Heterochronic evolution in a Late Pliocene-Early Pleistocene lineage of western European voles (Arvicolinae, Rodentia, Mammalia)

In this paper, the evolution of the lineage of western European populations of the genus Kislangia (Arvicolinae) is analysed, including the species Kislangia cappettai from Balaruc 2, Kislangia ischus from Zújar 11, and Kislangia gusii from Galera 2 and Almenara-Casablanca 1. The range of this linea...

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Detalles Bibliográficos
Autores: Agustí, Jordi|||0000-0002-7240-1992, Lozano-Fernández, Iván|||0000-0003-1036-7634, Piñero, Pedro|||0000-0002-5626-2777
Tipo de recurso: artículo
Fecha de publicación:2026
País:España
Institución:Universitat Autònoma de Barcelona
Repositorio:Dipòsit Digital de Documents de la UAB
Idioma:inglés
OAI Identifier:oai:ddd.uab.cat:325227
Acceso en línea:https://ddd.uab.cat/record/325227
https://dx.doi.org/urn:doi:10.1080/08912963.2025.2526016
Access Level:acceso embargado
Palabra clave:Iberian Peninsula
Kislangia
Quaternary
Southern France
ontogeny
Descripción
Sumario:In this paper, the evolution of the lineage of western European populations of the genus Kislangia (Arvicolinae) is analysed, including the species Kislangia cappettai from Balaruc 2, Kislangia ischus from Zújar 11, and Kislangia gusii from Galera 2 and Almenara-Casablanca 1. The range of this lineage covers the Late Pliocene and the Early Pleistocene. Our analysis has been focused on the m1. Measurements of size, hypsodonty, perimeter, and area of the teeth have been recorded. An increase in size is observed from K. cappettai to K. gusii, while hypsodonty also increases in a punctuated manner. The functional fitness of the m1 is calculated on the basis of the structural density. It is observed that at the individual level, as wear advances, there is an increase in the structural density of the teeth. Consequently, the adult tooth is functionally more efficient than at younger stages of wear. When considering the structural density across the evolution of the lineage, higher structural density values are found for the same ontogenetic stages. This indicates that older ontogenetic stages of the more archaic populations appear earlier in the descendant species. It is concluded that this evolutionary process corresponds to the heterochronic change known as acceleration.