2019
Díaz-Álvarez, E. A.; de la Barrera, E.
Drying protocol does not alter plant δ13C and δ15N: a baseline survey for ecological studies Journal Article
In: Isotopes in Environmental & Health Studies, vol. 55, pp. 526-531, 2019.
Abstract | Links | BibTeX | Tags: atmospheric pollution, biomonitoring, ecophysiology, microwave, stable isotopes
@article{Díaz-Álvarez2019c,
title = {Drying protocol does not alter plant δ13C and δ15N: a baseline survey for ecological studies},
author = {E. A. Díaz-Álvarez and E. de la Barrera},
doi = {10.1080/10256016.2019.1673747},
year = {2019},
date = {2019-10-09},
journal = {Isotopes in Environmental & Health Studies},
volume = {55},
pages = {526-531},
abstract = {The use of stable isotopes in plant ecological studies has become widespread over the past few decades, given the potential of this tool for integrating physiological processes within an individual and allowing to track ecosystem-wide processes at various scales, with applications ranging from determining past meteorological conditions and potential adaptations of ecosystems to climate change, to biomonitoring studies of atmospheric pollution. However, the drying protocol might alter the isotopic signatures of plant samples given that high temperatures can volatilize various organic compounds or delay the halting of physiological processes at lower drying temperatures. We thus evaluated the effect of four drying protocols on the carbon and nitrogen isotopic signatures for 23 species of plants. In particular, leaves were either freeze dried, placed in a herbarium drying stove (ca. 50 ºC), in a gravity convection oven (80 ºC), or microwaved (900 Watts) in 2-minute pulses, until constant weight. For each species, neither treatment led to significantly different δ13C values, which ranged from ‒31.7‰ to ‒12.4‰. The δ15N values of 21 of the species considered were not affected by the drying protocols, ranging from ‒11.6‰ to ‒8.8‰. For Tillandsia makoyana, significant differences were observed between the freeze dried and the microwaved samples and between the freeze dried samples and those dried at 50 ºC for Macroptilium gibbosifolium. },
keywords = {atmospheric pollution, biomonitoring, ecophysiology, microwave, stable isotopes},
pubstate = {published},
tppubtype = {article}
}
The use of stable isotopes in plant ecological studies has become widespread over the past few decades, given the potential of this tool for integrating physiological processes within an individual and allowing to track ecosystem-wide processes at various scales, with applications ranging from determining past meteorological conditions and potential adaptations of ecosystems to climate change, to biomonitoring studies of atmospheric pollution. However, the drying protocol might alter the isotopic signatures of plant samples given that high temperatures can volatilize various organic compounds or delay the halting of physiological processes at lower drying temperatures. We thus evaluated the effect of four drying protocols on the carbon and nitrogen isotopic signatures for 23 species of plants. In particular, leaves were either freeze dried, placed in a herbarium drying stove (ca. 50 ºC), in a gravity convection oven (80 ºC), or microwaved (900 Watts) in 2-minute pulses, until constant weight. For each species, neither treatment led to significantly different δ13C values, which ranged from ‒31.7‰ to ‒12.4‰. The δ15N values of 21 of the species considered were not affected by the drying protocols, ranging from ‒11.6‰ to ‒8.8‰. For Tillandsia makoyana, significant differences were observed between the freeze dried and the microwaved samples and between the freeze dried samples and those dried at 50 ºC for Macroptilium gibbosifolium.