cupressus arizonica pollen wall zonation and in vitro hydration
TRANSCRIPT
Cupressus arizonica pollen wall zonation and in vitro hydration
G. Chichiricco,1 E. Pacini2
1Department of Environmental Sciences, University of L’Aquila, L’Aquila, Italy2Department of Environmental Biology, Botany Section, University of Siena, Siena, Italy
Received 28 February 2007; Accepted 4 September 2007; Published online 4 December 2007
� Springer-Verlag 2007
Abstract. The structure of Cupressus arizonicapollen at different degrees of hydration was examined
by using cytochemical staining and light (LM) and
scanning electron (SEM) microscopy. Most pollen
grains are inaperturate and a minority are provided
with an operculate pore enveloped by a concave
annulus. Intine consists of: 1) a thin polysaccharidic
outer layer, 2) a large polysaccharidic middle layer
that is spongy and bordered by a mesh of large and
branched fibrils, and 3) an inner cellulosic thick layer
with callose concentrated on the inner side, which
forms a shell around the protoplast. The protoplast is
egg-shaped with PAS positive cytoplasm and prom-
inent nucleus. Exine splits during hydration and is cast
off according to three major steps: 1) the split opens
like a mouth and the underlying intine is expelled by
swelling like a balloon, 2) the protoplast enveloped by
the inner intine is sucked in the outgrowing side, and
3) the backside of the intine gets rid of the exine shell.
In water containing salts, exine is rapidly released and
the middle intine may expand up to break the outer
layer, with disgregation of the spongy material and
release of the intine shell including the protoplast. In
water lacking salts, the sporoderm hydration and
breaking are negatively influenced by the population
effect. Pollen when air dried after the exine release
become completely flat owing to disappearance of the
middle intine layer which may be restored by dipping
pollen in water. The results are discussed in relation to
the functional potentialities of the sporoderm.
Keywords: Cupressus arizonica pollen; structure;
in vitro hydration; intine; exine
Introduction
Pollen from both gymnosperms and angiosperms
consist of the sporoderm and the included proto-
plast. Exine and intine walls are the components
of the sporoderm (Erdtman 1960), however the
former may be lacking, i.e. in aquatic plants such
as Callitriche truncata (Osborn et al. 2001), so
common pollen wall is the intine. Exine that is
made up of sporopollenin ensures protection
during pollen dispersal, and after pollination, it
controls the male-female interactions together
with the intine. Intine is pecto-cellulosic and plays
key roles in the cell germination and extension in
the pollen tube. During shedding, angiosperm
pollen is invariably two or three celled, whereas a
variable number of cells, generally from one to
five, occurs in gymnosperms (Pacini et al. 1999,
Fernando et al. 2005). Another typical difference
Correspondence: G. Chichiricco, Department of Environmental Sciences, University of L’Aquila, Via Vetoil, 67100 L’Aquila, Italy
e-mail: [email protected]
Pl Syst Evol 270: 231–242 (2008)
DOI 10.1007/s00606-007-0610-6
Printed in The Netherlands
Plant Systematicsand Evolution
concerns the pollen physiology; gymnosperm
pollen grains generally hydrate in the pollination
drop held on the ovule micropyle and slowly
germinate after carried in the nucellus (Fernando
et al. 2005), whereas angiosperm pollen both
hydrate and germinate soon after landing on the
stigma surface. In conifers the pollen wall varies
widely both in structure and function; it may or
may not have apertures, sculptures, wings, and
orbicules, and the exine may be released during
pollen hydration (Pacini et al. 1999, Fernando
et al. 2005). The pollen of Cupressus is particular
with regard to its wide structural stratification
(Pacini et al. 1999), but few details are available
on this matter (Grilli et al. 2000); on the contrary,
the pollen is extensively studied for its allergenic
properties (see Suarez-Cervera et al. 2003, Canini
et al. 2004, Mothes et al. 2004, Charpin et al.
2005).
In the present study, we examined Cupressusarizonica pollen at different degrees of hydration
by using cytochemical staining and light (LM)
and scanning electron (SEM) microscopy, with
the aim of contributing to its structure that could
be also useful for studies on pollinosis.
Materials and methods
Pollen collecting and storage. Pollen of Cupressusarizonica Greene was collected in February 2005 and
2006, from a tree growing on the avenue of the
University of L’Aquila (Coppito) (Italy). Branches
with mature pollen sacs were removed and left in the
laboratory until the pollen release at conditions similar
to those outside the laboratory, that is, 35–39% relative
humidity (RH) and 10–14�C. Pollen grains that were
not used at once were maintained for 1–2 days at
ambient conditions and then stored at –10�C.
Light and fluorescence microscopy. Whole
pollen grains were stained with: 1) IKI plus sulfuric
acid for detecting cellulose (Johansen 1940), (2)
calcofluor for b-glucans (Hughes and McCully 1975),
3) aniline blue for callose (O’ Brien and McCully 1981),
and 4) DAPI for DNA (Coleman and Goff 1985). The
images were acquired with a Zeiss Axioplan 2
fluorescence microscope equipped with Leica DFC
350 FX digital camera.
Pollen structure. Pollen grains for sections were
fixed in 3% glutaraldehyde in cacodilate buffer, or in
acetic alcohol (1:3) to avoid rehydration during
fixation, or becoming acetolyzed (Erdtman 1960).
The samples were dehydrated in an ethanol series and
embedded in Technovit 7100 resin (Kulzer). Sections
were cut at 2–5 lm with a Reichert-Jung 2040
microtome and stained with: 1) periodic acid-
Schiff’s (PAS) reagent for insoluble polysaccharides
(O’Brien and McCully 1981), 2) Schiff’s reagent plus
calcofluor for pectocellulosic walls (Mori and Bellani
1996), and 3) 0.05% toluidine blue for general
observations. The sections of acetolyzed samples
were not stained.
Pollen hydration. Pollen was hydrated at ambient
temperature (20�C) by storing in: 1) water lacking salts
(milliQ water), 2) tap water (waterP) (see Table 1 for
the composition), 3) solutions of calcium and sodium
ions alone dissolved in milliQ water, either as chloride
or bicarbonate salts at the same concentration as in the
waterP. The basic concentrations of pollen grain
(number/ml) were evaluated by counting the number
of pollen grains in a known water volume with a
hemocytometer (Nageotte chamber), and the
concentrations to use for each experiment were
obtained by dilutions. At different time intervals
after dipping in water, the pollen grains were
observed with the light microscope to monitor the
different steps of the sporoderm release, and to
determine variations in the pollen diameter with an
ocular micrometer at a magnification X 400. Usually,
50 pollen grains were measured for each test, and each
experiment was performed in triplicate.
Dehydration and rehydration of the pollenwithout exine. Pollen grains were dipped in 1–2
drops of waterP on a slide, and after they released
exine were air dried for some hours. Afterwards, they
were again hydrated as aforementioned.
Table 1. Composition (mg/L) of tap water (WaterP)
Ca++ 74.40
Mg++ 11.90
Na++ 4.80
K++ 1.35
NH4+ 0.020
F– 0.06
SO4–– 5.67
NO3– 9.51
NO2– <0.05
Cl– 6.33
HCO3– 273.28
232 G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration
Scanning electron microscope (SEM). Pollen
grains either living or dead were treated for SEM as
previously described (Chichiricco 2006).
Results
Light microscope (LM). Shed pollen grains are
unicellular, and when observed in immersion oil
(Fig. 1) are roundish but with some infoldings,
and also its cell is irregularly roundish. Pollen,
when mounted in oil several hours after shedding
(Fig. 2), appear deformed with evident infoldings
and contracted cell.
Sections of shed pollen. The sections of
pollen grains stain homogeneously with either
toluidine blue or Schiff’s reagent but the pollen
components are not well defined (Fig. 9),
independently of whether the grains were fixed
immediately after shedding or several hours
later. In the sections of acetolyzed pollen, a
minority of pollen grains displays an exine gap
filled with a plug that protrudes from the exine
layer (Fig. 8).
Pollen hydration. Pollen, when dipped in
water, soon become roundish and its protoplast
becomes egg-shaped. Thereafter, the exine wall
breaks by a linear slit and is released according to
the following steps (Fig. 26): 1) the slit opens like a
mouth and the underlying intine is expelled by
swelling like a balloon, 2) the protoplast is sucked
in the expanded side, 3) the backside of the intine
comes out from the mouth and the exine shell is
cast off. Following exine release, the protoplast
becomes either centrally or eccentrically arranged,
and the intine continues to expand up to break, with
dispersal of the pollen components in the medium.
The course of sporoderm breakage and pollen
expansion vary according to both the rehydration
medium and the pollen concentration in the
medium (Figs. 27, 28). As reported in Fig. 27,
when using waterP, the exine is released within
5–10 min and the intine breaks 24–48 h after.
When using milliQ water (Fig. 27), the exine
breaks after 15–60 min if the pollen concentration
is under 140,000 grains/ml, whereas it breaks not
before 48 h if the pollen concentration is over
200,000 grains/ml. Moreover, at concentrations
under 10,000/ml, the intine is subject to break
within 6–10 days, whereas it does not at higher
pollen concentrations. Whatever the concentration
of pollen, its size increment is highest when using
waterP (Fig. 28).
When using solutions with calcium or sodium
alone dissolved in milliQ water at the same
concentration as in the waterP, the breaking of
exine occurs either after a few minutes, if the ions
were as bicarbonate salts, or after many hours, if
the ions were as chloride salts.
Sections of pollen after the exinerelease. The sections of pollen deprived of exine
show well defined images of the intine stratification
(Fig. 10) in the: thin outer layer, large middle layer,
and thick inner layer including the protoplast with a
prominent nucleus. These components, with the
exception of the protoplast, are homogeneously
stained with either toluidine blue or Schiff’s reagent
(PAS), and the middle layer alternatively shows
granules (Fig. 10) with both stainings. The inner
intine layer is bright fluorescent after double
staining with Schiff’s reagent and Calcofluor
(Fig. 11).
Staining of whole pollen. Whole pollen
grains soon after staining with calcofluor, display
a hemispheric protuberance with yellowish
fluorescence (Fig. 3). Within 20–30 min from
staining, the exine generally breaks in the area of
the fluorescent protuberance, so this is pushed out
(insert of Fig. 4) by the swelling intine. Soon after
the exine release, intine layers emit a bright blue
fluorescence (Fig. 4), which is more intense in the
cytoplasmic side of the innermost layer; a bright
fluorescence diffuses in the medium if the outer
intine layer is broken by a slight squashing. The
protuberance induced by calcofluor is also evident
when observing with a light microscope, and it is
formed only after treatment with calcofluor.
After treating with aniline blue (Fig. 5), a
bright yellowish fluorescence is observed in the
inner intine layer, and more intensely in the inner
ring (not shown because not evident in the
photographs).
The double IKI-H2SO4 treatment stains blue
both the outer and the inner intine layers, the
latter much more intensely (Fig. 6), whereas the
middle layer does not stain as detected by
G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration 233
breaking the outer layer with a slight squashing;
no pollen component stains in the controls treated
with IKI alone (Fig. 7).
Pollen walls by SEM. Most pollen grains
(87,5%) of tested ones (80 pollen grains) showed
no aperture on the exposed surface of the exine,
and a minority (12,5%) exhibited a pore with
concave annulus and globose operculoid just
protruding from the pore (Fig. 12). Pollen,
following hydration, split along a precise linear
tract of exine, which is half of the pollen
circumference (Fig. 21). The splitting divides the
exine shell into two valves that open like a mollusc
bivalve to eject intine (Fig. 13), showing a
homogenous profile of the breaking surface (Fig.
21), without indentations or thinnings. Sometimes,
the exine and intine split together along the same
tract displaying their loose connection and their
different thicknesses (Fig. 21). Intine has a
compact and homogeneously smooth surface
(Fig. 14). This wall, when ruptured by a
prolonged hydration (Figs. 15, 17, 21), exhibits
its small thickness and the underlying middle layer
consisting of large branched fibrils (Fig. 16)
enveloping a spongy mass (Fig. 17). The spongy
layer disgregates and is progressively released in
the medium (Fig. 18) until becoming a net that
entangles the pollen shells (Fig. 20). The
disgregation exposes the inner intine (Fig. 19),
which appears as a massive egg-shaped shell with
rugose surface (Fig. 19). This wall retains the
integrity in water.
The pollen treated with calcofluor exhibit a
mass of fibrous material emerging from exine and
including orbicules (Fig. 23). This mass may
detach from exine and disperse on the pollen
surface (Fig. 22).
Harmomegathic changes. Shed pollen
grains when air dried decrease in volume by
the sporoderm inflexion, without significantly
reducing the diameter. When air drying after
the exine release, the middle intine completely
collapses and the outer intine flats without
contracting, until spreading as a veil over the
inner intine and around this to form an exact
disk (Fig. 24). The flat pollen grains dipped in
water swell and restore the roundish outline
(Fig. 25).
Discussion
Pollen morphology and structure. The pollen
of the Cupressaceae is characterized by a pore with
convex annulus, which plays key roles in the
pollen hydration and exine breaking (Van Campo
1953, Duhoux 1982, Bortenschlager 1990,
Kurmann 1994). The pore of living pollen is
crossed by a prominent operculoid that during the
pollen rehydration is pushed out by a transient
bulge of the intine (Duhoux 1982).
In our specimens of C. arizonica, only a
minority either of living or dead pollen grains is
provided with a germinal aperture consisting
of an operculate pore with concave annulus.
Figs. 1–11. Whole pollen grains (Figs. 1–7) and pollen grain sections (Figs. 8–11) of Cupressus arizonica.
LMs. 1, 2 Pollen grains in immersion oil soon after shedding (Fig. 1) or several hours later (Fig. 2). Note the
extensive zonation between the protoplast and the exine in Fig. 1, and the deformation of the sporoderm and the
protoplast in Fig. 2. Bar = 10 lm. 3, 4 Calcofluor-induced fluorescence before (Fig. 3) and soon after (Fig. 4) the
exine release. Note in Fig. 3 the fluorescence of the cup-shaped protuberance (arrows), in Fig. 4, the fluorescence
of the intine, of the underlying layer and of the inner wall; in the insert, the fluorescence of the detached
protuberance. Bar = 50 lm. 5 Aniline blue induced fluorescence in the inner pollen wall (arrows) after the exine
release. Bar = 25 lm. 6, 7 Blue staining of the outer intine (OI) and the inner intine (arrow) after treatment with
IKI plus sulfuric acid (Fig. 6), and control (Fig. 7). Bar = 40 lm. 8 Section of acetolized pollen grains showing
exine aperture closed with the operculoid (arrows). E = exine. Bar = 20 lm. 9, 10 Pollen grains sectioned some
hours after shedding (Fig. 9) or after the exine release in water (Fig. 10), both stained with PAS reagent. Note the
indefinite pollen components in the first section, and the well defined outer intine (OI), middle intine (MI) and
inner intine (arrow) in the second section. Bar = 10 lm in Fig. 9 and 20 lm in Fig. 10. 11 Section of exine free
pollen stained with Schiff’s reagent and calcofluor; note the fluorescence of the inner intine. Bar = 20 lm
b
G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration 235
Figs. 12–17. SEM observations of pollen grains of Cupressus arizonica during in vitro hydration.
Bar = 10 lm. 12 Detail of the pollen surface showing numerous orbicules and a pore (arrow) with concave
arnulus and operculoid. 13 Breaking and opening of the exine (E) with ejection of the swelling intine. 14 Swelled
pollen after exine release. 15 Pollen ejection from the exine (E) with simultaneous splitting of the outer intine
(OI) and exhibition of the middle intine (MI). 16, 17 Middle intine (MI) showing in Fig. 16 the branched fibrils
and in Fig. 17 the spongy mass
236 G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration
Figs. 18–23. 18, 19 Disgregation of the middle intine with partial (Fig. 18) and complete (Fig. 19) release of the
inner intinous shell which encloses the protoplast. 20 Net around the exine shells, arising from disgregation of the
middle intine. 21 Exine (E) and outer intine (OI) simultaneously and correspondingly broken showing their
different thicknesses and their detachment after discharge of the midle intine. 22, 23 Pollen treated with
calcofluor. Note in Fig. 22 both the bulge emerging from exine and the bulge dispersion on the pollen surfaces
(arrows), and in Fig. 23 a particular of the bulge consisting of fibrous material. Bar = 5 lm in Fig. 22 and 2 lm
in Fig. 23
G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration 237
Likewise, a plugged exine gap is sometimes
evidenced in the sections of acelosized pollen. A
common feature after calcofluor treatment is the
formation of a fluorescent globose bulge, as
already reported by Duhoux (1982). However, in
the present case it is persistent, and when
observed by SEM it seems to be formed by a
material coming from the inside of the pollen,
which polymerizes and inglobates orbicules
during its release from the exine. Thus, it is
comparable to the pectic emission of the angio-
sperm germinal apertures (Heslop-Harrison and
Heslop-Harrison 1985). If that is the case,
however, two major points are questionable: 1)
the bulge forms only when pollen is rehydrated in
calcofluor, and 2) it is present in all pollen grains
despite only a minority of them is porate.
Particular attention deserves the intine.
According to the three-layered model (Heslop-
Harrison and Heslop-Harrison 1991), the intine
has a variety of structural and physiological
specializations and consists of an outer homoge-
neous layer and a middle inhomogeneous layer
(tubular, columnar or lamellar) both rich of
pectins, and of an inner layer rich of cellulose.
Our observations by SEM concerning the
morphology and the dynamics of release of the
intine layers, together with the staining tests, are
compatible with such a model.
The outer layer is about three time thinner
than the exine and is homogeneous and compact.
Figs. 24 and 25. Exine free pollen air dried. Note the outer intine (OI) spread around the inner intine shell to
form a disk surrounded by orbicules. Bar = 20 lm. 25 The same as in Fig. 24 after rehydration. Note the swollen
outer intine (OI) and the exine shell. Bar = 10 lm
Fig. 26. Stages of the pollen hydration. Note in
succession: the exine splitting, the intine swelling, the
displacement of the protoplast, and the exine release
238 G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration
The high plasticity of this layer allows pollen to
triplicate its diameter by hydration. It gives
positive reactions with stainings for polysaccha-
rides including that for cellulose (IKI), however,
the moderate mechanical resistance excludes a
cellulosic nature.
The middle layer is very thick and viscous,
with the polysaccharidic components strongly
stainable either with calcofluor or Schiff’s
reagent (PAS). It is spongy when observed by
SEM, and enveloped by a mesh of large and
branched fibrils resembling cellulose macrofi-
brils. Such organization confers high hydrody-
namic properties and scarce mechanical
resistance to the middle layer, which result in
exceptional harmomegathic changes. It is
remarkable as this layer, in absence of the exine,
either may become insubstantial in dry state to
make the dehydrated pollen flat like a disk, or
may restore the roundish outline after immersion
in water. These features reflect the strong muci-
laginous nature and the mechanical deficiency of
Fig. 27. Pollen rehydration in water containing salts (water P) (A) and in water lacking salts (milliQ) (B, C) by
using different pollen concentrations. When using water P (A) the sporoderm walls break with release of the
protoplast within 24–48 h, regardless of the pollen concentration. When using water milliQ, the sporoderm walls
are broken within a number of days if the pollen concentration is under 10,000 grains/ml (B), whereas the exine
only breaks if the pollen concentration is between 22,000–560,000 grains/ml (C)
G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration 239
the middle layer, which do not allow to hypoth-
esize a cellulosic framework.
The inner layer is the persistent wall of the
sporoderm. It is fluctuating within the mucilaginous
layer, and becomes well defined and thickened
during rehydration, parallel to the protoplast expan-
sion into an egg shape. Its polysaccharidic compo-
sition, based on the stainings tests, includes both
cellulose and callose with the latter concentrated on
the inner side. When observing by SEM, it is
compact and rugose resembling a nut shell. Such
intinous shell safeguards the protoplast, especially
during the harmomegathic changes which follow
the exine release, by replacing the mechanical
functions of the exine. At the same time, the
structural polarity predisposes pollen for the pollen
tube emission by the inner callosic layer.
The protoplast is weakly stainable, especially
in dry state and, as typical of the Cupressaceae
pollen (Fernando et al. 2005), it lacks insoluble
polysaccharides and includes a prominent nu-
cleus. Some traits such as the elongated shape
associated to the callosic wall, are signs of a
predisposed cell germination that do not meet
with the slow germination of conifer pollen, nor
with some factors ascribed to the slowness, such
as the absence of callose in the pollen tube wall
(see Fernando et al. 2005); in Pinus pinea pollen
(Pardi et al. 1996), the cytoplasm is rich of
callose for the pollen germination.
The morphological and cytochemical features
above described by LM and SEM agree, to some
extent, with studies by TEM on C. sempervirens(Grilli Caiola et al. 2000).
In vitro hydration. The absorbing capability
of the middle intine exceeds either the
mechanical resistance of the exine, or the
extensibility of the outer intine, so that pollen
may suck water up to break the sporoderm. The
exine, according to our observations by SEM,
breaks by a linear split that divides exine in two
valves with no indentations or thinnings along the
edges, which would indicate start points or
preferential pathways for the breaking. When
rehydration occurs in water containing ions such
as the waterP, the pollen concentration in the
water does not influence hydration and the exine
breaks after a few minutes, followed by intine
breaking in the next hours. When using milliQ
water, the hydration is negatively related to the
population effect. Both the temporal and the final
increments of pollen size are significatively
0
10
20
30
40
50
60
70
80
1 24 48
Time (h)
(rete
maidnello
Pµ
)m a b
a
b
a b
a
b a b
Fig. 28. Increasing diameter of pollen following hydration in water P (dotted) and in water milliQ (blank) by
using pollen concentrations of 200,000 grains/ml (a) and 5,000 grains/ml (b). The pollen diameter before
hydration was 26.4 lm
240 G. Chichiricco and E. Pacini: Cupressus arizonica pollen wall zonation and in vitro hydration
higher when hydrating in waterP than in milliQ
water, regardless of the pollen concentration.
Salts of both sodium and calcium have different
effects on the pollen rehydration according to
whether they are as chloride or bicarbonate.
These observations point out that the dynamics of
the pollen hydration is influenced by several
factors and the interactions of the mucilaginous
layer with the ionic species dissolved in water
play a key role.
Conclusion
The shedding pollen grains of Cupressus arizo-nica are unicellular microspores with highly
specialized sporoderm. This implies different
functionality as compared with other conifers,
as well as with angiosperm pollen. In particular,
the exine is a protective and weakly elastic wall
which, independently on whether it is or is not
provided with germinal aperture, is predisposed
for breaking during hydration. The intine with the
outer plastic layer enables pollen to expand and
to get rid of the exine. The middle mucilaginous
layer, despite being the largest pollen compart-
ment, lacks a substantial mechanical support and
represents the water sucker of the pollen, with
potential sugar reserves. The inner intine is the
real wall of the protoplast with structural and
physiological roles which support the cell viabil-
ity and germinability.
Such pollen wall zonation with shared and
coordinated roles makes the sporoderm highly
competent to control the hydrodynamics and the
pollen germination.
These observations stimulate further studies
to well understand the ultrastructure and compo-
sition of the sporoderm, which show some
questionable features that may be misinterpreted.
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