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Carbon Gain, Carbon Use, and Persistence: How Elevated CO₂ and Warming Reshape High-Elevation Plants
Pallavi Nautiyal1, Mohan Chandra Nautiyal1
1High Altitude Plant Physiology Research Centre (HAPPRC), H.N.B. Garhwal University, Srinagar, Uttarakhand, India.
Alpine plants face carbon limits. While elevated CO2 and warming boost photosynthesis, carbon storage is constrained by nutrient and demographic factors, making persistence key for mountain carbon stability.
Area of Science:
- Ecology
- Plant Physiology
- Climate Change Science
Background:
- High-elevation plants have limited carbon economies due to cold temperatures, short growing seasons, and low CO2.
- Global change (elevated CO2, warming) is expected to increase carbon uptake in alpine systems.
- However, observed biomass gains and carbon sequestration in these systems are inconsistent.
Purpose of the Study:
- To propose a three-gate framework (carbon gain, carbon use, persistence) explaining alpine plant responses to global change.
- To synthesize evidence from experimental, observational, and modeling studies.
- To highlight the importance of persistence over productivity for alpine carbon stability.
Main Methods:
- Synthesis of experimental, observational, and modeling evidence.
- Analysis of plant physiological responses (photosynthesis, water-use efficiency).
- Evaluation of carbon allocation, nutrient limitations, and demographic processes.
Main Results:
- Elevated CO2 increases photosynthesis and water-use efficiency; moderate warming can boost early productivity.
- Carbon gain is limited by sink strength, nutrient availability, respiration, and rhizosphere priming.
- Excess carbon is allocated to storage and defense, not durable biomass.
- Demographic factors like phenology, recruitment, and mortality control long-term persistence.
Conclusions:
- Persistence, not just productivity, dictates alpine carbon stability under global change.
- Carbon allocation constraints and demographic processes must be integrated into ecosystem models.
- Accurate projections of mountain carbon-climate feedbacks require considering these limitations.
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