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@ARTICLE{Ghirardo:15172,
author = {Ghirardo, A. and Gutknecht, J. and Zimmer, I. and
Brüggemann, N. and Schnitzler, J.P.},
title = {{B}iogenic {V}olatile {O}rganic {C}ompound and
{R}espiratory {CO}2 {E}missions after 13{C}-{L}abeling:
{O}nline {T}racing of {C} {T}ranslocation {D}ynamics in
{P}oplar {P}lants},
journal = {PLoS one},
volume = {6},
issn = {1932-6203},
address = {Lawrence, Kan.},
publisher = {PLoS},
reportid = {PreJuSER-15172},
pages = {e17393},
year = {2011},
note = {Financial support was given by the Human Frontier Science
Program ( to J. P. S. and A. G.) and the German Research
Foundation ( to J. P. S., DFG SCHN653/4). The funders had no
role in study design, data collection and analysis, decision
to publish, or preparation of the manuscript.},
abstract = {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.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.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
$(8-11\%).We$ 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 / Plants:
metabolism / Populus: metabolism / Staining and Labeling:
instrumentation / Staining and Labeling: methods / Volatile
Organic Compounds: metabolism / Carbon Isotopes (NLM
Chemicals) / Volatile Organic Compounds (NLM Chemicals) /
Carbon Dioxide (NLM Chemicals) / Carbon (NLM Chemicals) / J
(WoSType)},
cin = {IBG-3},
ddc = {500},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Biology},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:21387007},
pmc = {pmc:PMC3046154},
UT = {WOS:000287931400068},
doi = {10.1371/journal.pone.0017393},
url = {https://juser.fz-juelich.de/record/15172},
}