Title: Elizabeth Selig
1Causes of the Latitudinal Gradient in Richness
2Outline of the Talk
- Background
- Hypotheses explaining the gradient
- Papers
- Where do we go from here
3Background
- Among the oldest and broadest patterns in ecology
- Peak in species richness at the equator is
generally true regardless of biotas taxa,
geographic context, or time domain - Gradient has existed for at least 250 million
years
4Exceptions
- Narrow latitudinal gradients
- Species w/parasitic life histories
- Aquatic floras
- Marine mammals and birds
5A Cornucopia of Hypotheses
- Historical
- Spatial
- Environmental
- Biological
Rapoports Rule
Mid-Domain
Historical
Energy
Favorableness
Disturbance
Stability
Heterogeneity
6I. HISTORICAL Ecological
Following glaciation, dispersal is ongoing and
recolonization is not complete
Problem latitudinal gradient still exists in the
oceans
7I. HISTORICAL Evolutionary
Extinction and extirpation from glaciation
have limited richness in high latitudes
speciation is slow and not complete
8II. SPATIAL
- Area
- Tropics support more species because they
have more area
Problem More area in high latitudes in North
America and Eurasia
9II. SPATIAL
2. Geometric Constraint/Mid-Domain Effect
Bounded domain will have mid-domain peak in
species richness
Problem Unsupported in many areas e.g. Connelly,
2003 and Zapata, 2003
10III. ENVIRONMENTAL
- Energy Availability/Productivity
- Stability
- Favorableness
- Habitat heterogeneity
- Disturbance
11III. ENVIRONMENTAL
- Energy Availability/Productivity
- Stability
- Favorableness
- Habitat heterogeneity
- Disturbance
12III. ENVIRONMENTAL
1. Energy Availability/Productivity
- Annual input of solar radiation determines
energy availability, productivity, and biomass
and is inversely related to latitude
13III. ENVIRONMENTAL
1. Energy Availability/Productivity
-
- Energy controls rate of speciation (Rohde, 1992)
- More energy allows more species to persist
- Problem Fails to provide mechanism
Bromham and Cardillo
14III. ENVIRONMENTAL
2. Stability
- Temporal variation in the environment causes
higher extinction and lower speciation - Low latitudes, stability results in finer niche
division and lower extinction - High latitudes, environmental variation results
in biota that are speciation and extinction
resistant
15III. ENVIRONMENTAL
3. Favorableness
- Favorable environments require less
energetic cost of adaptation
16IV. BIOLOGICAL
- Predation and parasitism
- Mutualism
- Competition ? Increased niche partitioning
17Why these papers?
- Importance of scale
- Focus on multiple explanations for the gradient
- Ecological and evolutionary considerations
including life history
18Dynesius and Jansson Milankovitch oscillations
-
- Environmental stability
- Historical evolutionary and ecological
19Dynesius and Jansson Milankovitch oscillations
20Astorga et al. Patterns of latitudinal diversity
in crabs
- Environmental Energy Availability/Productivity
- Spatial Area
- Rapoports Rule
21Astorga et al. Patterns of latitudinal diversity
in crabs
- Importance of spatially structured SST as a
primary driver of gradient
22Astorga et al. Patterns of latitudinal diversity
in crabs
- Scale lt5 SSTs do not explain gradient in
diversity - Circulation patterns, geography, nutrient etc.
may diversity at small scales
23Astorga et al. Patterns of latitudinal diversity
in crabs
- Importance of larval development on patterns of
diversity
24Discussion Questions
- Does the paper by Astorga et al. identify a
causal mechanism to explain the latitudinal
gradient? - What does their conclusion about SST and larval
development mean for finding a general
explanation for the gradient? - Dynesisus and Jansson assume that speciation is
slow. Is this a fair assumption?
25Where do we go from here?Discussion Questions
- What are the drivers? What are the modifiers?
Can we create a hierarchical model to explain the
pattern?
Jansson, 2003
26Where do we go from here?Discussion Questions
- How can we incorporate scale into the model?
- Is there a silver bullet? Is it important to look
for one?