New ideas on the origins of Eukaryotes

In 1967 the American biologist Lyn Margulis developed an idea that had been considered earlier in the 20th century. It proposed that the complex architecture of eukaryote cells had arisen by several simpler prokaryote cells becoming incorporated inside a membrane to form other bodies or organelles that co-existed and interacted. That is, a complex of mutual dependence within a cell wall, called endosymbiosis. For instance, the mitochondria of modern animal cells resemble a class of aerobic bacteria or Proteobacteria (gram-negative bacteria), some of which are responsible for several modern diseases, such as tick-bite fevers. Another is the resemblance of the photosynthesising chloroplasts of plants to cyanobacteria. A similar origin might apply to eukaryote nuclei and other organelles inside eukaryote cells; some have their own DNA molecules. I summarised Margulis’s late-20th century concept of endosymbiosis in my 1999 book Stepping Stones.

AI generated cartoon of symbiogenesis. Credit PhysOrg

Since then the rapid development of genome analysis has seen major advances in the field now known as symbiogenesis. In the most general sense, that is now regarded as a sequence of mergers between early members of the two prokaryote domains of Archaea and Bacteria: not a simple topic! In 2017 a group of archaeons called Promethearchaeati – ‘Asgard’ for short – were found to contain proteins – and thus the genes that produce them – akin to those in eukaryotes. So the Asgards are prime candidates for a role in symbiogenesis. Their symbiotic merger with a Proteobacteria may have begun the evolution of all eukaryotes. The entry of cyanobacteria – a candidate for chloroplasts – into one of the evolving groups divided plants from animals. A new AI analysis of thousands of genomes in living microbial organisms by Catalan scientists in Barcelona has enabled them to flesh-out and critique this hypothesis to a remarkable extent (Bernabeu, M. et al. 2026. Gene ancestries reveal diverse microbial associations during eukaryogenesis. Nature, v. 654; DOI: 10.1038/s41586-026-10639-9). Their work possibly revolutionises the study of biological evolution

Moisès Bernabeu and his three colleagues drastically ‘pruned’ the eukaryotic tree of life, which over-represents animals and species found in common ecosystems. They also stripped the limited number of eukaryote genomes of genes that do simple jobs or are closely related – i.e. those that seem to duplicate large sections from the oldest, ancestral genes. Two further ‘edits’ enabled the team to judge from their analysis what sort of roles may have been played by the genetics of the last eukaryote common ancestor (LECA). At this level of simplification it appeared that our ancestors inhabited oxygenated environments and got their energy by eating other organisms or their dead remains.

About 30% of the genes in eukaryotes seem to be unique to them and evolved after LECA had emerged. Many of the rest came from diverse prokaryote organisms. Alphaproteobacteria (previously termed ‘purple’ bacteria) and the Asgard archaea figure strongly, together with a range of other bacteria. As suggested previously, a vital process could have been transfer of genes from one prokaryote to another. Bernabeu et al.’s study highlights waves of such gene transfers prior to LECA’s acquisition of mitochondria, widely deemed to have been incorporation of an early proteobacterium. They also provide evidence for a central role played by giant viruses in enabling such gene transfers, also hypothesised previously.

Rather than being a simple case of a ‘one-off’ symbiosis between two separate prokaryotes, an archaeon and a bacterium, with the other organelles and genes added during a later evolutionary stage, the genesis of LECA was probably a long and complex interaction that involved diverse participants. It also seems certain that all the prokaryotes must have interacted in a stable, long-lived ecosystem for such a complex process to reach a tangible and enduring outcome after innumerable fits and starts. That oxygen became such an essential inorganic ‘player’ clearly suggests a microbial-mat ecosystem of organisms that involved oxygenic photosynthesis. The whole ecosystem and its members, pro- and eukaryotic, seem likely to have been evolving together, like modern ecosystems but on a microscopic scale. All this may have taken millions of years during the Palaeoproterozoic Era (2.5 to 1.6 Ga)

See also: Timmer, J. 2026. The first complex cells had genes from a complex mix of species. Arstechnica.com, 11 June 2026;  Microbial alliances, not mitochondria alone, may have built first eukaryotic cells. Phys.org, 10 June 2026.

Snowball Earth and the rise of multi-celled life

You can follow my ‘reportage’ on the long running story of the Snowball Earth events during the Neoproterozoic Cryogenian Period (850 to 635 Ma) since 2000 through the index to annual Palaeoclimatology logs (15 posts). Once these dramatic events were over sedimentary rocks deposited around the world during the Ediacaran Period (635 to 541 Ma) record the sudden appearance of large-bodied fossils: the first multicellular animals. This explosion from slimy biofilms and colonies of single-celled prokaryotes and eukaryotes laid the basis for the myriad ecological niches that have characterised Planet Earth ever since. The change saw specialised eukaryote cells (see: The rise of the eukaryotes; December 2017), whose precursors had originated in single-celled forms, begin to cooperate inthe development of complex tissues, organs, and organ systems to form bodies rather than just cell walls. The pulsating evolution, diversification and repeated extinction that followed during the last one tenth of geological time shaped a planet that is unique in the Solar System and possibly in the galaxy, if not the entire universe. The simple biosphere that preceded it, on the other hand, may have emerged on innumerable rocky planets blessed with liquid water to survive little changed for billions of years, as have Earths’ prokaryotes, the Archaea and Bacteria.  

Artist’s impression of the Ediacaran Fauna (credit: Science)

The Ediacaran biological revolution followed repeated changes in the geochemistry of the oceans, which carbon isotope data from the Cryogenian and Ediacaran suggest to have ‘gone haywire’. This turmoil involved dramatic changes in the cycling of sulfur and phosphorus that help ‘fertilise’ the marine food chain and in the production of oxygen by photosynthesis that is essential for metazoan animals.  The episodes when the Earth was iced over reduced the availability of nutrients through decreased rates of ocean-floor burial of dead organisms. Such Snowball events would also have reduced penetration of sunlight in the oceans. Less photosynthesis would not only have reduced oxygen production but also the amounts of autotrophic organisms. Furthermore, decreased water temperature would have increased its viscosity thereby slowing the spread of nutrients. The food chain for heterotrophs was decimated. Each Snowball event ended with warming, ice-free conditions so that the marine biosphere could burgeon

A great deal of data and numerous theories have accumulated since the Snowball concept was first mooted, but there has been little progress in understanding the rise of multi-celled life. Four geoscientists from the Massachusetts Institute of Technology, the Santa Fe Institute and the University of Colorado (Boulder), USA have developed an interesting hypothesis for how this enormous evolutionary step may have developed (Crockett, W.W. et al. 2024. Physical constraints during Snowball Earth drive the evolution of multicellularity. Proceedings of the Royal Society B: Biological Sciences, v. 291; DOI: 10.1098/rspb.2023.2767). The concatenation of huge events during the Cryogenian and Ediacaran presented continually changing patterns of selective pressures on simple organisms that preceded that time period. Crockett et al. review them in the light of fundamental biology to suggest how multicellular animals emerged as the Ediacara Fauna. Intuitively, such harsh conditions suggest at worst mass, even complete, extinction, at best a general reduction in size of all organism to cope with scarce resources. That the size of eukaryotes should have grown hugely goes against the grain of most biologists’ outlook.

The authors consider the crucial factor to be fundamental differences between prokaryotes and early eukaryotes. Prokaryote cells are very small, and whether autotrophs of heterotrophs they absorb nutrients through their walls by diffusion. Single-celled eukaryotes are far larger than prokaryotes and typically have a flagellum or ‘tail’ so that they can move independently and more easily gather resources. Crockett et al. used computer modelling to simulate the type of life form that could grow and thrive under Snowball conditions. They found that prokaryotes could only grow smaller, being ‘stunted’ by scarce resources. On the other hand eukaryotes would be better equipped to gather resources, the more so if they adopted a simple multicellular form – a hollow, self-propelled sphere about the size of a pea, which the authors dub a choanoblastula. Although no such form is known today, it does resemble the green Volvox algae, and plausibly could have evolved further to the simple forms of the Ediacaran fauna. The next task is either to find a fossil of such an organism, or to grow one.