Unité Mixte de Recherche (Institut National de la Recherche
Agronomique-University Blaise Pascal), 234 avenue du Brézet,
63039 Clermont-Ferrand cedex 02, France (E.F., X.L.R., S.G.); and
Macaulay Land Use Research Institute, Craigiebuckler, Aberdeen AB15
8QH, Scotland, United Kingdom (E.F., P.M., R.W.)
 |
INTRODUCTION |
Because N is often the most limiting
factor for plant growth in terrestrial ecosystems (Cole, 1981
; Vitousek
and Howarth, 1991
), plant N economy is crucial for plant productivity
and survival (Chapin et al., 1990
). In contrast to annuals, perennial
herbaceous and woody species can remobilize N stored during the
previous years during growth in the spring (Millard, 1996
; Bausenwein
et al., 2001
). N storage and remobilization enable perennial plants to
be partially independent of external N availability for their growth
(Nambiar and Fife, 1991
; Millard and Proe, 1993
; Millard, 1996
),
because remobilization of stored N supports the growth of new shoots
before, or concurrently with, root uptake (Domenach and Kurdali, 1989
;
Millard and Proe, 1991
; Neilsen et al., 1997
; Millard et al., 2001
). N
storage occurs principally in autumn in perennial tissues such as roots
and stems (Millard, 1996
) in the form of bark and wood storage proteins
and amino acids (Wetzel et al., 1989
; Sagisaka, 1993
; Stepien et al.,
1994
). In general, leaf growth is the strongest sink for N
remobilization during spring growth, and remobilized N can reach nearly
up to 90% of total N used for leaf growth (Millard, 1996
; Neilsen et
al., 1997
).
The best approach currently available to quantify N storage and
remobilization relies on labeling techniques using
15N enrichment (Millard and Neilsen, 1989
) or
depletion (Deng et al., 1989
). Besides its cost, the applicability of
this method for field grown trees has been questioned because the
spatial and temporal stability of N enrichment in the rooting zone is difficult to monitor and control. Thus, no reliable, nondestructive method is presently available to directly measure N remobilization in
field-growing trees.
Coupling sap flow velocity and nitrogenous compounds translocated in
the xylem sap has been suggested as a means to estimate nutrient fluxes
to new shoots during spring growth in field-growing trees (Millard et
al., 1998
). For instance, coupling sap flow velocity and mineral
concentrations in xylem sap was found to provide adequate estimates of
the amount of nutrients recovered in new shoots of adult spruce tree
for Mg but not for Ca, P, and K (Dambrine et al., 1995
). However, such
an approach cannot distinguish between nutrients taken up by roots as
opposed to those remobilized. Several authors have recently
demonstrated that spring growth is characterized by an increase in the
concentration of one or a few amino acids in xylem sap after bud break
in trees. For instance, peaks of Asn, Asp, and Gln were observed after
bud burst in Malus spp. (Malaguti et al., 2001
), whereas
peaks of citruline (Cit) were observed in Alnus spp. (Lewis,
1986
), Betula spp. (Millard et al., 1998
), and
Juglans spp. (Prima-Putra and Botton, 1998
). Using
15N labeling, the increase in the amount of Cit
translocated in the xylem sap after bud break was shown to be
attributable to remobilization in Betula pendula by Millard
et al. (1998)
, who concluded that coupling the concentration of
specific amino acids in xylem sap with sap velocity was a promising,
nondestructive approach to measure N remobilization.
The objectives of this study were (a) to quantify the importance of N
remobilization versus N uptake for new shoot growth in walnut
(Juglans nigra × regia), (b) to identify
specific N forms translocated in xylem sap during N remobilization, and
(c) to test whether coupling the concentrations of specific amino acids
in xylem sap with sap velocity could quantify N remobilization. Sand-growing walnut trees were fed with a labeled
(15N) nutrient solution during year 1 and fed
with unlabeled N during year 2. Xylem sap velocity and the
concentrations and 15N signals of amino acids in
xylem sap were surveyed during a 3-month period after bud burst in the
second year. The dynamics of N remobilization estimated from this new
approach were then compared with that obtained by the destructive
15N-budget technique. Implications for measuring
N remobilization in large, field-growing trees are discussed.
 |
RESULTS |
Seasonal Dynamics of New Shoot Growth and N Remobilization by the
15N-Labeling Technique
Leaf biomass and area increased exponentially during the first
20 d after bud-break and reached a maximal value of 44 g and 0.66 m2 per tree around 50 d after bud
break, respectively (Fig. 1). Unlabeled
and labeled N (15N) in new shoots (mainly
represented by the leaves that contained around 82% of both the
labeled and unlabeled N in new shoots) exhibited similar temporal
dynamics (Fig. 2). N remobilization finished around 50 d after bud break and reached 520 mg N
tree
1. At this time, the
14N pool in new shoots reached 440 mg
tree
1. Remobilized N thus represented 54% of N
recovered in new shoots.

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Figure 1.
The pattern of leaf growth during 2000. Each point
represents one tree at the date of harvest. Data were fitted with
logistic curves: y = 0.0 + 44.9/(1 + EXP[ 0.13(x 30.1)]), n = 48, r2 = 0.96 and y = 0.0 + 0.66/(1 + EXP[ 0.16(x 25.9]), n = 48, r2 = 0.96 for leaf dry mass and leaf area,
respectively.
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Figure 2.
The recovery of labeled (white symbols) and
unlabeled (black symbols) N with time after bud break. The
15N and 14N dataset were
fitted with logistic curves: y = 0.0 + 500.5/(1 + EXP[ 0.16 (x 24.3)]), n = 48, r2 = 0.94, and y = 0.0 + 403.2/(1 + EXP[ 0.19 (x 24.3)]),
n = 48, r2 = 0.96, respectively.
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Analysis of the temporal dynamics of the 15N
contents in the different tree compartments allowed a determination of
which compartments were used for N storage during the winter (Fig.
3). Before bud break, labeled N was
mainly located in the root system (78% of total labeled N) and to a
lesser extent in old, aboveground parts (trunk and old branches).
During spring growth, the 15N pools in fine roots
(R
3 mm) and old branches did not change significantly over
time. In contrast, the 15N pools in tap roots
(R > 2 cm), medium roots (3 mm < R
2 cm), and trunk
significantly decreased with time (P < 0.001),
concurrently to the increase in the 15N pool in
new shoots.

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Figure 3.
Changes in the content of labeled N in different
tree compartments (WR, new growing white roots; R <3 mm, fine roots; R
3 mm-2 cm, medium roots; R > 2 cm, tap roots; T, trunk; Old B,
old branches; New S, new shoots including leaf lamina, petioles, and
new branches). Values are expressed as milligrams of labeled N per tree
and are means of four replicates. Bars are maximal SEs for
each tree compartment. Significant effects of time were observed for WR
(P < 0.0001), medium roots (P = 0.002), tap roots (P < 0.0001), T (P < 0.0001), and New S (P < 0.0001).
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N Translocation in Xylem Sap. Key Amino Acids and Diurnal and
Seasonal Variations
N was translocated in walnut xylem sap mainly as amino acids
(Table I). Five major amino acids were
identified: Arg, Cit,
-amino butyric acid (Gaba), Gln, and Asp,
which represent 85% and 79% of total amino acid N in xylem sap 20 and
70 d after bud burst, respectively (Table I). Pro and Thr also
represented significant amounts of N in xylem sap. Total amino acid N
concentration observed around 20 d after bud break (39 µg N
g
1 xylem sap) was 6-fold higher than that
observed 70 d after bud break. This trend was observed for all
amino acids, although the decrease was less marked for Gaba and Asp
than for the other amino acids (Table I).
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Table I.
Comparison of the recovery of N in amino acids in
the xylem sap of walnut trees harvested 20 and 70 d after bud
burst (BB)
Means are given for three and four trees for the two dates,
respectively. Values between brackets are SEs.
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Arg appeared in xylem sap in the very first days after bud break at
very high concentration (up to 110 µg N g
1
xylem sap) compared with the other amino acids (always less than 14 µg N g
1 xylem sap; Fig.
4). The concentration of this amino acid
remained high only during the first 10 d after bud burst, and
after 25 d, it was around 5 µg N g
1
xylem sap. At each sampling date, there was also a large variation in
the concentration of Arg recovered, which was attributable to the
natural variation between replicate samples, the precision of the
analysis of standards being better than 1 µg N
g
1 xylem sap. Uncertainty in the determination
of first bud burst occurrence for each tree could partly explain this,
because an error of a few days could lead to significant differences in
the concentration of this amino acid (Fig. 4). Gln, Cit, and Asp
exhibited maximum concentration values around 15, 17, and 22 d
after bud break, respectively, whereas low values (around 1 µg N
g
1 xylem sap) were observed just after bud
burst and after d 40. In contrast, Gaba-N concentration exhibited a
less pronounced peak through time, with relatively high values (>2
µg N g
1 xylem sap) observed just after bud
burst and after d 40 compared with maximum values (6.7 µg N
g
1 xylem sap). During the first 40 d after
bud burst, the APE of each amino acid remained quite stable and
thereafter declined for Gln and Asp (Fig. 4).

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Figure 4.
Temporal courses of the concentration and atom % excess (APE) of the five major amino acids present in xylem sap of
walnut. Values are means of four trees sampled during 4-d periods. Bars
are SEs. Lines are the fitted gaussians, the form of which
is: y = a + b/[(2* )0.5 * s] *
exp{[ (x m)2/2s2).
R2 values are 0.96, 0.67, 0.90, 0.97, and
0.58 for Arg, Gaba, Gln, Cit, and Asp, respectively. For concentration,
note the differences of scale between amino acids.
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The diurnal courses of incident radiation (PAR) and mean sap flow
velocity measured on a sample day (16 June 2000) are shown in Figure
5. Transpiration rate increased with a
slight delay compared with PAR, from 0.01 dm3
h
1 tree
1 in the early
morning to maximal values around 0.11 dm3
h
1 tree
1 at noon.
During the diurnal period, amino acid-N concentration in xylem sap
increased concurrently with the transpiration rate (Fig. 5), and
similar diurnal dynamics were observed for the five major amino acids
but with slightly different amplitude (data not shown). Thus, a
correction factor was used for each amino acid to compute N flux in
xylem sap.

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Figure 5.
Diurnal courses of incident photosynthetically
active radiation (PAR) measured on June 16 (top), transpiration rate
(T) measured on June 16 (middle), and the relative concentration of
total N-amino acids in xylem sap measured on May 27 ( ) and June 16 ( ; bottom). T values are means of sap flow measurements on four
trees. Concentrations are means for four trees. Relative concentration
refers to the ratio of actual to maximum diurnal values. Bars are
SEs and are presented only every 3 h for sake of
legibility. The fitted polynomial is y = 0.009x2 + 0.29x 1.49.
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Coupling of the temporal trends in amino acid concentrations and APE
with the temporal course of transpiration rate per tree was used to
compute daily values for total and labeled N translocated in xylem sap
(Fig. 6). Both fluxes exhibited similar
temporal courses, with maximal values from d 6 to 28 after bud burst
and a strong decrease from d 29 to 35. N fluxes then remained slow and
stable. Translocation of both total and labeled N was mainly insured by
Arg during the first 15 d after bud burst and by Gln and Cit from
d 15 to 30 (Fig. 6).

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Figure 6.
Temporal courses of measured daily transpiration
rate per tree, T (top), computed total N flux in xylem sap (middle),
and computed 15N flux in xylem sap (bottom).
Insets, The fluxes computed for individual amino acids. Bars for T are
SEs.
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Comparison of N Remobilization by the Two Methods
The temporal pattern of total and labeled N fluxes to new shoots
estimated from coupling amino acid concentrations and sap flow velocity
was in agreement with the patterns of total and 15N recovery measured by the
15N labeling technique (Fig.
7). However, the total N flux to new shoots estimated by the new method was higher than the recovery of
labeled N in shoots from d 10 to 20. In addition, after d 50, the
15N and total N pools in the new shoots observed
by the recovery of labeled N remained stable, whereas positive fluxes
to new shoots were observed in the xylem.

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Figure 7.
Temporal dynamics of the measured total N content
in new shoots ( ) and the total N flux in xylem sap computed by the
new method ( ) and of the measured 15N content
in new shoots ( ) and the 15N flux in xylem sap
computed by the new method ( ). Insets, The linear regression between
values measured by 15N technique (method 1) and
by new approach (method 2).
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 |
DISCUSSION |
Importance of N Remobilization for Spring Growth in
Walnut
Spring remobilization of N stored during the previous year played
an important role for new shoot growth in walnut. When shoot growth was
completed, N remobilization had provided around 54% of total N to new
shoots. This result is consistent with the values of 60% estimated for
larger walnut trees grown in the orchard by Weinbaum and Van
Kessel (1998)
, although higher values of 75% have also been reported
for field-growing walnut trees by Deng et al. (1989)
. Similar
percentages of N derived from remobilization for new growth were found
in young pear (Pyrus communis) trees (Taglivani et
al., 1997), in kiwifruit (Actinidia deliciosa) in orchard
conditions (Ledgard and Smith, 1992
), and in B. pendula, 40% (Millard et al., 1998
). Higher fractions were
reported for citrus trees growing in sand culture (Legaz et al.,
1995
), apple (Malus domestica) trees (Neilsen et al.,
1997
), and peach (Prunus persica) trees (Munoz et al.,
1993
). It should be noted that we estimated the importance of
remobilization of N stored during the previous year only. However, our
trees already had reserve organs (tap root and trunk mainly) in early
1999, and N stored during a given year can be used 2 years after, as
observed in walnut (Weinbaum and Van Kessel, 1998
). Thus, the
percentage of total N derived from remobilization for new shoot growth
in walnut was probably higher than 54%. This also explains why the APE
of amino acids in xylem sap was lower than that of fertilizer applied the previous year.
During growth in the spring, N uptake and remobilization were
concurrent. In contrast, N remobilization was found to provide more N
to new shoots during the early growing season, and N uptake then became
predominant in sycamore (Acer pseudoplatanus), B. pendula, and Sorbus aucuparia (Millard and Proe, 1991
;
Millard et al., 1998
, 2001
). This shows that new growth is less
decoupled to soil N availability during the early growing season in
walnut than the other species.
Different tree organs can be used as storage organs for N during the
winter. For instance, old leaves can store N (partly as Rubisco) in
evergreen trees, and recycling of N from old needles provides much of N
for new growth (Millard and Proe, 1992
; Legaz et al., 1995
). In
deciduous trees, woody roots and old stems are generally major storage
organs (Munoz et al., 1993
; Millard et al., 1998
) where bark- and
wood-storage proteins are accumulated (Sauter and Neumann, 1994
;
Stepien et al., 1994
). In the present study, the increase in the
labeled N content (i.e. derived from remobilized N) in new shoots was
concurrent with a decrease in the labeled N recovered in the trunk and
in coarse and medium roots (>3 mm). The pool of labeled N in the fine
roots did not change significantly with time, demonstrating that they
were not a site used for N storage during the winter, as was already
observed for B. pendula (Millard et al., 1998
).
Characteristics of N-Translocation in the Xylem
Throughout the experiment, N was translocated in the xylem sap
predominantly as Arg, Cit, Gaba, Gln, and Asp, whereas mineral N was
found to be negligible. Using data obtained in summer on 60 tree
species, Barnes (1963)
found that Gln, Cit, Arg, and Asp were the main
amino acids in xylem sap of 16, 13, 7, and 7 species, respectively. In
particular, Cit was the main amino acid in J. nigra. Cit
(and to a lesser extent Gln) was similarly the major amino acid in
J. regia (Prima-Putra and Botton, 1998
). In contrast to such
point measurements, comprehensive studies on the seasonal course of
amino acid concentrations in xylem sap are less frequent. Cit and Gln
are the major amino acids in xylem sap during spring growth in B. pendula (Millard et al., 1998
), whereas Gln remains the major
amino acid in xylem sap during the whole vegetative period in poplar
(Populus spp.; Sauter and Vancleve, 1992
; Schneider et al.,
1994
) and willow (Salix spp.; Sauter, 1981
). Asn, Asp, and
Gln were found to be translocated in xylem sap during spring growth in
apple trees (Malaguti et al., 2001
). In our study, five amino acids
accounted for the majority of N translocation in xylem sap. To our
knowledge, such a case has not been reported previously. Furthermore,
there was a strong seasonal variation in amino acid concentrations,
which differed significantly between individual amino acids. In
particular, Arg exhibited high concentrations very early after bud
burst, whereas Gln, Cit, and Asp exhibited maximum concentration values
at later dates. Gaba concentrations also peaked during N
remobilization, although the subsequent decrease in concentration was
not as pronounced as for Arg, Gln, and Cit. There is evidence from
herbaceous plants that Gaba has a role as a temporary N storage
compound, as well as being synthesized in response to stress (Bown and
Shelp, 1997
; Shelp et al., 1999
). It is possible, therefore, that the
presence of Gaba was due, in part, to a stress response by the trees to
being handled.
Our results could explain why point measurements (for example taken
around d 23 in our study) would identify Cit as the major amino acid in
walnut. The observed differences in temporal variations among
individual amino acids contrast with previous results on apple (Tromp
and Ovaa, 1969
), where the three major amino acids exhibited similar
seasonal variations in spring. To our knowledge, only the results of
Sauter and Vancleve (1992)
showed that the concentration peak for one
relatively minor amino acid (Asn) occurred 1 month later than the peaks
for the three other amino acids (including Gln, the major one). The
present study is the first, to our knowledge, to demonstrate a temporal
succession of the main amino acids involved in N remobilization. Our
results show the importance of the time step used when measuring
temporal trends in amino acid concentrations in xylem saps and the
importance of documenting accurately processes occurring very early
(i.e. during the 1st week after bud burst) for understanding N
remobilization in some species.
Toward a New Method for Assessing N Remobilization?
The amount of N remobilization, estimated by the approach of
coupling sap flow velocity and the concentration of N in the main amino
acids translocated in xylem sap, was in agreement with that measured by
the recovery of labeled in the new shoots. However, during early growth
(between 10 and 20 d after bud break), the new method
overestimated total N and to a lesser extent remobilized N to new
shoots. Also, the new method calculated significant total N and
remobilized N fluxes to new shoots after leaf growth was completed
(after 60 d), whereas the total and labeled N contents of new
shoots remained constant. The new method estimated gross N fluxes,
whereas the 15N labeling technique estimated net
fluxes. Given the importance of retranslocation of N in the phloem from
shoots to roots (Marschner et al., 1997
) and the rapid turnover of leaf
labile N pools (Dewar et al., 1998
; Frak et al., 2001
), the two methods
should be consistent when new shoots are the strongest N sinks and when
N retranslocation in the phloem is negligible compared with the flux in
the xylem (i.e. before completion of new shoot growth).
Both approaches provided similar amounts of N remobilized at the end of
growth in the spring (i.e. around 60 d after bud break). The data
suggest, therefore, that measuring amino acid fluxes in the xylem could
be used for quantification of N remobilization by large, field-growing
trees. However, there are some points that would need addressing before
the method could be applied with confidence.
First, the method is based on the hypothesis that one or several amino
acids are specific of remobilization. This would have to be verified
for a given species by a labeling technique (Millard et al., 1998
). In
our experiment, stored N was labeled during 1999 by using a nutrient
solution with 15N enriched at 4.98%. However,
the enrichment of the five amino acids involved in N remobilization in
2000 was lower (between 3.5 and 2 APE). A first hypothesis is that
these amino acids were not specific of N remobilization and that a
significant proportion of the flux of each amino acid came from root
uptake. A second hypothesis is that the amino acids were specific to N
remobilization, but that remobilization of N taken up in 1999 (hence
labeled N) and in 1998 (hence unlabeled N) occurred concurrently. The
latter hypothesis is supported by the fact that Weinbaum and Van Kessel (1998)
demonstrated that N assimilated in a given year can be remobilized 2 years later in walnut. In this case, changes in APE
during the 80 d after bud burst could be attributable to changes in the relative importance of remobilization from labeled N taken up in
1999 and unlabeled N taken up in 1998.
Second, the diurnal variations in amino acid concentrations should be
quantified and taken into account when necessary. The quantification of
N fluxes was found to be sensitive to the diurnal dynamics of amino
acids in the present study. Such diurnal variations make difficult the
use of a unique value of amino acid concentration measured at a given
time to estimate N fluxes without correcting factors. Very few studies
have quantified diurnal changes in amino acid concentrations. Weak
diurnal variations were observed in total amino acid concentration in
Vitis rotundifolia (Andersen and Brodbeck, 1989
),
Vitis hybrid sp., and pear (Pyrus communis; Andersen et al., 1995
), whereas marked variations were observed for
four amino acids (Asn, Asp, Gln, and Glu) in the xylem sap of peach
(Andersen et al., 1995
). The presence of any diurnal pattern of amino
acid concentrations in the xylem would, therefore, need to be evaluated.
Finally, given the importance of the N translocation observed in xylem
sap immediately after bud burst, sap flow velocity needs to be measured
accurately, when leaf area is small and shoot transpiration rates are
slow. In walnut, the most important variations in N concentration in
xylem sap were observed during the first 20 d after bud break.
However we could not measure sap velocity properly with the heat
balance system before leaf area was higher than 0.1 m2 (transpiration was measured by weighing before
then). Improvements of the techniques able to measure a slow sap flow
(such as the heat pulse technique) are thus important for the
application of the new method.
However, despite the methodological points discussed above, coupling
amino acid concentrations and sap flow velocity already appears to be a
promising tool for studying N remobilization in large, field-growing trees.
 |
MATERIALS AND METHODS |
Plant Material and Experimental Design
Forty eight, 1-year-old walnut (Juglans
nigra × regia) trees were planted in March
1999 in 35-dm3 pots filled with fine sand. The apical bud
of each plant was removed to stimulate auxiliary buds and branch
development. Plants were watered weekly and kept frost-free until bud
break. In late April, the trees were transferred outdoors and
randomized in four blocks. Each tree received 500 cm3 of
nutrient solution (8 mol N m
3) three times per week. N
was applied as
15NH415NO3 enriched
with 15N to 4.98 APE. Other nutrients were supplied as
described by Millard and Proe (1991)
. Depending on evaporative demand,
the trees were watered automatically during the other days. In early
November 1999, the trees were transferred under a shelter and kept
moist and frost-free during winter. In February 2000, each plant was carefully removed from its pot, and its root system was washed to
remove any remaining sand. The trees were then transplanted in a new
pot with fresh sand and kept sheltered until April. The nutrient
solution supplied in 2000 had the same composition as in 1999 but
contained a natural abundance of 15N. In spring, the number
of open buds was surveyed daily and the day of the first open bud was
designed as start of bud burst.
Tree Organ Dry Masses and 15N Content
Trees were harvested at 12 dates (April 21; May 3, 12, 18, 23, and 29; June 5, 13, 19, and 30; and July 13 and 21). At each date, one
plant from each block was carefully removed from its pot. The root
system was washed and sorted into four categories: R
3 mm, 3 mm < R
2 cm, R > 2 cm and newly grown white roots. Tree aboveground parts were separated into old branches, trunk, and new
shoots of the year, the latter including new stems, leaf laminas, and
leaf petioles. The total fresh leaf area of each tree was measured with
an area meter (LI-3100, LI-COR, Lincoln, NE). All samples were frozen
with liquid N, stored at
80°C, and then freeze-dried. Their dry
mass was measured, and the samples were milled before 15N
analyses. A Tracer Mat continuous flow mass spectrometer (Finningan MAT, Hemel Hempstead, UK) was used to determine the 15N
abundance and total N concentration of each sample.
Xylem Sap Collection and Amino Acid Analysis
Xylem sap was collected on branches cut at 9 h on each
sampled tree. Only the biggest branches (around 20 cm long) were used (two-three branches according to the tree). Around 10 cm of bark from
the apical part of branch was removed to avoid any contamination with
phloem sap. Branches were placed in a vacuum extraction system allowing
simultaneous extractions from the different branches by applying 0.1 MPa suction. Sap samples were collected in glass tubes and placed on
ice. Sap samples were pooled together when several branches were used
from the same tree. Lack of contamination of xylem by phloem sap, as
indicated by the presence of ATP (Schneider et al., 1996
), was checked
on subsamples using the Luciferine-luciferase reagent kit (ATP
bioluminescence assay kit CLS II, Roche Diagnostics, Mannheim, Germany).
Xylem sap samples were stored at
80°C. Particulate material was
removed by centrifugation in an MSE Micro-Centaur centrifuge for 5 min
at 5,800g. Samples (20 mg) were then diluted with 0.5 cm3 demineralized water and a 100-mm3 aliquot
of the dilute sap along with an internal standard of nor-Val (25 mm3 containing 0.18 µg) were added to a 1-CWV clear glass
crimp top tapered vial (Chromacol Ltd., Welwyn Garden City, UK) and
freeze dried. The derivatization reagent (100 mm3),
consisting of
N-(tert-butyldimethylsilyl)-N-methyltrifluoroacetamide containing 1% (w/v) tert-butyldimethylsilyl chloride
(Sigma-Aldrich, Gillingham, UK) in acetonitrile (1:4, v/v), was added
to the dried material and left at room temperature for 10 min. The
solution was then heated at 70°C for 35 min to convert the free amino
acids to their tert-butyldimethylsilyl derivatives. The
analyses of the derivatives were carried out using gas
chromatography/mass spectrometry (GC/MS) in the single-ion recording
mode. The instrumentation used was a Trace 2000 gas chromatograph,
fitted with an AS 2000 autosampler and interfaced to a Finnigan
Trace quadrupole mass spectrometer (ThermoFinnigan, Hemel Hempstead, UK).
Arg was determined as the N-heptafluorobutryl
n-butyl ester (MacKenzie and Tenaschuk, 1979
). Xylem sap
samples (10 mg) containing nor-Val (50 mm3 containing 0.36 µg) as internal standard were freeze-dried and esterified by heating
at 100°C for 30 min in 120 nm
3 reagent (acetyl
chloride:n-butanol, 1:10, v/v). After evaporating excess
reagent, the residue was acylated for 10 min at 150°C using 120 nm
3 heptafluorobutyric anhydride. After cooling, the
excess reagent was evaporated, the residue was dissolved in 100 mm
3 ethyl acetate, and the solution was analyzed using
GC/MS. The derivatives were analyzed by GC/MS.
The enrichment of 15N in individual amino acids was
calculated from the ratio of the ion monitored at natural abundance and enriched amino acids (Campbell, 1974
). Amino acid concentrations were
calculated using response factors obtained from the analysis of
solutions containing known weights of amino acids. Quality control was
assured by analyzing standard solutions of amino acids.
Diurnal Course of Amino Acid Concentrations
The diurnal dynamics of the concentration of amino acids in
xylem sap was surveyed at two dates (May 27 and June 16). On each date,
xylem sap was extracted from branches of four additional walnut trees
at four or three times during the diurnal period. The samples were
frozen in liquid N, stored in
80°C, and analyzed for five major
amino acids by GC/MS.
Measurements of Sap Velocity
Two methods were used to estimate tree transpiration: weighing
and heat balance. The plant plus pot system was weighed daily on 12 trees to measure transpiration from bud burst until the day of harvest.
The sand surface was covered to restrict evaporation. Water and
nutrient solution inputs were controlled manually and added water was
weighed. The heat balance method (Valancogne and Nasr, 1989
) was
concurrently applied on four of these trees. A sap flow meter was
installed on the trunk of each tree. Thermocouples were connected to a
data logger scanning and averaging data every 15 s and every 10 min, respectively. When leaf area was less than 0.1 m2 per
tree, the heat balance technique could not provide accurate transpiration measurements and so transpiration rates were measured by
the weighing method. Concurrent measurements of daily transpiration by
both methods were close (y = 0.96x,
n = 60, r2 = 0.82).
During the whole study period, the leaf area dynamics were measured on
the 12 trees by surveying the size of each leaflet and using an
allometric relationship (leaflet area = 0.705 × length × width, n = 50, r2 = 0.98).
Quantification of N Remobilization
N remobilization was quantified by two independent methods. In
the first one, the amount of N taken up and stored in 1999 and
remobilized in 2000 was measured by the recovery of 15N
pool in the new shoot compartment (Millard and Neilsen, 1989
). Because
N remobilized during spring growth is translocated in xylem sap as free
amino acids, the second method used amino acid concentration and
15N enrichment coupled with sap flow velocity measurements.
We took the diurnal and seasonal variations in amino acid concentration and 15N enrichment into account. The variations in relative
concentration (i.e. ratio of actual to maximum concentrations) measured
on May 27 and June 16 were fitted for each main amino acid present in xylem sap (Gaba, Asp, Cit, Gln, and Arg) with a second order
polynomial. In addition, the seasonal variation in concentration
measured at 9 AM was fitted for each amino acid with
gaussian curves. The fluxes of total and labeled N to new shoots were
computed as follows:
|
(1)
|
|
(2)
|
where Nt and N15 are total N and
15N translocated in xylem sap over a period of
n days after bud burst (mg N tree
1 and mg
15N tree
1), respectively, Ad,t,a
is the N concentration in amino acid a at a given time
t of date d (micrograms per gram of xylem
sap), Td,t is the measured sap flow velocity at a time
t of date d (kilograms per tree per
hour), and APEd,t,a is the 15N to total N ratio
computed from the APE for amino acid a at a given time
t of date d. No diurnal course of APE was
actually observed for the amino acids studied and a unique APE value
was thus used along a given diurnal period for each amino acid.
Data Fitting and Statistical Analyses
Data for leaf growth (dry mass and area) and temporal increase
in new shoot 15N and 14N were fitted with
logistic curves by using the Genstat 5 standard curve fitting
procedure. The same procedure was used to fit the seasonal patterns of
amino acid N concentrations with gaussian curves. The diurnal dynamics
of amino acid N concentration in xylem sap was fitted with polynomial function.
Effects of date of harvest on labeled N pools in different tree
compartments and in the whole tree, and on amino acid N concentration and N enrichment were tested with a one way analysis of variance.
We thank Stéphane Ploquin and Patrice Chaleil for tree
management; Thierry Améglio and Christian Bodet (Physiologie
Intégrée de l'Arbre Fruitier et Forestier [PIAF], Institut
National de la Recherche Agronomique, Clermont Ferrand) for help during
sap flow measurements; Marc Vandame, Brigitte Saint-Joanis, Jean-Pierre Richard, and Arlette Cissoire (PIAF, Institut National de la Recherche Agronomique, Clermont Ferrand) for help during tree sampling and analysis; and Alan Hepburn (Analytical Unit, Macaulay Institute, Aberdeen) for GC/MS analyses.
Received December 28, 2001; returned for revision April 22, 2002; accepted June 13, 2002.
Article, publication date, and citation information can be found at
www.plantphysiol.org/cgi/doi/10.1104/pp.002139.