Camurodon, Qayaqgruk, Kaniqsiqcosmodon: new multituberculates from Late Cretaceous of Alaska

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Ben Creisler

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May 18, 2026, 3:56:33 PM (20 hours ago) May 18
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Ben Creisler

A new paper:


Camurodon borealis gen. et sp. nov.
Qayaqgruk peregrinus gen. et sp. nov.
Kaniqsiqcosmodon polaris gen. et sp. nov.


Sarah L. Shelley, Jaelyn J. Eberle, Gregory M. Erickson, and Patrick S. Druckenmiller (2026)
Arctic ecosystems shaped mammalian dispersal and diversification before the Cretaceous–Paleogene mass extinction
Proceedings of the National Academy of Sciences 123(22): e2601794123
doi: https://doi.org/10.1073/pnas.2601794123
https://www.pnas.org/doi/10.1073/pnas.2601794123



Significance

Polar regions are often treated as evolutionary backwaters, yet they can connect continents and impose extreme selection. From the Late Cretaceous (73 Ma) Prince Creek Formation of Alaska (~80–85°N), we describe three species of multituberculate, an extinct mammal group, and analyze their relationships and biogeographic history. One species is closely allied to a Mongolian group, providing the earliest direct evidence of multituberculates dispersing between Asia and North America across a terrestrial Arctic corridor. Another is the oldest known microcosmodontid, implying a high-latitude origin for a derived North American lineage. Differences in tooth morphology indicate niche partitioning among multituberculates in polar communities. The Arctic ecosystem emerges as both corridor and cradle of mammalian diversification before the Cretaceous–Paleogene mass extinction.

Abstract

High-latitude terrestrial ecosystems are commonly viewed as marginal environments to deep-time evolutionary innovation, yet their role in shaping biotic dispersal, diversification, and survivorship remains poorly understood. The Upper Cretaceous Prince Creek Formation of northern Alaska (paleolatitude ~80–85°N) yields the most northerly known Mesozoic mammals and provides a rare opportunity to examine the ecological and biogeographic roles of polar terrestrial ecosystems. Here, we describe three multituberculate species, Camurodon borealis, Qayaqgruk peregrinus, and Kaniqsiqcosmodon polaris, and integrate comparative morphology with phylogenetic and biogeographic analyses to evaluate patterns and timing of dispersal and diversification across a high-latitude Asian–American terrestrial corridor. Qayaqgruk peregrinus is recovered within the Mongolian Djadochtatherioidea, representing the earliest direct evidence for multituberculate dispersal from Asia into North America. Kaniqsiqcosmodon polaris constitutes the oldest known member of the Microcosmodontidae, suggesting a high-latitude origin for a derived North American lineage that later diversified during the Paleocene following the Cretaceous–Paleogene mass extinction. Camurodon borealis represents the northernmost occurrence of the Cimolomyidae. Pronounced variation in dental morphology among the Prince Creek multituberculates indicates ecological differentiation and niche partitioning within an extreme, highly seasonal polar environment. Our findings indicate that Late Cretaceous Arctic ecosystems supported both sustained intercontinental exchanges as early as 91.82 Ma and endemism. Our results challenge interpretations of polar regions as evolutionary peripheries and instead identify them as important contributors to mammalian evolutionary dynamics prior to the Cretaceous–Paleogene mass extinction.

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