Published in

Wiley, Plant Biology, 5(18), p. 776-784

DOI: 10.1111/plb.12464

Links

Tools

Export citation

Search in Google Scholar

Diel variations in carbon isotopic composition and concentration of organic acids and their impact on plant dark respiration in different species

Journal article published in 2016 by M. M. Lehmann, F. Wegener, R. A. Werner ORCID, C. Werner
This paper was not found in any repository, but could be made available legally by the author.
This paper was not found in any repository, but could be made available legally by the author.

Full text: Unavailable

Green circle
Preprint: archiving allowed
Orange circle
Postprint: archiving restricted
Red circle
Published version: archiving forbidden
Data provided by SHERPA/RoMEO

Abstract

AbstractLeaf respiration in the dark and its C isotopic composition (δ13CR) contain information about internal metabolic processes and respiratory substrates. δ13CR is known to be less negative compared to potential respiratory substrates, in particular shortly after darkening during light enhanced dark respiration (LEDR). This phenomenon might be driven by respiration of accumulated 13C‐enriched organic acids, however, studies simultaneously measuring δ13CR during LEDR and potential respiratory substrates are rare. We determined δ13CR and respiration rates (R) during LEDR, as well as δ13C and concentrations of potential respiratory substrates using compound‐specific isotope analyses. The measurements were conducted throughout the diel cycle in several plant species under different environmental conditions. δ13CR and R patterns during LEDR were strongly species‐specific and showed an initial peak, which was followed by a progressive decrease in both values. The species‐specific differences in δ13CR and R during LEDR may be partially explained by the isotopic composition of organic acids (e.g., oxalate, isocitrate, quinate, shikimate, malate), which were 13C‐enriched compared to other respiratory substrates (e.g., sugars and amino acids). However, the diel variations in both δ13C and concentrations of the organic acids were generally low. Thus, additional factors such as the heterogeneous isotope distribution in organic acids and the relative contribution of the organic acids to respiration are required to explain the strong 13C enrichment in leaf dark‐respired CO2.