Growth decline and divergent tree ring isotopic composition (δ(13) C and δ(18) O) contradict predictions of CO2 stimulation in high altitudinal forests.

MLA

Gómez-Guerrero, Armando, et al. “Growth Decline and Divergent Tree Ring Isotopic Composition (δ(13) C and δ(18) O) Contradict Predictions of CO2 Stimulation in High Altitudinal Forests.” Global Change Biology, vol. 19, no. 6, June 2013, pp. 1748–58. EBSCOhost, https://doi.org/10.1111/gcb.12170.

APA

Gómez-Guerrero, A., Silva, L. C. R., Barrera-Reyes, M., Kishchuk, B., Velázquez-Martínez, A., Martínez-Trinidad, T., Plascencia-Escalante, F. O., & Horwath, W. R. (2013). Growth decline and divergent tree ring isotopic composition (δ(13) C and δ(18) O) contradict predictions of CO2 stimulation in high altitudinal forests. Global Change Biology, 19(6), 1748–1758. https://doi.org/10.1111/gcb.12170

Chicago

Gómez-Guerrero, Armando, Lucas C R Silva, Miguel Barrera-Reyes, Barbara Kishchuk, Alejandro Velázquez-Martínez, Tomás Martínez-Trinidad, Francisca Ofelia Plascencia-Escalante, and William R Horwath. 2013. “Growth Decline and Divergent Tree Ring Isotopic Composition (δ(13) C and δ(18) O) Contradict Predictions of CO2 Stimulation in High Altitudinal Forests.” Global Change Biology 19 (6): 1748–58. doi:10.1111/gcb.12170.