4.6 Review

The evolution of root hairs and rhizoids

Journal

ANNALS OF BOTANY
Volume 110, Issue 2, Pages 205-212

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/aob/mcs136

Keywords

Rhizoids; root hairs; Physcomitrella patens; Arabidopsis thaliana; root; root systems; nutrient uptake; soil; tip growth; life cycle; alternation of generations; streptophyte

Categories

Funding

  1. University of Oxford
  2. European Union-Marie Curie-Integrated Training Network (PLANTORIGINS)
  3. European Research Council [EVO500]
  4. Biotechnology and Biological Science Research Council of the UK

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Almost all land plants develop tip-growing filamentous cells at the interface between the plant and substrate (the soil). Root hairs form on the surface of roots of sporophytes (the multicellular diploid phase of the life cycle) in vascular plants. Rhizoids develop on the free-living gametophytes of vascular and non-vascular plants and on both gametophytes and sporophytes of the extinct rhyniophytes. Extant lycophytes (clubmosses and quillworts) and monilophytes (ferns and horsetails) develop both free-living gametophytes and free-living sporophytes. These gametophytes and sporophytes grow in close contact with the soil and develop rhizoids and root hairs, respectively. Here we review the development and function of rhizoids and root hairs in extant groups of land plants. Root hairs are important for the uptake of nutrients with limited mobility in the soil such as phosphate. Rhizoids have a variety of functions including water transport and adhesion to surfaces in some mosses and liverworts. A similar gene regulatory network controls the development of rhizoids in moss gametophytes and root hairs on the roots of vascular plant sporophytes. It is likely that this gene regulatory network first operated in the gametophyte of the earliest land plants. We propose that later it functioned in sporophytes as the diploid phase evolved a free-living habit and developed an interface with the soil. This transference of gene function from gametophyte to sporophyte could provide a mechanism that, at least in part, explains the increase in morphological diversity of sporophytes that occurred during the radiation of land plants in the Devonian Period.

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