Abstract

Both wild-type and teratological seed cones are described in the monoecious conifer Glyptostrobus pensilis and compared with those of other Cupressaceae sensu lato and other conifers. Some Cupressaceae apparently possess a proliferation of axillary structures in their cone scales. In our interpretation, in Glyptostrobus each bract of both typical and atypical seed cones bears two descending accessory shoots, interpreted here as seed scales (ovuliferous scales). The primary seed scale is fertile and forms the ovules, the second is sterile and forms characteristic tooth-like structures. The bract and the two axillary seed scales are each supplied with a single distinct vascular bundle that enters the cone axis as a separate strand; this vasculature also characterises the descending accessory short shoots in the vegetative parts of the crown. In wild-type seed cones, the fertile seed scale is reduced to its ovules, and the ovules are always axillary. In contrast, the ovules of some of the teratological seed cones examined were located at the centre of the cone scale. An additional tissue found on the upper surface of the sterile lower seed scale is here interpreted as the axis of the fertile seed scale. Thus, the central position of the ovules can be explained by recaulescent fusion of the upper fertile and lower sterile seed scales. In several teratological cone scales, the ovules were enveloped by an additional sterile tissue that is uniseriate and represents an epidermal outgrowth of the fertile seed scale. Close to the ovules, the epidermis was detached from lower tissue and surrounded the ovule completely, except at the micropyle. These teratological features are potentially significant in understanding seed-cone homologies among extant conifers.

Highlights

  • Current understanding of coniferous seed-cone structure, especially the cone scale, is based partly on comparisons with extinct species known only from fossils and partly on studies of living Pinaceae extended by inference to other coniferous groups (Florin, 1951)

  • Longitudinal section of a fertile cone scale; the bract, ovule and abaxial teeth are each supplied by an individual vascular bundle. (E) Sterile basal cone scale showing only axillary teeth. (F) Fertilised seed cone in lateral view. (G) Detail of a cone scale; a series of nine axillary teeth form an arc above the bract. (H) Seed cone after release of seeds. (I) Detail of a single cone scale removed from (H); a clear boundary layer is marked as white dotted line between the bract and the distal teeth

  • The observed developmental plasticity may be at least partly due to the highly condensed, integrated nature of the modern coniferous seed cone, in which each cone scale is interpreted as a congenitally fused lateral axis putatively derived from fertile branches similar to those of extinct cordaites (Florin, 1951)

Read more

Summary

Introduction

Current understanding of coniferous seed-cone structure, especially the cone scale, is based partly on comparisons with extinct species known only from fossils and partly on studies of living Pinaceae extended by inference to other coniferous groups (Florin, 1951). Conifer seed cones consist of numerous overlapping structures that each represent an integrated complex combining a bract and an ovuliferous scale, here termed the bract/scale complex (Coulter & Chamberlain, 1917; Florin, 1951; Wilde, 1975; Rudall et al, 2011). The seed cone represents a polyaxial, branched structure (Schuhmann, 1902; Herzfeld, 1914; Pilger, 1926; Florin, 1951, 1954; Schweitzer, 1963; Mundry, 2000; Rudall et al, 2011)

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call