Abstract

AbstractAtmospheric carbon dioxide (CO2) and ozone (O3) concentrations are rising, which may have opposing effects on tree C balance and allocation to fine roots. More information is needed on interactive CO2 and O3 effects on roots, particularly fine-root life span, a critical demographic parameter and determinant of soil C and N pools and cycling rates. We conducted a study in which ponderosa pine (Pinus ponderosa) seedlings were exposed to two levels of CO2 and O3 in sun-lit controlled-environment terracosms for three years. Minirhizotrons were used to monitor individual fine roots in three soil horizons every 28 days. Proportional hazards regression was used to analyze effects of CO2, O3, diameter, depth, and season of root initiation on fine-root survivorship. More fine roots were produced in the elevated CO2 treatment than in ambient CO2. Median life spans varied from 140-448 days depending on the season of root initiation. Elevated CO2, increasing root diameter, and increasing root depth all significantly increased fine-root survivorship and median life span. Life span was slightly, but not significantly, lower in elevated O3, and increased O3 did not reduce the effect of elevated CO2. These results indicate the potential for elevated CO2 to increase the number of fine roots and their residence time in the soil, which is also affected by root diameter, root depth, and phenology.

Highlights

  • Atmospheric carbon dioxide (CO2) and ozone (O3) concentrations are rising, which may have opposing effects on tree C balance and allocation to fine roots

  • We conducted a study in which ponderosa pine (Pinus ponderosa) seedlings were exposed to two levels of CO2 and O3 in sun-lit controlledenvironment terracosms for three years

  • These results indicate the potential for elevated CO2 to increase the number of fine roots and their residence time in the soil, which is affected by root diameter, root depth, and phenology

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Summary

Introduction

- CO2 and O3 are generally increasing worldwide - Leaves are sites of uptake and direct action, but CO2 and O3 can affect C assimilation and allocation with consequences for whole plant - Fine roots are especially important because of:. - role in water and nutrient uptake - significant contribution to NPP and its responses to CO2 and O3 - CO2 and O3 have potentially offsetting effects of on fine roots (allocation, growth, mortality) - Fine root life span is an important determinant of soil C pools and cycling rates - Multi-year studies are needed on CO2 & O3 effects on fine root longevity. 1. Elevated CO2 alone will increase life span 2. Elevated O3 will alone decrease life span 3. Elevated CO2 and O3 together will show additive compensatory effects on life span. 4. Life span will increase with root diameter, soil depth, and vary with season of root formation

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