Search bioRxiv⌕ Search

bioRxiv · 10.64898/2026.03.25.714154

Clade dynamics support an early origin of crown eukaryotes

Abstract

The timing of the last eukaryotic common ancestor (LECA) remains a fundamental question in evolutionary biology and palaeontology. Unambiguous eukaryotic-grade fossils appear from 1780 Ma, but no crown-group supergroups are confidently identified before the end of the Mesoproterozoic (ca. 1050 Ma). The late LECA hypothesis suggests that this absence of crown-assignable fossils and biosignatures implies a late Mesoproterozoic origin of the crown. Here we show that this hypothesis is incompatible with the evolutionary dynamics of the eukaryote clade, even under the limited constraints of the fossil record. Studying stem-crown dynamics based on a birth-death model, we show that a late crown age requires diversification rates well below the minimum rate needed to generate observed living eukaryote diversity (~2.5 - 10 million species) for any plausible total group age. Our results suggest that only an early LECA can bridge evolutionary dynamics with the eukaryotic-grade fossil record, the living diversity, and the molecular clock estimates. Based on these constraints, we suggest a feasible minimum age estimate for LECA of ca. 1696 Ma, supported by current fossil evidence and supporting molecular clock estimates. These results also provide a fossil-testable prediction: crown-group eukaryotes likely exist in early Mesoproterozoic assemblages, albeit undetected with current morphology-based approaches.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Loron, C. C., Rodgers, N.. 2026-03-27. Clade dynamics support an early origin of crown eukaryotes. https://doi.org/10.64898/2026.03.25.714154

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related preprints

Bone diagenesis in Iron Age Siberia: a histological and microtomographic study of Tunnug 1 (Russia, 2nd-4th c. CE)

The Siberian site of Tunnug 1, located in the Uyuk Valley (Tuva Republic, Russia), encompasses an Early Scythian burial mound (9th century BCE) and a peripheral cemetery attributed to the Kokel culture (2nd-4th centuries CE). Situated within a permafrost-affected environment, the site offers an opportunity to investigate bone preservation under long-term freeze-thaw cycle conditions and explore the relationship between funerary treatment and bone diagenesis. This study presents a combined histological and microtomographic analysis of 76 bone samples from 71 individuals across 36 burials. Transmitted light microscopy, scanning electron microscopy (SEM) and micro-computed tomography (micro-CT) were employed to document biological, chemical and physical degradation. Bone preservation was evaluated through three approaches: the traditional Oxford Histological Index (OHI), quantitative image analysis and assessment of (micro)cracking. The results revealed moderate bone preservation (OHI 2-4). Biological degradation in the form of Microscopical Focal Destruction (MFD) and chemical alteration were identified in six individuals. Enlarged canaliculi were observed in every bone sample. Microcracks were present in all individuals, visible exclusively under SEM. No clear diagenetic signatures linked to specific funerary practices were identified, though variations in preservation suggest a possible influence of burial depth. The distinct impact of permafrost and long-term freeze-thaw cycles on bone microstructure could not be isolated, underscoring the multifactorial nature of diagenesis. This study highlights the complementary value of combining multiple analytical methods assessing bone diagenesis and emphasises the need for continued experimental research into the effects of freezing environments on human remains.

paleontology↗

NOTE ON RHEIFORMES (AVES: PALAEOGNATHAE) FROM A QUATERNARY CAVE IN THE LAGOA SANTA KARST, EASTERN BRAZIL

Rheiformes are a South American lineage of large, flightless palaeognathous birds, currently represented by the genus Rhea and the two extant species R. americana and R. pennata. The fossil record of the group extends back to the Eocene, with its greatest diversification occurring during the Neogene. During the Quaternary, Rheiformes were widely distributed across southern and central South America. The Lagoa Santa region is particularly notable for its rich paleontological and archaeological record. Quaternary records of Rheiformes from caves in this region provide important evidence for understanding the distribution of the group in Brazil, although their chronological context remains uncertain owing to the absence of direct dating. Here, we describe and illustrate two rheiform bones recovered from a cave in the Lagoa Santa karst region. The material comprises a partially complete tibiotarsus and a fragmented tarsometatarsus, interpreted as belonging to a single individual. Comparative anatomical and morphometric analyses support their attribution to Rhea americana, based on morphological features and dimensions consistent with adult specimens of the species. This occurrence extends the Quaternary record of Rheiformes in the Lagoa Santa region and contributes to the fossil and subfossil record of Rhea in Brazil. The absence of stratigraphic and geochronological control precludes a precise age determination. Although the association with an extinct dasypodid indicates the presence of Late Pleistocene or Early Holocene faunal elements at the locality, a Holocene or even recent age for the rheiform remains cannot be excluded.

paleontology↗

Nanoscale chemical tomography reveals organic and inorganic clusters in fossilised dinosaur tooth

Mineralized dental tissues are formed through biomineralization processes involving the growth and self-organisation of hydroxylapatite (HAP) nanoscale grains. There remain open questions regarding the way elements such as Mg or Na are incorporated in the organic matter between HAP grains or within the grain structure where they influence the nucleation and growth of HAP. Here, mapping the enamel structure and composition of a well-preserved ca. 150-million-year-old Giraffatitan brancai sauropod dinosaur tooth from millimeters down to the near-atomic scale, we reveal the nanoscale accumulation of Mg at HAP grain boundaries, alongside F arising from diagenesis. Within the HAP grains and at HAP grain boundaries organic matter forms clusters that we propose contribute to the fast growth rate of the tooth. Moreover, unexpected Cu3As particles are found across the entire enamel structure. These elements are not in the dentine, that exhibits empty tubules, which suggests that they were integrated during the tooth growth itself. Our multiscale analysis provides new information encouraging to reconsider aspects of the biomineralization and fossilization processes.

paleontology↗