The relationships among the four major embryophyte lineages (mosses, liverworts, hornworts, vascular plants) and the timing of the origin of land plants are enigmatic problems in plant evolution. Here, we resolve the monophyly of bryophytes by improving taxon sampling of hornworts and eliminating the effect of synonymous substitutions. We then estimate the divergence time of crown embryophytes based on three fossil calibration strategies, and reveal that maximum calibration constraints have a major effect on estimating the time of origin of land plants. Moreover, comparison of priors and posteriors provides a guide for evaluating the optimal calibration strategy. By considering the reliability of fossil calibrations and the influences of molecular data, we estimate that land plants originated in the Precambrian (980 − 682 Ma), much older than widely recognized. Our study highlights the important contribution of molecular data when faced with contentious fossil evidence, and that fossil calibrations used in estimating the timescale of plant evolution require critical scrutiny.

The chlorophyte green algae (Chlorophyta) are species-rich ancient groups ubiquitous in various habitats with high cytological diversity, ranging from microscopic to macroscopic organisms. However, the deep phylogeny within core Chlorophyta remains unresolved, in part due to the relatively sparse taxon and gene sampling in previous studies. Here we contribute new transcriptomic data and reconstruct phylogenetic relationships of core Chlorophyta based on four large datasets up to 2698 genes of 70 species, representing 80% of extant orders. The impacts of outgroup choice, missing data, bootstrap-support cutoffs, and model misspecification in phylogenetic inference of core Chlorophyta are examined. The species tree topologies of core Chlorophyta from different analyses are highly congruent, with strong supports at many relationships (e.g., the Bryopsidales and the Scotinosphaerales-Dasycladales clade). The monophyly of Chlorophyceae and of Trebouxiophyceae as well as the uncertain placement of Chlorodendrophyceae and Pedinophyceae corroborate results from previous studies. The reconstruction of ancestral scenarios illustrates the evolution of the freshwater-sea and microscopic-macroscopic transition in the Ulvophyceae, and the transformation of unicellular→colonial→multicellular in the chlorophyte green algae. In addition, we provided new evidence that serine is encoded by both canonical codons and non-canonical TAG code in Scotinosphaerales, and stop-to-sense codon reassignment in the Ulvophyceae has originated independently at least three times. Our robust phylogenetic framework of core Chlorophyta unveils the evolutionary history of phycoplast, cyto-morphology and non-canonical genetic codes in chlorophyte green algae.

The Ulvophyceae, a major group of green algae, is of particular evolutionary interest because of its remarkable morphological and ecological diversity. Its phylogenetic relationships and diversification timeline, however, are still not fully resolved. In this study, using an extensive nuclear gene dataset, we apply coalescent- and concatenation-based approaches to reconstruct the phylogeny of the Ulvophyceae and to explore the sources of conflict in previous phylogenomic studies. The Ulvophyceae is recovered as a paraphyletic group, with the Bryopsidales being a sister group to the Chlorophyceae, and the remaining taxa forming a clade (Ulvophyceae sensu stricto). Molecular clock analyses with different calibration strategies emphasize the large impact of fossil calibrations, and indicate a Meso-Neoproterozoic origin of the Ulvophyceae (sensu stricto), earlier than previous estimates. The results imply that ulvophyceans may have had a profound influence on oceanic redox structures and global biogeochemical cycles at the Mesoproterozoic-Neoproterozoic transition.

Alpine dwarfism is widely observed in alpine plant populations and often considered a high-altitude adaptation, yet its molecular basis and ecological relevance remain unclear. In this study, we used map-based cloning and field transplant experiments to investigate dwarfism in natural Arabidopsis (Arabidopsis thaliana) accessions collected from the Swiss Alps. A loss-of-function mutation due to a single nucleotide deletion in gibberellin20-oxidase1 (GA5) was identified as the cause of dwarfism in an alpine accession. The mutated allele, ga5-184, was found in two natural Arabidopsis populations collected from one geographic region at high altitude, but was different from all other reported ga5 null alleles, suggesting that this allele has evolved locally. In field transplant experiments, the dwarf accession with ga5-184 exhibited a fitness pattern consistent with adaptation to high altitude. Across a wider array of accessions from the Swiss Alps, plant height decreased with altitude of origin, but fitness patterns in the transplant experiments were variable and general altitudinal adaptation was not evident. In general, our study provides new insights into molecular basis and possible ecological roles of alpine dwarfism, and demonstrates the importance of the GA-signaling pathway for the generation of ecologically relevant variation in higher plants.

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