Epilobium roseum (Onagraceae, rosids) and Paranomus reflexus (Proteaceae, basal eudicots) both simultaneously produce several different pollen morphs that differ in their aperture number (within the same anther and even in some cases within the same tetrads). In E. roseum, pollen grains have two or three apertures, while in P. reflexus pollen grains can have two, three or four apertures. The formation of microspores with different aperture numbers is directly associated with variations in the shape of the tetrads in both species. To study the processes underlying the formation of these different morphs, the different developmental events during microsporogenesis that are known to influence aperture pattern ontogeny were studied. Although cell-plate formation occurs centripetally in both species, the completion of cytokinesis differs between the two in terms of the distribution of additional thick callose deposited onto the cell plates. Observations on the pattern of intersporal wall formation and the shape of mature pollen tetrads in E. roseum, and of intersporal wall formation and post-meiotic tetrads in P. reflexus clearly show that the location of aperture groups within tetrads of both species coincide with the places where callose was deposited last. This supports the hypothesis that aperture pattern ontogeny is linked to post-meiotic cytokinesis.
Within any given tetrad, the positions of final callose deposition coincide with the positions in which apertures will be formed. Intersporal wall formation is a two step process in both species. Isolated callose cell plates are first formed centripetally, after which wall formation is completed through the deposition of additional thick callose deposits. Callose is not evenly deposited onto the cell plates, but is concentrated at specific positions that differ between the two species. In E. roseum, callose deposits are thick at cell plate intersections in the centre of the tetrad and at the intersection of the cleavage walls, becoming thinner towards the periphery of the tetrad. In P. reflexus callose deposits are the thickest in the middle of each cell plate and in the centre of the tetrad, decreasing in thickness towards the intersections of the cleavage walls. In both species the deposition of additional callose deposits relative to the cell plates does not depend on the number of cell plates (whatever the number of cleavage planes, the deposition within a cleavage plane is the same). But, different tetrad shapes correspond to different numbers of cleavage planes. As a result, tetrad shape affects the number and distribution of the places where callose is deposited last.
Although apertures were not observable within post-meiotic tetrads, the aperture distribution within tetrads could be deduced in both species. In
Epilobium, mature pollen grains are dispersed in tetrads, enabling the description of aperture distribution within tetrads even if aperture formation occurs late in development (
Rowley and Skvarla, 2004). In this species, tetragonal tetrads include four diporate pollen grains, tetrahedral tetrads include four triporate pollen grains, and rhomboidal tetrads include two diporate and two triporate pollen grains. In all of these tetrads apertures are joined in pairs, following Fischer's rule. Mature rhomboidal and tetragonal tetrads are not formed by post-meiotic alterations such as tetrahedral tetrad break-down or shape modification. Indeed these two tetrad types, although rare (around 1 % of the tetrads within an anther), can be observed at different stages of development in post-meiotic tetrads still enclosed within callose. In pollen mature tetrads of all shapes, apertures meet precisely where callose is deposited last, namely close to the last point of contact between the cytoplasms of the future microspores at the end of cytokinesis. In
Paranomus, the aperture type can be deduced from the shape of the mature pollen grains, despite not being visible while microspores are still assembled in tetrads. As expected in the Proteaceae, the apertures of this species are distributed according to Garside's rule (
Garside, 1946;
Blackmore and Barnes, 1995). The triangular-shaped triporate pollen grains are produced in tetrahedral tetrads (Fig. I,a–c), while diporate pollen grains are produced by planar tetragonal tetrads (Fig. Ea). Both triporate and diporate pollen grains are also produced in intermediate tetrads (Fig. J,a–c). As in
E. roseum, the aperture arrangements in tetrads in
P. reflexus coincide with the positions where additional callose was deposited last. In both species, the observations collected at all different stages converge to indicate that aperture pattern ontogeny is linked to the completion of the intersporal wall formation in association with tetrad shape.
In 1935, Wodehouse hypothesized that apertures are formed at the last points of contact of the cytoplasm of the resultant microspores at the end of cytokinesis (further developed by
Blackmore and Crane, 1988,
1998; reviewed by
Blackmore et al., 2007).
Ressayre et al. (2002a) developed a model that, in some cases, predicts intra-individual variation in aperture number in plants with simultaneous cytokinesis. This model was based on a schematic description of cytokinesis and is insufficient to accommodate the wide range of variation in microsporogenesis in angiosperms. Results from the two species studied here indicate two further shortcomings in this model. Firstly, although the different tetrad shapes observed in
E. roseum can be categorized into three discrete types, this was not the case in
P. reflexus. Besides the ‘normal’ tetrahedral and rhomboidal tetrads, no true rhomboidal planar tetrads were observed. Instead, intermediate tetrads that are not perfectly planar were observed (Fig. C). Such a level of continuous variation in tetrad shape must be taken into account to fully interpret and describe the consequences of tetrad shape. Previous studies focused on monocot species already pointed to this need. Many monocot species produce irregular tetrahedral tetrads with cleavage walls of different sizes, leading to continuous variation in tetrad shape (
Penet et al., 2005;
Ressayre et al., 2005;
Nadot et al., 2006;
Sannier et al., 2006).
The second shortcoming of the model of
Ressayre et al. (2002a) is the over-simplification of cytokinesis. Classically, intersporal wall formation during microsporogenesis in eudicots was described as happening through infurrowing (
Farr, 1916;
Wodehouse, 1935;
Horner and Lersten, 1971;
Albertsen and Palmer, 1979;
Longly and Waterkeyn, 1979a;
Blackmore and Barnes, 1988;
Brown and Lemmon, 1988;
Ressayre et al., 2002b). Infurrowing entails the synchronization of cell-plate formation and additional callose deposition leading to a highly recognisable pattern with future microspores separated by callose deposits that are thick at the periphery of the tetrad and decrease sharply in thickness towards the cytoplasmic regions that are still connected (see
Blackmore et al., 2007, fig. , plate f). Such a synchronization was believed to be the rule in all core eudicots, and was indeed found in various families (e.g. Solanaceae, Brassicaceae and Asteraceae) studied to date (
Wodehouse, 1935;
Longly and Waterkeyn, 1979a,
b;
Ressayre et al., 2002b). Results in similar studies on species in the Onagraceae, Euphorbiaceae, Ranunculaceae and Proteaceae have, however, revealed that this synchronization can be broken (
Blackmore and Barnes, 1995;
Rowley and Skvarla, 2004;
Ressayre et al., 2005;
Albert et al., 2009). When isolated cell plates are first produced and subsequently embedded in callose as observed in the two species studied here, the cytoplasm of the separating microspores is separated by thin walls of callose of constant thickness (see, for example,
Rowley and Skvarla, 2004, plate 1). It appears then that cytokinesis is not exclusively achieved through infurrowing in higher eudicots either.
When infurrowing takes place, the last cytoplasmic junctions between the developing microspores coincide with last sites of callose deposition. This correlation can be broken when there is a desynchronization of cell wall formation. Recent detailed observations of microsporogenesis are therefore challenging Wodehouse's last contact point hypothesis (
Wodehouse, 1935). Desynchronization between cell-plate formation and additional callose deposition have made it possible to see that the last additional callose deposits – and not the actual last connection points between the cytoplasms – coincide with the positions in which apertures are formed in several different species from different families. These include: Proteaceae (
Paranomus reflexus, this study;
Protea lepidocarpodendron,
Ressayre et al., 2005), Onagraceae (
Epilobium roseum, this study), and several monocots [Pontederiaceae (
Pontederia cordata,
Ressayre et al., 2001), Asphodelaceae (
Asphodelus albus,
Ressayre et al., 2005), Hemerocallidaceae (
Phormium tenax,
Ressayre et al., 2005), Bromeliaceae, (
Tillandsia leiboldiana,
Albert et al., 2010)].