Auxin conjugates: their role for plant development and in the evolution of land plants

Auxin conjugates are thought to play important roles as storage forms for the active plant hormone indole-3-acetic acid (IAA). In its free form, IAA comprises only up to 25% of the total amount of IAA, depending on the tissue and the plant species studied. The major forms of IAA conjugate are low molecular weight ester or amide forms, but there is increasing evidence of the occurrence of peptides and proteins modified by IAA. Since the discovery of genes and enzymes involved in synthesis and hydrolysis of auxin conjugates, much knowledge has been gained on the biochemistry and function of these compounds, but there is still much to discover. For example, recent work has shown that some auxin conjugate hydrolases prefer conjugates with longer-chain auxins such as indole-3-propionic acid and indole-3-butyric acid as substrate. Also, the compartmentation of these reactions in the cell or in tissues has not been resolved in great detail. The function of auxin conjugates has been mainly elucidated by mutant analysis in genes for synthesis or hydrolysis and a possible function for conjugates inferred from these results. In the evolution of land plants auxin conjugates seem to be connected with the development of certain traits such as embryo, shoot, and vasculature. Most likely, the synthesis of auxin conjugates was developed first, since it has been already detected in moss, whereas sequences typical of auxin conjugate hydrolases were found according to database entries first in moss ferns. The implications for the regulation of auxin levels in different species will be discussed.     

Major transitions in the evolution of early land plants: a bryological perspective

Background Molecular phylogeny has resolved the liverworts as the earliest-divergent clade of land plants and mosses as the sister group to hornworts plus tracheophytes, with alternative topologies resolving the hornworts as sister to mosses plus tracheophytes less well supported. The tracheophytes plus fossil plants putatively lacking lignified vascular tissue form the polysporangiophyte clade. Scope This paper reviews phylogenetic, developmental, anatomical, genetic and paleontological data with the aim of reconstructing the succession of events that shaped major land plant lineages. Conclusions Fundamental land plant characters primarily evolved in the bryophyte grade, and hence the key to a better understanding of the early evolution of land plants is in bryophytes. The last common ancestor of land plants was probably a leafless axial gametophyte bearing simple unisporangiate sporophytes. Water-conducting tissue, if present, was restricted to the gametophyte and presumably consisted of perforate cells similar to those in the early-divergent bryophytes Haplomitrium and Takakia. Stomata were a sporophyte innovation with the possible ancestral functions of producing a transpiration-driven flow of water and solutes from the parental gametophyte and facilitating spore separation before release. Stomata in mosses, hornworts and polysporangiophytes are viewed as homologous, and hence these three lineages are collectively referred to as the 'stomatophytes'. An indeterminate sporophyte body (the sporophyte shoot) developing from an apical meristem was the key innovation in polysporangiophytes. Poikilohydry is the ancestral condition in land plants; homoiohydry evolved in the sporophyte of polysporangiophytes. Fungal symbiotic associations ancestral to modern arbuscular mycorrhizas evolved in the gametophytic generation before the separation of major present-living lineages. Hydroids are imperforate water-conducting cells specific to advanced mosses. Xylem vascular cells in polysporangiophytes arose either from perforate cells or de novo. Food-conducting cells were a very early innovation in land plant evolution. The inferences presented here await testing by molecular genetics.     

Evidence for the most basal split in land plants dividing bryophyte and tracheophyte lineages

The problem of relationships among the major basal living groups of land plants is long standing, yet the uncertainty as to the phylogenetic affinity of these lines persists in the literature. Molecular and modern cladistic studies of the phylogenetic relationships of the above groups resulted in a large number of conflicting topologies. However, with the exception of the cladistic analyses of spermatogenesis, suggesting monophyly of extant bryophytes, these studies agree the paraphyletic bryophyte grade is basal within the embryophyte tree. Here we would like to present analyses on the basis of the concatenated datasets of nucleotide and amino-acid sequences of 57 protein-coding genes common to 17 chloroplast genomes of land plants and a charophyte alga Chaetosphaeridium globosum. Character-wise, these are the largest datasets currently available to address the problem of basal relationships within embryophytes. Main lineages of bryophytes, i.e liverworts, hornworts and mosses are represented in our alignments with a single taxon, whereas 14 taxa represent the tracheophytes. With our data, phylogeny with liverwort basal appears to be and artifact related to high and unequal A+T contents among the sequences analysed. Reducing this compositional bias and applying methods developed to counter it, we recovered an alternative, strongly supported topology wherein both bryophytes and tracheophytes are monophyletic. Within bryophytes, hornworts are basal and liverworts are sister to mosses.     

Unresolved problems on the origin and early evolution of land plants.

The origin of land plants or embryophytes from the Charophyceae is generally accepted today by the botanists. In fact, numerous morphological, cytological, ultrastructural, biochemical and molecular characters are shared in these organisms. A fundamental problem is still constituted by the evolution of the sporophyte, i.e. the appearance of two different phase cycles (gametophyte/sporophyte alternance), although two theories ("antithetic" and "homologous") try to explain this evolutionary event.However, another phylogenetic dilemma is represented, in my opinion, either by the formation of bryophytes or by the transition from these first land plants to the pteridophytes, considering them at whole organism level.The bryophyte gametophyte is the most elaborate of the land plants. It presents several complex characters, principally the growth developmental form, the appearance of multicellular sex organs, antheridia and archegonia. Also the sporophyte shows a complicated structure that is not found in the other land plants or tracheophytes. The sporangium, in particular, exhibits some intricate morphological traits such as the peristome of true mosses for spore dispersion, the elaters of liverworts and the indeterminate growth in the hornworts.The pteridophytes are represented especially by their dominant sporophyte. This latter has the capacity to produce multiple sporangia and, in many cases, two kinds of spores which develop in male and female gametophyte (heterosporous pteridophytes). Another important characteristic of this sporophyte is its ability to become independent of the gametophyte. However, one of the most innovative character is the formation of true vascular elements (xylem and phloem).All these very large evolutionary jumps are discussed on the basis of the phyletic gradualistic neo-Darwinian theory and the punctuated equilibrium theory of Eldredge and Gould. In this context other genetic evolutionary mechanisms are also considered.Nevertheless, the origin of bryophytes and pteridophytes remain, at the moment, a mystery.     

On introgressive hybridization and its significance in the evolution of plants

Hybrid forms arisen in the process of introgression are of low stability. Changes in climate lead to absorption of hybrids by the ancestor for which this change is most favourable. Though the forms created by hybrid introgression are able to exist for thousands or even millions of years, introgressive hybridization in the cases known to us, as well as in the genera Picea, Larix, Pinus, has not opened and is not opening any evolutionary prospects.     

How plants conquered land: evolution of terrestrial adaptation

The transition of plants from water to land is considered one of the most significant events in the evolution of life on Earth. The colonization of land by plants, accompanied by their morphological, physiological and developmental changes, resulted in plant biodiversity. Besides significantly influencing oxygen levels in the air and on land, plants manufacture organic matter from CO₂ and water with the help of sunlight, paving the way for the diversification of nonplant lineages ranging from microscopic organisms to animals. Land plants regulate the climate by adjusting total biomass and energy flow. At the genetic level, these innovations are achieved through the rearrangement of pre-existing genetic information. Advances in genome sequencing technology are revamping our understanding of plant evolution. This study highlights the morphological and genomic innovations that allow plants to integrate life on Earth.     

Auxin action on growth in intact plants: Threshold turgor is regulated

The guillotine thermocouple psychrometer allows auxin action on cell enlargement to be investigated in intact plants. Because the technique measures all the physical parameters affecting enlargement in the same plants, close comparisons can be made of the changes brought about by this growth regulator. In etiolated seedlings of soybean (Glycine max L. Merr.), auxin was supplied endogenously by the intact plant or was depleted by removing the apical portion of the stem. We observed that, when stem growth was rapid in the intact plant, the water potential of the growing region was lower than in the nongrowing region but, as growth slowed during auxin depletion, the water potential rose until it became essentially the same as in the nongrowing region. This indicated that gradients in water potential had been induced by the demand for water during rapid growth but had decreased as growth decreased in the auxin-depleted cells. The turgor appeared to rise slightly as growth slowed which is in the wrong direction to account for the growth change unless compensating changes occurred in wall properties and/or synthesis. As growth ceased in the auxin-depleted tissue, the threshold turgor rose until it became nearly the same as the cell turgor, which indicates that auxin affected this wall parameter. The osmotic potential increased slightly, probably because of a dilution of the cell contents by the residual growth occurring after the stem apex (and cotyledons) had been removed. The hydraulic conductance for water was unaffected by auxin status whether it was measured in the whole enlarging region or in individual cortical cells from the region. It was concluded that auxin acts mainly on the metabolism of the cell walls manifested by the change in growth rate and threshold turgor. The other changes were passive responses to the changed growth rate.Abbreviations and Symbols G relative growth rate - L conductance of tissue - Lp hydraulic conductivity of cell - m extensibility of cell walls - T threshold turgor - t_1/2 halftime for turgor relaxation - V volume of water - bulk elastic modulus - _o water potential of nongrowing tissue - (_{o w}) growth-induced water potential - _p turgor - (_p T) growth-active turgor - _s osmotic potential - _w water potential of growing tissue This work was supported by a grant from the Science and Technology Agency of Japan to S.M. and grants from the DuPont Company and the Department of Energy DE-FG02-87ER13776 to J.S.B. We thank Dr. Douglas Miller for help with the statistics.     

The mitochondrial genomes of the early land plants Treubia lacunosa and Anomodon rugelii: dynamic and conservative evolution

Early land plant mitochondrial genomes captured important changes of mitochondrial genome evolution when plants colonized land. The chondromes of seed plants show several derived characteristics, e.g., large genome size variation, rapid intra-genomic rearrangement, abundant introns, and highly variable levels of RNA editing. On the other hand, the chondromes of charophytic algae are still largely ancestral in these aspects, resembling those of early eukaryotes. When the transition happened has been a long-standing question in studies of mitochondrial genome evolution. Here we report complete mitochondrial genome sequences from an early-diverging liverwort, Treubia lacunosa, and a late-evolving moss, Anomodon rugelii. The two genomes, 151,983 and 104,239 base pairs in size respectively, contain standard sets of protein coding genes for respiration and protein synthesis, as well as nearly full sets of rRNA and tRNA genes found in the chondromes of the liverworts Marchantia polymorpha and Pleurozia purpurea and the moss Physcomitrella patens. The gene orders of these two chondromes are identical to those of the other liverworts and moss. Their intron contents, with all cis-spliced group I or group II introns, are also similar to those in the previously sequenced liverwort and moss chondromes. These five chondromes plus the two from the hornworts Phaeoceros laevis and Megaceros aenigmaticus for the first time allowed comprehensive comparative analyses of structure and organization of mitochondrial genomes both within and across the three major lineages of bryophytes. These analyses led to the conclusion that the mitochondrial genome experienced dynamic evolution in genome size, gene content, intron acquisition, gene order, and RNA editing during the origins of land plants and their major clades. However, evolution of this organellar genome has remained rather conservative since the origin and initial radiation of early land plants, except within vascular plants.     

Green land: Multiple perspectives on green algal evolution and the earliest land plants

Green plants, broadly defined as green algae and the land plants (together, Viridiplantae), constitute the primary eukaryotic lineage that successfully colonized Earth's emergent landscape. Members of various clades of green plants have independently made the transition from fully aquatic to subaerial habitats many times throughout Earth's history. The transition, from unicells or simple filaments to complex multicellular plant bodies with functionally differentiated tissues and organs, was accompanied by innovations built upon a genetic and phenotypic toolkit that have served aquatic green phototrophs successfully for at least a billion years. These innovations opened an enormous array of new, drier places to live on the planet and resulted in a huge diversity of land plants that have dominated terrestrial ecosystems over the past 500 million years. This review examines the greening of the land from several perspectives, from paleontology to phylogenomics, to water stress responses and the genetic toolkit shared by green algae and plants, to the genomic evolution of the sporophyte generation. We summarize advances on disparate fronts in elucidating this important event in the evolution of the biosphere and the lacunae in our understanding of it. We present the process not as a step-by-step advancement from primitive green cells to an inevitable success of embryophytes, but rather as a process of adaptations and exaptations that allowed multiple clades of green plants, with various combinations of morphological and physiological terrestrialized traits, to become diverse and successful inhabitants of the land habitats of Earth.     

The class III peroxidase multigenic family in rice and its evolution in land plants

Plant peroxidases (class III peroxidases, E.C. 1.11.1.7) are secreted glycoproteins known to be involved in the mechanism of cell elongation, in cell wall construction and differentiation, and in the defense against pathogens. They usually form large multigenic families in angiosperms. The recent completion of rice (Oryza sativa japonica c.v. Nipponbare) genome sequencing allowed drawing up the full inventory of the genes encoding class III peroxidases in this plant. We found 138 peroxidase genes distributed among the 12 rice chromosomes. In contrast to several other gene families studied so far, peroxidase genes are twice as numerous in rice as in Arabidopsis. This large number of genes results from various duplication events that were tentatively traced back using a phylogenetic tree based on the alignment of conserved amino acid sequences. We also searched for peroxidase encoding genes in the major phyla of plant kingdom. In addition to gymnosperms and angiosperms, sequences were found in liverworts, mosses and ferns, but not in unicellular green algae. Two rice and one Arabidopsis peroxidase genes appeared to be rather close to the only known sequence from the liverwort Marchantia polymorpha. The possible relationship of these peroxidases with the putative ancestor of peroxidase genes is discussed, as well as the connection between the development of the class III peroxidase multigenic family and the emergence of the first land plants.     

Morphological evolution in land plants: new designs with old genes

The colonization and radiation of multicellular plants on land that started over 470 Ma was one of the defining events in the history of this planet. For the first time, large amounts of primary productivity occurred on the continental surface, paving the way for the evolution of complex terrestrial ecosystems and altering global biogeochemical cycles; increased weathering of continental silicates and organic carbon burial resulted in a 90 per cent reduction in atmospheric carbon dioxide levels. The evolution of plants on land was itself characterized by a series of radical transformations of their body plans that included the formation of three-dimensional tissues, de novo evolution of a multicellular diploid sporophyte generation, evolution of multicellular meristems, and the development of specialized tissues and organ systems such as vasculature, roots, leaves, seeds and flowers. In this review, we discuss the evolution of the genes and developmental mechanisms that drove the explosion of plant morphologies on land. Recent studies indicate that many of the gene families which control development in extant plants were already present in the earliest land plants. This suggests that the evolution of novel morphologies was to a large degree driven by the reassembly and reuse of pre-existing genetic mechanisms.     

Phylogenetic distribution and evolution of mycorrhizas in land plants

A survey of 659 papers mostly published since 1987 was conducted to compile a checklist of mycorrhizal occurrence among 3,617 species (263 families) of land plants. A plant phylogeny was then used to map the mycorrhizal information to examine evolutionary patterns. Several findings from this survey enhance our understanding of the roles of mycorrhizas in the origin and subsequent diversification of land plants. First, 80 and 92% of surveyed land plant species and families are mycorrhizal. Second, arbuscular mycorrhiza (AM) is the predominant and ancestral type of mycorrhiza in land plants. Its occurrence in a vast majority of land plants and early-diverging lineages of liverworts suggests that the origin of AM probably coincided with the origin of land plants. Third, ectomycorrhiza (ECM) and its derived types independently evolved from AM many times through parallel evolution. Coevolution between plant and fungal partners in ECM and its derived types has probably contributed to diversification of both plant hosts and fungal symbionts. Fourth, mycoheterotrophy and loss of the mycorrhizal condition also evolved many times independently in land plants through parallel evolution.