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ARS Home » Midwest Area » Urbana, Illinois » Soybean/maize Germplasm, Pathology, and Genetics Research » Research » Publications at this Location » Publication #240558


Location: Soybean/maize Germplasm, Pathology, and Genetics Research

Title: Responses of Soybean Cultivars to Elevated CO2 and O3

item Nelson, Randall
item Ainsworth, Elizabeth - Lisa
item Long, Stephen
item Ort, Donald

Submitted to: Soybean Research World Conference Proceedings
Publication Type: Proceedings
Publication Acceptance Date: 5/12/2009
Publication Date: 8/9/2009
Citation: Nelson, R.L., Ainsworth, E.A., Long, S., Ort, D.R. 2009. Responses of Soybean Cultivars to Elevated CO2 and O3 [abstract]. In: Proceedings of the World Soybean Research Conference VIII, August 9-16, 2009, Beijing, China. 2009 CDROM.

Interpretive Summary:

Technical Abstract: The objective of our research is to measure soybean genetic variation for responses to increased CO2 and O3 concentrations under field conditions at the SoyFACE facility at the University of Illinois. Averaged over all cultivars and years, elevated CO2 significantly delayed the onset of flowering, seed filling, and maturity, whereas elevated O3 significantly hastened each of these three growth stages. Elevated CO2 significantly increased plant height, lodging, seed weight and seed yield, and elevated O3 significantly reduced each of these traits. Although these general trends exist, there were differential responses among the cultivars for every trait measured including seed yield. These results demonstrate that even among a relatively small sample of soybean cultivars it is possible to select for types that produce larger seed yield increases in elevated CO2 and smaller yield losses to elevated O3. The future response of the soybean crop to atmospheric changes will depend not only on the concentrations of CO2 and O3 but also on which cultivars are being grown. Genetic differences in responses to CO2 and O3 can be exploited by plant breeders to mitigate the losses to O3 and increase the gains from CO2.