Woese and Fox's 1977 paper on the discovery of the Archaea triggered a revolution in the field of evolutionary biology by showing that life was divided into not only prokaryotes and eukaryotes. Rather, they revealed that prokaryotes comprise two distinct types of organisms, the Bacteria and the Archaea. In subsequent years, molecular phylogenetic analyses indicated that eukaryotes and the Archaea represent sister groups in the tree of life. During the genomic era, it became evident that eukaryotic cells possess a mixture of archaeal and bacterial features in addition to eukaryotic-specific features. Although it has been generally accepted for some time that mitochondria descend from endosymbiotic alphaproteobacteria, the precise evolutionary relationship between eukaryotes and archaea has continued to be a subject of debate. In this Review, we outline a brief history of the changing shape of the tree of life and examine how the recent discovery of a myriad of diverse archaeal lineages has changed our understanding of the evolutionary relationships between the three domains of life and the origin of eukaryotes. Furthermore, we revisit central questions regarding the process of eukaryogenesis and discuss what can currently be inferred about the evolutionary transition from the first to the last eukaryotic common ancestor.

All cell membranes are composed of glycerol phosphate phospholipids, and this commonality argues for the presence of such phospholipids in the last common ancestor, or cenancestor. However, phospholipid biosynthesis is very different between bacteria and archaea, leading to the suggestion that the cenancestor was devoid of phospholipid membranes. Recent phylogenomic studies challenge this view, suggesting that the cenancestor did possess complex phospholipid membranes. Here, we discuss the implications of these recent findings for membrane evolution in archaea and bacteria, and for the origin of the eukaryotic cell.

Isoprenoids are a very diverse family of organic compounds widespread in the three domains of life. Although they are produced from the condensation of the same precursors in all organisms (isopentenyl pyrophosphate and dimethylallyl diphosphate), the evolutionary origin of their biosynthesis remains controversial. Two independent nonhomologous metabolic pathways are known: the mevalonate (MVA) pathway in eukaryotes and archaea and the methylerythritol phosphate (MEP) pathway in bacteria and several photosynthetic eukaryotes. The MVA pathway is also found in a few bacteria, what has been explained in previous works by recent acquisition by horizontal gene transfer (HGT) from eukaryotic or archaeal donors. To reconsider the question of the evolutionary origin of the MVA pathway, we have studied the origin and the evolution of the enzymes of this pathway using phylogenomic analyses upon a taxon-rich sequence database. On the one hand, our results confirm the conservation in archaea of an MVA pathway partially different from eukaryotes. This implies that each domain of life possesses a characteristic major isoprenoid biosynthesis pathway: the classical MVA pathway in eukaryotes, a modified MVA pathway in archaea, and the MEP pathway in bacteria. On the other hand, despite the identification of several HGT events, our analyses support that the MVA pathway was ancestral not only in archaea and eukaryotes but also in bacteria, in contradiction with previous claims that the presence of this pathway in bacteria was due to HGT from other domains. Therefore, the MVA pathway is likely an ancestral metabolic route in all the three domains of life, and hence, it was probably present in the last common ancestor of all organisms (the cenancestor). These findings open the possibility that the cenancestor had membranes containing isoprenoids.

Large reservoirs of natural gas in the oceanic subsurface sustain complex communities of anaerobic microbes, including archaeal lineages with potential to mediate oxidation of hydrocarbons such as methane and butane. Here we describe a previously unknown archaeal phylum, Helarchaeota, belonging to the Asgard superphylum and with the potential for hydrocarbon oxidation. We reconstruct Helarchaeota genomes from metagenomic data derived from hydrothermal deep-sea sediments in the hydrocarbon-rich Guaymas Basin. The genomes encode methyl-CoM reductase-like enzymes that are similar to those found in butane-oxidizing archaea, as well as several enzymes potentially involved in alkyl-CoA oxidation and the Wood-Ljungdahl pathway. We suggest that members of the Helarchaeota have the potential to activate and subsequently anaerobically oxidize hydrothermally generated short-chain hydrocarbons.

The origin of eukaryotes represents an unresolved puzzle in evolutionary biology. Current research suggests that eukaryotes evolved from a merger between a host of archaeal descent and an alphaproteobacterial endosymbiont. The discovery of the Asgard archaea, a proposed archaeal superphylum that includes Loki-, Thor-, Odin-and Heimdallarchaeota suggested to comprise the closest archaeal relatives of eukaryotes, has helped elucidating the identity of the putative archaeal host. While Lokiarchaeota are assumed to employ a hydrogen-dependent metabolism, little is known about the metabolic potential of other members of the Asgard superphylum. We infer the central metabolic pathways of Asgard archaea using comparative genomics and phylogenetics to be able to refine current models for the origin of eukaryotes. Our analyses indicate that Thor-and Lokiarchaeota encode proteins necessary for carbon fixation via the Wood-Ljungdahl pathway and for obtaining reducing equivalents from organic substrates. In contrast, Heimdallarchaeum LC2 and LC3 genomes encode enzymes potentially enabling the oxidation of organic substrates using nitrate or oxygen as electron acceptors. The gene repertoire of Heimdallarchaeum AB125 and Odinarchaeum indicates that these organisms can ferment organic substrates and conserve energy by coupling ferredoxin re-oxidation to respiratory proton reduction. Altogether, our genome analyses suggest that Asgard representatives are primarily organoheterotrophs with variable capacity for hydrogen consumption and production. On this basis, we propose the 'reverse flow model', an updated symbiogenetic model for the origin of eukaryotes that involves electron or hydrogen flow from an organoheterotrophic archaeal host to a bacterial symbiont. Moreira, D. & Lopez-Garcia, P. Symbiosis between methanogenic archaea and deltaproteobacteria as the origin of eukaryotes: the syntrophic hypothesis.

No abstract

All modern cells are bounded by cell membranes best described by the fluid mosaic model. This statement is so widely accepted by biologists that little attention is generally given to the theoretical importance of cell membranes in describing the cell. This has not always been the case. When the Cell Theory was first formulated in the XIXth century, almost nothing was known about the cell membranes. It was not until well into the XXth century that the existence of the plasma membrane was broadly accepted and, even then, the fluid mosaic model did not prevail until the 1970s. How were the cell boundaries considered between the articulation of the Cell Theory around 1839 and the formulation of the fluid mosaic model that has described the cell membranes since 1972? In this review I will summarize the major historical discoveries and theories that tackled the existence and structure of membranes and I will analyze how these theories impacted the understanding of the cell. Apart from its purely historical relevance, this account can provide a starting point for considering the theoretical significance of membranes to the definition of the cell and could have implications for research on early life.ReviewersThis article was reviewed by Dr. Étienne Joly, Dr. Eugene V. Koonin and Dr. Armen Mulkidjanian.

BackgroundThe N-glycosylation is an essential protein modification taking place in the membranes of the endoplasmic reticulum (ER) in eukaryotes and the plasma membranes in archaea. It shares mechanistic similarities based on the use of polyisoprenol lipid carriers with other glycosylation pathways involved in the synthesis of bacterial cell wall components (e.g. peptidoglycan and teichoic acids). Here, a phylogenomic analysis was carried out to examine the validity of rival hypotheses suggesting alternative archaeal or bacterial origins to the eukaryotic N-glycosylation pathway.ResultsThe comparison of several polyisoprenol-based glycosylation pathways from the three domains of life shows that most of the implicated proteins belong to a limited number of superfamilies. The N-glycosylation pathway enzymes are ancestral to the eukaryotes, but their origins are mixed: Alg7, Dpm and maybe also one gene of the glycosyltransferase 1 (GT1) superfamily and Stt3 have proteoarchaeal (TACK superphylum) origins; alg2/alg11 may have resulted from the duplication of the original GT1 gene; the lumen glycosyltransferases were probably co-opted and multiplied through several gene duplications during eukaryogenesis; Alg13/Alg14 are more similar to their bacterial homologues; and Alg1, Alg5 and a putative flippase have unknown origins.ConclusionsThe origin of the eukaryotic N-glycosylation pathway is not unique and less straightforward than previously thought: some basic components likely have proteoarchaeal origins, but the pathway was extensively developed before the eukaryotic diversification through multiple gene duplications, protein co-options, neofunctionalizations and even possible horizontal gene transfers from bacteria. These results may have important implications for our understanding of the ER evolution and eukaryogenesis.ReviewersThis article was reviewed by Pr. Patrick Forterre and Dr. Sergei Mekhedov (nominated by Editorial Board member Michael Galperin).Electronic supplementary materialThe online version of this article (doi:10.1186/s13062-016-0137-2) contains supplementary material, which is available to authorized users.