Search bioRxiv⌕ Search

bioRxiv · 10.64898/2026.10.05.756825

The trilobite nervous system and the early evolution of the mandibulate central complex

Abstract

Fossil central nervous systems (CNS) have illuminated several facets of total-group euarthropod evolution, including their phylogenetic affinities, the origin of the head, and their ancestral neuroanatomical organization. However, the CNS remains unknown in trilobites, the most diverse and earliest group of Palaeozoic euarthropods, but can potentially clarify fundamental questions that remain disputed despite thousands of described species and countless studies spanning over two centuries, such as their affinities relative to modern representatives. Here, we describe the CNS of the cheirurid Anacheirurus adserai from the Lower Ordovician Fezouata Shale. Anacheirurus features a brain with well-developed proto, deuto- and tritocerebral neuromeres, an anteriomedian protocerebral protrusion, a central complex, an esophageal foramen, and a ganglionated ventral nerve cord. The CNS is replicated in framboidal iron that differs in texture and composition from the exoskeleton and rock matrix. The overall organization of Anacheirurus's CNS most closely resembles that of Cambrian stem-group mandibulates, and critically shares the presence of a central complex with a protocerebral bridge and lateral accessory lobes with extant pancrustaceans. Our findings provide new morphological support for the hypothesis that Trilobita belongs to the mandibulate stem lineage and bring new insights into the ancestral morphology and evolutionary history of the euarthropod central complex. More broadly, our findings offer direct anatomical evidence of the key sensorimotor system innovations that originated during the Cambrian Information Revolution.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Losso, S. R., Becker-Kerber, B., Weaver, J. C., Perez-Peris, F., Ortega-Hernandez, J.. 2026-10-07. The trilobite nervous system and the early evolution of the mandibulate central complex. https://doi.org/10.64898/2026.10.05.756825

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

KEEP EXPLORING

Related preprints

Diversity in early animal communities of the Ediacaran, Avalon assemblage

Diversity is an emergent property of macroecological and macroevolutionary processes. The Avalon assemblage preserves near-census snapshots of Ediacaran communities, enabling tests of the drivers of diversity. However, it remains unclear how alpha diversity varied among surfaces or whether variation reflected uneven sampling, abiotic context or biotic processes. We analysed diversity for 11,342 specimens across 22 surfaces and examined abiotic and biotic correlates. Despite compositional variation, most surfaces fell into four community types dominated by Fractofusus andersoni, F. misrai and/or Pectinifrons, Bradgatia, or upright fronds, with potential substructure within the upright-frond type, whereas Clapham's Pigeon Cove and Shingle Head communities, from the oldest and youngest formations, respectively, may indicate greater community differentiation near the sampled stratigraphic limits. Sampling effort varied widely, yet taxon-area curves showed richness was well captured on 12 of 22 surfaces, and Shannon and Simpson diversity remained consistent across sampling completeness and taxonomic treatments. Diversity showed no clear associations with locality or stratigraphic affiliation, but differed among community types and declined with increasing vertical segregation. Overall, these results suggest that, among the predominantly Newfoundland communities sampled, Avalon alpha diversity may have been shaped more by local community assembly and organisation than by broader geographic, environmental and temporal context.

paleontology↗

Durophagous adaptations in a new crocodyliform from the Santonian of Hungary and a systematic reassessment of European Cretaceous atoposaurids

Atoposauridae comprises a group of diminutive, semiterrestrial, brevirostrine neosuchian crocodyliforms that represents a characteristic component of European Jurassic-Cretaceous tetrapod faunas. Although frequently evaluated within the context of crown-group Crocodylia origins, their highly contested phylogenetic relationships continue to obscure their precise role in crocodylomorph evolutionary history. Particular ambiguity surrounds the monophyly of the genus Theriosuchus - with some hypotheses inferring long-term persistence of the lineage in Mesozoic Europe, whereas others interpreting select Cretaceous species as representatives of separate, even non-atoposaurid clades (e.g. Sabresuchus spp). We describe a new, stratigraphically intermediate taxon from the Santonian of Hungary based on isolated cranial elements, consistently placed as the sister taxon of Sabresuchus (Theriosuchus) sympiestodon from the Maastrichtian of Romania by our comprehensive set of phylogenetic analyses using three separate datasets. Sabresuchus tribodon sp. nov. is either recovered within Atoposauridae (global datasets) or Paralligatoridae (ingroup analysis) and can be distinguished from all other representatives of these groups by a specialized morphology consisting of massive, thick-enameled bulbous posterior maxillary teeth ornamented with apicobasal ridges, an extremely short rostrum with a reduced number of maxillary and dentary teeth, and the significantly upturned dorsal margin of the posterior dentary and surangular. Comparable anatomical adaptations are present in ecomorphologically convergent extinct crocodyliforms whose inferred feeding ecology included durophagy. However, this complete suite of characters has not been previously documented in either atoposaurids or paralligatorids. Our systematic reassessment results in an up-to-date taxonomy of Cretaceous European atoposaurids and tentatively confirms the polyphyly of Theriosuchus, though more definitive conclusions require combining individual, differently focused datasets. We reinterpret Aprosuchus ghirai from the Maastrichtian of Romania as a junior synonym of Sabresuchus sympiestodon and the putative European notosuchian Ogresuchus furatus from the Maastrichtian of Spain as an indeterminate atoposaurid.

paleontology↗

Causal analysis of rock-biodiversity relationships over the global Phanerozoic challenges rock record bias and common cause hypothesis

Sampled marine biodiversity covaries strongly with sedimentary rock quantity over the Phanerozoic, but the respective contributions of different potential causes remain unsettled. Although regional studies show that rock-record bias accounts for more variation in sampled marine biodiversity than common-cause mechanisms, evaluating this relationship across the global Phanerozoic record remains difficult because fossil databases are inherently biased toward fossiliferous strata. To address this limitation, we compiled literature-derived measures of global marine biodiversity and sedimentary strata, along with an existing sea-level curve. Using an information-theoretic causal framework, we then evaluated the relative contributions of rock-record bias and common-cause hypotheses to Phanerozoic-scale variation in sampled marine biodiversity. Our results show a strong contemporaneous causality of marine strata on sampled biodiversity, indicating that rock record bias detected at regional scales extends to the global scale. However, neither rock record bias nor common-cause mechanisms accounts for most Phanerozoic-scale patterns in sampled biodiversity, and additional unmeasured factors likely contribute. Finally, we find tentative evidence that synergistic causality between geologically mediated sampling biases and forces shaping the underlying biological signal contributes to global Phanerozoic patterns in sampled biodiversity.

paleontology↗