Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractNeedle removal by pine sawfly larvae increases branch-level VOC emissions and reduces below-ground emissions of Scots pine    Next AbstractFunction of defensive volatiles in pedunculate oak (Quercus robur) is tricked by the moth Tortrix viridana »

PLoS One


Title:Biogenic volatile organic compound and respiratory CO2 emissions after 13C-labeling: online tracing of C translocation dynamics in poplar plants
Author(s):Ghirardo A; Gutknecht J; Zimmer I; Bruggemann N; Schnitzler JP;
Address:"Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Garmisch-Partenkirchen, Germany"
Journal Title:PLoS One
Year:2011
Volume:20110228
Issue:2
Page Number:e17393 -
DOI: 10.1371/journal.pone.0017393
ISSN/ISBN:1932-6203 (Electronic) 1932-6203 (Linking)
Abstract:"BACKGROUND: Globally plants are the primary sink of atmospheric CO(2), but are also the major contributor of a large spectrum of atmospheric reactive hydrocarbons such as terpenes (e.g. isoprene) and other biogenic volatile organic compounds (BVOC). The prediction of plant carbon (C) uptake and atmospheric oxidation capacity are crucial to define the trajectory and consequences of global environmental changes. To achieve this, the biosynthesis of BVOC and the dynamics of C allocation and translocation in both plants and ecosystems are important. METHODOLOGY: We combined tunable diode laser absorption spectrometry (TDLAS) and proton transfer reaction mass spectrometry (PTR-MS) for studying isoprene biosynthesis and following C fluxes within grey poplar (Populus x canescens) saplings. This was achieved by feeding either (13)CO(2) to leaves or (13)C-glucose to shoots via xylem uptake. The translocation of (13)CO(2) from the source to other plant parts could be traced by (13)C-labeled isoprene and respiratory (13)CO(2) emission. PRINCIPAL FINDING: In intact plants, assimilated (13)CO(2) was rapidly translocated via the phloem to the roots within 1 hour, with an average phloem transport velocity of 20.3+/-2.5 cm h(-1). (13)C label was stored in the roots and partially reallocated to the plants' apical part one day after labeling, particularly in the absence of photosynthesis. The daily C loss as BVOC ranged between 1.6% in mature leaves and 7.0% in young leaves. Non-isoprene BVOC accounted under light conditions for half of the BVOC C loss in young leaves and one-third in mature leaves. The C loss as isoprene originated mainly (76-78%) from recently fixed CO(2), to a minor extent from xylem-transported sugars (7-11%) and from photosynthetic intermediates with slower turnover rates (8-11%). CONCLUSION: We quantified the plants' C loss as respiratory CO(2) and BVOC emissions, allowing in tandem with metabolic analysis to deepen our understanding of ecosystem C flux"
Keywords:"Algorithms Biological Transport/physiology Carbon/*pharmacokinetics Carbon Dioxide/*metabolism Carbon Isotopes/pharmacokinetics Cell Respiration/physiology Models, Biological Online Systems/instrumentation Plant Leaves/metabolism Plant Shoots/metabolism P;"
Notes:"MedlineGhirardo, Andrea Gutknecht, Jessica Zimmer, Ina Bruggemann, Nicolas Schnitzler, Jorg-Peter eng Research Support, Non-U.S. Gov't 2011/03/10 PLoS One. 2011 Feb 28; 6(2):e17393. doi: 10.1371/journal.pone.0017393"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 24-11-2024