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Temperature as a control over ecosystem CO2 fluxes in a high-elevation, subalpine forest
T E Huxman1, A A Turnipseed, J P Sparks
1Department of EPO Biology, University of Colorado, Boulder 80309-0334, USA. huxman@email.arizona.edu
Oecologia
|March 21, 2003
Summary
Cool temperatures do not limit CO(2) uptake in subalpine forests. Instead, warm mid-summer temperatures increase ecosystem respiration, reducing the forest
Area of Science:
- Forest Ecology
- Ecosystem Science
- Climate Change Research
Background:
- Subalpine coniferous forests play a role in carbon sequestration.
- Previous studies suggested cool temperatures limit CO(2) uptake in these ecosystems.
- Understanding temperature effects on forest carbon exchange is crucial for climate modeling.
Purpose of the Study:
- To test the hypothesis that cool growing season temperatures limit CO(2) uptake in a subalpine coniferous forest.
- To quantify the impact of temperature on net ecosystem CO(2) exchange (NEE) and ecosystem respiration (R(e)).
- To differentiate the effects of temperature on photosynthesis versus respiration.
Main Methods:
- Utilized the eddy covariance approach to measure NEE over two growing seasons.
- Analyzed light-saturated NEE (NEE(sat)) and ecosystem respiration (R(e)) in relation to temperature.
- Employed path analysis to isolate the seasonal effects of temperature on ecosystem fluxes.
Main Results:
- NEE(sat) showed a temperature optimum between 7-12°C.
- Increasing temperatures from 7°C to 18°C reduced net CO(2) uptake capacity by 15% due to increased R(e).
- Both ecosystem quantum yield and PPFD compensation point decreased at higher temperatures.
Conclusions:
- Contrary to previous hypotheses, cool temperatures do not limit CO(2) uptake in this forest.
- Warm mid-summer temperatures increase ecosystem respiration, significantly reducing carbon sequestration potential.
- Temperature's dynamic role influences seasonal carbon fluxes, with respiration being a key limiting factor at warmer temperatures.