As decomposers, fungi are key players in recycling plant material in global carbon cycles. We hypothesized that genomes of early diverging fungi may have inherited pectinases from an ancestral species that had been able to extract nutrients from pectin-containing land plants and their algal allies (Streptophytes). We aimed to infer, based on pectinase gene expansions and on the organismal phylogeny, the geological timing of the plant–fungus association. We analyzed 40 fungal genomes, three of which, including Gonapodya prolifera, were sequenced for this study. In the organismal phylogeny from 136 housekeeping loci, Rozella diverged first from all other fungi. Gonapodya prolifera was included among the flagellated, predominantly aquatic fungal species in Chytridiomycota. Sister to Chytridiomycota were the predominantly terrestrial fungi including zygomycota I and zygomycota II, along with the ascomycetes and basidiomycetes that comprise Dikarya. The Gonapodya genome has 27 genes representing five of the seven classes of pectin-specific enzymes known from fungi. Most of these share a common ancestry with pectinases from Dikarya. Indicating functional and sequence similarity, Gonapodya, like many Dikarya, can use pectin as a carbon source for growth in pure culture. Shared pectinases of Dikarya and Gonapodya provide evidence that even ancient aquatic fungi had adapted to extract nutrients from the plants in the green lineage. This implies that 750 million years, the estimated maximum age of origin of the pectin-containing streptophytes represents a maximum age for the divergence of Chytridiomycota from the lineage including Dikarya.

We performed a numerical analysis of 148 phenotypic characteristics of 20 strains of root nodule bacteria isolated from an arid saline desert soil in the Xinjiang region of northwestern People's Republic of China and compared these organisms with 28 Rhizobium and Bradyrhizobium strains obtained from different regions of the People's Republic of China and from other countries, including nine type strains of different species. All of the strains examined clustered into two groups at a similarity level of more than 63%. Group I included all of the previously described Rhizobium species and was divided into eight subgroups, which corresponded to previously described Rhizobium species, at a similarity level of more than 82%. Group I1 was divided into the following three subgroups at a similarity level of more than 80% Bradyrhizubium japonicum, a cluster containing 17 moderately and slowly growing strains isolated in the Xinjiang region, and a small subgroup containing three fast-growing strains. The generation times of the moderately and slowly growing strains were 5 to 15 h, and these organisms produced acid in medium containing mannitol. The DNA G+C contents of the members of this group ranged from 59 to 63 mol%. DNA-DNA hybridization experiments revealed that the levels of DNA homology among all of the moderately and slowly growing strains obtained from Xinjiang were more than 70% and that the levels of DNA homology between representative strains of this group and the type strains of all previously described species of root-and stem-nodulating bacteria were low. All of our experimental data indicated that the moderately and slowly growing rhizobia isolated from Xinjiang are members of a new species. Partial 16s rRNA gene sequencing of the type strain. A-1BS (= CCBAU3306), and a comparison of the resulting sequence with the sequences of previously described species revealed that strain A-1BS is closely related to Rhizobium loti, Rhizobium huakuii, and Rhizobium galegae, but not to B. japonicum and Azorhizobium caulinodans. On the basis of our results, we propose that the strains which we studied are members of a new species, Rhizobium tianshanense. The type strain, A-1BS (= CCBAU3306), has been deposited in the Culture Collection of Beijing Agricultural University, Beijing, People's Republic of China.At the present time, all bacteria that induce nodules on the roots of leguminous plants are assigned to three genera (8,14). The genus Rhizobium comprises a group of fast growers and includes eight species, Rhizobium leguminosarum, Rhizobium meliloti, Rhizobium loti (14), Rhizobium fredii (20), Rhizobium huakuii (2), Rhizobium galegae (15), Rhizobium tropici (16), and Rhizobium etli (21). Each of these species is associated with a group of host plants and is distinguished from the other species mainly on the basis of DNA relatedness values, 16s rRNA homology values, and some phenotypic characteristics. The genus Bradyrhizobium comprises a group of slow growers and contains one species, Bradyrhizobium japonicum, which i...

Elucidating the timescale of the evolution of Alphaproteobacteria, one of the most prevalent microbial lineages in marine and terrestrial ecosystems, is key to testing hypotheses on their co-evolution with eukaryotic hosts and Earth’s systems, which, however, is largely limited by the scarcity of bacterial fossils. Here, we incorporate eukaryotic fossils to date the divergence times of Alphaproteobacteria, based on the mitochondrial endosymbiosis that mitochondria evolved from an alphaproteobacterial lineage. We estimate that Alphaproteobacteria arose ~1900 million years (Ma) ago, followed by rapid divergence of their major clades. We show that the origin of Rickettsiales, an order of obligate intracellular bacteria whose hosts are mostly animals, predates the emergence of animals for ~700 Ma but coincides with that of eukaryotes. This, together with reconstruction of ancestral hosts, strongly suggests that early Rickettsiales lineages had established previously underappreciated interactions with unicellular eukaryotes. Moreover, the mitochondria-based approach displays higher robustness to uncertainties in calibrations compared with the traditional strategy using cyanobacterial fossils. Further, our analyses imply the potential of dating the (bacterial) tree of life based on endosymbiosis events, and suggest that previous applications using divergence times of the modern hosts of symbiotic bacteria to date bacterial evolution might need to be revisited.

Summary Climate and land‐use change are expected to substantially alter future plant species distributions leading to higher extinction rates. However, little is known about how plant species ranges, richness and phylogenetic diversity of continents will be affected by these dynamics. We address this gap here by examining the patterns of species' distributions and phylogenetic relationships for 7465 seed plant taxa in North America. An ensemble of species distribution models was used to estimate the potential suitable habitat of species under different sets of climate, land‐use and dispersal constraint scenarios. We then evaluated the vulnerability and extinction risk of individual species to changes in climate and land use, and examined whether rare, endangered and evolutionarily distinct species were disproportionally threatened by climate and land‐use change. We show that ~2000 species may lose >80% of their suitable habitats under the A1b emission scenario for the 2080s, while ~100 species may experience >80% range expansions (a 20 : 1 ratio of loss to gain). When considering >50% range retraction and expansion, the ratio of loss to gain was 13 : 1. A greater loss of species diversity is expected at low latitudes, while larger gains are expected at high latitudes. Evolutionarily distinct species are predicted to have significantly higher extinction risks than extant species. This suggests a disproportionate future loss of phylogenetic diversity for the North American flora. Synthesis and applications. Our study provides continental‐scale evidence of plant species extinction risk caused by future climate and land‐use change, and highlights the importance of integrating phylogenetic measures into conservation risk assessments. This work provides insight into the status, trends and threats for a large share of North America's plant species by identifying risks and prioritizing conservation in a rapidly changing world.

Dapper homolog (DACT) 2 is one of the Dact gene family members, which are important modulators of Wnt signaling pathway. We aim to clarify its epigenetic inactivation, biological function and clinical implication in colon cancer. DACT2 was silenced in five out of eight colon cancer cell lines, but robustly expressed in normal colon tissues. The loss of DACT2 expression was regulated by promoter hypermethylation. Restoring DACT2 expression in colon cancer cell lines suppressed tumor cell growth by inducing cell apoptosis and inhibiting cell proliferation both in vitro and in vivo. Moreover, DACT2 overexpression effectively reduced lung metastasis of colon cancer cells in nude mice. These effects by DACT2 were attributed to inhibition of Wnt/β-catenin signaling. Reexpression of DACT2 significantly suppressed the transcriptional activity of both wild-type β-catenin and degradation-resistant form mutant β-catenin (S33Y). DACT2 could actively shuttle into and out of nuclei, with its predominant steady-state localization in the cytoplasm dependent on its nuclear export signal. Co-immunoprecipitation results indicated that DACT2 strongly associated β-catenin as well as lymphoid enhancer-binding factor 1 (LEF1) and directly disrupted the formation of the β-catenin-LEF1 complex in the nucleus. Whereas in the cytoplasm, DACT2 restored junctional localization of E-cadherin-β-catenin complexes and prevented β-catenin nuclear translocation through direct interaction with β-catenin. DACT2 methylation was detected in 43.3% (29/67) of colon cancer tissues, but none in normal controls. Multivariate analysis revealed that patients with DACT2 methylation had a significant decrease in overall survival (P = 0.006). Kaplan-Meier survival curves showed that DACT2 methylation was significantly associated with shortened survival in stage I-III colon cancer patients. In conclusion, DACT2 acts as a functional tumor suppressor in colon cancer through inhibiting Wnt/β-catenin signaling. Its methylation at early stages of colon carcinogenesis is an independent prognostic factor.