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4/19/06 Historical Range of Variability, Part 2.

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Presentation on theme: "4/19/06 Historical Range of Variability, Part 2."— Presentation transcript:

1 4/19/06 Historical Range of Variability, Part 2. The role of fires in grasslands.

2 disturbances Climate, topography, parent material Biotic interactions with abiotic conditions (changes in physical and chemical environment for biota) Old community “new” biotic community regional pool of biota including native & non-native species

3 Fire return intervals The most fire- prone ecosystem in North America
Aber and Melillo 1991) The most fire- prone ecosystem in North America was in the semi- humid zone!!!

4 The grasslands WERE the largest biome type in the lower 48.

5 (determines fire return interval (see next graph)
Probability of Fire: Fuel load * Moisture (determines fire return interval (see next graph) Fuel Load fuel Zero fuel Low precip high precip.

6 wet Wet, low fuel (a lake!) wet, high fuel… The asbestos forests Moisture index Highest Fire return intervals Any ecosystems Over here don’t Last long! Dry, low fuel (desert) dry Zero lots biomass Fuel Index (Note that very dry systems rarely have large biomass!)

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9 Frequent fire: 1. Loss of N. 2. Increase photosynth. 3. Increase C storage in soil. 4. Immobilize N in soil

10 Burning removes canopy, volatilizes N, warms soil

11 Fire 1) attracts grazers to area (a fact known to indigenous peoples) 2) Sends large amounts of N up in smoke…makes N less available. 3) In spite of reduced N availability, stimulation of Ps Grasses generally results in higher NPP. Fire only, or grazer only systems “aren’t natural”

12 Grazing: 1) lowers probability of fire (lower fuel load) 2) lowers intensity, amount of fuel loss of fire 3) Removes the canopy to enhance light on the surface 4) deposits N onto soil rather than into atmosphere (makes N more available to plants) 5)neutral/reduces C input to soil!

13 In the absence of fire, all North American grasslands
would likely become shrublands or forest. The rate at which these become “woody” systems is a function of precipitation AND the availability of woody seeds.

14 Long-term Dynamics Keeping the tallgrass prairie within its historical
range of variability maintains native cover. Long-term Dynamics


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