1. OBJECTIVES Species Diversity at scales above local Regional effects on local SD Equilibrium theory + Island Biog. Theory Regional SD Latitudinal SD Continental SD Global SD

2. What explains great variation in species richness over the earth? Figure 1

3. Multiple scales of species diversity Local Regional Latitudinal Continental Global

4. Many factors influence regional and local species richness.

5. Local diversity as f (regional diversity). Figure 2

6. Comparing diversities of communities in similar habitats in different regions can reveal regional effects. Figure 3

7. Saturation of local communities hypothesis: test how local and regional diversity relate. Figure 2 Figure 4

8. Variation in local species diversity depends on regional diversity. ***Are these local communities saturated? Figure 5

9. Equilibrium theories: diversity reflects a balance between processes that add vs. remove species. ***What processes add species? speciation immigration What processes subtract species? extinction emigration Differences in diversity between communities reflect differences in relative rates of these processes.

10. *** What is the pattern? What two equilibrium factors may explain it? Figure 6

11. Equilibrium theory of island biogeography: # species = balance of immigration on a regional scale vs. extinction on local scale. Figure 7

12. Islands closer to the mainland support more species because of higher immigration rates. Figure 8

13. Larger islands support more species because of lower extinction rates. Figure 9

14. Which hypotheses are illustrated in Figure (a) + (b)? Figure 10

15. *** Do experimental results support ETIB? Figure 11

16. Applications of Island Biogeography Theory to: Terrestrial systems mountain tops as islands fragmented remnants as islands Design of nature reserves

17. Regional-scale patterns of diversity also reflect: Habitat heterogeneity Suitability of physical conditions Isolation from centers of diversity

18. ***What are three patterns in regional species diversity? What factor accounts for each pattern? Figure 12

19. How do patterns of species richness differ among taxa? Why? Figure 13

20. ***What are major changes among regions from Tertiary to present? What accounts for them? What are major differences today? Figure 14

21. ***Why did climate change during the Ice Age contribute to Europe’s low species richness? Figure 15

22. What is relationship between tolerance of low temperature / rainfall and extinction? Figure 16

23. Multiple scales of species diversity Local Regional Latitudinal Continental Global

24. ***What is latitudinal gradient in woody species diversity? What explains it? Figure 17

25. Hypotheses to explain latitudinal gradient in species diversity… Time and stability Heterogeneity in space and time (Vegetation and food complexity) Herbivore and pathogen pressure Competition/niches Disturbance

26. Multiple scales of species diversity Local Regional Latitudinal Continental Global

27. How do history + biogeography + climate change influence species diversity?

28. History of life is gauged by geologic time scale. Cretaceous 150mya Cambrian 600mya --> Permian 286mya

29. Equilibrium theory in continental communities: balance between speciation and extinction on regional scale Figure 21

30. Has diversification been faster in tropics than temperate area? Figure 22

31. ***Has diversity been constant? What is role of extinction vs. additions? Figure 18

32. Did species richness increase through time? To what did richness correspond? All species turned over during this time period. Figure 19

33. Catastrophes --> what are consequences - short- and long-term? ***Asteroid impact--> extinctions of what? Figure 20

34. Multiple scales of species diversity Local Regional Latitudinal Continental Global

35. Continental drift --> positions of continents change over geologic time. Climate changes too --> influences geography of evolution Figure 23

36. Continental drift changed routes of dispersal via separation + joining. Figure 24

37. Wallace: Major zoogeographic regions reflect long-term evolutionary isolation. Figure 25

38. Exchanges of biotas after joining of continents: e.g. The Panama land bridge Figure 26

39. ***How explain same body form in multiple continents? Convergence or divergence? Figure 27

40. Climate change influences distributions of organisms. How does the historical extent of climate zones help to explain global patterns of species richness? Figure 28

41. Where does more diversification occur? Why? How does this relate to more species near 0 than at higher latitudes? Figure 29

42. Climate change in N.A. shifted species diversity; Miocene drier with grasslands. Fig Figure 30

43. Oak trees shifted their distributions after end of most recent glacial period. Figure 31

44. How does ‘dispersal limitation’ explain differences in post-glacial expansion? A,b = small; c,d = large seeded species Figure 32

45. How does climatic history determine species distributions + community composition? Figure 33