island biogeography

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Ecosystem Ecology

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Island Biogeography. Dan Simberloff and Mangrove Islands. Simberloff’s defaunation experiment on Mangroves. Simberloff’s defaunation experiment on Mangroves. Results from Simberloff’s Experiment. Islands recovered to pre-defaunation number of species, but only 30% - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Island Biogeography

Ecosystem Ecology

Page 2: Island Biogeography
Page 3: Island Biogeography
Page 4: Island Biogeography
Page 5: Island Biogeography

Raymond Lindeman Sir Arthur Tansley

Page 6: Island Biogeography
Page 7: Island Biogeography

Some Energy Flow Definitions• Gross primary production (GPP) - total fixation of energy

by autotrophs - usually just due to photosynthesis, primarily by plants

• Net primary production (NPP) = GPP - respiration, autotrophs use some energy for their own growth and that is lost as respiratory heat, so NPP represents what is available to heterotrophs - NPP is often 10% of GPP

• Secondary productivity - production of biomass by heterotrophs

• Standing crop - amount of biomass of living organisms in a unit of area

Page 8: Island Biogeography
Page 9: Island Biogeography
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Page 11: Island Biogeography
Page 12: Island Biogeography

P – productivity tn/ha/yr; B – biomass tn/ha; R - solar radiation – kcal/m2/yr

Page 13: Island Biogeography

Temperature, Precipitation and Productivity

Page 14: Island Biogeography

Limits to Terrestrial Productivity

a) shortage of water restricts rate of photosynthesisb) shortage of mineral nutrients slows down rate of

production of photosynthetic tissue and the effectiveness of photosynthesis

c) temperatures that are lethal or too low for growthd) insufficient depth of soil (deserts, mountain tops)e) incomplete vegetation canopy cover so that much

sunlight lands on the ground and not on foliage

Page 15: Island Biogeography

Comparison of productivity by a deciduous tree and an evergreen tree

Page 16: Island Biogeography

Limits to Aquatic Productivity

a) Lack of nutrientsb) Light is limiting – suspended particles in

water reduce light penetrationc) Intensity of grazing

Page 17: Island Biogeography

Coastal Upwelling

Page 18: Island Biogeography

Light Penetration in Oceanic Waters

Page 19: Island Biogeography

Basic ecosystem - nutrient cycling in red, energy flow in grey

Page 20: Island Biogeography

Basic Energy Flow

Page 21: Island Biogeography

Basic Energy Flow

Page 22: Island Biogeography
Page 23: Island Biogeography

Energy Flow Expanded

Page 24: Island Biogeography

Energy Flow in Different Ecosystems

Page 25: Island Biogeography

Transfer Efficiency

Page 26: Island Biogeography

10% Rule for Transfer Efficiency

Page 27: Island Biogeography

Consumption Efficiency• CE = food ingested/food produced• How much of prey population that consumer eats• For herbivores – 5% in forests, 25% in grasslands,

50% in phytoplankton ecosystems• For vertebrate predators – up to 50-100% vertebrate

prey; 5% invertebrate prey• For invertebrate predators – 25% invertebrate prey

Page 28: Island Biogeography

Assimilation Efficiency

• AE = food assimilated/food ingested• How much of prey eaten is digested• AE usually low for herbivores,

microbivores, detritivores – 20-50%• AE usually high for carnivores – 80%

Page 29: Island Biogeography

Production Efficiency

• PE = new biomass produced/food assimilated• How much of prey digested is converted to

consumer biomass and used in reproduction – rest is lost as respiratory heat

• PE high for invertebrates – 30-40%• Intermediate for ectotherm vertebrates – 10-20%• Low for endotherm vertebrates – 1-2%

Page 30: Island Biogeography

Lindeman’s Efficiency

• LE = assimilation at trophic level n assimilation at trophic level n – 1

LE examines efficiency of transfer between trophic levels – often assumed to be 10% but…is actually more complex

Page 31: Island Biogeography

Light Absorption

Page 32: Island Biogeography

Lindeman’s Efficiencies