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Rook, L.

Publications and source records attributed to Rook, L..

3 recordsLinked to original sources

Palaeoproteomic insights into the deep roots of the cave bear lineage in Europe

Palaeoproteomics has emerged as a powerful tool for reconstructing the evolutionary history of extinct species, particularly when ancient DNA is poorly preserved or beyond recovery. Here, we present the first large-scale enamel proteomic study focused on the cave bear, spanning specimens from the Early to Late Pleistocene. A primary objective was to determine whether the ursid population from level TD4 of Gran Dolina (Sierra de Atapuerca, Spain) belongs to the cave or the brown bear lineage, a long-standing taxonomic debate. We analyzed specimens from the Atapuerca sites, alongside comparative material from other southwestern European localities. Using LC-MS/MS and an acid demineralization protocol without enzymatic digestion, we successfully recovered enamel proteomes from all fossil samples, including the oldest specimens. Protein profiles were obtained for each extinct ursid, enabling the identification of taxonomically informative peptides across multiple individuals per taxon. Notably, two novel single amino acid polymorphisms (SAPs), found in ameloblastin (AMBN) and alpha-1 antitrypsin (SERPINA1), were restricted to Middle and Late Pleistocene cave bears and may represent new phylogenetic markers for this clade. This study provides the first molecular phylogenetic placement of Ursus dolinensis, supporting its basal position within the speloid lineage, consistent with its proposed ancestral status. Our results highlight the strong phylogenetic signal preserved in dental enamel and the exceptional biomolecular preservation at Atapuerca, providing a robust framework for reconstructing the evolutionary history of Ursidae. Moreover, the consistent recovery of systemic proteins, such as serpins, underscores the potential of enamel proteomes to capture not only evolutionary relationships but also physiological signals relevant to extinct ursids. SignificanceThe phylogenetic position of Ursus dolinensis within the Ursidae family has been a subject of long-standing debate. While some authors place it within the speloid lineage, others suggest affinities with arctoid bears. Here, we analyze the bear population from level TD4 of Gran Dolina (Sierra de Atapuerca, Spain) using palaeoproteomic methods for the first time. Molecular evidence supports the inclusion of U. dolinensis within the speloid lineage, in a basal position, supporting its potential ancestral position. These findings extend the evolutionary depth of the speloid clade in Europe and demonstrate the power of enamel palaeoproteomics to resolve deep-time relationships beyond the limits of ancient DNA, revealing the deep evolutionary roots of the lineage.

evolutionary biology↗

Genomic analyses of the extinct Sardinian dhole (Cynotherium sardous) reaveal its evolutionary history

The Sardinian dhole (Cynotherium sardous)1 was an iconic and unique canid species of canid that was endemic of Sardinia and Corsica until it became extinct at the end of the Late Pleistocene2-5. Given its peculiar dental morphology, small body size and high level of endemism, several canids have been proposed as possible ancestors of the Sardinian dhole, including the Asian dhole and African hunting dog ancestor 3,6-9. Morphometric analyses3,6,8-12 have failed to clarify the evolutionary relationship with other canids. We sequenced the genome of a ca 21,100 year old Sardinian dhole in order to understand its genomic history and clarify its phylogenetic position. We found it represents a separate taxon from all other living canids from Eurasia, Africa and North America, and that the Sardinian and Asian dhole lineages diverged ca 885 ka. We additionally detected historical gene flow between the Sardinian and Asian dhole lineages, that ended approximately 500-300 ka, when the landbridge between Sardinia and mainland Italy was broken, severing their population connectivity. Our sample showed low genome-wide diversity compared to other extant canids - probably a result of the long-term isolation - that could have contributed to the subsequent extinction of the Sardinian dhole.

genomics↗

Early Pleistocene enamel proteome sequences from Dmanisi resolve Stephanorhinus phylogeny.

Ancient DNA (aDNA) sequencing has enabled unprecedented reconstruction of speciation, migration, and admixture events for extinct taxa1. Outside the permafrost, however, irreversible aDNA post-mortem degradation2 has so far limited aDNA recovery within the {small tilde}0.5 million years (Ma) time range3. Tandem mass spectrometry (MS)-based collagen type I (COL1) sequencing provides direct access to older biomolecular information4, though with limited phylogenetic use. In the absence of molecular evidence, the speciation of several Early and Middle Pleistocene extinct species remain contentious. In this study, we address the phylogenetic relationships of the Eurasian Pleistocene Rhinocerotidae5-7 using {small tilde}1.77 million years (Ma) old dental enamel proteome sequences of a Stephanorhinus specimen from the Dmanisi archaeological site in Georgia (South Caucasus)8. Molecular phylogenetic analyses place the Dmanisi Stephanorhinus as a sister group to the woolly (Coelodonta antiquitatis) and Mercks rhinoceros (S. kirchbergensis) clade. We show that Coelodonta evolved from an early Stephanorhinus lineage and that this genus includes at least two distinct evolutionary lines. As such, the genus Stephanorhinus is currently paraphyletic and its systematic revision is therefore needed. We demonstrate that Early Pleistocene dental enamel proteome sequencing overcomes the limits of ancient collagen- and aDNA-based phylogenetic inference, and also provides additional information about the sex and taxonomic assignment of the specimens analysed. Dental enamel, the hardest tissue in vertebrates, is highly abundant in the fossil record. Our findings reveal that palaeoproteomic investigation of this material can push biomolecular investigation further back into the Early Pleistocene.

evolutionary biology↗