fall 2010 ib workshop series sponsored by ib academic advisors

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Fall 2010 IB Workshop Series sponsored by IB academic advisors What can I do with a B.S. in IB? Thursday, Oct. 27 4:00-5:00pm 162 Noyes Lab Career Center Staff will be on hand to discuss the job search, and job opportunities and ideas for IB

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Fall 2010 IB Workshop Series sponsored by IB academic advisors. What can I do with a B.S. in IB? Thursday, Oct. 27 4:00-5:00pm 162 Noyes Lab Career Center Staff will be on hand to discuss the job search, and job opportunities and ideas for IB majors. OBJECTIVES. - PowerPoint PPT Presentation

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Page 1: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Fall 2010 IB Workshop Seriessponsored by IB academic advisors

What can I do with a B.S. in IB?Thursday, Oct. 27

4:00-5:00pm 162 Noyes LabCareer Center Staff will be on hand to discuss the job search, and job

opportunities and ideas for IB majors.

Page 2: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Page 3: Fall 2010 IB Workshop Series sponsored by IB academic advisors

What affects regional species diversity?

• Area• Equilibrium Theories• A. Additions = Losses B. Island Biogeography Theory • Habitat heterogeneity• Suitability of physical conditions• Isolation from centers of diversity

Page 4: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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.

Page 5: Fall 2010 IB Workshop Series sponsored by IB academic advisors

*** What is the pattern? What two equilibrium factors may explain it?

Figure 1

Page 6: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 2

Page 7: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 3

Page 8: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Larger islands support more species because of lower extinction rates.

Figure 4

Page 9: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 5

Page 10: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Applications of Island Biogeography Theory to:

• Terrestrial systems• mountain tops as islands• fragmented remnants as islands

• Design of nature reserves

Page 11: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Regional-scale patterns of diversity also reflect:

• Habitat heterogeneity• Suitability of physical conditions• Isolation from centers of diversity

Page 12: Fall 2010 IB Workshop Series sponsored by IB academic advisors

***What are three patterns in regional species diversity? What factor accounts for each pattern?

Figure 7

Page 13: Fall 2010 IB Workshop Series sponsored by IB academic advisors

How do patterns of species richness differ among taxa? Why?

Figure 8

Page 14: Fall 2010 IB Workshop Series sponsored by IB academic advisors

What are two patterns of species turnover (beta diversity) at regional scales?

Figure 9

Page 15: Fall 2010 IB Workshop Series sponsored by IB academic advisors

What is the major change in longitudinal beta diversity with increasing latitude?Which latitude has more climatic uniformity?

Figure 10

Page 16: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Multiple scales of species diversity

• Local• Regional• Latitudinal• Continental• Global

Page 17: Fall 2010 IB Workshop Series sponsored by IB academic advisors

***What is latitudinal gradient in woody species diversity? What explains it?

Figure 11

Page 18: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Compare the relationship of climate variablesand species richness along latitude.

Figure 12

Page 19: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Page 20: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Multiple scales of species diversity

• Local• Regional• Latitudinal• Continental• Global

Page 21: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Page 22: Fall 2010 IB Workshop Series sponsored by IB academic advisors

History of life is gauged by geologic time scale.

Cretaceous 150mya

Cambrian 600mya --> Permian 286mya

Page 23: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Equilibrium theory in continental communities: balance between speciation and extinction on regional scale

Figure 13

Page 24: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 14

Page 25: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Catastrophes --> what are consequences - short- and long-term?

***Asteroidimpact-->extinctionsof what?

Figure 15

Page 26: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Multiple scales of species diversity

• Local• Regional• Latitudinal• Continental• Global

Page 27: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 16

Page 28: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Continental drift changed routes of dispersal via separation + joining.

Figure 17

Page 29: Fall 2010 IB Workshop Series sponsored by IB academic advisors

What explains great variation in species richness over the earth?

Figure 18

Page 30: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Wallace: Major zoogeographic regionsreflect long-term evolutionary isolation.

Figure 19

Page 31: Fall 2010 IB Workshop Series sponsored by IB academic advisors

***How explain same body form in multiple continents?

Convergence ordivergence?

Figure 20

Page 32: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 21

Page 33: Fall 2010 IB Workshop Series sponsored by IB academic advisors

***What are major changes among regions from Tertiary to present? What accounts for them?What are majordifferences today?

Figure 22

Page 34: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Climate change in N.A. shifted species diversity; Miocene drier with grasslands.

FigFigure 23

Page 35: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 15

Figure 24

Page 36: Fall 2010 IB Workshop Series sponsored by IB academic advisors

What is relationship between tolerance of low temperature / rainfall and extinction?

Figure 25

Page 37: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Oak trees shifted their distributions afterend of most recent glacial period.

Figure 26

Page 38: Fall 2010 IB Workshop Series sponsored by IB academic advisors

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

Figure 27

Page 39: Fall 2010 IB Workshop Series sponsored by IB academic advisors

How doesclimatic historydeterminespeciesdistributions +communitycomposition?

Figure 28

Page 40: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Climate change influences distributions oforganisms. How does the historical extent of climate zones help to explain global patterns ofspecies richness?

Figure 29

Page 41: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Has diversification been faster in tropicsthan temperate area?

Figure 30

Page 42: Fall 2010 IB Workshop Series sponsored by IB academic advisors

Where does more diversification occur?Why? How does this relate to more speciesnear 0 than at higher latitudes?

Figure 31

Page 43: Fall 2010 IB Workshop Series sponsored by IB academic advisors

5. HISTORY/BIOGEOGRAPHY (17 points) Last, first name___________________ These data are for birds in the islands of southeast Asia and the southwest Pacific Oceans.

A. Summarize in one sentence the major result in Fig. A. B. Summarize in one sentence the major result in Fig. B. C. What general theory do these results support? D. What are three possible explanations for the pattern in Fig. A. 1. 2. 3. E. Add a line to Fig A. that characterizes the predicted species-area relationship for a continent (rather than islands). What is one possible explanation for your new lineÕs position, relative to the one illustrated??