sources. Iridium concentrations in the layer at the K-T boundary are so high that it could not have been deposited by normal deposition, must have been a massive, sudden extraterrestrial source. • Most iridium on earth is in core, concentration in asteroids are much higher than on earth’s surface The Cretaceous-Tertiary (K-T) Mass Extinction(see chapter 1 also)

9. Estimated size of meteorite, from amount of iridium, = 10km diameter • Example of a “shock” to the earth system. The climate, biosphere, recovered, but at different rates. Biosphere “recovery” was very different from prior biosphere. The Cretaceous-Tertiary (K-T) Mass Extinction(see chapter 1 also)

10. The Cretaceous-Tertiary (K-T) Mass Extinction • What caused it, and how did the earth system respond? • This has been the most studied, and perhaps most controversial, extinction event. Big debate in the scientific literature in the 1980s – 90s • Realistic possibilities: • Sudden sea level or climate change • Volcanic eruptions • Meteorite (comet or asteroid, extraterrestrial) impact

11. The Cretaceous-Tertiary (K-T) Mass Extinction Sudden sea level or climate change Not likely, because some of the times of greatest climate and/or sea level changes have not coincided with mass extinctions Volcanic eruptions or extraterrestrial impacts the idea is that the heat and explosion from the impact would kill everything regionally, and that the subsequent cooling from dust / soot would kill many things globally. Volcanic eruptions could result in global cooling from sulfur aerosols in the stratosphere. Impact would also send hot particles across the globe starting fires; destroy the ozone layer for several years; caused tsunamis; food would be scarce for survivors; CO2 would have been released increasing temperatures for thousands of years; toxics across the globe; slow recovery time of biosphere.

12. The Cretaceous-Tertiary (K-T) Mass Extinction • Meteorite impact theory • Luis Alvarez’s 13 predictions which indicate that the geological evidence is consistent with the meteorite impact theory (only some listed here) • Iridium layer should be at the K-T boundary worldwide • Frequency of large meteorites is sufficient to explain the record frequency of collisions of large objects with Earth.

13. The Cretaceous-Tertiary (K-T) Mass Extinction • Meteorite impact theory • Luis Alvarez’s 13 predictions that show that the geological evidence is consistent with the meteorite impact theory • Both plants and animalsshould have been affected • clays in the iridium layershould be identical worldwide, be differentthan the layers aboveand below, and have an extraterrestrialsignature Evidence for mass extinction of plants

14. The Cretaceous-Tertiary (K-T) Mass Extinction • Meteorite impact theory • Luis Alvarez’s 13 predictions that show that the geological evidence is consistent with the meteorite impact theory • There should be evidenceof high temperature and high pressure at impact.Sphericals (from cooling of molten droplets in air)and shocked quartz (only forms when quarts is underhigh pressure) are there. • Evidence of wildfires • Layer should be between a change in fossils Evidence for mass extinction of plants

15. The Cretaceous-Tertiary (K-T) Mass Extinction • Meteorite impact theory • Luis Alvarez says that the geological evidence is inconsistent with the volcano theory • Volcanoes would notdistribute the spherules globally • Shocked quartz has neverbeen found in volcanicdeposits, but is often foundin meteorite impact craters • Volcanic deposits tend to havelow iridium concentrations Evidence for mass extinction of plants

16. The Cretaceous-Tertiary (K-T) Mass Extinction • Meteorite impact theory • Additional evidence: • Helium isotopes found in the layer are extraterrestrial • The Chicxulub Crater: - associated with cenotes-contain spherules and shocked quartz-enriched in iridium-in the right age range Location of the Chicxulub impact crater Size of impact crater

17. The Cretaceous-Tertiary (K-T) Mass Extinction Did the biological pump shut down for hundreds of thousands of years? Currently, and prior to K-T, there is adifference in C13/C12 ~2o/oo Difference is caused by the biologicalpump, algae preferentially take up C12, then sink to bottom and decompose After K-T, much smaller difference.

18. Extraterrestrial influences and extinctions Asteroids: rocky material composed of minerals and metals from dust to 100km in size found mostly in the asteroid belt (between Mars and Jupiter) Comets: materials that are volatile on earth but solid in space, plus some minerals and metals found mostly in the Oort Cloud

19. Extraterrestrial influences and extinctions Both asteroids and comets can be deflected, by collision, into different orbits that might cause them to collide with a planet, including earth. Jupiter acts as a major gravitational attraction to deflected asteroids, affecting their paths and possibly sending them towards other planets

20. Extraterrestrial influences and extinctions • Is there a 26 million year periodicity in the extinction record? • 4 possible explanations: • Galactic plane hypothesis • Companion star hypothesis • Planet X hypothesis • Artifact of the way the data are collected Vertical lines drawn every 26 million years

21. Location of the Chicxulub impact crater Support for meteorite impact as a cause for the K-T mass extinction: frequency of collisions of large objects with Earth. Size of impact crater Evidence supporting meteorite impact and its effect on plants at the K-T boundary

22. Extraterrestrial influences and extinctions • Is there a 26 million year periodicity in the extinction record? • 4 possible explanations: • Galactic plane hypothesis: our solar system moves up and down in a 26 million year cycle through the plane of the galaxy. When we pass through the center, we encounter more gas/dust, higher chance of disturbing the orbit of an asteroid or comet

23. Extraterrestrial influences and extinctions • Is there a 26 million year periodicity in the extinction record? • 4 possible explanations: • Companion star hypothesis: our sun has a companion star (small brown dwarf, <.08 size of sun) in an orbit that passes through the Oort cloud every 26 million years

24. Extraterrestrial influences and extinctions • Is there a 26 million year periodicity in the extinction record? • 4 possible explanations: • Planet X hypothesis: there isa planet that we have never seen,located in an orbit beyond Pluto,that disturbs the Kuiper Belt

25. Extraterrestrial influences and extinctions • Is there a 26 million year periodicity in the extinction record? • 4 possible explanations: • Artifact of the way the data are collected:data are collected in stages, perhaps this results in some funnycyclicity in the data Vertical lines drawn every 26 million years