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@ARTICLE{Gangi:173296,
author = {Gangi, Laura and Tappe, Wolfgang and Vereecken, Harry and
Brüggemann, Nicolas},
title = {{E}ffect of short-term variations of environmental
conditions on atmospheric {CO}18{O} isoforcing of different
plant species},
journal = {Agricultural and forest meteorology},
volume = {201},
issn = {0168-1923},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2014-06707},
pages = {128 - 140},
year = {2015},
abstract = {The oxygen isotope signature of atmospheric carbon dioxide
(δ18O–CO2) is significantly influenced by terrestrial
vegetation through 18O-exchange between CO2 and leaf water.
However, the impact of short-term variations of
environmental conditions on this 18O-exchange has not been
sufficiently characterized yet for different plant
functional types. In the present study, δ18O of CO2 and
water vapor were measured online in chamber-based
experiments with spruce, wheat, poplar and maize using
infrared laser spectroscopy. The impact of the plants on
ambient δ18O–CO2 was inferred from the chamber-based
CO18O isoforcing (CO18O-Iso), i.e., the product of the net
CO2 flux through the chamber and the δ18O–CO2 of this
flux obtained from differential measurements at the chamber
inlet and outlet. The measured CO18O-Iso was compared to the
CO18O isoforcing (CO18O-Isosim) calculated as a function of
the δ18O of leaf water at the evaporation site
(δ18O–H2Oev) and the degree of oxygen isotope
equilibration between CO2 and leaf water (θ). Plants were
exposed to elevated air temperature (35 °C) and cessation
of water supply. CO18O-Iso was reduced at 35 °C due to the
reduction of stomatal conductance (gs) in all plant species
except for maize, and at decreasing water availability in
all four plant species due to a reduction of θ,
assimilation rate (Ar) and gs, while leaf water became
progressively 18O-enriched. The combination of θ, gs, Ar
and δ18O–H2Oev accounted for up to $98\%$ of the
variations in CO18O-Iso, which were well represented by
CO18O-Isosim, whereas the relationship between individual
determinants and CO18O-Iso was weaker. The degree of
isotopic CO2–H2O equilibration calculated from isotopic
gas exchange reached maximum values of 0.51 and 0.53 in
maize and spruce, and 0.67 and 0.74 in wheat and poplar,
respectively. Although θ was highly sensitive to the
parameterization of mesophyll conductance (gm), most of the
gm literature values for each species yielded values for θ
significantly lower than previously reported for the
respective plant species. This finding, as well as the
observed temporal variations in the oxygen isotopic exchange
introduced by varying environmental conditions, should be
considered for the parameterization of δ18O–CO2 models.},
cin = {IBG-3},
ddc = {630},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255) / 255 - Terrestrial Systems: From Observation to
Prediction (POF3-255)},
pid = {G:(DE-HGF)POF3-255 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000347863900013},
doi = {10.1016/j.agrformet.2014.10.015},
url = {https://juser.fz-juelich.de/record/173296},
}