Abstract

Sporopollenin is the main constituent of the exine layer of spore and pollen walls. The anther-specific chalcone synthase-like (ASCL) enzyme of Physcomitrella patens, PpASCL, has previously been implicated in the biosynthesis of sporopollenin, the main constituent of exine and perine, the two outermost layers of the moss spore cell wall. We made targeted knockouts of the corresponding gene, PpASCL, and phenotypically characterized ascl sporophytes and spores at different developmental stages. Ascl plants developed normally until late in sporophytic development, when the spores produced were structurally aberrant and inviable. The development of the ascl spore cell wall appeared to be arrested early in microspore development, resulting in small, collapsed spores with altered surface morphology. The typical stratification of the spore cell wall was absent with only an abnormal perine recognisable above an amorphous layer possibly representing remnants of compromised intine and/or exine. Equivalent resistance of the spore walls of ascl mutants and the control strain to acetolysis suggests the presence of chemically inert, defective sporopollenin in the mutants. Anatomical abnormalities of late-stage ascl sporophytes include a persistent large columella and an air space incompletely filled with spores. Our results indicate that the evolutionarily conserved PpASCL gene is needed for proper construction of the spore wall and for normal maturation and viability of moss spores.

Highlights

  • The transition of plants from aquatic to terrestrial environments about 500 million years ago is one of the most important events in the evolution of life on earth

  • The Physcomitrella genome contains orthologues of Arabidopsis genes involved in exine formation, in the biosynthesis of sporopollenin

  • Ara et al reported that PpCYP703B2 partially rescued a defect in the exine layer of the pollen wall of the rice mutant, cyp703a3 [41]

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Summary

Introduction

The transition of plants from aquatic to terrestrial environments about 500 million years ago is one of the most important events in the evolution of life on earth. Sporopollenin is the main polymeric component of the outer exine layer of spore and pollen walls, and consists of medium- to long-chain fatty acids and oxygenated aromatic compounds [3]. These constituents are coupled via extensive ester and ether linkages, resulting in a robust polymer that enables spore and pollen grains to tolerate physical abrasion, desiccation and UV-B irradiation [4, 5]. A double pksa pksb knockout mutant was male sterile and produced defective pollen grains with no apparent exine, providing evidence for the involvement of ASCL in sporopollenin biosynthesis [14]

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