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Extending the Stress-Gradient hypothesis: increased local adaptation between teosinte and soil biota at the stressful end of a climate gradient
Anna M. O’Brien, Ruairidh J.H. Sawers, Jeffrey Ross-Ibarra, Sharon Y. Strauss
doi: https://doi.org/10.1101/031195
Anna M. O’Brien
1Center for Population Biology, University of California, Davis, CA 95616
2Dept. of Plant Sciences, University of California, Davis, CA 95616
3Dept. of Evolution and Ecology, University of California, Davis, CA 95616
Ruairidh J.H. Sawers
4Laboratorio Nacional de Genómica para la Biodiversidad (LANGEBIO), Centro de Investigatión y de Estudios Avanzados del Instituto Politécnico Nacional (CINVESTAV-IPN), Irapuato, 36821, Guanajuato, Mexico
Jeffrey Ross-Ibarra
1Center for Population Biology, University of California, Davis, CA 95616
2Dept. of Plant Sciences, University of California, Davis, CA 95616
5Genome Center, University of California, Davis, CA 95616
Sharon Y. Strauss
1Center for Population Biology, University of California, Davis, CA 95616
3Dept. of Evolution and Ecology, University of California, Davis, CA 95616
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Posted November 11, 2015.
Extending the Stress-Gradient hypothesis: increased local adaptation between teosinte and soil biota at the stressful end of a climate gradient
Anna M. O’Brien, Ruairidh J.H. Sawers, Jeffrey Ross-Ibarra, Sharon Y. Strauss
bioRxiv 031195; doi: https://doi.org/10.1101/031195
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